Hillslope soil moisture temporal stability under two contrasting land use types during different time periods

Abstract Knowledge of soil moisture temporal stability and its controlling factors is important for hydrological and environmental management decisions. This study analyzed the influences of soil and terrain on soil moisture temporal stability (relative difference of soil moisture—δ and standard dev...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Lv, Ligang [verfasserIn] Liao, Kaihua Lai, Xiaoming Zhu, Qing Zhou, Shenglu

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2016

Schlagwörter:	Hydropedology Soil water content Temporal stability Land use

Anmerkung:	© Springer-Verlag Berlin Heidelberg 2016

Übergeordnetes Werk:	Enthalten in: Environmental earth sciences - Berlin : Springer, 2009, 75(2016), 7 vom: 26. März
Übergeordnetes Werk:	volume:75 ; year:2016 ; number:7 ; day:26 ; month:03

Links:	Volltext

DOI / URN:	10.1007/s12665-015-5238-1

Katalog-ID:	SPR026728850

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245	1	0	\|a Hillslope soil moisture temporal stability under two contrasting land use types during different time periods
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520			\|a Abstract Knowledge of soil moisture temporal stability and its controlling factors is important for hydrological and environmental management decisions. This study analyzed the influences of soil and terrain on soil moisture temporal stability (relative difference of soil moisture—δ and standard deviation of δ − Sδ) on two contrasting land use hillslopes [tea garden (TG) and bamboo forest (BF)] in the hilly area of Taihu Lake Basin, China. Soil moisture temporal stabilities were considered at two depths (0.1 and 0.3 m) and during eight different periods (entire, dry, wet, rain, spring, summer, fall and winter periods). Results showed that for each land use and soil depth, values of δ in summer were largely deviated from those during the entire period, while values of Sδ after rain storms were strongly deviated from those during the entire period. Correlation coefficients between soil/terrain and δ were generally greater on the BF hillslope (ranged from 0.35 to 0.70) than on the TG hillslope (ranged from 0.30 to 0.55). This suggested that soil moisture distribution was more spatially organized on the BF hillslope than on the TG hillslope. This can be attributed to that the management practices disturbed and mixed the soils on the TG hillslope, which made the soil moisture more randomly distributed. The controls on Sδ substantially varied with season, soil depth and land use. On the TG hillslope, soil/terrain had weak correlations with Sδ, while on the BF hillslope, rock fragment, slope and elevation had decent correlation with Sδ. This varied controlling factors of Sδ on different hillslopes, period and soil depth suggested that spatial distributions of Sδ were influenced by the occurrence of subsurface preferential flow. Findings of this study suggested that soil moisture temporal stability and its controlling factors were land use type and time period dependent.
650		4	\|a Hydropedology \|7 (dpeaa)DE-He213
650		4	\|a Soil water content \|7 (dpeaa)DE-He213
650		4	\|a Temporal stability \|7 (dpeaa)DE-He213
650		4	\|a Land use \|7 (dpeaa)DE-He213
700	1		\|a Liao, Kaihua \|4 aut
700	1		\|a Lai, Xiaoming \|4 aut
700	1		\|a Zhu, Qing \|4 aut
700	1		\|a Zhou, Shenglu \|4 aut
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allfields	10.1007/s12665-015-5238-1 doi (DE-627)SPR026728850 (SPR)s12665-015-5238-1-e DE-627 ger DE-627 rakwb eng Lv, Ligang verfasserin aut Hillslope soil moisture temporal stability under two contrasting land use types during different time periods 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract Knowledge of soil moisture temporal stability and its controlling factors is important for hydrological and environmental management decisions. This study analyzed the influences of soil and terrain on soil moisture temporal stability (relative difference of soil moisture—δ and standard deviation of δ − Sδ) on two contrasting land use hillslopes [tea garden (TG) and bamboo forest (BF)] in the hilly area of Taihu Lake Basin, China. Soil moisture temporal stabilities were considered at two depths (0.1 and 0.3 m) and during eight different periods (entire, dry, wet, rain, spring, summer, fall and winter periods). Results showed that for each land use and soil depth, values of δ in summer were largely deviated from those during the entire period, while values of Sδ after rain storms were strongly deviated from those during the entire period. Correlation coefficients between soil/terrain and δ were generally greater on the BF hillslope (ranged from 0.35 to 0.70) than on the TG hillslope (ranged from 0.30 to 0.55). This suggested that soil moisture distribution was more spatially organized on the BF hillslope than on the TG hillslope. This can be attributed to that the management practices disturbed and mixed the soils on the TG hillslope, which made the soil moisture more randomly distributed. The controls on Sδ substantially varied with season, soil depth and land use. On the TG hillslope, soil/terrain had weak correlations with Sδ, while on the BF hillslope, rock fragment, slope and elevation had decent correlation with Sδ. This varied controlling factors of Sδ on different hillslopes, period and soil depth suggested that spatial distributions of Sδ were influenced by the occurrence of subsurface preferential flow. Findings of this study suggested that soil moisture temporal stability and its controlling factors were land use type and time period dependent. Hydropedology (dpeaa)DE-He213 Soil water content (dpeaa)DE-He213 Temporal stability (dpeaa)DE-He213 Land use (dpeaa)DE-He213 Liao, Kaihua aut Lai, Xiaoming aut Zhu, Qing aut Zhou, Shenglu aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 7 vom: 26. März (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:7 day:26 month:03 https://dx.doi.org/10.1007/s12665-015-5238-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 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_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_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_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 7 26 03
spelling	10.1007/s12665-015-5238-1 doi (DE-627)SPR026728850 (SPR)s12665-015-5238-1-e DE-627 ger DE-627 rakwb eng Lv, Ligang verfasserin aut Hillslope soil moisture temporal stability under two contrasting land use types during different time periods 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract Knowledge of soil moisture temporal stability and its controlling factors is important for hydrological and environmental management decisions. This study analyzed the influences of soil and terrain on soil moisture temporal stability (relative difference of soil moisture—δ and standard deviation of δ − Sδ) on two contrasting land use hillslopes [tea garden (TG) and bamboo forest (BF)] in the hilly area of Taihu Lake Basin, China. Soil moisture temporal stabilities were considered at two depths (0.1 and 0.3 m) and during eight different periods (entire, dry, wet, rain, spring, summer, fall and winter periods). Results showed that for each land use and soil depth, values of δ in summer were largely deviated from those during the entire period, while values of Sδ after rain storms were strongly deviated from those during the entire period. Correlation coefficients between soil/terrain and δ were generally greater on the BF hillslope (ranged from 0.35 to 0.70) than on the TG hillslope (ranged from 0.30 to 0.55). This suggested that soil moisture distribution was more spatially organized on the BF hillslope than on the TG hillslope. This can be attributed to that the management practices disturbed and mixed the soils on the TG hillslope, which made the soil moisture more randomly distributed. The controls on Sδ substantially varied with season, soil depth and land use. On the TG hillslope, soil/terrain had weak correlations with Sδ, while on the BF hillslope, rock fragment, slope and elevation had decent correlation with Sδ. This varied controlling factors of Sδ on different hillslopes, period and soil depth suggested that spatial distributions of Sδ were influenced by the occurrence of subsurface preferential flow. Findings of this study suggested that soil moisture temporal stability and its controlling factors were land use type and time period dependent. Hydropedology (dpeaa)DE-He213 Soil water content (dpeaa)DE-He213 Temporal stability (dpeaa)DE-He213 Land use (dpeaa)DE-He213 Liao, Kaihua aut Lai, Xiaoming aut Zhu, Qing aut Zhou, Shenglu aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 7 vom: 26. März (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:7 day:26 month:03 https://dx.doi.org/10.1007/s12665-015-5238-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 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_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_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_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 7 26 03
allfields_unstemmed	10.1007/s12665-015-5238-1 doi (DE-627)SPR026728850 (SPR)s12665-015-5238-1-e DE-627 ger DE-627 rakwb eng Lv, Ligang verfasserin aut Hillslope soil moisture temporal stability under two contrasting land use types during different time periods 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract Knowledge of soil moisture temporal stability and its controlling factors is important for hydrological and environmental management decisions. This study analyzed the influences of soil and terrain on soil moisture temporal stability (relative difference of soil moisture—δ and standard deviation of δ − Sδ) on two contrasting land use hillslopes [tea garden (TG) and bamboo forest (BF)] in the hilly area of Taihu Lake Basin, China. Soil moisture temporal stabilities were considered at two depths (0.1 and 0.3 m) and during eight different periods (entire, dry, wet, rain, spring, summer, fall and winter periods). Results showed that for each land use and soil depth, values of δ in summer were largely deviated from those during the entire period, while values of Sδ after rain storms were strongly deviated from those during the entire period. Correlation coefficients between soil/terrain and δ were generally greater on the BF hillslope (ranged from 0.35 to 0.70) than on the TG hillslope (ranged from 0.30 to 0.55). This suggested that soil moisture distribution was more spatially organized on the BF hillslope than on the TG hillslope. This can be attributed to that the management practices disturbed and mixed the soils on the TG hillslope, which made the soil moisture more randomly distributed. The controls on Sδ substantially varied with season, soil depth and land use. On the TG hillslope, soil/terrain had weak correlations with Sδ, while on the BF hillslope, rock fragment, slope and elevation had decent correlation with Sδ. This varied controlling factors of Sδ on different hillslopes, period and soil depth suggested that spatial distributions of Sδ were influenced by the occurrence of subsurface preferential flow. Findings of this study suggested that soil moisture temporal stability and its controlling factors were land use type and time period dependent. Hydropedology (dpeaa)DE-He213 Soil water content (dpeaa)DE-He213 Temporal stability (dpeaa)DE-He213 Land use (dpeaa)DE-He213 Liao, Kaihua aut Lai, Xiaoming aut Zhu, Qing aut Zhou, Shenglu aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 7 vom: 26. März (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:7 day:26 month:03 https://dx.doi.org/10.1007/s12665-015-5238-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 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_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_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_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 7 26 03
allfieldsGer	10.1007/s12665-015-5238-1 doi (DE-627)SPR026728850 (SPR)s12665-015-5238-1-e DE-627 ger DE-627 rakwb eng Lv, Ligang verfasserin aut Hillslope soil moisture temporal stability under two contrasting land use types during different time periods 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract Knowledge of soil moisture temporal stability and its controlling factors is important for hydrological and environmental management decisions. This study analyzed the influences of soil and terrain on soil moisture temporal stability (relative difference of soil moisture—δ and standard deviation of δ − Sδ) on two contrasting land use hillslopes [tea garden (TG) and bamboo forest (BF)] in the hilly area of Taihu Lake Basin, China. Soil moisture temporal stabilities were considered at two depths (0.1 and 0.3 m) and during eight different periods (entire, dry, wet, rain, spring, summer, fall and winter periods). Results showed that for each land use and soil depth, values of δ in summer were largely deviated from those during the entire period, while values of Sδ after rain storms were strongly deviated from those during the entire period. Correlation coefficients between soil/terrain and δ were generally greater on the BF hillslope (ranged from 0.35 to 0.70) than on the TG hillslope (ranged from 0.30 to 0.55). This suggested that soil moisture distribution was more spatially organized on the BF hillslope than on the TG hillslope. This can be attributed to that the management practices disturbed and mixed the soils on the TG hillslope, which made the soil moisture more randomly distributed. The controls on Sδ substantially varied with season, soil depth and land use. On the TG hillslope, soil/terrain had weak correlations with Sδ, while on the BF hillslope, rock fragment, slope and elevation had decent correlation with Sδ. This varied controlling factors of Sδ on different hillslopes, period and soil depth suggested that spatial distributions of Sδ were influenced by the occurrence of subsurface preferential flow. Findings of this study suggested that soil moisture temporal stability and its controlling factors were land use type and time period dependent. Hydropedology (dpeaa)DE-He213 Soil water content (dpeaa)DE-He213 Temporal stability (dpeaa)DE-He213 Land use (dpeaa)DE-He213 Liao, Kaihua aut Lai, Xiaoming aut Zhu, Qing aut Zhou, Shenglu aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 7 vom: 26. März (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:7 day:26 month:03 https://dx.doi.org/10.1007/s12665-015-5238-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 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_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_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_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 7 26 03
allfieldsSound	10.1007/s12665-015-5238-1 doi (DE-627)SPR026728850 (SPR)s12665-015-5238-1-e DE-627 ger DE-627 rakwb eng Lv, Ligang verfasserin aut Hillslope soil moisture temporal stability under two contrasting land use types during different time periods 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract Knowledge of soil moisture temporal stability and its controlling factors is important for hydrological and environmental management decisions. This study analyzed the influences of soil and terrain on soil moisture temporal stability (relative difference of soil moisture—δ and standard deviation of δ − Sδ) on two contrasting land use hillslopes [tea garden (TG) and bamboo forest (BF)] in the hilly area of Taihu Lake Basin, China. Soil moisture temporal stabilities were considered at two depths (0.1 and 0.3 m) and during eight different periods (entire, dry, wet, rain, spring, summer, fall and winter periods). Results showed that for each land use and soil depth, values of δ in summer were largely deviated from those during the entire period, while values of Sδ after rain storms were strongly deviated from those during the entire period. Correlation coefficients between soil/terrain and δ were generally greater on the BF hillslope (ranged from 0.35 to 0.70) than on the TG hillslope (ranged from 0.30 to 0.55). This suggested that soil moisture distribution was more spatially organized on the BF hillslope than on the TG hillslope. This can be attributed to that the management practices disturbed and mixed the soils on the TG hillslope, which made the soil moisture more randomly distributed. The controls on Sδ substantially varied with season, soil depth and land use. On the TG hillslope, soil/terrain had weak correlations with Sδ, while on the BF hillslope, rock fragment, slope and elevation had decent correlation with Sδ. This varied controlling factors of Sδ on different hillslopes, period and soil depth suggested that spatial distributions of Sδ were influenced by the occurrence of subsurface preferential flow. Findings of this study suggested that soil moisture temporal stability and its controlling factors were land use type and time period dependent. Hydropedology (dpeaa)DE-He213 Soil water content (dpeaa)DE-He213 Temporal stability (dpeaa)DE-He213 Land use (dpeaa)DE-He213 Liao, Kaihua aut Lai, Xiaoming aut Zhu, Qing aut Zhou, Shenglu aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 7 vom: 26. März (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:7 day:26 month:03 https://dx.doi.org/10.1007/s12665-015-5238-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_65 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_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_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_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 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_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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 7 26 03
language	English
source	Enthalten in Environmental earth sciences 75(2016), 7 vom: 26. März volume:75 year:2016 number:7 day:26 month:03
sourceStr	Enthalten in Environmental earth sciences 75(2016), 7 vom: 26. März volume:75 year:2016 number:7 day:26 month:03
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Hydropedology Soil water content Temporal stability Land use
isfreeaccess_bool	false
container_title	Environmental earth sciences
authorswithroles_txt_mv	Lv, Ligang @@aut@@ Liao, Kaihua @@aut@@ Lai, Xiaoming @@aut@@ Zhu, Qing @@aut@@ Zhou, Shenglu @@aut@@
publishDateDaySort_date	2016-03-26T00:00:00Z
hierarchy_top_id	599673451
id	SPR026728850
language_de	englisch
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author	Lv, Ligang
spellingShingle	Lv, Ligang misc Hydropedology misc Soil water content misc Temporal stability misc Land use Hillslope soil moisture temporal stability under two contrasting land use types during different time periods
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topic_title	Hillslope soil moisture temporal stability under two contrasting land use types during different time periods Hydropedology (dpeaa)DE-He213 Soil water content (dpeaa)DE-He213 Temporal stability (dpeaa)DE-He213 Land use (dpeaa)DE-He213
topic	misc Hydropedology misc Soil water content misc Temporal stability misc Land use
topic_unstemmed	misc Hydropedology misc Soil water content misc Temporal stability misc Land use
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title	Hillslope soil moisture temporal stability under two contrasting land use types during different time periods
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title_full	Hillslope soil moisture temporal stability under two contrasting land use types during different time periods
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author_browse	Lv, Ligang Liao, Kaihua Lai, Xiaoming Zhu, Qing Zhou, Shenglu
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doi_str_mv	10.1007/s12665-015-5238-1
title_sort	hillslope soil moisture temporal stability under two contrasting land use types during different time periods
title_auth	Hillslope soil moisture temporal stability under two contrasting land use types during different time periods
abstract	Abstract Knowledge of soil moisture temporal stability and its controlling factors is important for hydrological and environmental management decisions. This study analyzed the influences of soil and terrain on soil moisture temporal stability (relative difference of soil moisture—δ and standard deviation of δ − Sδ) on two contrasting land use hillslopes [tea garden (TG) and bamboo forest (BF)] in the hilly area of Taihu Lake Basin, China. Soil moisture temporal stabilities were considered at two depths (0.1 and 0.3 m) and during eight different periods (entire, dry, wet, rain, spring, summer, fall and winter periods). Results showed that for each land use and soil depth, values of δ in summer were largely deviated from those during the entire period, while values of Sδ after rain storms were strongly deviated from those during the entire period. Correlation coefficients between soil/terrain and δ were generally greater on the BF hillslope (ranged from 0.35 to 0.70) than on the TG hillslope (ranged from 0.30 to 0.55). This suggested that soil moisture distribution was more spatially organized on the BF hillslope than on the TG hillslope. This can be attributed to that the management practices disturbed and mixed the soils on the TG hillslope, which made the soil moisture more randomly distributed. The controls on Sδ substantially varied with season, soil depth and land use. On the TG hillslope, soil/terrain had weak correlations with Sδ, while on the BF hillslope, rock fragment, slope and elevation had decent correlation with Sδ. This varied controlling factors of Sδ on different hillslopes, period and soil depth suggested that spatial distributions of Sδ were influenced by the occurrence of subsurface preferential flow. Findings of this study suggested that soil moisture temporal stability and its controlling factors were land use type and time period dependent. © Springer-Verlag Berlin Heidelberg 2016
abstractGer	Abstract Knowledge of soil moisture temporal stability and its controlling factors is important for hydrological and environmental management decisions. This study analyzed the influences of soil and terrain on soil moisture temporal stability (relative difference of soil moisture—δ and standard deviation of δ − Sδ) on two contrasting land use hillslopes [tea garden (TG) and bamboo forest (BF)] in the hilly area of Taihu Lake Basin, China. Soil moisture temporal stabilities were considered at two depths (0.1 and 0.3 m) and during eight different periods (entire, dry, wet, rain, spring, summer, fall and winter periods). Results showed that for each land use and soil depth, values of δ in summer were largely deviated from those during the entire period, while values of Sδ after rain storms were strongly deviated from those during the entire period. Correlation coefficients between soil/terrain and δ were generally greater on the BF hillslope (ranged from 0.35 to 0.70) than on the TG hillslope (ranged from 0.30 to 0.55). This suggested that soil moisture distribution was more spatially organized on the BF hillslope than on the TG hillslope. This can be attributed to that the management practices disturbed and mixed the soils on the TG hillslope, which made the soil moisture more randomly distributed. The controls on Sδ substantially varied with season, soil depth and land use. On the TG hillslope, soil/terrain had weak correlations with Sδ, while on the BF hillslope, rock fragment, slope and elevation had decent correlation with Sδ. This varied controlling factors of Sδ on different hillslopes, period and soil depth suggested that spatial distributions of Sδ were influenced by the occurrence of subsurface preferential flow. Findings of this study suggested that soil moisture temporal stability and its controlling factors were land use type and time period dependent. © Springer-Verlag Berlin Heidelberg 2016
abstract_unstemmed	Abstract Knowledge of soil moisture temporal stability and its controlling factors is important for hydrological and environmental management decisions. This study analyzed the influences of soil and terrain on soil moisture temporal stability (relative difference of soil moisture—δ and standard deviation of δ − Sδ) on two contrasting land use hillslopes [tea garden (TG) and bamboo forest (BF)] in the hilly area of Taihu Lake Basin, China. Soil moisture temporal stabilities were considered at two depths (0.1 and 0.3 m) and during eight different periods (entire, dry, wet, rain, spring, summer, fall and winter periods). Results showed that for each land use and soil depth, values of δ in summer were largely deviated from those during the entire period, while values of Sδ after rain storms were strongly deviated from those during the entire period. Correlation coefficients between soil/terrain and δ were generally greater on the BF hillslope (ranged from 0.35 to 0.70) than on the TG hillslope (ranged from 0.30 to 0.55). This suggested that soil moisture distribution was more spatially organized on the BF hillslope than on the TG hillslope. This can be attributed to that the management practices disturbed and mixed the soils on the TG hillslope, which made the soil moisture more randomly distributed. The controls on Sδ substantially varied with season, soil depth and land use. On the TG hillslope, soil/terrain had weak correlations with Sδ, while on the BF hillslope, rock fragment, slope and elevation had decent correlation with Sδ. This varied controlling factors of Sδ on different hillslopes, period and soil depth suggested that spatial distributions of Sδ were influenced by the occurrence of subsurface preferential flow. Findings of this study suggested that soil moisture temporal stability and its controlling factors were land use type and time period dependent. © Springer-Verlag Berlin Heidelberg 2016
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title_short	Hillslope soil moisture temporal stability under two contrasting land use types during different time periods
url	https://dx.doi.org/10.1007/s12665-015-5238-1
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up_date	2024-07-03T22:25:42.184Z
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fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR026728850</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230401020239.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201007s2016 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s12665-015-5238-1</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR026728850</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s12665-015-5238-1-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="100" ind1="1" ind2=" "><subfield code="a">Lv, Ligang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Hillslope soil moisture temporal stability under two contrasting land use types during different time periods</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016</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="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag Berlin Heidelberg 2016</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Knowledge of soil moisture temporal stability and its controlling factors is important for hydrological and environmental management decisions. This study analyzed the influences of soil and terrain on soil moisture temporal stability (relative difference of soil moisture—δ and standard deviation of δ − Sδ) on two contrasting land use hillslopes [tea garden (TG) and bamboo forest (BF)] in the hilly area of Taihu Lake Basin, China. Soil moisture temporal stabilities were considered at two depths (0.1 and 0.3 m) and during eight different periods (entire, dry, wet, rain, spring, summer, fall and winter periods). Results showed that for each land use and soil depth, values of δ in summer were largely deviated from those during the entire period, while values of Sδ after rain storms were strongly deviated from those during the entire period. Correlation coefficients between soil/terrain and δ were generally greater on the BF hillslope (ranged from 0.35 to 0.70) than on the TG hillslope (ranged from 0.30 to 0.55). This suggested that soil moisture distribution was more spatially organized on the BF hillslope than on the TG hillslope. This can be attributed to that the management practices disturbed and mixed the soils on the TG hillslope, which made the soil moisture more randomly distributed. The controls on Sδ substantially varied with season, soil depth and land use. On the TG hillslope, soil/terrain had weak correlations with Sδ, while on the BF hillslope, rock fragment, slope and elevation had decent correlation with Sδ. This varied controlling factors of Sδ on different hillslopes, period and soil depth suggested that spatial distributions of Sδ were influenced by the occurrence of subsurface preferential flow. 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Hillslope soil moisture temporal stability under two contrasting land use types during different time periods

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