Impact of land use covers upon karst processes in a typical Fengcong depression system of Nongla, Guangxi, China

Abstract The direction and intensity of karst processes can be deeply affected by soil physical and chemical variations which were resulted from land use. Taking Nongla Fengcong depression area, Mashan County, Guangxi as an example, authors discussed the impact of land use on karst processes based o...
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Autor*in:	Zhang, Cheng [verfasserIn] Pei, Jianguo Xie, Yunqiu Cao, Jianhua Wang, Lanling

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2007

Schlagwörter:	Land use Karst processes Corrosional rate Nongla Guangxi China

Anmerkung:	© Springer-Verlag 2007

Übergeordnetes Werk:	Enthalten in: Environmental geology - Berlin : Springer, 1975, 55(2007), 8 vom: 14. Nov.
Übergeordnetes Werk:	volume:55 ; year:2007 ; number:8 ; day:14 ; month:11

Links:	Volltext

DOI / URN:	10.1007/s00254-007-1111-1

Katalog-ID:	SPR003060896

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allfields	10.1007/s00254-007-1111-1 doi (DE-627)SPR003060896 (SPR)s00254-007-1111-1-e DE-627 ger DE-627 rakwb eng Zhang, Cheng verfasserin aut Impact of land use covers upon karst processes in a typical Fengcong depression system of Nongla, Guangxi, China 2007 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2007 Abstract The direction and intensity of karst processes can be deeply affected by soil physical and chemical variations which were resulted from land use. Taking Nongla Fengcong depression area, Mashan County, Guangxi as an example, authors discussed the impact of land use on karst processes based on the data of field limestone tablet. The results showed that the corrosional rates at varied soil depth are quite different. Corrosional rate in woodland and orchard is mostly bigger than 20 mg/a, which is much higher than that in tilled land and shrub. Generally, corrosional rate decreased from orchard, woodland, tilled land, fallow land and shrub successively, in which soil organic matter (OM) and soil pH are two major controlling factors: corrosion process is controlled remarkably by soil OM in woodland and orchard. The higher the organic matter content is and the less the pH value is, the higher the corrosional rate is. Owing to lower organic matter content, the corrosional rate is mainly affected by soil $ CO_{2} $ in tilled land and shrub. Land use (dpeaa)DE-He213 Karst processes (dpeaa)DE-He213 Corrosional rate (dpeaa)DE-He213 Nongla Guangxi China (dpeaa)DE-He213 Pei, Jianguo aut Xie, Yunqiu aut Cao, Jianhua aut Wang, Lanling aut Enthalten in Environmental geology Berlin : Springer, 1975 55(2007), 8 vom: 14. Nov. (DE-627)253722586 (DE-600)1459034-7 1432-0495 nnns volume:55 year:2007 number:8 day:14 month:11 https://dx.doi.org/10.1007/s00254-007-1111-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 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_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4338 AR 55 2007 8 14 11
spelling	10.1007/s00254-007-1111-1 doi (DE-627)SPR003060896 (SPR)s00254-007-1111-1-e DE-627 ger DE-627 rakwb eng Zhang, Cheng verfasserin aut Impact of land use covers upon karst processes in a typical Fengcong depression system of Nongla, Guangxi, China 2007 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2007 Abstract The direction and intensity of karst processes can be deeply affected by soil physical and chemical variations which were resulted from land use. Taking Nongla Fengcong depression area, Mashan County, Guangxi as an example, authors discussed the impact of land use on karst processes based on the data of field limestone tablet. The results showed that the corrosional rates at varied soil depth are quite different. Corrosional rate in woodland and orchard is mostly bigger than 20 mg/a, which is much higher than that in tilled land and shrub. Generally, corrosional rate decreased from orchard, woodland, tilled land, fallow land and shrub successively, in which soil organic matter (OM) and soil pH are two major controlling factors: corrosion process is controlled remarkably by soil OM in woodland and orchard. The higher the organic matter content is and the less the pH value is, the higher the corrosional rate is. Owing to lower organic matter content, the corrosional rate is mainly affected by soil $ CO_{2} $ in tilled land and shrub. Land use (dpeaa)DE-He213 Karst processes (dpeaa)DE-He213 Corrosional rate (dpeaa)DE-He213 Nongla Guangxi China (dpeaa)DE-He213 Pei, Jianguo aut Xie, Yunqiu aut Cao, Jianhua aut Wang, Lanling aut Enthalten in Environmental geology Berlin : Springer, 1975 55(2007), 8 vom: 14. Nov. (DE-627)253722586 (DE-600)1459034-7 1432-0495 nnns volume:55 year:2007 number:8 day:14 month:11 https://dx.doi.org/10.1007/s00254-007-1111-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 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_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4338 AR 55 2007 8 14 11
allfields_unstemmed	10.1007/s00254-007-1111-1 doi (DE-627)SPR003060896 (SPR)s00254-007-1111-1-e DE-627 ger DE-627 rakwb eng Zhang, Cheng verfasserin aut Impact of land use covers upon karst processes in a typical Fengcong depression system of Nongla, Guangxi, China 2007 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2007 Abstract The direction and intensity of karst processes can be deeply affected by soil physical and chemical variations which were resulted from land use. Taking Nongla Fengcong depression area, Mashan County, Guangxi as an example, authors discussed the impact of land use on karst processes based on the data of field limestone tablet. The results showed that the corrosional rates at varied soil depth are quite different. Corrosional rate in woodland and orchard is mostly bigger than 20 mg/a, which is much higher than that in tilled land and shrub. Generally, corrosional rate decreased from orchard, woodland, tilled land, fallow land and shrub successively, in which soil organic matter (OM) and soil pH are two major controlling factors: corrosion process is controlled remarkably by soil OM in woodland and orchard. The higher the organic matter content is and the less the pH value is, the higher the corrosional rate is. Owing to lower organic matter content, the corrosional rate is mainly affected by soil $ CO_{2} $ in tilled land and shrub. Land use (dpeaa)DE-He213 Karst processes (dpeaa)DE-He213 Corrosional rate (dpeaa)DE-He213 Nongla Guangxi China (dpeaa)DE-He213 Pei, Jianguo aut Xie, Yunqiu aut Cao, Jianhua aut Wang, Lanling aut Enthalten in Environmental geology Berlin : Springer, 1975 55(2007), 8 vom: 14. Nov. (DE-627)253722586 (DE-600)1459034-7 1432-0495 nnns volume:55 year:2007 number:8 day:14 month:11 https://dx.doi.org/10.1007/s00254-007-1111-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 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_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4338 AR 55 2007 8 14 11
allfieldsGer	10.1007/s00254-007-1111-1 doi (DE-627)SPR003060896 (SPR)s00254-007-1111-1-e DE-627 ger DE-627 rakwb eng Zhang, Cheng verfasserin aut Impact of land use covers upon karst processes in a typical Fengcong depression system of Nongla, Guangxi, China 2007 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2007 Abstract The direction and intensity of karst processes can be deeply affected by soil physical and chemical variations which were resulted from land use. Taking Nongla Fengcong depression area, Mashan County, Guangxi as an example, authors discussed the impact of land use on karst processes based on the data of field limestone tablet. The results showed that the corrosional rates at varied soil depth are quite different. Corrosional rate in woodland and orchard is mostly bigger than 20 mg/a, which is much higher than that in tilled land and shrub. Generally, corrosional rate decreased from orchard, woodland, tilled land, fallow land and shrub successively, in which soil organic matter (OM) and soil pH are two major controlling factors: corrosion process is controlled remarkably by soil OM in woodland and orchard. The higher the organic matter content is and the less the pH value is, the higher the corrosional rate is. Owing to lower organic matter content, the corrosional rate is mainly affected by soil $ CO_{2} $ in tilled land and shrub. Land use (dpeaa)DE-He213 Karst processes (dpeaa)DE-He213 Corrosional rate (dpeaa)DE-He213 Nongla Guangxi China (dpeaa)DE-He213 Pei, Jianguo aut Xie, Yunqiu aut Cao, Jianhua aut Wang, Lanling aut Enthalten in Environmental geology Berlin : Springer, 1975 55(2007), 8 vom: 14. Nov. (DE-627)253722586 (DE-600)1459034-7 1432-0495 nnns volume:55 year:2007 number:8 day:14 month:11 https://dx.doi.org/10.1007/s00254-007-1111-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 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_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4338 AR 55 2007 8 14 11
allfieldsSound	10.1007/s00254-007-1111-1 doi (DE-627)SPR003060896 (SPR)s00254-007-1111-1-e DE-627 ger DE-627 rakwb eng Zhang, Cheng verfasserin aut Impact of land use covers upon karst processes in a typical Fengcong depression system of Nongla, Guangxi, China 2007 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag 2007 Abstract The direction and intensity of karst processes can be deeply affected by soil physical and chemical variations which were resulted from land use. Taking Nongla Fengcong depression area, Mashan County, Guangxi as an example, authors discussed the impact of land use on karst processes based on the data of field limestone tablet. The results showed that the corrosional rates at varied soil depth are quite different. Corrosional rate in woodland and orchard is mostly bigger than 20 mg/a, which is much higher than that in tilled land and shrub. Generally, corrosional rate decreased from orchard, woodland, tilled land, fallow land and shrub successively, in which soil organic matter (OM) and soil pH are two major controlling factors: corrosion process is controlled remarkably by soil OM in woodland and orchard. The higher the organic matter content is and the less the pH value is, the higher the corrosional rate is. Owing to lower organic matter content, the corrosional rate is mainly affected by soil $ CO_{2} $ in tilled land and shrub. Land use (dpeaa)DE-He213 Karst processes (dpeaa)DE-He213 Corrosional rate (dpeaa)DE-He213 Nongla Guangxi China (dpeaa)DE-He213 Pei, Jianguo aut Xie, Yunqiu aut Cao, Jianhua aut Wang, Lanling aut Enthalten in Environmental geology Berlin : Springer, 1975 55(2007), 8 vom: 14. Nov. (DE-627)253722586 (DE-600)1459034-7 1432-0495 nnns volume:55 year:2007 number:8 day:14 month:11 https://dx.doi.org/10.1007/s00254-007-1111-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_24 GBV_ILN_31 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 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_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4338 AR 55 2007 8 14 11
language	English
source	Enthalten in Environmental geology 55(2007), 8 vom: 14. Nov. volume:55 year:2007 number:8 day:14 month:11
sourceStr	Enthalten in Environmental geology 55(2007), 8 vom: 14. Nov. volume:55 year:2007 number:8 day:14 month:11
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Land use Karst processes Corrosional rate Nongla Guangxi China
isfreeaccess_bool	false
container_title	Environmental geology
authorswithroles_txt_mv	Zhang, Cheng @@aut@@ Pei, Jianguo @@aut@@ Xie, Yunqiu @@aut@@ Cao, Jianhua @@aut@@ Wang, Lanling @@aut@@
publishDateDaySort_date	2007-11-14T00:00:00Z
hierarchy_top_id	253722586
id	SPR003060896
language_de	englisch
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author	Zhang, Cheng
spellingShingle	Zhang, Cheng misc Land use misc Karst processes misc Corrosional rate misc Nongla Guangxi China Impact of land use covers upon karst processes in a typical Fengcong depression system of Nongla, Guangxi, China
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topic_title	Impact of land use covers upon karst processes in a typical Fengcong depression system of Nongla, Guangxi, China Land use (dpeaa)DE-He213 Karst processes (dpeaa)DE-He213 Corrosional rate (dpeaa)DE-He213 Nongla Guangxi China (dpeaa)DE-He213
topic	misc Land use misc Karst processes misc Corrosional rate misc Nongla Guangxi China
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title	Impact of land use covers upon karst processes in a typical Fengcong depression system of Nongla, Guangxi, China
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title_full	Impact of land use covers upon karst processes in a typical Fengcong depression system of Nongla, Guangxi, China
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title_sort	impact of land use covers upon karst processes in a typical fengcong depression system of nongla, guangxi, china
title_auth	Impact of land use covers upon karst processes in a typical Fengcong depression system of Nongla, Guangxi, China
abstract	Abstract The direction and intensity of karst processes can be deeply affected by soil physical and chemical variations which were resulted from land use. Taking Nongla Fengcong depression area, Mashan County, Guangxi as an example, authors discussed the impact of land use on karst processes based on the data of field limestone tablet. The results showed that the corrosional rates at varied soil depth are quite different. Corrosional rate in woodland and orchard is mostly bigger than 20 mg/a, which is much higher than that in tilled land and shrub. Generally, corrosional rate decreased from orchard, woodland, tilled land, fallow land and shrub successively, in which soil organic matter (OM) and soil pH are two major controlling factors: corrosion process is controlled remarkably by soil OM in woodland and orchard. The higher the organic matter content is and the less the pH value is, the higher the corrosional rate is. Owing to lower organic matter content, the corrosional rate is mainly affected by soil $ CO_{2} $ in tilled land and shrub. © Springer-Verlag 2007
abstractGer	Abstract The direction and intensity of karst processes can be deeply affected by soil physical and chemical variations which were resulted from land use. Taking Nongla Fengcong depression area, Mashan County, Guangxi as an example, authors discussed the impact of land use on karst processes based on the data of field limestone tablet. The results showed that the corrosional rates at varied soil depth are quite different. Corrosional rate in woodland and orchard is mostly bigger than 20 mg/a, which is much higher than that in tilled land and shrub. Generally, corrosional rate decreased from orchard, woodland, tilled land, fallow land and shrub successively, in which soil organic matter (OM) and soil pH are two major controlling factors: corrosion process is controlled remarkably by soil OM in woodland and orchard. The higher the organic matter content is and the less the pH value is, the higher the corrosional rate is. Owing to lower organic matter content, the corrosional rate is mainly affected by soil $ CO_{2} $ in tilled land and shrub. © Springer-Verlag 2007
abstract_unstemmed	Abstract The direction and intensity of karst processes can be deeply affected by soil physical and chemical variations which were resulted from land use. Taking Nongla Fengcong depression area, Mashan County, Guangxi as an example, authors discussed the impact of land use on karst processes based on the data of field limestone tablet. The results showed that the corrosional rates at varied soil depth are quite different. Corrosional rate in woodland and orchard is mostly bigger than 20 mg/a, which is much higher than that in tilled land and shrub. Generally, corrosional rate decreased from orchard, woodland, tilled land, fallow land and shrub successively, in which soil organic matter (OM) and soil pH are two major controlling factors: corrosion process is controlled remarkably by soil OM in woodland and orchard. The higher the organic matter content is and the less the pH value is, the higher the corrosional rate is. Owing to lower organic matter content, the corrosional rate is mainly affected by soil $ CO_{2} $ in tilled land and shrub. © Springer-Verlag 2007
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title_short	Impact of land use covers upon karst processes in a typical Fengcong depression system of Nongla, Guangxi, China
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Impact of land use covers upon karst processes in a typical Fengcong depression system of Nongla, Guangxi, China

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