Comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay
Summary The aim of this work is to find a possible correlation between the weathering indices obtained from samples of one type of sedimentary rock, a greywacke, altered to various degrees and those obtained after laboratory aging tests on the same rocks. In a first part the process of natural alter...
Ausführliche Beschreibung
Autor*in: |
Aires-Barros, L. [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
1978 |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: Bulletin of engineering geology and the environment - Berlin : Springer, 1970, 18(1978), 1 vom: 01. Dez., Seite 169-174 |
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Übergeordnetes Werk: |
volume:18 ; year:1978 ; number:1 ; day:01 ; month:12 ; pages:169-174 |
Links: |
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DOI / URN: |
10.1007/BF02635366 |
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Katalog-ID: |
SPR008452725 |
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245 | 1 | 0 | |a Comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay |
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520 | |a Summary The aim of this work is to find a possible correlation between the weathering indices obtained from samples of one type of sedimentary rock, a greywacke, altered to various degrees and those obtained after laboratory aging tests on the same rocks. In a first part the process of natural alteration is studied taking samples of three different alteration stages. These samples were collected in a vertical borehole and the natural weathering process was followed by geochemical and petrological observations. Geochemical calculations were made, in order to obtain the amount of gain and loss of chemical elements. The quantification of the weathering through the application of weathering indices and finally an attempt was made to apply an alterability index to these rocks. Samples of the same rocks were submitted to laboratory thermal fatigue tests (Aires-Barros et al. 1975), in order to follow the alteration by laboratory aging and to obtain weatherability indices. Physical values of sonic velocity, porosity, permeability and swelling were also determined. The presentation of the corresponding results forms the second part of this paper. In the third part, the values obtained in the two preceding parts are compared in order to test the laboratory work and to determine the correlation between the “one laboratory year test” and natural weathering. | ||
650 | 4 | |a Silicate Rock |7 (dpeaa)DE-He213 | |
650 | 4 | |a Thermal Fatigue |7 (dpeaa)DE-He213 | |
650 | 4 | |a Altered Rock |7 (dpeaa)DE-He213 | |
650 | 4 | |a Natural Weathering |7 (dpeaa)DE-He213 | |
650 | 4 | |a Weatherability Index |7 (dpeaa)DE-He213 | |
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1978 |
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38.58 56.00 56.20 |
publishDate |
1978 |
allfields |
10.1007/BF02635366 doi (DE-627)SPR008452725 (SPR)BF02635366-e DE-627 ger DE-627 rakwb eng 550 600 ASE 38.58 bkl 56.00 bkl 56.20 bkl Aires-Barros, L. verfasserin aut Comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay 1978 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary The aim of this work is to find a possible correlation between the weathering indices obtained from samples of one type of sedimentary rock, a greywacke, altered to various degrees and those obtained after laboratory aging tests on the same rocks. In a first part the process of natural alteration is studied taking samples of three different alteration stages. These samples were collected in a vertical borehole and the natural weathering process was followed by geochemical and petrological observations. Geochemical calculations were made, in order to obtain the amount of gain and loss of chemical elements. The quantification of the weathering through the application of weathering indices and finally an attempt was made to apply an alterability index to these rocks. Samples of the same rocks were submitted to laboratory thermal fatigue tests (Aires-Barros et al. 1975), in order to follow the alteration by laboratory aging and to obtain weatherability indices. Physical values of sonic velocity, porosity, permeability and swelling were also determined. The presentation of the corresponding results forms the second part of this paper. In the third part, the values obtained in the two preceding parts are compared in order to test the laboratory work and to determine the correlation between the “one laboratory year test” and natural weathering. Silicate Rock (dpeaa)DE-He213 Thermal Fatigue (dpeaa)DE-He213 Altered Rock (dpeaa)DE-He213 Natural Weathering (dpeaa)DE-He213 Weatherability Index (dpeaa)DE-He213 Enthalten in Bulletin of engineering geology and the environment Berlin : Springer, 1970 18(1978), 1 vom: 01. Dez., Seite 169-174 (DE-627)271597011 (DE-600)1480689-7 1435-9537 nnns volume:18 year:1978 number:1 day:01 month:12 pages:169-174 https://dx.doi.org/10.1007/BF02635366 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 38.58 ASE 56.00 ASE 56.20 ASE AR 18 1978 1 01 12 169-174 |
spelling |
10.1007/BF02635366 doi (DE-627)SPR008452725 (SPR)BF02635366-e DE-627 ger DE-627 rakwb eng 550 600 ASE 38.58 bkl 56.00 bkl 56.20 bkl Aires-Barros, L. verfasserin aut Comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay 1978 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary The aim of this work is to find a possible correlation between the weathering indices obtained from samples of one type of sedimentary rock, a greywacke, altered to various degrees and those obtained after laboratory aging tests on the same rocks. In a first part the process of natural alteration is studied taking samples of three different alteration stages. These samples were collected in a vertical borehole and the natural weathering process was followed by geochemical and petrological observations. Geochemical calculations were made, in order to obtain the amount of gain and loss of chemical elements. The quantification of the weathering through the application of weathering indices and finally an attempt was made to apply an alterability index to these rocks. Samples of the same rocks were submitted to laboratory thermal fatigue tests (Aires-Barros et al. 1975), in order to follow the alteration by laboratory aging and to obtain weatherability indices. Physical values of sonic velocity, porosity, permeability and swelling were also determined. The presentation of the corresponding results forms the second part of this paper. In the third part, the values obtained in the two preceding parts are compared in order to test the laboratory work and to determine the correlation between the “one laboratory year test” and natural weathering. Silicate Rock (dpeaa)DE-He213 Thermal Fatigue (dpeaa)DE-He213 Altered Rock (dpeaa)DE-He213 Natural Weathering (dpeaa)DE-He213 Weatherability Index (dpeaa)DE-He213 Enthalten in Bulletin of engineering geology and the environment Berlin : Springer, 1970 18(1978), 1 vom: 01. Dez., Seite 169-174 (DE-627)271597011 (DE-600)1480689-7 1435-9537 nnns volume:18 year:1978 number:1 day:01 month:12 pages:169-174 https://dx.doi.org/10.1007/BF02635366 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 38.58 ASE 56.00 ASE 56.20 ASE AR 18 1978 1 01 12 169-174 |
allfields_unstemmed |
10.1007/BF02635366 doi (DE-627)SPR008452725 (SPR)BF02635366-e DE-627 ger DE-627 rakwb eng 550 600 ASE 38.58 bkl 56.00 bkl 56.20 bkl Aires-Barros, L. verfasserin aut Comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay 1978 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary The aim of this work is to find a possible correlation between the weathering indices obtained from samples of one type of sedimentary rock, a greywacke, altered to various degrees and those obtained after laboratory aging tests on the same rocks. In a first part the process of natural alteration is studied taking samples of three different alteration stages. These samples were collected in a vertical borehole and the natural weathering process was followed by geochemical and petrological observations. Geochemical calculations were made, in order to obtain the amount of gain and loss of chemical elements. The quantification of the weathering through the application of weathering indices and finally an attempt was made to apply an alterability index to these rocks. Samples of the same rocks were submitted to laboratory thermal fatigue tests (Aires-Barros et al. 1975), in order to follow the alteration by laboratory aging and to obtain weatherability indices. Physical values of sonic velocity, porosity, permeability and swelling were also determined. The presentation of the corresponding results forms the second part of this paper. In the third part, the values obtained in the two preceding parts are compared in order to test the laboratory work and to determine the correlation between the “one laboratory year test” and natural weathering. Silicate Rock (dpeaa)DE-He213 Thermal Fatigue (dpeaa)DE-He213 Altered Rock (dpeaa)DE-He213 Natural Weathering (dpeaa)DE-He213 Weatherability Index (dpeaa)DE-He213 Enthalten in Bulletin of engineering geology and the environment Berlin : Springer, 1970 18(1978), 1 vom: 01. Dez., Seite 169-174 (DE-627)271597011 (DE-600)1480689-7 1435-9537 nnns volume:18 year:1978 number:1 day:01 month:12 pages:169-174 https://dx.doi.org/10.1007/BF02635366 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 38.58 ASE 56.00 ASE 56.20 ASE AR 18 1978 1 01 12 169-174 |
allfieldsGer |
10.1007/BF02635366 doi (DE-627)SPR008452725 (SPR)BF02635366-e DE-627 ger DE-627 rakwb eng 550 600 ASE 38.58 bkl 56.00 bkl 56.20 bkl Aires-Barros, L. verfasserin aut Comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay 1978 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary The aim of this work is to find a possible correlation between the weathering indices obtained from samples of one type of sedimentary rock, a greywacke, altered to various degrees and those obtained after laboratory aging tests on the same rocks. In a first part the process of natural alteration is studied taking samples of three different alteration stages. These samples were collected in a vertical borehole and the natural weathering process was followed by geochemical and petrological observations. Geochemical calculations were made, in order to obtain the amount of gain and loss of chemical elements. The quantification of the weathering through the application of weathering indices and finally an attempt was made to apply an alterability index to these rocks. Samples of the same rocks were submitted to laboratory thermal fatigue tests (Aires-Barros et al. 1975), in order to follow the alteration by laboratory aging and to obtain weatherability indices. Physical values of sonic velocity, porosity, permeability and swelling were also determined. The presentation of the corresponding results forms the second part of this paper. In the third part, the values obtained in the two preceding parts are compared in order to test the laboratory work and to determine the correlation between the “one laboratory year test” and natural weathering. Silicate Rock (dpeaa)DE-He213 Thermal Fatigue (dpeaa)DE-He213 Altered Rock (dpeaa)DE-He213 Natural Weathering (dpeaa)DE-He213 Weatherability Index (dpeaa)DE-He213 Enthalten in Bulletin of engineering geology and the environment Berlin : Springer, 1970 18(1978), 1 vom: 01. Dez., Seite 169-174 (DE-627)271597011 (DE-600)1480689-7 1435-9537 nnns volume:18 year:1978 number:1 day:01 month:12 pages:169-174 https://dx.doi.org/10.1007/BF02635366 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 38.58 ASE 56.00 ASE 56.20 ASE AR 18 1978 1 01 12 169-174 |
allfieldsSound |
10.1007/BF02635366 doi (DE-627)SPR008452725 (SPR)BF02635366-e DE-627 ger DE-627 rakwb eng 550 600 ASE 38.58 bkl 56.00 bkl 56.20 bkl Aires-Barros, L. verfasserin aut Comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay 1978 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary The aim of this work is to find a possible correlation between the weathering indices obtained from samples of one type of sedimentary rock, a greywacke, altered to various degrees and those obtained after laboratory aging tests on the same rocks. In a first part the process of natural alteration is studied taking samples of three different alteration stages. These samples were collected in a vertical borehole and the natural weathering process was followed by geochemical and petrological observations. Geochemical calculations were made, in order to obtain the amount of gain and loss of chemical elements. The quantification of the weathering through the application of weathering indices and finally an attempt was made to apply an alterability index to these rocks. Samples of the same rocks were submitted to laboratory thermal fatigue tests (Aires-Barros et al. 1975), in order to follow the alteration by laboratory aging and to obtain weatherability indices. Physical values of sonic velocity, porosity, permeability and swelling were also determined. The presentation of the corresponding results forms the second part of this paper. In the third part, the values obtained in the two preceding parts are compared in order to test the laboratory work and to determine the correlation between the “one laboratory year test” and natural weathering. Silicate Rock (dpeaa)DE-He213 Thermal Fatigue (dpeaa)DE-He213 Altered Rock (dpeaa)DE-He213 Natural Weathering (dpeaa)DE-He213 Weatherability Index (dpeaa)DE-He213 Enthalten in Bulletin of engineering geology and the environment Berlin : Springer, 1970 18(1978), 1 vom: 01. Dez., Seite 169-174 (DE-627)271597011 (DE-600)1480689-7 1435-9537 nnns volume:18 year:1978 number:1 day:01 month:12 pages:169-174 https://dx.doi.org/10.1007/BF02635366 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 38.58 ASE 56.00 ASE 56.20 ASE AR 18 1978 1 01 12 169-174 |
language |
English |
source |
Enthalten in Bulletin of engineering geology and the environment 18(1978), 1 vom: 01. Dez., Seite 169-174 volume:18 year:1978 number:1 day:01 month:12 pages:169-174 |
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Enthalten in Bulletin of engineering geology and the environment 18(1978), 1 vom: 01. Dez., Seite 169-174 volume:18 year:1978 number:1 day:01 month:12 pages:169-174 |
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Silicate Rock Thermal Fatigue Altered Rock Natural Weathering Weatherability Index |
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Aires-Barros, L. @@aut@@ |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR008452725</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220110203331.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201005s1978 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF02635366</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR008452725</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)BF02635366-e</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="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="a">600</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.58</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">56.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">56.20</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Aires-Barros, L.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1978</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="520" ind1=" " ind2=" "><subfield code="a">Summary The aim of this work is to find a possible correlation between the weathering indices obtained from samples of one type of sedimentary rock, a greywacke, altered to various degrees and those obtained after laboratory aging tests on the same rocks. In a first part the process of natural alteration is studied taking samples of three different alteration stages. These samples were collected in a vertical borehole and the natural weathering process was followed by geochemical and petrological observations. Geochemical calculations were made, in order to obtain the amount of gain and loss of chemical elements. The quantification of the weathering through the application of weathering indices and finally an attempt was made to apply an alterability index to these rocks. Samples of the same rocks were submitted to laboratory thermal fatigue tests (Aires-Barros et al. 1975), in order to follow the alteration by laboratory aging and to obtain weatherability indices. Physical values of sonic velocity, porosity, permeability and swelling were also determined. The presentation of the corresponding results forms the second part of this paper. 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Aires-Barros, L. |
spellingShingle |
Aires-Barros, L. ddc 550 bkl 38.58 bkl 56.00 bkl 56.20 misc Silicate Rock misc Thermal Fatigue misc Altered Rock misc Natural Weathering misc Weatherability Index Comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay |
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550 600 ASE 38.58 bkl 56.00 bkl 56.20 bkl Comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay Silicate Rock (dpeaa)DE-He213 Thermal Fatigue (dpeaa)DE-He213 Altered Rock (dpeaa)DE-He213 Natural Weathering (dpeaa)DE-He213 Weatherability Index (dpeaa)DE-He213 |
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ddc 550 bkl 38.58 bkl 56.00 bkl 56.20 misc Silicate Rock misc Thermal Fatigue misc Altered Rock misc Natural Weathering misc Weatherability Index |
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Comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay |
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comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay |
title_auth |
Comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay |
abstract |
Summary The aim of this work is to find a possible correlation between the weathering indices obtained from samples of one type of sedimentary rock, a greywacke, altered to various degrees and those obtained after laboratory aging tests on the same rocks. In a first part the process of natural alteration is studied taking samples of three different alteration stages. These samples were collected in a vertical borehole and the natural weathering process was followed by geochemical and petrological observations. Geochemical calculations were made, in order to obtain the amount of gain and loss of chemical elements. The quantification of the weathering through the application of weathering indices and finally an attempt was made to apply an alterability index to these rocks. Samples of the same rocks were submitted to laboratory thermal fatigue tests (Aires-Barros et al. 1975), in order to follow the alteration by laboratory aging and to obtain weatherability indices. Physical values of sonic velocity, porosity, permeability and swelling were also determined. The presentation of the corresponding results forms the second part of this paper. In the third part, the values obtained in the two preceding parts are compared in order to test the laboratory work and to determine the correlation between the “one laboratory year test” and natural weathering. |
abstractGer |
Summary The aim of this work is to find a possible correlation between the weathering indices obtained from samples of one type of sedimentary rock, a greywacke, altered to various degrees and those obtained after laboratory aging tests on the same rocks. In a first part the process of natural alteration is studied taking samples of three different alteration stages. These samples were collected in a vertical borehole and the natural weathering process was followed by geochemical and petrological observations. Geochemical calculations were made, in order to obtain the amount of gain and loss of chemical elements. The quantification of the weathering through the application of weathering indices and finally an attempt was made to apply an alterability index to these rocks. Samples of the same rocks were submitted to laboratory thermal fatigue tests (Aires-Barros et al. 1975), in order to follow the alteration by laboratory aging and to obtain weatherability indices. Physical values of sonic velocity, porosity, permeability and swelling were also determined. The presentation of the corresponding results forms the second part of this paper. In the third part, the values obtained in the two preceding parts are compared in order to test the laboratory work and to determine the correlation between the “one laboratory year test” and natural weathering. |
abstract_unstemmed |
Summary The aim of this work is to find a possible correlation between the weathering indices obtained from samples of one type of sedimentary rock, a greywacke, altered to various degrees and those obtained after laboratory aging tests on the same rocks. In a first part the process of natural alteration is studied taking samples of three different alteration stages. These samples were collected in a vertical borehole and the natural weathering process was followed by geochemical and petrological observations. Geochemical calculations were made, in order to obtain the amount of gain and loss of chemical elements. The quantification of the weathering through the application of weathering indices and finally an attempt was made to apply an alterability index to these rocks. Samples of the same rocks were submitted to laboratory thermal fatigue tests (Aires-Barros et al. 1975), in order to follow the alteration by laboratory aging and to obtain weatherability indices. Physical values of sonic velocity, porosity, permeability and swelling were also determined. The presentation of the corresponding results forms the second part of this paper. In the third part, the values obtained in the two preceding parts are compared in order to test the laboratory work and to determine the correlation between the “one laboratory year test” and natural weathering. |
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Comparative study between rates of experimental laboratory weathering of rocks and their natural environmental weathering decay |
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score |
7.4011784 |