Effects of freeze-thaw on soil properties and water erosion

Freeze-thaw erosion occurs primarily at high latitudes and altitudes. Temperature controlled freeze-thaw events dislodge soil particles and serve as a catalyst for erosion. This review paper provided an overview of the effects of freeze-thaw on soil properties and water erosion. The process of freez...
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Autor*in:	Baoyang Sun [verfasserIn] Feipeng Ren [verfasserIn] Wenfeng Ding [verfasserIn] Guanhua Zhang [verfasserIn] Jinquan Huang [verfasserIn] Jianming Li [verfasserIn] Lei Zhang [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2021

Schlagwörter:	erosion amount erosion process freeze-thaw cycles soil properties soil moisture transport

Übergeordnetes Werk:	In: Soil and Water Research - Czech Academy of Agricultural Sciences, 2016, 16(2021), 4, Seite 205-216
Übergeordnetes Werk:	volume:16 ; year:2021 ; number:4 ; pages:205-216

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.17221/143/2020-SWR

Katalog-ID:	DOAJ08280981X

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520			\|a Freeze-thaw erosion occurs primarily at high latitudes and altitudes. Temperature controlled freeze-thaw events dislodge soil particles and serve as a catalyst for erosion. This review paper provided an overview of the effects of freeze-thaw on soil properties and water erosion. The process of freeze-thaw cycles results in temporary and inconsistent changes in the soil moisture, and affects the soil's mechanical, physical and chemical properties, such as the soil moisture content, porosity, bulk density, aggregates stability, shear strength and organic matter content and so on. The variation trend and range of the soil properties were related to the soil texture, water content and freeze-thaw degree. Furthermore, the soil erosion was affected by the freeze-thaw processes, as thawing and water erosion reinforce each other. However, research of different experimental conditions on indoor simulations have numerous limitations compared with field experiments. The use of indoor and field experiments to further reveal the freeze-thaw effect on the soil erosion would facilitate improved forecasting.
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allfields	10.17221/143/2020-SWR doi (DE-627)DOAJ08280981X (DE-599)DOAJdfe24f0e09504941a467260932b8915f DE-627 ger DE-627 rakwb eng Baoyang Sun verfasserin aut Effects of freeze-thaw on soil properties and water erosion 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Freeze-thaw erosion occurs primarily at high latitudes and altitudes. Temperature controlled freeze-thaw events dislodge soil particles and serve as a catalyst for erosion. This review paper provided an overview of the effects of freeze-thaw on soil properties and water erosion. The process of freeze-thaw cycles results in temporary and inconsistent changes in the soil moisture, and affects the soil's mechanical, physical and chemical properties, such as the soil moisture content, porosity, bulk density, aggregates stability, shear strength and organic matter content and so on. The variation trend and range of the soil properties were related to the soil texture, water content and freeze-thaw degree. Furthermore, the soil erosion was affected by the freeze-thaw processes, as thawing and water erosion reinforce each other. However, research of different experimental conditions on indoor simulations have numerous limitations compared with field experiments. The use of indoor and field experiments to further reveal the freeze-thaw effect on the soil erosion would facilitate improved forecasting. erosion amount erosion process freeze-thaw cycles soil properties soil moisture transport Agriculture S Feipeng Ren verfasserin aut Wenfeng Ding verfasserin aut Guanhua Zhang verfasserin aut Jinquan Huang verfasserin aut Jianming Li verfasserin aut Lei Zhang verfasserin aut In Soil and Water Research Czech Academy of Agricultural Sciences, 2016 16(2021), 4, Seite 205-216 (DE-627)585506779 (DE-600)2465020-1 18059384 nnns volume:16 year:2021 number:4 pages:205-216 https://doi.org/10.17221/143/2020-SWR kostenfrei https://doaj.org/article/dfe24f0e09504941a467260932b8915f kostenfrei https://swr.agriculturejournals.cz/artkey/swr-202104-0002_effects-of-freeze-thaw-on-soil-properties-and-water-erosion.php kostenfrei https://doaj.org/toc/1801-5395 Journal toc kostenfrei https://doaj.org/toc/1805-9384 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 16 2021 4 205-216
spelling	10.17221/143/2020-SWR doi (DE-627)DOAJ08280981X (DE-599)DOAJdfe24f0e09504941a467260932b8915f DE-627 ger DE-627 rakwb eng Baoyang Sun verfasserin aut Effects of freeze-thaw on soil properties and water erosion 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Freeze-thaw erosion occurs primarily at high latitudes and altitudes. Temperature controlled freeze-thaw events dislodge soil particles and serve as a catalyst for erosion. This review paper provided an overview of the effects of freeze-thaw on soil properties and water erosion. The process of freeze-thaw cycles results in temporary and inconsistent changes in the soil moisture, and affects the soil's mechanical, physical and chemical properties, such as the soil moisture content, porosity, bulk density, aggregates stability, shear strength and organic matter content and so on. The variation trend and range of the soil properties were related to the soil texture, water content and freeze-thaw degree. Furthermore, the soil erosion was affected by the freeze-thaw processes, as thawing and water erosion reinforce each other. However, research of different experimental conditions on indoor simulations have numerous limitations compared with field experiments. The use of indoor and field experiments to further reveal the freeze-thaw effect on the soil erosion would facilitate improved forecasting. erosion amount erosion process freeze-thaw cycles soil properties soil moisture transport Agriculture S Feipeng Ren verfasserin aut Wenfeng Ding verfasserin aut Guanhua Zhang verfasserin aut Jinquan Huang verfasserin aut Jianming Li verfasserin aut Lei Zhang verfasserin aut In Soil and Water Research Czech Academy of Agricultural Sciences, 2016 16(2021), 4, Seite 205-216 (DE-627)585506779 (DE-600)2465020-1 18059384 nnns volume:16 year:2021 number:4 pages:205-216 https://doi.org/10.17221/143/2020-SWR kostenfrei https://doaj.org/article/dfe24f0e09504941a467260932b8915f kostenfrei https://swr.agriculturejournals.cz/artkey/swr-202104-0002_effects-of-freeze-thaw-on-soil-properties-and-water-erosion.php kostenfrei https://doaj.org/toc/1801-5395 Journal toc kostenfrei https://doaj.org/toc/1805-9384 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 16 2021 4 205-216
allfields_unstemmed	10.17221/143/2020-SWR doi (DE-627)DOAJ08280981X (DE-599)DOAJdfe24f0e09504941a467260932b8915f DE-627 ger DE-627 rakwb eng Baoyang Sun verfasserin aut Effects of freeze-thaw on soil properties and water erosion 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Freeze-thaw erosion occurs primarily at high latitudes and altitudes. Temperature controlled freeze-thaw events dislodge soil particles and serve as a catalyst for erosion. This review paper provided an overview of the effects of freeze-thaw on soil properties and water erosion. The process of freeze-thaw cycles results in temporary and inconsistent changes in the soil moisture, and affects the soil's mechanical, physical and chemical properties, such as the soil moisture content, porosity, bulk density, aggregates stability, shear strength and organic matter content and so on. The variation trend and range of the soil properties were related to the soil texture, water content and freeze-thaw degree. Furthermore, the soil erosion was affected by the freeze-thaw processes, as thawing and water erosion reinforce each other. However, research of different experimental conditions on indoor simulations have numerous limitations compared with field experiments. The use of indoor and field experiments to further reveal the freeze-thaw effect on the soil erosion would facilitate improved forecasting. erosion amount erosion process freeze-thaw cycles soil properties soil moisture transport Agriculture S Feipeng Ren verfasserin aut Wenfeng Ding verfasserin aut Guanhua Zhang verfasserin aut Jinquan Huang verfasserin aut Jianming Li verfasserin aut Lei Zhang verfasserin aut In Soil and Water Research Czech Academy of Agricultural Sciences, 2016 16(2021), 4, Seite 205-216 (DE-627)585506779 (DE-600)2465020-1 18059384 nnns volume:16 year:2021 number:4 pages:205-216 https://doi.org/10.17221/143/2020-SWR kostenfrei https://doaj.org/article/dfe24f0e09504941a467260932b8915f kostenfrei https://swr.agriculturejournals.cz/artkey/swr-202104-0002_effects-of-freeze-thaw-on-soil-properties-and-water-erosion.php kostenfrei https://doaj.org/toc/1801-5395 Journal toc kostenfrei https://doaj.org/toc/1805-9384 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 16 2021 4 205-216
allfieldsGer	10.17221/143/2020-SWR doi (DE-627)DOAJ08280981X (DE-599)DOAJdfe24f0e09504941a467260932b8915f DE-627 ger DE-627 rakwb eng Baoyang Sun verfasserin aut Effects of freeze-thaw on soil properties and water erosion 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Freeze-thaw erosion occurs primarily at high latitudes and altitudes. Temperature controlled freeze-thaw events dislodge soil particles and serve as a catalyst for erosion. This review paper provided an overview of the effects of freeze-thaw on soil properties and water erosion. The process of freeze-thaw cycles results in temporary and inconsistent changes in the soil moisture, and affects the soil's mechanical, physical and chemical properties, such as the soil moisture content, porosity, bulk density, aggregates stability, shear strength and organic matter content and so on. The variation trend and range of the soil properties were related to the soil texture, water content and freeze-thaw degree. Furthermore, the soil erosion was affected by the freeze-thaw processes, as thawing and water erosion reinforce each other. However, research of different experimental conditions on indoor simulations have numerous limitations compared with field experiments. The use of indoor and field experiments to further reveal the freeze-thaw effect on the soil erosion would facilitate improved forecasting. erosion amount erosion process freeze-thaw cycles soil properties soil moisture transport Agriculture S Feipeng Ren verfasserin aut Wenfeng Ding verfasserin aut Guanhua Zhang verfasserin aut Jinquan Huang verfasserin aut Jianming Li verfasserin aut Lei Zhang verfasserin aut In Soil and Water Research Czech Academy of Agricultural Sciences, 2016 16(2021), 4, Seite 205-216 (DE-627)585506779 (DE-600)2465020-1 18059384 nnns volume:16 year:2021 number:4 pages:205-216 https://doi.org/10.17221/143/2020-SWR kostenfrei https://doaj.org/article/dfe24f0e09504941a467260932b8915f kostenfrei https://swr.agriculturejournals.cz/artkey/swr-202104-0002_effects-of-freeze-thaw-on-soil-properties-and-water-erosion.php kostenfrei https://doaj.org/toc/1801-5395 Journal toc kostenfrei https://doaj.org/toc/1805-9384 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 16 2021 4 205-216
allfieldsSound	10.17221/143/2020-SWR doi (DE-627)DOAJ08280981X (DE-599)DOAJdfe24f0e09504941a467260932b8915f DE-627 ger DE-627 rakwb eng Baoyang Sun verfasserin aut Effects of freeze-thaw on soil properties and water erosion 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Freeze-thaw erosion occurs primarily at high latitudes and altitudes. Temperature controlled freeze-thaw events dislodge soil particles and serve as a catalyst for erosion. This review paper provided an overview of the effects of freeze-thaw on soil properties and water erosion. The process of freeze-thaw cycles results in temporary and inconsistent changes in the soil moisture, and affects the soil's mechanical, physical and chemical properties, such as the soil moisture content, porosity, bulk density, aggregates stability, shear strength and organic matter content and so on. The variation trend and range of the soil properties were related to the soil texture, water content and freeze-thaw degree. Furthermore, the soil erosion was affected by the freeze-thaw processes, as thawing and water erosion reinforce each other. However, research of different experimental conditions on indoor simulations have numerous limitations compared with field experiments. The use of indoor and field experiments to further reveal the freeze-thaw effect on the soil erosion would facilitate improved forecasting. erosion amount erosion process freeze-thaw cycles soil properties soil moisture transport Agriculture S Feipeng Ren verfasserin aut Wenfeng Ding verfasserin aut Guanhua Zhang verfasserin aut Jinquan Huang verfasserin aut Jianming Li verfasserin aut Lei Zhang verfasserin aut In Soil and Water Research Czech Academy of Agricultural Sciences, 2016 16(2021), 4, Seite 205-216 (DE-627)585506779 (DE-600)2465020-1 18059384 nnns volume:16 year:2021 number:4 pages:205-216 https://doi.org/10.17221/143/2020-SWR kostenfrei https://doaj.org/article/dfe24f0e09504941a467260932b8915f kostenfrei https://swr.agriculturejournals.cz/artkey/swr-202104-0002_effects-of-freeze-thaw-on-soil-properties-and-water-erosion.php kostenfrei https://doaj.org/toc/1801-5395 Journal toc kostenfrei https://doaj.org/toc/1805-9384 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 16 2021 4 205-216
language	English
source	In Soil and Water Research 16(2021), 4, Seite 205-216 volume:16 year:2021 number:4 pages:205-216
sourceStr	In Soil and Water Research 16(2021), 4, Seite 205-216 volume:16 year:2021 number:4 pages:205-216
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topic_facet	erosion amount erosion process freeze-thaw cycles soil properties soil moisture transport Agriculture S
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authorswithroles_txt_mv	Baoyang Sun @@aut@@ Feipeng Ren @@aut@@ Wenfeng Ding @@aut@@ Guanhua Zhang @@aut@@ Jinquan Huang @@aut@@ Jianming Li @@aut@@ Lei Zhang @@aut@@
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author	Baoyang Sun
spellingShingle	Baoyang Sun misc erosion amount misc erosion process misc freeze-thaw cycles misc soil properties misc soil moisture transport misc Agriculture misc S Effects of freeze-thaw on soil properties and water erosion
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topic_title	Effects of freeze-thaw on soil properties and water erosion erosion amount erosion process freeze-thaw cycles soil properties soil moisture transport
topic	misc erosion amount misc erosion process misc freeze-thaw cycles misc soil properties misc soil moisture transport misc Agriculture misc S
topic_unstemmed	misc erosion amount misc erosion process misc freeze-thaw cycles misc soil properties misc soil moisture transport misc Agriculture misc S
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title	Effects of freeze-thaw on soil properties and water erosion
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title_full	Effects of freeze-thaw on soil properties and water erosion
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title_sort	effects of freeze-thaw on soil properties and water erosion
title_auth	Effects of freeze-thaw on soil properties and water erosion
abstract	Freeze-thaw erosion occurs primarily at high latitudes and altitudes. Temperature controlled freeze-thaw events dislodge soil particles and serve as a catalyst for erosion. This review paper provided an overview of the effects of freeze-thaw on soil properties and water erosion. The process of freeze-thaw cycles results in temporary and inconsistent changes in the soil moisture, and affects the soil's mechanical, physical and chemical properties, such as the soil moisture content, porosity, bulk density, aggregates stability, shear strength and organic matter content and so on. The variation trend and range of the soil properties were related to the soil texture, water content and freeze-thaw degree. Furthermore, the soil erosion was affected by the freeze-thaw processes, as thawing and water erosion reinforce each other. However, research of different experimental conditions on indoor simulations have numerous limitations compared with field experiments. The use of indoor and field experiments to further reveal the freeze-thaw effect on the soil erosion would facilitate improved forecasting.
abstractGer	Freeze-thaw erosion occurs primarily at high latitudes and altitudes. Temperature controlled freeze-thaw events dislodge soil particles and serve as a catalyst for erosion. This review paper provided an overview of the effects of freeze-thaw on soil properties and water erosion. The process of freeze-thaw cycles results in temporary and inconsistent changes in the soil moisture, and affects the soil's mechanical, physical and chemical properties, such as the soil moisture content, porosity, bulk density, aggregates stability, shear strength and organic matter content and so on. The variation trend and range of the soil properties were related to the soil texture, water content and freeze-thaw degree. Furthermore, the soil erosion was affected by the freeze-thaw processes, as thawing and water erosion reinforce each other. However, research of different experimental conditions on indoor simulations have numerous limitations compared with field experiments. The use of indoor and field experiments to further reveal the freeze-thaw effect on the soil erosion would facilitate improved forecasting.
abstract_unstemmed	Freeze-thaw erosion occurs primarily at high latitudes and altitudes. Temperature controlled freeze-thaw events dislodge soil particles and serve as a catalyst for erosion. This review paper provided an overview of the effects of freeze-thaw on soil properties and water erosion. The process of freeze-thaw cycles results in temporary and inconsistent changes in the soil moisture, and affects the soil's mechanical, physical and chemical properties, such as the soil moisture content, porosity, bulk density, aggregates stability, shear strength and organic matter content and so on. The variation trend and range of the soil properties were related to the soil texture, water content and freeze-thaw degree. Furthermore, the soil erosion was affected by the freeze-thaw processes, as thawing and water erosion reinforce each other. However, research of different experimental conditions on indoor simulations have numerous limitations compared with field experiments. The use of indoor and field experiments to further reveal the freeze-thaw effect on the soil erosion would facilitate improved forecasting.
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title_short	Effects of freeze-thaw on soil properties and water erosion
url	https://doi.org/10.17221/143/2020-SWR https://doaj.org/article/dfe24f0e09504941a467260932b8915f https://swr.agriculturejournals.cz/artkey/swr-202104-0002_effects-of-freeze-thaw-on-soil-properties-and-water-erosion.php https://doaj.org/toc/1801-5395 https://doaj.org/toc/1805-9384
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Effects of freeze-thaw on soil properties and water erosion

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