The Origin of Clay Minerals in Soils and Weathered Rocks
Of huge relevance in a number of fields, this is a survey of the different processes of soil clay mineral formation and the consequences of these processes concerning the soil ecosystem, especially plant and mineral. Two independent systems form soil materials. The first is the interaction of rocks...
Ausführliche Beschreibung
Autor*in: |
Meunier, Alain - 1948- |
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Format: |
E-Book |
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Sprache: |
Englisch |
Erschienen: |
Berlin, Heidelberg: Springer-Verlag Berlin Heidelberg ; 2008 |
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Schlagwörter: |
Bodenbildung / Verwitterung / Tonmineral Gestein / Ton, Geologie / Geochemie / Chemische Verwitterung / Tonmineralogie Tonmineral / Boden / Verwitterung / Gestein |
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Schlagwörter: |
Systematik: |
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Anmerkung: |
Includes bibliographical references and index |
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Umfang: |
Online-Ressource (digital) |
Weitere Ausgabe: |
Buchausg. u.d.T. Velde, Bruce: The origin of clay minerals in soils and weathered rocks ; with 23 tables - Berlin : Springer, 2008 |
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Reihe: |
SpringerLink ; Bücher |
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Links: |
Link aufrufen |
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ISBN: |
978-3-540-75634-7 |
DOI / URN: |
10.1007/978-3-540-75634-7 |
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Katalog-ID: |
1647264014 |
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245 | 1 | 4 | |a The Origin of Clay Minerals in Soils and Weathered Rocks |c by Bruce Velde, Alain Meunier |
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505 | 8 | 0 | |a Preface; Contents; Introduction; Chapter 1 Fundamentals of Clay Mineral Crystal Structure and Physicochemical Properties; Chapter 2 Basics for the Study of Soil and Weathered Rock Geochemical Systems; Chapter 3 The Development of Soils and Weathering Profile; Chapter 4 Clay Mineral Formation in Weathered Rocks: Water/Rock Interaction; Chapter 5 Plants and Soil Clay Minerals; Chapter 6 Clays and Climate - Clay Assemblages Formed under Extreme Humidity Conditions; Chapter 7 Physical Disequilibrium and Transportation of Soil Material |
505 | 8 | 0 | |a Chapter 8 The Place of Clay Mineral Species in Soils and AlteritesAnnex 1 Polytypes; Annex 2 Mixed Layer Minerals; Annex 3 Cation Exchange Capacity; Annex 4 Hydroxy-Interlayered Minerals (HIMs); Annex 5 Phase Diagrams Applied to Clay Mineral Assemblages; Annex 6 Kinetics; References; Index |
520 | |a Of huge relevance in a number of fields, this is a survey of the different processes of soil clay mineral formation and the consequences of these processes concerning the soil ecosystem, especially plant and mineral. Two independent systems form soil materials. The first is the interaction of rocks and water, unstable minerals adjusting to surface conditions. The second is the interaction of the biosphere with clays in the upper parts of alteration profiles. | ||
520 | |a The importance of clay minerals and their origin is crucial to an understanding of the physico-chemical functions of the interface at the Earth’s surface. Their place is that of contact between the mineral world and the living world, plants and finally mankind. This contact zone is the realm of much of the environment as we see it today. If we can understand the way clays function in their interaction with plants, we can understand the major forces which shape our immediate environment. We see increasingly that human activity interacts with the plant and mineral interface through the use of more powerful chemicals, either by purposeful application of accidental dispersion. Knowledge of the origin and transformation of clay minerals, their dynamic response to changing chemistry, is the key to a rational use of this natural boundary which affects our lives. The information and the analysis presented here is an attempt to set trends of research in the direction of preventive and creative use of the plant – soil interface. Clays are the product of slow transformations of high temperature rocks into reactive, fine grained material. This material, once in the sphere of plant interaction, becomes highly reactive with transformation periods of tens to hundreds of years. The challenge of the future is to use these rapid responses to the benefit of mankind. This book aims to further a better understanding of such mechanisms, and it is thus destined for an audience of ecologists, pedologists, agronomists and other researchers involved in earth surface science | ||
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9783540756347 978-3-540-75634-7 10.1007/978-3-540-75634-7 doi (DE-627)1647264014 (DE-576)285794760 (DE-599)BSZ285794760 (OCoLC)272298878 (OCoLC)315990349 (DE-He213)978-3-540-75634-7 DE-627 ger DE-627 rakwb eng XA-DE QE389.625 PNV bicssc SCI048000 bisacsh TY 2000 SEPA rvk (DE-625)rvk/145062: RB 10162 BVB rvk (DE-625)rvk/142220:12642 38.61 bkl 38.30 bkl The Origin of Clay Minerals in Soils and Weathered Rocks by Bruce Velde, Alain Meunier Berlin, Heidelberg Springer-Verlag Berlin Heidelberg 2008 Online-Ressource (digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier SpringerLink Bücher Includes bibliographical references and index Preface; Contents; Introduction; Chapter 1 Fundamentals of Clay Mineral Crystal Structure and Physicochemical Properties; Chapter 2 Basics for the Study of Soil and Weathered Rock Geochemical Systems; Chapter 3 The Development of Soils and Weathering Profile; Chapter 4 Clay Mineral Formation in Weathered Rocks: Water/Rock Interaction; Chapter 5 Plants and Soil Clay Minerals; Chapter 6 Clays and Climate - Clay Assemblages Formed under Extreme Humidity Conditions; Chapter 7 Physical Disequilibrium and Transportation of Soil Material Chapter 8 The Place of Clay Mineral Species in Soils and AlteritesAnnex 1 Polytypes; Annex 2 Mixed Layer Minerals; Annex 3 Cation Exchange Capacity; Annex 4 Hydroxy-Interlayered Minerals (HIMs); Annex 5 Phase Diagrams Applied to Clay Mineral Assemblages; Annex 6 Kinetics; References; Index Of huge relevance in a number of fields, this is a survey of the different processes of soil clay mineral formation and the consequences of these processes concerning the soil ecosystem, especially plant and mineral. Two independent systems form soil materials. The first is the interaction of rocks and water, unstable minerals adjusting to surface conditions. The second is the interaction of the biosphere with clays in the upper parts of alteration profiles. The importance of clay minerals and their origin is crucial to an understanding of the physico-chemical functions of the interface at the Earth’s surface. Their place is that of contact between the mineral world and the living world, plants and finally mankind. This contact zone is the realm of much of the environment as we see it today. If we can understand the way clays function in their interaction with plants, we can understand the major forces which shape our immediate environment. We see increasingly that human activity interacts with the plant and mineral interface through the use of more powerful chemicals, either by purposeful application of accidental dispersion. Knowledge of the origin and transformation of clay minerals, their dynamic response to changing chemistry, is the key to a rational use of this natural boundary which affects our lives. The information and the analysis presented here is an attempt to set trends of research in the direction of preventive and creative use of the plant – soil interface. Clays are the product of slow transformations of high temperature rocks into reactive, fine grained material. This material, once in the sphere of plant interaction, becomes highly reactive with transformation periods of tens to hundreds of years. The challenge of the future is to use these rapid responses to the benefit of mankind. This book aims to further a better understanding of such mechanisms, and it is thus destined for an audience of ecologists, pedologists, agronomists and other researchers involved in earth surface science Geography Geology Physical geography Mines and mineral resources Mineralogy Sedimentology Soil conservation Earth Sciences Geography Geology Physical geography Mines and mineral resources Mineralogy Sedimentology Soil conservation s (DE-588)4146131-9 (DE-627)104324937 (DE-576)20974670X Bodenbildung gnd s (DE-588)4063385-8 (DE-627)106128302 (DE-576)209148365 Verwitterung gnd s (DE-588)4185687-9 (DE-627)105285358 (DE-576)210034033 Tonmineral gnd DE-101 s (DE-588)4020734-1 (DE-627)106316923 (DE-576)208934618 Gestein gnd s (DE-588)4185646-6 (DE-627)104789557 (DE-576)210033797 Ton Geologie gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4238806-5 (DE-627)104876751 (DE-576)210416106 Chemische Verwitterung gnd s (DE-588)4185688-0 (DE-627)10528534X (DE-576)210034041 Tonmineralogie gnd (DE-627) s (DE-588)4185687-9 (DE-627)105285358 (DE-576)210034033 Tonmineral gnd s (DE-588)4007348-8 (DE-627)106373889 (DE-576)208869859 Boden gnd s (DE-588)4063385-8 (DE-627)106128302 (DE-576)209148365 Verwitterung gnd s (DE-588)4020734-1 (DE-627)106316923 (DE-576)208934618 Gestein gnd (DE-627) Velde, Bruce (DE-588)120623013 (DE-627)080788696 (DE-576)16951241X oth Meunier, Alain 1948- (DE-588)1145752241 (DE-627)1006899111 (DE-576)169517640 oth 9783540756330 Buchausg. u.d.T. Velde, Bruce The origin of clay minerals in soils and weathered rocks ; with 23 tables Berlin : Springer, 2008 XII, 406 S. (DE-627)544000641 (DE-576)272865133 3540756337 9783540756330 https://doi.org/10.1007/978-3-540-75634-7 Verlag Volltext http://dx.doi.org/10.1007/978-3-540-75634-7 Resolving-System lizenzpflichtig Volltext https://swbplus.bsz-bw.de/bsz285794760cov.jpg V:DE-576 X:springer image/jpeg 20130327143601 Cover https://swbplus.bsz-bw.de/bsz272865133inh.htm V:DE-576 text/html Inhaltsverzeichnis http://deposit.dnb.de/cgi-bin/dokserv?id=3002275&prov=M&dok_var=1&dok_ext=htm X: MVB text/html 20130501 Verlag Inhaltstext (DE-627)577106635 ZDB-2-EES 2008 GBV_ILN_23 ISIL_DE-830 SYSFLAG_1 GBV_KXP SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_60 ISIL_DE-705 GBV_ILN_65 ISIL_DE-3 GBV_ILN_120 ISIL_DE-715 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2148 ISIL_DE-950 GBV ExPruef TY 2000 Sedimentäre (exogene) Bildungen Geowissenschaften Angewandte Geologie Lagerstättenkunde Bildungsvorgänge der Lagerstätten Sedimentäre (exogene) Bildungen (DE-627)1271953471 (DE-625)rvk/145062: (DE-576)201953471 RB 10162 Spezielle Bodenkunde (Klassifikation, Benennung, Bodenart und Bodentypen, Klima und Böden) Geografie Nicht regional gebundene Darstellungen Allgemeine Geografie Hilfswissenschaften Bodenkunde (Pedologie) Spezielle Bodenkunde (Klassifikation, Benennung, Bodenart und Bodentypen, Klima und Böden) (DE-627)1271490188 (DE-625)rvk/142220:12642 (DE-576)201490188 TH 7000 Tonige Gesteine Geologie und Paläontologie Petrographie Sedimentgesteine Klastisches Sediment Tonige Gesteine (DE-627)1271933829 (DE-625)rvk/144019: (DE-576)201933829 Ungueltig 38.61 Bodenbildung Bodenentwicklung SEPA (DE-627)181569949 38.30 Mineralogie SEPA (DE-627)106419471 BO 045F 551.305015496 045F 549/.6 23 01 0830 89000000X 00 --%%-- --%%-- s --%%-- olr-springer i z 08-09-08 60 01 0705 4304950746 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 65 01 0003 1655658468 03 --%%-- ebook --%%-- --%%-- OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. k3o 02-01-17 120 01 0715 1840107871 OLR-ESP Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden. z 13-01-19 120 02 0715 3581156342 00 --%%-- --%%-- g --%%-- alma z 24-01-20 370 01 4370 201230313 olr-springer Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. i z 28-01-09 2027 01 DE-105 3322210537 00 --%%-- --%%-- n --%%-- Campuslizenz l01 01-03-10 2050 01 DE-Zi4 3322210553 00 --%%-- --%%-- n --%%-- Elektronischer Volltext - Campuslizenz l01 01-03-10 2148 01 DE-950 3322210588 00 --%%-- eBook Springer --%%-- n Elektronischer Volltext - Campuslizenz l01 17-09-08 23 01 0830 Springer EBook https://doi.org/10.1007/978-3-540-75634-7 60 01 0705 Volltextzugang Campus https://doi.org/10.1007/978-3-540-75634-7 65 01 0003 Volltextzugang Campus https://doi.org/10.1007/978-3-540-75634-7 120 01 0715 http://dx.doi.org/10.1007/978-3-540-75634-7 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991016136295803501 370 01 4370 E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich https://doi.org/10.1007/978-3-540-75634-7 2050 01 DE-Zi4 http://dx.doi.org/10.1007/978-3-540-75634-7 2148 01 DE-950 http://dx.doi.org/10.1007/978-3-540-75634-7 2027 01 DE-105 00 s ebook 120 00 DE-715 99 ww 2027 01 DE-105 00 (DE-627)1292502630 DK 549.623.9 2027 01 DE-105 00 (DE-627)1294202073 DK 549.01 2027 01 DE-105 00 (DE-627)1299854869 DK 549.02 2027 01 DE-105 00 (DE-627)1292553715 DK 552.11 2027 01 DE-105 00 (DE-627)1292331534 DK 548.5 2027 01 DE-105 00 (DE-627)1292218487 DK 552.52 2027 01 DE-105 00 (DE-627)1292683104 DK 548.3 2027 01 DE-105 00 (DE-627)1292790490 DK 551.3.053 2027 01 DE-105 00 (DE-627)1293807990 DK 551.311.23 2027 01 DE-105 00 (DE-627)1292536969 DK 631.41 23 01 0830 2007-06282, 2007-06284, 2007-06285, 2007-06286, 2007-06287, 2007-06289, 2007-06291 120 01 0715 YH 2020 23 01 0830 olr-springer 60 01 0705 SpringerLink 65 01 0003 OLR-SEB-ZDB-2-EES 120 01 0715 OLR-ESP 120 02 0715 alma 370 01 4370 olr-springer 23 01 0830 2008.09.08 |
spelling |
9783540756347 978-3-540-75634-7 10.1007/978-3-540-75634-7 doi (DE-627)1647264014 (DE-576)285794760 (DE-599)BSZ285794760 (OCoLC)272298878 (OCoLC)315990349 (DE-He213)978-3-540-75634-7 DE-627 ger DE-627 rakwb eng XA-DE QE389.625 PNV bicssc SCI048000 bisacsh TY 2000 SEPA rvk (DE-625)rvk/145062: RB 10162 BVB rvk (DE-625)rvk/142220:12642 38.61 bkl 38.30 bkl The Origin of Clay Minerals in Soils and Weathered Rocks by Bruce Velde, Alain Meunier Berlin, Heidelberg Springer-Verlag Berlin Heidelberg 2008 Online-Ressource (digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier SpringerLink Bücher Includes bibliographical references and index Preface; Contents; Introduction; Chapter 1 Fundamentals of Clay Mineral Crystal Structure and Physicochemical Properties; Chapter 2 Basics for the Study of Soil and Weathered Rock Geochemical Systems; Chapter 3 The Development of Soils and Weathering Profile; Chapter 4 Clay Mineral Formation in Weathered Rocks: Water/Rock Interaction; Chapter 5 Plants and Soil Clay Minerals; Chapter 6 Clays and Climate - Clay Assemblages Formed under Extreme Humidity Conditions; Chapter 7 Physical Disequilibrium and Transportation of Soil Material Chapter 8 The Place of Clay Mineral Species in Soils and AlteritesAnnex 1 Polytypes; Annex 2 Mixed Layer Minerals; Annex 3 Cation Exchange Capacity; Annex 4 Hydroxy-Interlayered Minerals (HIMs); Annex 5 Phase Diagrams Applied to Clay Mineral Assemblages; Annex 6 Kinetics; References; Index Of huge relevance in a number of fields, this is a survey of the different processes of soil clay mineral formation and the consequences of these processes concerning the soil ecosystem, especially plant and mineral. Two independent systems form soil materials. The first is the interaction of rocks and water, unstable minerals adjusting to surface conditions. The second is the interaction of the biosphere with clays in the upper parts of alteration profiles. The importance of clay minerals and their origin is crucial to an understanding of the physico-chemical functions of the interface at the Earth’s surface. Their place is that of contact between the mineral world and the living world, plants and finally mankind. This contact zone is the realm of much of the environment as we see it today. If we can understand the way clays function in their interaction with plants, we can understand the major forces which shape our immediate environment. We see increasingly that human activity interacts with the plant and mineral interface through the use of more powerful chemicals, either by purposeful application of accidental dispersion. Knowledge of the origin and transformation of clay minerals, their dynamic response to changing chemistry, is the key to a rational use of this natural boundary which affects our lives. The information and the analysis presented here is an attempt to set trends of research in the direction of preventive and creative use of the plant – soil interface. Clays are the product of slow transformations of high temperature rocks into reactive, fine grained material. This material, once in the sphere of plant interaction, becomes highly reactive with transformation periods of tens to hundreds of years. The challenge of the future is to use these rapid responses to the benefit of mankind. This book aims to further a better understanding of such mechanisms, and it is thus destined for an audience of ecologists, pedologists, agronomists and other researchers involved in earth surface science Geography Geology Physical geography Mines and mineral resources Mineralogy Sedimentology Soil conservation Earth Sciences Geography Geology Physical geography Mines and mineral resources Mineralogy Sedimentology Soil conservation s (DE-588)4146131-9 (DE-627)104324937 (DE-576)20974670X Bodenbildung gnd s (DE-588)4063385-8 (DE-627)106128302 (DE-576)209148365 Verwitterung gnd s (DE-588)4185687-9 (DE-627)105285358 (DE-576)210034033 Tonmineral gnd DE-101 s (DE-588)4020734-1 (DE-627)106316923 (DE-576)208934618 Gestein gnd s (DE-588)4185646-6 (DE-627)104789557 (DE-576)210033797 Ton Geologie gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4238806-5 (DE-627)104876751 (DE-576)210416106 Chemische Verwitterung gnd s (DE-588)4185688-0 (DE-627)10528534X (DE-576)210034041 Tonmineralogie gnd (DE-627) s (DE-588)4185687-9 (DE-627)105285358 (DE-576)210034033 Tonmineral gnd s (DE-588)4007348-8 (DE-627)106373889 (DE-576)208869859 Boden gnd s (DE-588)4063385-8 (DE-627)106128302 (DE-576)209148365 Verwitterung gnd s (DE-588)4020734-1 (DE-627)106316923 (DE-576)208934618 Gestein gnd (DE-627) Velde, Bruce (DE-588)120623013 (DE-627)080788696 (DE-576)16951241X oth Meunier, Alain 1948- (DE-588)1145752241 (DE-627)1006899111 (DE-576)169517640 oth 9783540756330 Buchausg. u.d.T. Velde, Bruce The origin of clay minerals in soils and weathered rocks ; with 23 tables Berlin : Springer, 2008 XII, 406 S. (DE-627)544000641 (DE-576)272865133 3540756337 9783540756330 https://doi.org/10.1007/978-3-540-75634-7 Verlag Volltext http://dx.doi.org/10.1007/978-3-540-75634-7 Resolving-System lizenzpflichtig Volltext https://swbplus.bsz-bw.de/bsz285794760cov.jpg V:DE-576 X:springer image/jpeg 20130327143601 Cover https://swbplus.bsz-bw.de/bsz272865133inh.htm V:DE-576 text/html Inhaltsverzeichnis http://deposit.dnb.de/cgi-bin/dokserv?id=3002275&prov=M&dok_var=1&dok_ext=htm X: MVB text/html 20130501 Verlag Inhaltstext (DE-627)577106635 ZDB-2-EES 2008 GBV_ILN_23 ISIL_DE-830 SYSFLAG_1 GBV_KXP SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_60 ISIL_DE-705 GBV_ILN_65 ISIL_DE-3 GBV_ILN_120 ISIL_DE-715 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2148 ISIL_DE-950 GBV ExPruef TY 2000 Sedimentäre (exogene) Bildungen Geowissenschaften Angewandte Geologie Lagerstättenkunde Bildungsvorgänge der Lagerstätten Sedimentäre (exogene) Bildungen (DE-627)1271953471 (DE-625)rvk/145062: (DE-576)201953471 RB 10162 Spezielle Bodenkunde (Klassifikation, Benennung, Bodenart und Bodentypen, Klima und Böden) Geografie Nicht regional gebundene Darstellungen Allgemeine Geografie Hilfswissenschaften Bodenkunde (Pedologie) Spezielle Bodenkunde (Klassifikation, Benennung, Bodenart und Bodentypen, Klima und Böden) (DE-627)1271490188 (DE-625)rvk/142220:12642 (DE-576)201490188 TH 7000 Tonige Gesteine Geologie und Paläontologie Petrographie Sedimentgesteine Klastisches Sediment Tonige Gesteine (DE-627)1271933829 (DE-625)rvk/144019: (DE-576)201933829 Ungueltig 38.61 Bodenbildung Bodenentwicklung SEPA (DE-627)181569949 38.30 Mineralogie SEPA (DE-627)106419471 BO 045F 551.305015496 045F 549/.6 23 01 0830 89000000X 00 --%%-- --%%-- s --%%-- olr-springer i z 08-09-08 60 01 0705 4304950746 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 65 01 0003 1655658468 03 --%%-- ebook --%%-- --%%-- OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. k3o 02-01-17 120 01 0715 1840107871 OLR-ESP Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden. z 13-01-19 120 02 0715 3581156342 00 --%%-- --%%-- g --%%-- alma z 24-01-20 370 01 4370 201230313 olr-springer Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. i z 28-01-09 2027 01 DE-105 3322210537 00 --%%-- --%%-- n --%%-- Campuslizenz l01 01-03-10 2050 01 DE-Zi4 3322210553 00 --%%-- --%%-- n --%%-- Elektronischer Volltext - Campuslizenz l01 01-03-10 2148 01 DE-950 3322210588 00 --%%-- eBook Springer --%%-- n Elektronischer Volltext - Campuslizenz l01 17-09-08 23 01 0830 Springer EBook https://doi.org/10.1007/978-3-540-75634-7 60 01 0705 Volltextzugang Campus https://doi.org/10.1007/978-3-540-75634-7 65 01 0003 Volltextzugang Campus https://doi.org/10.1007/978-3-540-75634-7 120 01 0715 http://dx.doi.org/10.1007/978-3-540-75634-7 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991016136295803501 370 01 4370 E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich https://doi.org/10.1007/978-3-540-75634-7 2050 01 DE-Zi4 http://dx.doi.org/10.1007/978-3-540-75634-7 2148 01 DE-950 http://dx.doi.org/10.1007/978-3-540-75634-7 2027 01 DE-105 00 s ebook 120 00 DE-715 99 ww 2027 01 DE-105 00 (DE-627)1292502630 DK 549.623.9 2027 01 DE-105 00 (DE-627)1294202073 DK 549.01 2027 01 DE-105 00 (DE-627)1299854869 DK 549.02 2027 01 DE-105 00 (DE-627)1292553715 DK 552.11 2027 01 DE-105 00 (DE-627)1292331534 DK 548.5 2027 01 DE-105 00 (DE-627)1292218487 DK 552.52 2027 01 DE-105 00 (DE-627)1292683104 DK 548.3 2027 01 DE-105 00 (DE-627)1292790490 DK 551.3.053 2027 01 DE-105 00 (DE-627)1293807990 DK 551.311.23 2027 01 DE-105 00 (DE-627)1292536969 DK 631.41 23 01 0830 2007-06282, 2007-06284, 2007-06285, 2007-06286, 2007-06287, 2007-06289, 2007-06291 120 01 0715 YH 2020 23 01 0830 olr-springer 60 01 0705 SpringerLink 65 01 0003 OLR-SEB-ZDB-2-EES 120 01 0715 OLR-ESP 120 02 0715 alma 370 01 4370 olr-springer 23 01 0830 2008.09.08 |
allfields_unstemmed |
9783540756347 978-3-540-75634-7 10.1007/978-3-540-75634-7 doi (DE-627)1647264014 (DE-576)285794760 (DE-599)BSZ285794760 (OCoLC)272298878 (OCoLC)315990349 (DE-He213)978-3-540-75634-7 DE-627 ger DE-627 rakwb eng XA-DE QE389.625 PNV bicssc SCI048000 bisacsh TY 2000 SEPA rvk (DE-625)rvk/145062: RB 10162 BVB rvk (DE-625)rvk/142220:12642 38.61 bkl 38.30 bkl The Origin of Clay Minerals in Soils and Weathered Rocks by Bruce Velde, Alain Meunier Berlin, Heidelberg Springer-Verlag Berlin Heidelberg 2008 Online-Ressource (digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier SpringerLink Bücher Includes bibliographical references and index Preface; Contents; Introduction; Chapter 1 Fundamentals of Clay Mineral Crystal Structure and Physicochemical Properties; Chapter 2 Basics for the Study of Soil and Weathered Rock Geochemical Systems; Chapter 3 The Development of Soils and Weathering Profile; Chapter 4 Clay Mineral Formation in Weathered Rocks: Water/Rock Interaction; Chapter 5 Plants and Soil Clay Minerals; Chapter 6 Clays and Climate - Clay Assemblages Formed under Extreme Humidity Conditions; Chapter 7 Physical Disequilibrium and Transportation of Soil Material Chapter 8 The Place of Clay Mineral Species in Soils and AlteritesAnnex 1 Polytypes; Annex 2 Mixed Layer Minerals; Annex 3 Cation Exchange Capacity; Annex 4 Hydroxy-Interlayered Minerals (HIMs); Annex 5 Phase Diagrams Applied to Clay Mineral Assemblages; Annex 6 Kinetics; References; Index Of huge relevance in a number of fields, this is a survey of the different processes of soil clay mineral formation and the consequences of these processes concerning the soil ecosystem, especially plant and mineral. Two independent systems form soil materials. The first is the interaction of rocks and water, unstable minerals adjusting to surface conditions. The second is the interaction of the biosphere with clays in the upper parts of alteration profiles. The importance of clay minerals and their origin is crucial to an understanding of the physico-chemical functions of the interface at the Earth’s surface. Their place is that of contact between the mineral world and the living world, plants and finally mankind. This contact zone is the realm of much of the environment as we see it today. If we can understand the way clays function in their interaction with plants, we can understand the major forces which shape our immediate environment. We see increasingly that human activity interacts with the plant and mineral interface through the use of more powerful chemicals, either by purposeful application of accidental dispersion. Knowledge of the origin and transformation of clay minerals, their dynamic response to changing chemistry, is the key to a rational use of this natural boundary which affects our lives. The information and the analysis presented here is an attempt to set trends of research in the direction of preventive and creative use of the plant – soil interface. Clays are the product of slow transformations of high temperature rocks into reactive, fine grained material. This material, once in the sphere of plant interaction, becomes highly reactive with transformation periods of tens to hundreds of years. The challenge of the future is to use these rapid responses to the benefit of mankind. This book aims to further a better understanding of such mechanisms, and it is thus destined for an audience of ecologists, pedologists, agronomists and other researchers involved in earth surface science Geography Geology Physical geography Mines and mineral resources Mineralogy Sedimentology Soil conservation Earth Sciences Geography Geology Physical geography Mines and mineral resources Mineralogy Sedimentology Soil conservation s (DE-588)4146131-9 (DE-627)104324937 (DE-576)20974670X Bodenbildung gnd s (DE-588)4063385-8 (DE-627)106128302 (DE-576)209148365 Verwitterung gnd s (DE-588)4185687-9 (DE-627)105285358 (DE-576)210034033 Tonmineral gnd DE-101 s (DE-588)4020734-1 (DE-627)106316923 (DE-576)208934618 Gestein gnd s (DE-588)4185646-6 (DE-627)104789557 (DE-576)210033797 Ton Geologie gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4238806-5 (DE-627)104876751 (DE-576)210416106 Chemische Verwitterung gnd s (DE-588)4185688-0 (DE-627)10528534X (DE-576)210034041 Tonmineralogie gnd (DE-627) s (DE-588)4185687-9 (DE-627)105285358 (DE-576)210034033 Tonmineral gnd s (DE-588)4007348-8 (DE-627)106373889 (DE-576)208869859 Boden gnd s (DE-588)4063385-8 (DE-627)106128302 (DE-576)209148365 Verwitterung gnd s (DE-588)4020734-1 (DE-627)106316923 (DE-576)208934618 Gestein gnd (DE-627) Velde, Bruce (DE-588)120623013 (DE-627)080788696 (DE-576)16951241X oth Meunier, Alain 1948- (DE-588)1145752241 (DE-627)1006899111 (DE-576)169517640 oth 9783540756330 Buchausg. u.d.T. Velde, Bruce The origin of clay minerals in soils and weathered rocks ; with 23 tables Berlin : Springer, 2008 XII, 406 S. (DE-627)544000641 (DE-576)272865133 3540756337 9783540756330 https://doi.org/10.1007/978-3-540-75634-7 Verlag Volltext http://dx.doi.org/10.1007/978-3-540-75634-7 Resolving-System lizenzpflichtig Volltext https://swbplus.bsz-bw.de/bsz285794760cov.jpg V:DE-576 X:springer image/jpeg 20130327143601 Cover https://swbplus.bsz-bw.de/bsz272865133inh.htm V:DE-576 text/html Inhaltsverzeichnis http://deposit.dnb.de/cgi-bin/dokserv?id=3002275&prov=M&dok_var=1&dok_ext=htm X: MVB text/html 20130501 Verlag Inhaltstext (DE-627)577106635 ZDB-2-EES 2008 GBV_ILN_23 ISIL_DE-830 SYSFLAG_1 GBV_KXP SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_60 ISIL_DE-705 GBV_ILN_65 ISIL_DE-3 GBV_ILN_120 ISIL_DE-715 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2148 ISIL_DE-950 GBV ExPruef TY 2000 Sedimentäre (exogene) Bildungen Geowissenschaften Angewandte Geologie Lagerstättenkunde Bildungsvorgänge der Lagerstätten Sedimentäre (exogene) Bildungen (DE-627)1271953471 (DE-625)rvk/145062: (DE-576)201953471 RB 10162 Spezielle Bodenkunde (Klassifikation, Benennung, Bodenart und Bodentypen, Klima und Böden) Geografie Nicht regional gebundene Darstellungen Allgemeine Geografie Hilfswissenschaften Bodenkunde (Pedologie) Spezielle Bodenkunde (Klassifikation, Benennung, Bodenart und Bodentypen, Klima und Böden) (DE-627)1271490188 (DE-625)rvk/142220:12642 (DE-576)201490188 TH 7000 Tonige Gesteine Geologie und Paläontologie Petrographie Sedimentgesteine Klastisches Sediment Tonige Gesteine (DE-627)1271933829 (DE-625)rvk/144019: (DE-576)201933829 Ungueltig 38.61 Bodenbildung Bodenentwicklung SEPA (DE-627)181569949 38.30 Mineralogie SEPA (DE-627)106419471 BO 045F 551.305015496 045F 549/.6 23 01 0830 89000000X 00 --%%-- --%%-- s --%%-- olr-springer i z 08-09-08 60 01 0705 4304950746 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 65 01 0003 1655658468 03 --%%-- ebook --%%-- --%%-- OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. k3o 02-01-17 120 01 0715 1840107871 OLR-ESP Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden. z 13-01-19 120 02 0715 3581156342 00 --%%-- --%%-- g --%%-- alma z 24-01-20 370 01 4370 201230313 olr-springer Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. i z 28-01-09 2027 01 DE-105 3322210537 00 --%%-- --%%-- n --%%-- Campuslizenz l01 01-03-10 2050 01 DE-Zi4 3322210553 00 --%%-- --%%-- n --%%-- Elektronischer Volltext - Campuslizenz l01 01-03-10 2148 01 DE-950 3322210588 00 --%%-- eBook Springer --%%-- n Elektronischer Volltext - Campuslizenz l01 17-09-08 23 01 0830 Springer EBook https://doi.org/10.1007/978-3-540-75634-7 60 01 0705 Volltextzugang Campus https://doi.org/10.1007/978-3-540-75634-7 65 01 0003 Volltextzugang Campus https://doi.org/10.1007/978-3-540-75634-7 120 01 0715 http://dx.doi.org/10.1007/978-3-540-75634-7 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991016136295803501 370 01 4370 E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich https://doi.org/10.1007/978-3-540-75634-7 2050 01 DE-Zi4 http://dx.doi.org/10.1007/978-3-540-75634-7 2148 01 DE-950 http://dx.doi.org/10.1007/978-3-540-75634-7 2027 01 DE-105 00 s ebook 120 00 DE-715 99 ww 2027 01 DE-105 00 (DE-627)1292502630 DK 549.623.9 2027 01 DE-105 00 (DE-627)1294202073 DK 549.01 2027 01 DE-105 00 (DE-627)1299854869 DK 549.02 2027 01 DE-105 00 (DE-627)1292553715 DK 552.11 2027 01 DE-105 00 (DE-627)1292331534 DK 548.5 2027 01 DE-105 00 (DE-627)1292218487 DK 552.52 2027 01 DE-105 00 (DE-627)1292683104 DK 548.3 2027 01 DE-105 00 (DE-627)1292790490 DK 551.3.053 2027 01 DE-105 00 (DE-627)1293807990 DK 551.311.23 2027 01 DE-105 00 (DE-627)1292536969 DK 631.41 23 01 0830 2007-06282, 2007-06284, 2007-06285, 2007-06286, 2007-06287, 2007-06289, 2007-06291 120 01 0715 YH 2020 23 01 0830 olr-springer 60 01 0705 SpringerLink 65 01 0003 OLR-SEB-ZDB-2-EES 120 01 0715 OLR-ESP 120 02 0715 alma 370 01 4370 olr-springer 23 01 0830 2008.09.08 |
allfieldsGer |
9783540756347 978-3-540-75634-7 10.1007/978-3-540-75634-7 doi (DE-627)1647264014 (DE-576)285794760 (DE-599)BSZ285794760 (OCoLC)272298878 (OCoLC)315990349 (DE-He213)978-3-540-75634-7 DE-627 ger DE-627 rakwb eng XA-DE QE389.625 PNV bicssc SCI048000 bisacsh TY 2000 SEPA rvk (DE-625)rvk/145062: RB 10162 BVB rvk (DE-625)rvk/142220:12642 38.61 bkl 38.30 bkl The Origin of Clay Minerals in Soils and Weathered Rocks by Bruce Velde, Alain Meunier Berlin, Heidelberg Springer-Verlag Berlin Heidelberg 2008 Online-Ressource (digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier SpringerLink Bücher Includes bibliographical references and index Preface; Contents; Introduction; Chapter 1 Fundamentals of Clay Mineral Crystal Structure and Physicochemical Properties; Chapter 2 Basics for the Study of Soil and Weathered Rock Geochemical Systems; Chapter 3 The Development of Soils and Weathering Profile; Chapter 4 Clay Mineral Formation in Weathered Rocks: Water/Rock Interaction; Chapter 5 Plants and Soil Clay Minerals; Chapter 6 Clays and Climate - Clay Assemblages Formed under Extreme Humidity Conditions; Chapter 7 Physical Disequilibrium and Transportation of Soil Material Chapter 8 The Place of Clay Mineral Species in Soils and AlteritesAnnex 1 Polytypes; Annex 2 Mixed Layer Minerals; Annex 3 Cation Exchange Capacity; Annex 4 Hydroxy-Interlayered Minerals (HIMs); Annex 5 Phase Diagrams Applied to Clay Mineral Assemblages; Annex 6 Kinetics; References; Index Of huge relevance in a number of fields, this is a survey of the different processes of soil clay mineral formation and the consequences of these processes concerning the soil ecosystem, especially plant and mineral. Two independent systems form soil materials. The first is the interaction of rocks and water, unstable minerals adjusting to surface conditions. The second is the interaction of the biosphere with clays in the upper parts of alteration profiles. The importance of clay minerals and their origin is crucial to an understanding of the physico-chemical functions of the interface at the Earth’s surface. Their place is that of contact between the mineral world and the living world, plants and finally mankind. This contact zone is the realm of much of the environment as we see it today. If we can understand the way clays function in their interaction with plants, we can understand the major forces which shape our immediate environment. We see increasingly that human activity interacts with the plant and mineral interface through the use of more powerful chemicals, either by purposeful application of accidental dispersion. Knowledge of the origin and transformation of clay minerals, their dynamic response to changing chemistry, is the key to a rational use of this natural boundary which affects our lives. The information and the analysis presented here is an attempt to set trends of research in the direction of preventive and creative use of the plant – soil interface. Clays are the product of slow transformations of high temperature rocks into reactive, fine grained material. This material, once in the sphere of plant interaction, becomes highly reactive with transformation periods of tens to hundreds of years. The challenge of the future is to use these rapid responses to the benefit of mankind. This book aims to further a better understanding of such mechanisms, and it is thus destined for an audience of ecologists, pedologists, agronomists and other researchers involved in earth surface science Geography Geology Physical geography Mines and mineral resources Mineralogy Sedimentology Soil conservation Earth Sciences Geography Geology Physical geography Mines and mineral resources Mineralogy Sedimentology Soil conservation s (DE-588)4146131-9 (DE-627)104324937 (DE-576)20974670X Bodenbildung gnd s (DE-588)4063385-8 (DE-627)106128302 (DE-576)209148365 Verwitterung gnd s (DE-588)4185687-9 (DE-627)105285358 (DE-576)210034033 Tonmineral gnd DE-101 s (DE-588)4020734-1 (DE-627)106316923 (DE-576)208934618 Gestein gnd s (DE-588)4185646-6 (DE-627)104789557 (DE-576)210033797 Ton Geologie gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4238806-5 (DE-627)104876751 (DE-576)210416106 Chemische Verwitterung gnd s (DE-588)4185688-0 (DE-627)10528534X (DE-576)210034041 Tonmineralogie gnd (DE-627) s (DE-588)4185687-9 (DE-627)105285358 (DE-576)210034033 Tonmineral gnd s (DE-588)4007348-8 (DE-627)106373889 (DE-576)208869859 Boden gnd s (DE-588)4063385-8 (DE-627)106128302 (DE-576)209148365 Verwitterung gnd s (DE-588)4020734-1 (DE-627)106316923 (DE-576)208934618 Gestein gnd (DE-627) Velde, Bruce (DE-588)120623013 (DE-627)080788696 (DE-576)16951241X oth Meunier, Alain 1948- (DE-588)1145752241 (DE-627)1006899111 (DE-576)169517640 oth 9783540756330 Buchausg. u.d.T. Velde, Bruce The origin of clay minerals in soils and weathered rocks ; with 23 tables Berlin : Springer, 2008 XII, 406 S. (DE-627)544000641 (DE-576)272865133 3540756337 9783540756330 https://doi.org/10.1007/978-3-540-75634-7 Verlag Volltext http://dx.doi.org/10.1007/978-3-540-75634-7 Resolving-System lizenzpflichtig Volltext https://swbplus.bsz-bw.de/bsz285794760cov.jpg V:DE-576 X:springer image/jpeg 20130327143601 Cover https://swbplus.bsz-bw.de/bsz272865133inh.htm V:DE-576 text/html Inhaltsverzeichnis http://deposit.dnb.de/cgi-bin/dokserv?id=3002275&prov=M&dok_var=1&dok_ext=htm X: MVB text/html 20130501 Verlag Inhaltstext (DE-627)577106635 ZDB-2-EES 2008 GBV_ILN_23 ISIL_DE-830 SYSFLAG_1 GBV_KXP SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_60 ISIL_DE-705 GBV_ILN_65 ISIL_DE-3 GBV_ILN_120 ISIL_DE-715 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2148 ISIL_DE-950 GBV ExPruef TY 2000 Sedimentäre (exogene) Bildungen Geowissenschaften Angewandte Geologie Lagerstättenkunde Bildungsvorgänge der Lagerstätten Sedimentäre (exogene) Bildungen (DE-627)1271953471 (DE-625)rvk/145062: (DE-576)201953471 RB 10162 Spezielle Bodenkunde (Klassifikation, Benennung, Bodenart und Bodentypen, Klima und Böden) Geografie Nicht regional gebundene Darstellungen Allgemeine Geografie Hilfswissenschaften Bodenkunde (Pedologie) Spezielle Bodenkunde (Klassifikation, Benennung, Bodenart und Bodentypen, Klima und Böden) (DE-627)1271490188 (DE-625)rvk/142220:12642 (DE-576)201490188 TH 7000 Tonige Gesteine Geologie und Paläontologie Petrographie Sedimentgesteine Klastisches Sediment Tonige Gesteine (DE-627)1271933829 (DE-625)rvk/144019: (DE-576)201933829 Ungueltig 38.61 Bodenbildung Bodenentwicklung SEPA (DE-627)181569949 38.30 Mineralogie SEPA (DE-627)106419471 BO 045F 551.305015496 045F 549/.6 23 01 0830 89000000X 00 --%%-- --%%-- s --%%-- olr-springer i z 08-09-08 60 01 0705 4304950746 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 65 01 0003 1655658468 03 --%%-- ebook --%%-- --%%-- OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. k3o 02-01-17 120 01 0715 1840107871 OLR-ESP Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden. z 13-01-19 120 02 0715 3581156342 00 --%%-- --%%-- g --%%-- alma z 24-01-20 370 01 4370 201230313 olr-springer Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. i z 28-01-09 2027 01 DE-105 3322210537 00 --%%-- --%%-- n --%%-- Campuslizenz l01 01-03-10 2050 01 DE-Zi4 3322210553 00 --%%-- --%%-- n --%%-- Elektronischer Volltext - Campuslizenz l01 01-03-10 2148 01 DE-950 3322210588 00 --%%-- eBook Springer --%%-- n Elektronischer Volltext - Campuslizenz l01 17-09-08 23 01 0830 Springer EBook https://doi.org/10.1007/978-3-540-75634-7 60 01 0705 Volltextzugang Campus https://doi.org/10.1007/978-3-540-75634-7 65 01 0003 Volltextzugang Campus https://doi.org/10.1007/978-3-540-75634-7 120 01 0715 http://dx.doi.org/10.1007/978-3-540-75634-7 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991016136295803501 370 01 4370 E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich https://doi.org/10.1007/978-3-540-75634-7 2050 01 DE-Zi4 http://dx.doi.org/10.1007/978-3-540-75634-7 2148 01 DE-950 http://dx.doi.org/10.1007/978-3-540-75634-7 2027 01 DE-105 00 s ebook 120 00 DE-715 99 ww 2027 01 DE-105 00 (DE-627)1292502630 DK 549.623.9 2027 01 DE-105 00 (DE-627)1294202073 DK 549.01 2027 01 DE-105 00 (DE-627)1299854869 DK 549.02 2027 01 DE-105 00 (DE-627)1292553715 DK 552.11 2027 01 DE-105 00 (DE-627)1292331534 DK 548.5 2027 01 DE-105 00 (DE-627)1292218487 DK 552.52 2027 01 DE-105 00 (DE-627)1292683104 DK 548.3 2027 01 DE-105 00 (DE-627)1292790490 DK 551.3.053 2027 01 DE-105 00 (DE-627)1293807990 DK 551.311.23 2027 01 DE-105 00 (DE-627)1292536969 DK 631.41 23 01 0830 2007-06282, 2007-06284, 2007-06285, 2007-06286, 2007-06287, 2007-06289, 2007-06291 120 01 0715 YH 2020 23 01 0830 olr-springer 60 01 0705 SpringerLink 65 01 0003 OLR-SEB-ZDB-2-EES 120 01 0715 OLR-ESP 120 02 0715 alma 370 01 4370 olr-springer 23 01 0830 2008.09.08 |
allfieldsSound |
9783540756347 978-3-540-75634-7 10.1007/978-3-540-75634-7 doi (DE-627)1647264014 (DE-576)285794760 (DE-599)BSZ285794760 (OCoLC)272298878 (OCoLC)315990349 (DE-He213)978-3-540-75634-7 DE-627 ger DE-627 rakwb eng XA-DE QE389.625 PNV bicssc SCI048000 bisacsh TY 2000 SEPA rvk (DE-625)rvk/145062: RB 10162 BVB rvk (DE-625)rvk/142220:12642 38.61 bkl 38.30 bkl The Origin of Clay Minerals in Soils and Weathered Rocks by Bruce Velde, Alain Meunier Berlin, Heidelberg Springer-Verlag Berlin Heidelberg 2008 Online-Ressource (digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier SpringerLink Bücher Includes bibliographical references and index Preface; Contents; Introduction; Chapter 1 Fundamentals of Clay Mineral Crystal Structure and Physicochemical Properties; Chapter 2 Basics for the Study of Soil and Weathered Rock Geochemical Systems; Chapter 3 The Development of Soils and Weathering Profile; Chapter 4 Clay Mineral Formation in Weathered Rocks: Water/Rock Interaction; Chapter 5 Plants and Soil Clay Minerals; Chapter 6 Clays and Climate - Clay Assemblages Formed under Extreme Humidity Conditions; Chapter 7 Physical Disequilibrium and Transportation of Soil Material Chapter 8 The Place of Clay Mineral Species in Soils and AlteritesAnnex 1 Polytypes; Annex 2 Mixed Layer Minerals; Annex 3 Cation Exchange Capacity; Annex 4 Hydroxy-Interlayered Minerals (HIMs); Annex 5 Phase Diagrams Applied to Clay Mineral Assemblages; Annex 6 Kinetics; References; Index Of huge relevance in a number of fields, this is a survey of the different processes of soil clay mineral formation and the consequences of these processes concerning the soil ecosystem, especially plant and mineral. Two independent systems form soil materials. The first is the interaction of rocks and water, unstable minerals adjusting to surface conditions. The second is the interaction of the biosphere with clays in the upper parts of alteration profiles. The importance of clay minerals and their origin is crucial to an understanding of the physico-chemical functions of the interface at the Earth’s surface. Their place is that of contact between the mineral world and the living world, plants and finally mankind. This contact zone is the realm of much of the environment as we see it today. If we can understand the way clays function in their interaction with plants, we can understand the major forces which shape our immediate environment. We see increasingly that human activity interacts with the plant and mineral interface through the use of more powerful chemicals, either by purposeful application of accidental dispersion. Knowledge of the origin and transformation of clay minerals, their dynamic response to changing chemistry, is the key to a rational use of this natural boundary which affects our lives. The information and the analysis presented here is an attempt to set trends of research in the direction of preventive and creative use of the plant – soil interface. Clays are the product of slow transformations of high temperature rocks into reactive, fine grained material. This material, once in the sphere of plant interaction, becomes highly reactive with transformation periods of tens to hundreds of years. The challenge of the future is to use these rapid responses to the benefit of mankind. This book aims to further a better understanding of such mechanisms, and it is thus destined for an audience of ecologists, pedologists, agronomists and other researchers involved in earth surface science Geography Geology Physical geography Mines and mineral resources Mineralogy Sedimentology Soil conservation Earth Sciences Geography Geology Physical geography Mines and mineral resources Mineralogy Sedimentology Soil conservation s (DE-588)4146131-9 (DE-627)104324937 (DE-576)20974670X Bodenbildung gnd s (DE-588)4063385-8 (DE-627)106128302 (DE-576)209148365 Verwitterung gnd s (DE-588)4185687-9 (DE-627)105285358 (DE-576)210034033 Tonmineral gnd DE-101 s (DE-588)4020734-1 (DE-627)106316923 (DE-576)208934618 Gestein gnd s (DE-588)4185646-6 (DE-627)104789557 (DE-576)210033797 Ton Geologie gnd s (DE-588)4020198-3 (DE-627)104529571 (DE-576)20893233X Geochemie gnd s (DE-588)4238806-5 (DE-627)104876751 (DE-576)210416106 Chemische Verwitterung gnd s (DE-588)4185688-0 (DE-627)10528534X (DE-576)210034041 Tonmineralogie gnd (DE-627) s (DE-588)4185687-9 (DE-627)105285358 (DE-576)210034033 Tonmineral gnd s (DE-588)4007348-8 (DE-627)106373889 (DE-576)208869859 Boden gnd s (DE-588)4063385-8 (DE-627)106128302 (DE-576)209148365 Verwitterung gnd s (DE-588)4020734-1 (DE-627)106316923 (DE-576)208934618 Gestein gnd (DE-627) Velde, Bruce (DE-588)120623013 (DE-627)080788696 (DE-576)16951241X oth Meunier, Alain 1948- (DE-588)1145752241 (DE-627)1006899111 (DE-576)169517640 oth 9783540756330 Buchausg. u.d.T. Velde, Bruce The origin of clay minerals in soils and weathered rocks ; with 23 tables Berlin : Springer, 2008 XII, 406 S. 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Preface; Contents; Introduction; Chapter 1 Fundamentals of Clay Mineral Crystal Structure and Physicochemical Properties; Chapter 2 Basics for the Study of Soil and Weathered Rock Geochemical Systems; Chapter 3 The Development of Soils and Weathering Profile; Chapter 4 Clay Mineral Formation in Weathered Rocks: Water/Rock Interaction; Chapter 5 Plants and Soil Clay Minerals; Chapter 6 Clays and Climate - Clay Assemblages Formed under Extreme Humidity Conditions; Chapter 7 Physical Disequilibrium and Transportation of Soil Material Chapter 8 The Place of Clay Mineral Species in Soils and AlteritesAnnex 1 Polytypes; Annex 2 Mixed Layer Minerals; Annex 3 Cation Exchange Capacity; Annex 4 Hydroxy-Interlayered Minerals (HIMs); Annex 5 Phase Diagrams Applied to Clay Mineral Assemblages; Annex 6 Kinetics; References; Index |
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Preface; Contents; Introduction; Chapter 1 Fundamentals of Clay Mineral Crystal Structure and Physicochemical Properties; Chapter 2 Basics for the Study of Soil and Weathered Rock Geochemical Systems; Chapter 3 The Development of Soils and Weathering Profile; Chapter 4 Clay Mineral Formation in Weathered Rocks: Water/Rock Interaction; Chapter 5 Plants and Soil Clay Minerals; Chapter 6 Clays and Climate - Clay Assemblages Formed under Extreme Humidity Conditions; Chapter 7 Physical Disequilibrium and Transportation of Soil Material Chapter 8 The Place of Clay Mineral Species in Soils and AlteritesAnnex 1 Polytypes; Annex 2 Mixed Layer Minerals; Annex 3 Cation Exchange Capacity; Annex 4 Hydroxy-Interlayered Minerals (HIMs); Annex 5 Phase Diagrams Applied to Clay Mineral Assemblages; Annex 6 Kinetics; References; Index misc QE389.625 rvk TY 2000 rvk RB 10162 bkl 38.61 bkl 38.30 misc Geography misc Geology misc Physical geography misc Mines and mineral resources misc Mineralogy misc Sedimentology misc Soil conservation misc Earth Sciences gnd Bodenbildung gnd Verwitterung gnd Tonmineral gnd Gestein gnd Ton gnd Geochemie gnd Chemische Verwitterung gnd Tonmineralogie gnd Boden 2027 ebook The Origin of Clay Minerals in Soils and Weathered Rocks |
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origin of clay minerals in soils and weathered rocks |
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The Origin of Clay Minerals in Soils and Weathered Rocks |
abstract |
Of huge relevance in a number of fields, this is a survey of the different processes of soil clay mineral formation and the consequences of these processes concerning the soil ecosystem, especially plant and mineral. Two independent systems form soil materials. The first is the interaction of rocks and water, unstable minerals adjusting to surface conditions. The second is the interaction of the biosphere with clays in the upper parts of alteration profiles. The importance of clay minerals and their origin is crucial to an understanding of the physico-chemical functions of the interface at the Earth’s surface. Their place is that of contact between the mineral world and the living world, plants and finally mankind. This contact zone is the realm of much of the environment as we see it today. If we can understand the way clays function in their interaction with plants, we can understand the major forces which shape our immediate environment. We see increasingly that human activity interacts with the plant and mineral interface through the use of more powerful chemicals, either by purposeful application of accidental dispersion. Knowledge of the origin and transformation of clay minerals, their dynamic response to changing chemistry, is the key to a rational use of this natural boundary which affects our lives. The information and the analysis presented here is an attempt to set trends of research in the direction of preventive and creative use of the plant – soil interface. Clays are the product of slow transformations of high temperature rocks into reactive, fine grained material. This material, once in the sphere of plant interaction, becomes highly reactive with transformation periods of tens to hundreds of years. The challenge of the future is to use these rapid responses to the benefit of mankind. This book aims to further a better understanding of such mechanisms, and it is thus destined for an audience of ecologists, pedologists, agronomists and other researchers involved in earth surface science Includes bibliographical references and index |
abstractGer |
Of huge relevance in a number of fields, this is a survey of the different processes of soil clay mineral formation and the consequences of these processes concerning the soil ecosystem, especially plant and mineral. Two independent systems form soil materials. The first is the interaction of rocks and water, unstable minerals adjusting to surface conditions. The second is the interaction of the biosphere with clays in the upper parts of alteration profiles. The importance of clay minerals and their origin is crucial to an understanding of the physico-chemical functions of the interface at the Earth’s surface. Their place is that of contact between the mineral world and the living world, plants and finally mankind. This contact zone is the realm of much of the environment as we see it today. If we can understand the way clays function in their interaction with plants, we can understand the major forces which shape our immediate environment. We see increasingly that human activity interacts with the plant and mineral interface through the use of more powerful chemicals, either by purposeful application of accidental dispersion. Knowledge of the origin and transformation of clay minerals, their dynamic response to changing chemistry, is the key to a rational use of this natural boundary which affects our lives. The information and the analysis presented here is an attempt to set trends of research in the direction of preventive and creative use of the plant – soil interface. Clays are the product of slow transformations of high temperature rocks into reactive, fine grained material. This material, once in the sphere of plant interaction, becomes highly reactive with transformation periods of tens to hundreds of years. The challenge of the future is to use these rapid responses to the benefit of mankind. This book aims to further a better understanding of such mechanisms, and it is thus destined for an audience of ecologists, pedologists, agronomists and other researchers involved in earth surface science Includes bibliographical references and index |
abstract_unstemmed |
Of huge relevance in a number of fields, this is a survey of the different processes of soil clay mineral formation and the consequences of these processes concerning the soil ecosystem, especially plant and mineral. Two independent systems form soil materials. The first is the interaction of rocks and water, unstable minerals adjusting to surface conditions. The second is the interaction of the biosphere with clays in the upper parts of alteration profiles. The importance of clay minerals and their origin is crucial to an understanding of the physico-chemical functions of the interface at the Earth’s surface. Their place is that of contact between the mineral world and the living world, plants and finally mankind. This contact zone is the realm of much of the environment as we see it today. If we can understand the way clays function in their interaction with plants, we can understand the major forces which shape our immediate environment. We see increasingly that human activity interacts with the plant and mineral interface through the use of more powerful chemicals, either by purposeful application of accidental dispersion. Knowledge of the origin and transformation of clay minerals, their dynamic response to changing chemistry, is the key to a rational use of this natural boundary which affects our lives. The information and the analysis presented here is an attempt to set trends of research in the direction of preventive and creative use of the plant – soil interface. Clays are the product of slow transformations of high temperature rocks into reactive, fine grained material. This material, once in the sphere of plant interaction, becomes highly reactive with transformation periods of tens to hundreds of years. The challenge of the future is to use these rapid responses to the benefit of mankind. This book aims to further a better understanding of such mechanisms, and it is thus destined for an audience of ecologists, pedologists, agronomists and other researchers involved in earth surface science Includes bibliographical references and index |
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title_short |
The Origin of Clay Minerals in Soils and Weathered Rocks |
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Contents Introduction … Fundamentals of Clay Mineral Crystal Structure and Physicochemical Properties … Introduction … The Common Structure of Phyllosilicates … From Atomic Sheets to Layers … Negatively Charged Layers … The Different Layer-to-Layer Chemical Bonds … Polytypes and Mixed Layer Minerals … Layers of Identical Composition: Polytypes … Layers of Different Composition: Mixed Layer Minerals … Crystallites Particles Aggregates … Crystallites: The Limit of the Mineralogical Definition … Particles and Aggregates … The Principal Clay Mineral Species … The Cation Substitutions … The Principal Mineral Species of the … Phyllosilicate Group … Principal Mineral Species of the … Phyllosilicates Group without Interlayer Sheet … The … Phyllosilicates with an Interlayer Ion Sheet (Micas) … Phyllosilicates with a Brucite-type Interlayer Sheet … 1) … The Fibrous Clay Minerals: Sepiolite and Palygorskite … Typical Properties of Intermediate Charge Clay Minerals … Hydration and Swelling … The Crystallite Outer Surfaces … The Ion Exchange Capacity … Particularities of Clay Minerals: Size and Continuity … Clay Minerals are always Small … The Reduced Number of Layers in the Stacks Typical of Clay Minerals … From Order-Disorder to Crystal Defects … Composition Heterogeneity at the Scale of a Single Layer … How Do Clay Minerals Grow? … Phyllosilicate Growth Principles … Contents … Speculative Interpretation of Growth Processes Crystal Morphology Relations … Nucleation Processes in Clay-Bearing Rocks … Summary: Clay Minerals in Soils and Weathered Rocks … The … Clay Structure and Its Importance in Soils … The Illitic Minerals in Soils and Weathered Rocks … Expandable Minerals (Smectites Vermiculites) … Hydroxy Interlayered Minerals … Mixed Layer Minerals in Soils … Kaolinite and Kaolinite/Smectite Mixed Layer Minerals (K/S) … Allophane and Imogolite … The Non-Phyllosilicate Minerals in Soils and Weathered Rocks … Stability of Clay Minerals Formed under Weathering Conditions … Suggested Reading … Basics for the Study of Soil and Weathered Rock Geochemical Systems … Introduction … Definition of the Systems … The Size of the Systems under Consideration … The Solutions in Systems of Different Size … The Physicochemical Forces Acting in the Systems … Basic Definitions … The Chemical Potential … A Particular Chemical Potential: The pH … The Oxidation-Reduction Potential (Redox) … Mineral Reactions in Alteration Systems … Conditions at Equilibrium … Kinetics of Alteration Reactions … Suggested Reading … The Development of Soils and Weathering Profile … Introduction … Physical Description of Soils and Weathering Profiles … The Development of Weathering Profiles … The Development of Soils … Conclusion in a YES or NO Question Series … Dynamics of the Alteration Process under Temperate Conditions: An Investigation Comparing Soil and Rock Alteration in Profiles … Alteration in Temperate Climates … Kinetics of Alteration Processes … Kinetics of Soil Formation … The Inter-Relation of the Dynamics of the Alteration-Soil Profile Sequence … Overview of Soil and Weathering Mineralogy … The Mineralogy of Soil Horizons … Mineralogical and Chemical Differences between Alteration and Soil Zones … What Are the Clay Mineral Assemblages? … Formation of Different Clay Mineral Phases in A Horizon … General Schema of Alteration Zone and Soil Relations … Overview of Alteration in the Soil Zone in Temperate Climates … Suggested Reading … Clay Mineral Formation in Weathered Rocks: Water Rock Interaction … Introduction … Weathered Rock Profiles in Temperate Climates … Weathering at the Landscape Scale … The Parent Rock Control on Weathering Profiles … The Climate Control on Weathering Profiles … From Macro- to Microscopic Scale … The Internal Destabilization of Primary Minerals (Primary Plasmic Microsystems) … Porosity-Permeability and Microsystems in Crystalline Rocks … Petrography of Contact Microsystems … Petrography of the Primary Plasmic Microsystems … Mineral Reactions in the Secondary Plasmic Microsystems … Petrography of the Secondary Plasmic Microsystems … Clays Forming in Secondary Plasmic Microsystems … The Ultimate Weathering Stages … The Fissural Microsystems: Cutans … Accumulations (Absolute and Residual) … The Weathering of Porous Sedimentary Rocks … Glauconitic Sandstones … Weathering of Marls … Possible Models for Weathering Processes … From Heterogeneity to Homogeneity … Mass Balance and Weathering Rates … From Qualitative to Quantitative Models … Summary of the Water/Rock Interaction Clay-Forming Processes … Suggested Reading … Plants and Soil Clay Minerals … Introduction … Dynamics of Clay Reactions in the Soil (Plant/Clay Interaction) Zone of the A Horizon … Disequilibrium in Plant Soil Zone Clays … Dynamics of Clay Reactions in the Soils … Clay Mineral Types in the Plant Soil Interaction Zone … Illite … Kaolinite … Contents … Oxides and Oxyhydroxides … Mixed Layer Minerals … Soil Clay Mineral Assemblages by Ecological Type … Prairie Soils … Forest Soils … Chemical Control in Soil Horzion by Plant Action … Silica … Potassium … Element Loss and Element Gain … Agricultural Influences … Prairie Soil Clay Mineralogy in Agriculture … Effect of Fertilizer on Clay Minerals … Plants and Soil Clay Minerals: Some Thoughts for Further Consideration … Suggested Reading … Clays and Climate Clay Assemblages Formed under Extreme Humidity Conditions … Introduction … Impact of High Rainfall on Clay Mineralogy … Soil Development as a Function of Rainfall … Very High Rainfall … Rainfall and Vitreous Rocks (Andosols) … Andosol Characteristics … Weathering Processes Affecting Vitreous Rocks under Constantly Humid Conditions … Mineralogy and Hydration State of Andosols … Weathering Trends as a Function of Time … Weathering Trends as a Function of Time under Tropical Conditions … Weathering Trends in Semi-Arid and Arid Climates … Summary … Suggested Reading … Physical Disequilibrium and Transportation of Soil Material … Introduction … Slope Effects and Physical Disequilibrium … High Slopes in Mountains … Moderate Slopes … Wind and Water … Movement of Coarse Grained Material … Fine Grained Material … Wind Transport and Loess … Reaction Rates due to Plant/Loess Interaction … River Transport and Salt Marsh Sediments … Catena Movement of Fine Grained Material on Slopes … Topographically Controlled Soil Sequences … Slope and Smectite Genesis (Catenas) … Summary … Suggested Reading … The Place of Clay Mineral Species in Soils and Alterites … Introduction … Where Clay Mineral Types Occur in Alterites and Soils … The … Minerals … Kaolinite and Kaolinite/Smectite Mixed Layer Minerals … Gibbsite … Iron Oxyhydroxides … Imogolite and Allophane … Chlorites … Palygorskite, Sepiolite … Clay Minerals Present in Soils as a Response to Climate … Physical Factors and Their Effect on Alteration and Soil Clay Mineral Facies … Weathering Trend (Water Silicate Chemical Trends) … The Impact of Plant Regime on Clay Minerals in Soils … Reactivity of Clay Minerals in Ecosystems … Convergence of Soil Clay Mineralogies … Effect of Chemical Translocation by Plants on Clay Mineral Stabilities … Equilibrium and Disequilibrium of Soil Clays … The Structure of Alteration and Clay Formation … Water/Rock Interaction … Source Rock and Clays … Plant/Soil Interaction … Clay Transport … Kinetics of Clay Change in the Soil Zone … Minerals Present and Their Change in the Soil/Plant Interaction Zone … Conclusions … Perspectives for Clay Mineral Science in Surface Environments: Challenges for the Future … Soils and Crops … Soils as a Natural Safety Net for Modern Society … Suggested Reading … Annexes … Annex … Polytypes … Definition … An Example: The Mica or Illite Polytypes … References … Contents Annex … Mixed Layer Minerals … Conditions of Interstratification … Random Stacking Sequence (R0) … Ordered Stacking Sequences (R1) … References … Annex … Cation Exchange Capacity … The Chemical Reaction of Cation Exchange … Deviation from Ideality … The Variable Charges … References … Annex … Hydroxy-Interlayered Minerals (HIMs) … The XRD Properties of Hydroxy-Interlayered Minerals … The Incorporation of Al Ions in the Interlayer Region of HIMs … The Crystallochemical Composition of HIMs … The Mixed Layer Model … Conclusion … References … Annex … Phase Diagrams Applied to Clay Mineral Assemblages … Fundamentals … Clay Minerals: The Stable Phases at Surface of the Earth … References … Annex … Kinetics … Fundamentals … The Fick s Laws … Suggested Reading … References … Subject Index … |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000cam a22002652 4500</leader><controlfield tag="001">1647264014</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240918203505.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">080917s2008 gw |||||o 00| ||eng c</controlfield><datafield tag="020" ind1=" " ind2=" "><subfield code="a">9783540756347</subfield><subfield code="9">978-3-540-75634-7</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/978-3-540-75634-7</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)1647264014</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-576)285794760</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)BSZ285794760</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)272298878</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)315990349</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)978-3-540-75634-7</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="044" ind1=" " ind2=" "><subfield code="c">XA-DE</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">QE389.625</subfield></datafield><datafield tag="072" ind1=" " ind2="7"><subfield code="a">PNV</subfield><subfield code="2">bicssc</subfield></datafield><datafield tag="072" ind1=" " ind2="7"><subfield code="a">SCI048000</subfield><subfield code="2">bisacsh</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">TY 2000</subfield><subfield code="q">SEPA</subfield><subfield code="2">rvk</subfield><subfield code="0">(DE-625)rvk/145062:</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RB 10162</subfield><subfield code="q">BVB</subfield><subfield code="2">rvk</subfield><subfield code="0">(DE-625)rvk/142220:12642</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.61</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.30</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="245" ind1="1" ind2="4"><subfield code="a">The Origin of Clay Minerals in Soils and Weathered Rocks</subfield><subfield code="c">by Bruce Velde, Alain Meunier</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Berlin, Heidelberg</subfield><subfield code="b">Springer-Verlag Berlin Heidelberg</subfield><subfield code="c">2008</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">Online-Ressource (digital)</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="490" ind1="0" ind2=" "><subfield code="a">SpringerLink</subfield><subfield code="a">Bücher</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">Includes bibliographical references and index</subfield></datafield><datafield tag="505" ind1="8" ind2="0"><subfield code="a">Preface; Contents; Introduction; Chapter 1 Fundamentals of Clay Mineral Crystal Structure and Physicochemical Properties; Chapter 2 Basics for the Study of Soil and Weathered Rock Geochemical Systems; Chapter 3 The Development of Soils and Weathering Profile; Chapter 4 Clay Mineral Formation in Weathered Rocks: Water/Rock Interaction; Chapter 5 Plants and Soil Clay Minerals; Chapter 6 Clays and Climate - Clay Assemblages Formed under Extreme Humidity Conditions; Chapter 7 Physical Disequilibrium and Transportation of Soil Material</subfield></datafield><datafield tag="505" ind1="8" ind2="0"><subfield code="a">Chapter 8 The Place of Clay Mineral Species in Soils and AlteritesAnnex 1 Polytypes; Annex 2 Mixed Layer Minerals; Annex 3 Cation Exchange Capacity; Annex 4 Hydroxy-Interlayered Minerals (HIMs); Annex 5 Phase Diagrams Applied to Clay Mineral Assemblages; Annex 6 Kinetics; References; Index</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Of huge relevance in a number of fields, this is a survey of the different processes of soil clay mineral formation and the consequences of these processes concerning the soil ecosystem, especially plant and mineral. Two independent systems form soil materials. The first is the interaction of rocks and water, unstable minerals adjusting to surface conditions. The second is the interaction of the biosphere with clays in the upper parts of alteration profiles.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The importance of clay minerals and their origin is crucial to an understanding of the physico-chemical functions of the interface at the Earth’s surface. Their place is that of contact between the mineral world and the living world, plants and finally mankind. This contact zone is the realm of much of the environment as we see it today. If we can understand the way clays function in their interaction with plants, we can understand the major forces which shape our immediate environment. We see increasingly that human activity interacts with the plant and mineral interface through the use of more powerful chemicals, either by purposeful application of accidental dispersion. Knowledge of the origin and transformation of clay minerals, their dynamic response to changing chemistry, is the key to a rational use of this natural boundary which affects our lives. The information and the analysis presented here is an attempt to set trends of research in the direction of preventive and creative use of the plant – soil interface. Clays are the product of slow transformations of high temperature rocks into reactive, fine grained material. This material, once in the sphere of plant interaction, becomes highly reactive with transformation periods of tens to hundreds of years. The challenge of the future is to use these rapid responses to the benefit of mankind. 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