Black slate : surface alteration due to fungal activity

Black slates of different oxidation states and graphite samples as pure carbon source were incubated with the white-rot fungus Schizophyllum commune 4-39 for 3 months. Investigations by SEM showed fungal affinity to rough surfaces. Oxidatively weathered, bleached black slate samples have more microp...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Siegel, Daniela - 1980- [verfasserIn]
Körperschaften:	Friedrich-Schiller-Universität Jena [Grad-verleihende Institution]
Hochschulschrift:	Dissertation ; Friedrich-Schiller-Universität Jena ; 2010

Format:	E-Book
Sprache:	Englisch

Erschienen:	Jena: 2010

Schlagwörter:	Schwarzschiefer / Spaltblättling / Gesteinsoberfläche / Mikrobieller Abbau
Formangabe:	Hochschulschrift

Umfang:	1 Online-Ressource (141 Seiten)

Weitere Ausgabe:	Erscheint auch als Druck-Ausgabe Siegel, Daniela, 1980 -: Black slate - Jena, 2010

Links:	Link aufrufen Link aufrufen Volltext Volltext

DOI / URN:	urn:nbn:de:gbv:27-20101110-150704-4

Katalog-ID:	638874149

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Indexfelder

author_variant	d s ds
matchkey_str	siegeldaniela:2010----:lcs
oclc_num	713545365
hierarchy_sort_str	2010
bklnumber	43.13
publishDate	2010
allfields	11,O04 dnb 1010318284 DE-101 urn:nbn:de:gbv:27-20101110-150704-4 urn (DE-627)638874149 (DE-599)GBV638874149 (OCoLC)713545365 DE-627 ger DE-627 rda eng XA-DE 552.5 22/ger 579.61714 OCLC 22/ger 550 570 DNB 43.13 bkl Siegel, Daniela 1980- verfasserin (DE-588)142471941 (DE-627)636294773 (DE-576)330897829 aut Black slate surface alteration due to fungal activity vorgelegt von Daniela Siegel Jena 2010 1 Online-Ressource (141 Seiten) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Friedrich-Schiller-Universität Jena 2010 Black slates of different oxidation states and graphite samples as pure carbon source were incubated with the white-rot fungus Schizophyllum commune 4-39 for 3 months. Investigations by SEM showed fungal affinity to rough surfaces. Oxidatively weathered, bleached black slate samples have more micropores and increased surface roughness than unweathered samples. Unpolished and polished bleached black slate samples were colonized best by fungal hyphae. The hyphae often entered pores. Etch pits induced by fungal activity could be observed which were then quantified by vertical scanning interferometry (VSI). The etch pits measured 3 4 ?m in width and 180 200 nm in depth. In contrast to black slate samples, more etch pits were found on graphite surfaces. Moreover, they showed a more elongated morphology and branches reminiscent of fungal growth morphology. Under laboratory conditions, Schizophyllum commune was able to degrade about 0.03 ?m3/?m2 rock material during 3 months of incubation. It could be shown that collapsed hyphae material remained in their etch pits even after sample preparation which was caused by strong fungal fixation to the rock surfaces. The higher carbon content and the softness of pressed graphite thus allow for earlier fungal attachment and higher dissolution rates. Amounts of nitrogen could be proved by chemical analyzing techniques (x-ray photoelectron spectroscopy and electron microprobe) at all incubated rock samples. Nitrogen increased eminently on rock surfaces due to fungal colonization. Amounts of nitrogen were detected both on hyphae and former hyphae attachment areas. This indicates the presence of fungus and/or fungal excreted proteins such as hydrophobins for attachment or enzymes for degradation. Kurzfassung in dt. Sprache Archivierung/Langzeitarchivierung gewährleistet XA-DE-TH pdager DE-27 Archivierung/Langzeitarchivierung gewährleistet pdager DE-101 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content s (DE-588)4126782-5 (DE-627)105729744 (DE-576)209588020 Schwarzschiefer gnd s (DE-588)4221680-1 (DE-627)105008109 (DE-576)210275073 Spaltblättling gnd s (DE-588)4157161-7 (DE-627)105502979 (DE-576)209832274 Gesteinsoberfläche gnd s (DE-588)4039197-8 (DE-627)104409657 (DE-576)209034041 Mikrobieller Abbau gnd (DE-627) Friedrich-Schiller-Universität Jena Grad-verleihende Institution (DE-588)36164-1 (DE-627)100833012 (DE-576)190344695 dgg Jena (DE-588)4028557-1 (DE-627)104814411 (DE-576)208977872 uvp Erscheint auch als Druck-Ausgabe Siegel, Daniela, 1980 - Black slate Jena, 2010 102, XXV S. (DE-627)635633221 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 Langzeitarchivierung Resolving-System kostenfrei http://d-nb.info/1010318284/34 Langzeitarchivierung Nationalbibliothek Volltext https://www.db-thueringen.de/servlets/DerivateServlet/Derivate-21723/Siegel/Dissertation.pdf Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_31 ISIL_DE-27 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_213 ISIL_DE-551 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 43.13 Umwelttoxikologie (DE-627)106417037 BO 045F 552.5 045F 579.61714 20 01 0084 1231858052 x 10-03-11 21 01 0046 1252579632 z 19-06-11 22 01 0018 1252605951 SUBolrd xu 19-06-11 23 01 0830 125263109X olr-d x 19-06-11 30 01 0104 1252646437 z 19-06-11 31 01 0027 1194484204 z 07-04-09 40 01 0007 1252661037 xsn 19-06-11 60 01 0705 1252687133 OLRD z 20-06-11 63 01 3401 1595702059 ORD x 21-01-16 65 01 0003 416605919X GBV-ODiss Open Access z 14-07-22 70 01 0089 125271615X OA z 29-07-13 105 01 0841 1596515260 z 21-01-16 110 01 3110 1252698267 x 20-06-11 132 01 0959 149760849X OLR-DISS x 11-08-14 151 01 0546 3594118959 OLR-ODISS z 13-02-20 161 01 0960 1597470376 ORD x 28-01-16 213 01 0551 1252740905 ORD x 20-06-11 293 01 3293 1597913030 ORD xf 28-01-16 370 01 4370 1252713916 x 20-06-11 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 31 01 0027 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 LF 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 70 01 0089 http://edok01.tib.uni-hannover.de/edoks/e01dd13/638874149.pdf OA 70 01 0089 Leseprobe http://edok01.tib.uni-hannover.de/edoks/e01dd13/638874149l.pdf OA 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 213 01 0551 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 31 00 DE-27 00 Universitätsbibliographie Jena 31 00 DE-27 01 Chemisch-Geowissenschaftliche Fakultät 40 00 DE-7 00 (DE-627)644784881 VUA 000 Teilfragen {Geobiologie} 40 00 DE-7 01 (DE-627)625046501 VAH 000 Verwitterung {Geologie} 60 01 0705 10 ho 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 213 01 0551 ORD 293 01 3293 ORD 23 01 0830 2011-06-19:22:33:57
spelling	11,O04 dnb 1010318284 DE-101 urn:nbn:de:gbv:27-20101110-150704-4 urn (DE-627)638874149 (DE-599)GBV638874149 (OCoLC)713545365 DE-627 ger DE-627 rda eng XA-DE 552.5 22/ger 579.61714 OCLC 22/ger 550 570 DNB 43.13 bkl Siegel, Daniela 1980- verfasserin (DE-588)142471941 (DE-627)636294773 (DE-576)330897829 aut Black slate surface alteration due to fungal activity vorgelegt von Daniela Siegel Jena 2010 1 Online-Ressource (141 Seiten) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Friedrich-Schiller-Universität Jena 2010 Black slates of different oxidation states and graphite samples as pure carbon source were incubated with the white-rot fungus Schizophyllum commune 4-39 for 3 months. Investigations by SEM showed fungal affinity to rough surfaces. Oxidatively weathered, bleached black slate samples have more micropores and increased surface roughness than unweathered samples. Unpolished and polished bleached black slate samples were colonized best by fungal hyphae. The hyphae often entered pores. Etch pits induced by fungal activity could be observed which were then quantified by vertical scanning interferometry (VSI). The etch pits measured 3 4 ?m in width and 180 200 nm in depth. In contrast to black slate samples, more etch pits were found on graphite surfaces. Moreover, they showed a more elongated morphology and branches reminiscent of fungal growth morphology. Under laboratory conditions, Schizophyllum commune was able to degrade about 0.03 ?m3/?m2 rock material during 3 months of incubation. It could be shown that collapsed hyphae material remained in their etch pits even after sample preparation which was caused by strong fungal fixation to the rock surfaces. The higher carbon content and the softness of pressed graphite thus allow for earlier fungal attachment and higher dissolution rates. Amounts of nitrogen could be proved by chemical analyzing techniques (x-ray photoelectron spectroscopy and electron microprobe) at all incubated rock samples. Nitrogen increased eminently on rock surfaces due to fungal colonization. Amounts of nitrogen were detected both on hyphae and former hyphae attachment areas. This indicates the presence of fungus and/or fungal excreted proteins such as hydrophobins for attachment or enzymes for degradation. Kurzfassung in dt. Sprache Archivierung/Langzeitarchivierung gewährleistet XA-DE-TH pdager DE-27 Archivierung/Langzeitarchivierung gewährleistet pdager DE-101 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content s (DE-588)4126782-5 (DE-627)105729744 (DE-576)209588020 Schwarzschiefer gnd s (DE-588)4221680-1 (DE-627)105008109 (DE-576)210275073 Spaltblättling gnd s (DE-588)4157161-7 (DE-627)105502979 (DE-576)209832274 Gesteinsoberfläche gnd s (DE-588)4039197-8 (DE-627)104409657 (DE-576)209034041 Mikrobieller Abbau gnd (DE-627) Friedrich-Schiller-Universität Jena Grad-verleihende Institution (DE-588)36164-1 (DE-627)100833012 (DE-576)190344695 dgg Jena (DE-588)4028557-1 (DE-627)104814411 (DE-576)208977872 uvp Erscheint auch als Druck-Ausgabe Siegel, Daniela, 1980 - Black slate Jena, 2010 102, XXV S. (DE-627)635633221 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 Langzeitarchivierung Resolving-System kostenfrei http://d-nb.info/1010318284/34 Langzeitarchivierung Nationalbibliothek Volltext https://www.db-thueringen.de/servlets/DerivateServlet/Derivate-21723/Siegel/Dissertation.pdf Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_31 ISIL_DE-27 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_213 ISIL_DE-551 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 43.13 Umwelttoxikologie (DE-627)106417037 BO 045F 552.5 045F 579.61714 20 01 0084 1231858052 x 10-03-11 21 01 0046 1252579632 z 19-06-11 22 01 0018 1252605951 SUBolrd xu 19-06-11 23 01 0830 125263109X olr-d x 19-06-11 30 01 0104 1252646437 z 19-06-11 31 01 0027 1194484204 z 07-04-09 40 01 0007 1252661037 xsn 19-06-11 60 01 0705 1252687133 OLRD z 20-06-11 63 01 3401 1595702059 ORD x 21-01-16 65 01 0003 416605919X GBV-ODiss Open Access z 14-07-22 70 01 0089 125271615X OA z 29-07-13 105 01 0841 1596515260 z 21-01-16 110 01 3110 1252698267 x 20-06-11 132 01 0959 149760849X OLR-DISS x 11-08-14 151 01 0546 3594118959 OLR-ODISS z 13-02-20 161 01 0960 1597470376 ORD x 28-01-16 213 01 0551 1252740905 ORD x 20-06-11 293 01 3293 1597913030 ORD xf 28-01-16 370 01 4370 1252713916 x 20-06-11 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 31 01 0027 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 LF 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 70 01 0089 http://edok01.tib.uni-hannover.de/edoks/e01dd13/638874149.pdf OA 70 01 0089 Leseprobe http://edok01.tib.uni-hannover.de/edoks/e01dd13/638874149l.pdf OA 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 213 01 0551 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 31 00 DE-27 00 Universitätsbibliographie Jena 31 00 DE-27 01 Chemisch-Geowissenschaftliche Fakultät 40 00 DE-7 00 (DE-627)644784881 VUA 000 Teilfragen {Geobiologie} 40 00 DE-7 01 (DE-627)625046501 VAH 000 Verwitterung {Geologie} 60 01 0705 10 ho 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 213 01 0551 ORD 293 01 3293 ORD 23 01 0830 2011-06-19:22:33:57
allfields_unstemmed	11,O04 dnb 1010318284 DE-101 urn:nbn:de:gbv:27-20101110-150704-4 urn (DE-627)638874149 (DE-599)GBV638874149 (OCoLC)713545365 DE-627 ger DE-627 rda eng XA-DE 552.5 22/ger 579.61714 OCLC 22/ger 550 570 DNB 43.13 bkl Siegel, Daniela 1980- verfasserin (DE-588)142471941 (DE-627)636294773 (DE-576)330897829 aut Black slate surface alteration due to fungal activity vorgelegt von Daniela Siegel Jena 2010 1 Online-Ressource (141 Seiten) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Friedrich-Schiller-Universität Jena 2010 Black slates of different oxidation states and graphite samples as pure carbon source were incubated with the white-rot fungus Schizophyllum commune 4-39 for 3 months. Investigations by SEM showed fungal affinity to rough surfaces. Oxidatively weathered, bleached black slate samples have more micropores and increased surface roughness than unweathered samples. Unpolished and polished bleached black slate samples were colonized best by fungal hyphae. The hyphae often entered pores. Etch pits induced by fungal activity could be observed which were then quantified by vertical scanning interferometry (VSI). The etch pits measured 3 4 ?m in width and 180 200 nm in depth. In contrast to black slate samples, more etch pits were found on graphite surfaces. Moreover, they showed a more elongated morphology and branches reminiscent of fungal growth morphology. Under laboratory conditions, Schizophyllum commune was able to degrade about 0.03 ?m3/?m2 rock material during 3 months of incubation. It could be shown that collapsed hyphae material remained in their etch pits even after sample preparation which was caused by strong fungal fixation to the rock surfaces. The higher carbon content and the softness of pressed graphite thus allow for earlier fungal attachment and higher dissolution rates. Amounts of nitrogen could be proved by chemical analyzing techniques (x-ray photoelectron spectroscopy and electron microprobe) at all incubated rock samples. Nitrogen increased eminently on rock surfaces due to fungal colonization. Amounts of nitrogen were detected both on hyphae and former hyphae attachment areas. This indicates the presence of fungus and/or fungal excreted proteins such as hydrophobins for attachment or enzymes for degradation. Kurzfassung in dt. Sprache Archivierung/Langzeitarchivierung gewährleistet XA-DE-TH pdager DE-27 Archivierung/Langzeitarchivierung gewährleistet pdager DE-101 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content s (DE-588)4126782-5 (DE-627)105729744 (DE-576)209588020 Schwarzschiefer gnd s (DE-588)4221680-1 (DE-627)105008109 (DE-576)210275073 Spaltblättling gnd s (DE-588)4157161-7 (DE-627)105502979 (DE-576)209832274 Gesteinsoberfläche gnd s (DE-588)4039197-8 (DE-627)104409657 (DE-576)209034041 Mikrobieller Abbau gnd (DE-627) Friedrich-Schiller-Universität Jena Grad-verleihende Institution (DE-588)36164-1 (DE-627)100833012 (DE-576)190344695 dgg Jena (DE-588)4028557-1 (DE-627)104814411 (DE-576)208977872 uvp Erscheint auch als Druck-Ausgabe Siegel, Daniela, 1980 - Black slate Jena, 2010 102, XXV S. (DE-627)635633221 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 Langzeitarchivierung Resolving-System kostenfrei http://d-nb.info/1010318284/34 Langzeitarchivierung Nationalbibliothek Volltext https://www.db-thueringen.de/servlets/DerivateServlet/Derivate-21723/Siegel/Dissertation.pdf Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_31 ISIL_DE-27 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_213 ISIL_DE-551 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 43.13 Umwelttoxikologie (DE-627)106417037 BO 045F 552.5 045F 579.61714 20 01 0084 1231858052 x 10-03-11 21 01 0046 1252579632 z 19-06-11 22 01 0018 1252605951 SUBolrd xu 19-06-11 23 01 0830 125263109X olr-d x 19-06-11 30 01 0104 1252646437 z 19-06-11 31 01 0027 1194484204 z 07-04-09 40 01 0007 1252661037 xsn 19-06-11 60 01 0705 1252687133 OLRD z 20-06-11 63 01 3401 1595702059 ORD x 21-01-16 65 01 0003 416605919X GBV-ODiss Open Access z 14-07-22 70 01 0089 125271615X OA z 29-07-13 105 01 0841 1596515260 z 21-01-16 110 01 3110 1252698267 x 20-06-11 132 01 0959 149760849X OLR-DISS x 11-08-14 151 01 0546 3594118959 OLR-ODISS z 13-02-20 161 01 0960 1597470376 ORD x 28-01-16 213 01 0551 1252740905 ORD x 20-06-11 293 01 3293 1597913030 ORD xf 28-01-16 370 01 4370 1252713916 x 20-06-11 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 31 01 0027 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 LF 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 70 01 0089 http://edok01.tib.uni-hannover.de/edoks/e01dd13/638874149.pdf OA 70 01 0089 Leseprobe http://edok01.tib.uni-hannover.de/edoks/e01dd13/638874149l.pdf OA 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 213 01 0551 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 31 00 DE-27 00 Universitätsbibliographie Jena 31 00 DE-27 01 Chemisch-Geowissenschaftliche Fakultät 40 00 DE-7 00 (DE-627)644784881 VUA 000 Teilfragen {Geobiologie} 40 00 DE-7 01 (DE-627)625046501 VAH 000 Verwitterung {Geologie} 60 01 0705 10 ho 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 213 01 0551 ORD 293 01 3293 ORD 23 01 0830 2011-06-19:22:33:57
allfieldsGer	11,O04 dnb 1010318284 DE-101 urn:nbn:de:gbv:27-20101110-150704-4 urn (DE-627)638874149 (DE-599)GBV638874149 (OCoLC)713545365 DE-627 ger DE-627 rda eng XA-DE 552.5 22/ger 579.61714 OCLC 22/ger 550 570 DNB 43.13 bkl Siegel, Daniela 1980- verfasserin (DE-588)142471941 (DE-627)636294773 (DE-576)330897829 aut Black slate surface alteration due to fungal activity vorgelegt von Daniela Siegel Jena 2010 1 Online-Ressource (141 Seiten) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Friedrich-Schiller-Universität Jena 2010 Black slates of different oxidation states and graphite samples as pure carbon source were incubated with the white-rot fungus Schizophyllum commune 4-39 for 3 months. Investigations by SEM showed fungal affinity to rough surfaces. Oxidatively weathered, bleached black slate samples have more micropores and increased surface roughness than unweathered samples. Unpolished and polished bleached black slate samples were colonized best by fungal hyphae. The hyphae often entered pores. Etch pits induced by fungal activity could be observed which were then quantified by vertical scanning interferometry (VSI). The etch pits measured 3 4 ?m in width and 180 200 nm in depth. In contrast to black slate samples, more etch pits were found on graphite surfaces. Moreover, they showed a more elongated morphology and branches reminiscent of fungal growth morphology. Under laboratory conditions, Schizophyllum commune was able to degrade about 0.03 ?m3/?m2 rock material during 3 months of incubation. It could be shown that collapsed hyphae material remained in their etch pits even after sample preparation which was caused by strong fungal fixation to the rock surfaces. The higher carbon content and the softness of pressed graphite thus allow for earlier fungal attachment and higher dissolution rates. Amounts of nitrogen could be proved by chemical analyzing techniques (x-ray photoelectron spectroscopy and electron microprobe) at all incubated rock samples. Nitrogen increased eminently on rock surfaces due to fungal colonization. Amounts of nitrogen were detected both on hyphae and former hyphae attachment areas. This indicates the presence of fungus and/or fungal excreted proteins such as hydrophobins for attachment or enzymes for degradation. Kurzfassung in dt. Sprache Archivierung/Langzeitarchivierung gewährleistet XA-DE-TH pdager DE-27 Archivierung/Langzeitarchivierung gewährleistet pdager DE-101 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content s (DE-588)4126782-5 (DE-627)105729744 (DE-576)209588020 Schwarzschiefer gnd s (DE-588)4221680-1 (DE-627)105008109 (DE-576)210275073 Spaltblättling gnd s (DE-588)4157161-7 (DE-627)105502979 (DE-576)209832274 Gesteinsoberfläche gnd s (DE-588)4039197-8 (DE-627)104409657 (DE-576)209034041 Mikrobieller Abbau gnd (DE-627) Friedrich-Schiller-Universität Jena Grad-verleihende Institution (DE-588)36164-1 (DE-627)100833012 (DE-576)190344695 dgg Jena (DE-588)4028557-1 (DE-627)104814411 (DE-576)208977872 uvp Erscheint auch als Druck-Ausgabe Siegel, Daniela, 1980 - Black slate Jena, 2010 102, XXV S. (DE-627)635633221 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 Langzeitarchivierung Resolving-System kostenfrei http://d-nb.info/1010318284/34 Langzeitarchivierung Nationalbibliothek Volltext https://www.db-thueringen.de/servlets/DerivateServlet/Derivate-21723/Siegel/Dissertation.pdf Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_31 ISIL_DE-27 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_213 ISIL_DE-551 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 43.13 Umwelttoxikologie (DE-627)106417037 BO 045F 552.5 045F 579.61714 20 01 0084 1231858052 x 10-03-11 21 01 0046 1252579632 z 19-06-11 22 01 0018 1252605951 SUBolrd xu 19-06-11 23 01 0830 125263109X olr-d x 19-06-11 30 01 0104 1252646437 z 19-06-11 31 01 0027 1194484204 z 07-04-09 40 01 0007 1252661037 xsn 19-06-11 60 01 0705 1252687133 OLRD z 20-06-11 63 01 3401 1595702059 ORD x 21-01-16 65 01 0003 416605919X GBV-ODiss Open Access z 14-07-22 70 01 0089 125271615X OA z 29-07-13 105 01 0841 1596515260 z 21-01-16 110 01 3110 1252698267 x 20-06-11 132 01 0959 149760849X OLR-DISS x 11-08-14 151 01 0546 3594118959 OLR-ODISS z 13-02-20 161 01 0960 1597470376 ORD x 28-01-16 213 01 0551 1252740905 ORD x 20-06-11 293 01 3293 1597913030 ORD xf 28-01-16 370 01 4370 1252713916 x 20-06-11 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 31 01 0027 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 LF 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 70 01 0089 http://edok01.tib.uni-hannover.de/edoks/e01dd13/638874149.pdf OA 70 01 0089 Leseprobe http://edok01.tib.uni-hannover.de/edoks/e01dd13/638874149l.pdf OA 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 213 01 0551 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 31 00 DE-27 00 Universitätsbibliographie Jena 31 00 DE-27 01 Chemisch-Geowissenschaftliche Fakultät 40 00 DE-7 00 (DE-627)644784881 VUA 000 Teilfragen {Geobiologie} 40 00 DE-7 01 (DE-627)625046501 VAH 000 Verwitterung {Geologie} 60 01 0705 10 ho 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 213 01 0551 ORD 293 01 3293 ORD 23 01 0830 2011-06-19:22:33:57
allfieldsSound	11,O04 dnb 1010318284 DE-101 urn:nbn:de:gbv:27-20101110-150704-4 urn (DE-627)638874149 (DE-599)GBV638874149 (OCoLC)713545365 DE-627 ger DE-627 rda eng XA-DE 552.5 22/ger 579.61714 OCLC 22/ger 550 570 DNB 43.13 bkl Siegel, Daniela 1980- verfasserin (DE-588)142471941 (DE-627)636294773 (DE-576)330897829 aut Black slate surface alteration due to fungal activity vorgelegt von Daniela Siegel Jena 2010 1 Online-Ressource (141 Seiten) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Friedrich-Schiller-Universität Jena 2010 Black slates of different oxidation states and graphite samples as pure carbon source were incubated with the white-rot fungus Schizophyllum commune 4-39 for 3 months. Investigations by SEM showed fungal affinity to rough surfaces. Oxidatively weathered, bleached black slate samples have more micropores and increased surface roughness than unweathered samples. Unpolished and polished bleached black slate samples were colonized best by fungal hyphae. The hyphae often entered pores. Etch pits induced by fungal activity could be observed which were then quantified by vertical scanning interferometry (VSI). The etch pits measured 3 4 ?m in width and 180 200 nm in depth. In contrast to black slate samples, more etch pits were found on graphite surfaces. Moreover, they showed a more elongated morphology and branches reminiscent of fungal growth morphology. Under laboratory conditions, Schizophyllum commune was able to degrade about 0.03 ?m3/?m2 rock material during 3 months of incubation. It could be shown that collapsed hyphae material remained in their etch pits even after sample preparation which was caused by strong fungal fixation to the rock surfaces. The higher carbon content and the softness of pressed graphite thus allow for earlier fungal attachment and higher dissolution rates. Amounts of nitrogen could be proved by chemical analyzing techniques (x-ray photoelectron spectroscopy and electron microprobe) at all incubated rock samples. Nitrogen increased eminently on rock surfaces due to fungal colonization. Amounts of nitrogen were detected both on hyphae and former hyphae attachment areas. This indicates the presence of fungus and/or fungal excreted proteins such as hydrophobins for attachment or enzymes for degradation. Kurzfassung in dt. Sprache Archivierung/Langzeitarchivierung gewährleistet XA-DE-TH pdager DE-27 Archivierung/Langzeitarchivierung gewährleistet pdager DE-101 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content s (DE-588)4126782-5 (DE-627)105729744 (DE-576)209588020 Schwarzschiefer gnd s (DE-588)4221680-1 (DE-627)105008109 (DE-576)210275073 Spaltblättling gnd s (DE-588)4157161-7 (DE-627)105502979 (DE-576)209832274 Gesteinsoberfläche gnd s (DE-588)4039197-8 (DE-627)104409657 (DE-576)209034041 Mikrobieller Abbau gnd (DE-627) Friedrich-Schiller-Universität Jena Grad-verleihende Institution (DE-588)36164-1 (DE-627)100833012 (DE-576)190344695 dgg Jena (DE-588)4028557-1 (DE-627)104814411 (DE-576)208977872 uvp Erscheint auch als Druck-Ausgabe Siegel, Daniela, 1980 - Black slate Jena, 2010 102, XXV S. 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topic_facet	Schwarzschiefer Spaltblättling Gesteinsoberfläche Mikrobieller Abbau
hochschulschrift_txt_mv	Dissertation Friedrich-Schiller-Universität Jena 2010
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publishDateDaySort_date	2010-01-01T00:00:00Z
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Investigations by SEM showed fungal affinity to rough surfaces. Oxidatively weathered, bleached black slate samples have more micropores and increased surface roughness than unweathered samples. Unpolished and polished bleached black slate samples were colonized best by fungal hyphae. The hyphae often entered pores. Etch pits induced by fungal activity could be observed which were then quantified by vertical scanning interferometry (VSI). The etch pits measured 3 4 ?m in width and 180 200 nm in depth. In contrast to black slate samples, more etch pits were found on graphite surfaces. Moreover, they showed a more elongated morphology and branches reminiscent of fungal growth morphology. Under laboratory conditions, Schizophyllum commune was able to degrade about 0.03 ?m3/?m2 rock material during 3 months of incubation. 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title	Black slate surface alteration due to fungal activity
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title_full	Black slate surface alteration due to fungal activity vorgelegt von Daniela Siegel
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title_sub	surface alteration due to fungal activity
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title_sort	black slatesurface alteration due to fungal activity
title_auth	Black slate surface alteration due to fungal activity
abstract	Black slates of different oxidation states and graphite samples as pure carbon source were incubated with the white-rot fungus Schizophyllum commune 4-39 for 3 months. Investigations by SEM showed fungal affinity to rough surfaces. Oxidatively weathered, bleached black slate samples have more micropores and increased surface roughness than unweathered samples. Unpolished and polished bleached black slate samples were colonized best by fungal hyphae. The hyphae often entered pores. Etch pits induced by fungal activity could be observed which were then quantified by vertical scanning interferometry (VSI). The etch pits measured 3 4 ?m in width and 180 200 nm in depth. In contrast to black slate samples, more etch pits were found on graphite surfaces. Moreover, they showed a more elongated morphology and branches reminiscent of fungal growth morphology. Under laboratory conditions, Schizophyllum commune was able to degrade about 0.03 ?m3/?m2 rock material during 3 months of incubation. It could be shown that collapsed hyphae material remained in their etch pits even after sample preparation which was caused by strong fungal fixation to the rock surfaces. The higher carbon content and the softness of pressed graphite thus allow for earlier fungal attachment and higher dissolution rates. Amounts of nitrogen could be proved by chemical analyzing techniques (x-ray photoelectron spectroscopy and electron microprobe) at all incubated rock samples. Nitrogen increased eminently on rock surfaces due to fungal colonization. Amounts of nitrogen were detected both on hyphae and former hyphae attachment areas. This indicates the presence of fungus and/or fungal excreted proteins such as hydrophobins for attachment or enzymes for degradation.
abstractGer	Black slates of different oxidation states and graphite samples as pure carbon source were incubated with the white-rot fungus Schizophyllum commune 4-39 for 3 months. Investigations by SEM showed fungal affinity to rough surfaces. Oxidatively weathered, bleached black slate samples have more micropores and increased surface roughness than unweathered samples. Unpolished and polished bleached black slate samples were colonized best by fungal hyphae. The hyphae often entered pores. Etch pits induced by fungal activity could be observed which were then quantified by vertical scanning interferometry (VSI). The etch pits measured 3 4 ?m in width and 180 200 nm in depth. In contrast to black slate samples, more etch pits were found on graphite surfaces. Moreover, they showed a more elongated morphology and branches reminiscent of fungal growth morphology. Under laboratory conditions, Schizophyllum commune was able to degrade about 0.03 ?m3/?m2 rock material during 3 months of incubation. It could be shown that collapsed hyphae material remained in their etch pits even after sample preparation which was caused by strong fungal fixation to the rock surfaces. The higher carbon content and the softness of pressed graphite thus allow for earlier fungal attachment and higher dissolution rates. Amounts of nitrogen could be proved by chemical analyzing techniques (x-ray photoelectron spectroscopy and electron microprobe) at all incubated rock samples. Nitrogen increased eminently on rock surfaces due to fungal colonization. Amounts of nitrogen were detected both on hyphae and former hyphae attachment areas. This indicates the presence of fungus and/or fungal excreted proteins such as hydrophobins for attachment or enzymes for degradation.
abstract_unstemmed	Black slates of different oxidation states and graphite samples as pure carbon source were incubated with the white-rot fungus Schizophyllum commune 4-39 for 3 months. Investigations by SEM showed fungal affinity to rough surfaces. Oxidatively weathered, bleached black slate samples have more micropores and increased surface roughness than unweathered samples. Unpolished and polished bleached black slate samples were colonized best by fungal hyphae. The hyphae often entered pores. Etch pits induced by fungal activity could be observed which were then quantified by vertical scanning interferometry (VSI). The etch pits measured 3 4 ?m in width and 180 200 nm in depth. In contrast to black slate samples, more etch pits were found on graphite surfaces. Moreover, they showed a more elongated morphology and branches reminiscent of fungal growth morphology. Under laboratory conditions, Schizophyllum commune was able to degrade about 0.03 ?m3/?m2 rock material during 3 months of incubation. It could be shown that collapsed hyphae material remained in their etch pits even after sample preparation which was caused by strong fungal fixation to the rock surfaces. The higher carbon content and the softness of pressed graphite thus allow for earlier fungal attachment and higher dissolution rates. Amounts of nitrogen could be proved by chemical analyzing techniques (x-ray photoelectron spectroscopy and electron microprobe) at all incubated rock samples. Nitrogen increased eminently on rock surfaces due to fungal colonization. Amounts of nitrogen were detected both on hyphae and former hyphae attachment areas. This indicates the presence of fungus and/or fungal excreted proteins such as hydrophobins for attachment or enzymes for degradation.
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title_short	Black slate
url	http://nbn-resolving.de/urn:nbn:de:gbv:27-20101110-150704-4 http://d-nb.info/1010318284/34 https://www.db-thueringen.de/servlets/DerivateServlet/Derivate-21723/Siegel/Dissertation.pdf
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GND_txt_mv	Siegel, Daniela Hochschulschrift Schwarzschiefer Schizophyllum commune Spaltblättling Gestein / Oberfläche Gesteinsoberfläche Bakterieller Abbau Abbau <Mikrobiologie> Mikrobielle Biodegradation Mikrobieller Abbau Schiller-Universität Jena University (Jena) University of Jena Universitet Imeni Fridricha Šillera (Jena) Schiller University (Jena) Universität Jena Friedrich-Schiller-Universität Jena. Rektor Friedrich Schiller University (Jena) Gosudarstvennyj Universitet Imeni Fridricha Šillera (Jena) Universidad Friedrich Schiller FSU Jena Universitas Litterarum Jenensis Jenskij Gosudarstvennyj Universitet Imeni Fridricha Šillera Universitas Litterarum Ienensis Alma Mater Jenensis Friedrich-Schiller-Universität Jena Jhena Ihena Stadt Jena City of Jena Iena Iéna Jena (Lichtstadt) Jehna Giena Gena Jena
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up_date	2024-07-20T07:07:27.205Z
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