Changes in Cultivated Land Area and Associated Soil and SOC Losses in Northeastern China: The Role of Land Use Policies

Land use policy is the driving factor influencing land use; however, little research has been conducted to identify the role of agricultural policy in influencing land cultivation and associated soil and soil organic carbon (SOC) losses. The aims of this study were to explore temporal changes in cul...

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Autor principal: Haiyan Fang
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Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:667b26aa72c641d48eca47932fd525bf2021-11-11T16:27:35ZChanges in Cultivated Land Area and Associated Soil and SOC Losses in Northeastern China: The Role of Land Use Policies10.3390/ijerph1821113141660-46011661-7827https://doaj.org/article/667b26aa72c641d48eca47932fd525bf2021-10-01T00:00:00Zhttps://www.mdpi.com/1660-4601/18/21/11314https://doaj.org/toc/1661-7827https://doaj.org/toc/1660-4601Land use policy is the driving factor influencing land use; however, little research has been conducted to identify the role of agricultural policy in influencing land cultivation and associated soil and soil organic carbon (SOC) losses. The aims of this study were to explore temporal changes in cultivated land, soil erosion, and SOC loss and to identify the role of land use policy. The present study was conducted using the revised universal soil loss equation by integrating remote sensing images from 1980, 1990, 2000, and 2017. The study found that cultivated land areas increased from 275.11 thousand km<sup>2</sup> in 1980, to 300.03 thousand km<sup>2</sup> in 2000, and to 344.16 thousand km<sup>2</sup> in 2010, and then decreased by 326.94 thousand km<sup>2</sup>. The mean soil loss rates changed from 590.66 t·km<sup>−2</sup>·yr<sup>−1</sup> in 1980 to 634.25 t·km<sup>−2</sup>·yr<sup>−1</sup> in 2010, and then decreased to 495.66 t·km<sup>−2</sup>·yr<sup>−1</sup> in 2017. Soil loss rate increased with increasing slope gradient. The changes in SOC loss rates demonstrated the same pattern as that of soil loss, with the largest loss rate of 728.27 kg·km<sup>−2</sup>·yr<sup>−1</sup>. These changes can be explained by changed land use policy and population growth. In future land use management, reasonable implementation of soil conservation measures should be undertaken to reduce soil and SOC losses in the black soil region of northeastern China.Haiyan FangMDPI AGarticlecultivated landsoil erosionSOC lossesland use policyblack soil regionMedicineRENInternational Journal of Environmental Research and Public Health, Vol 18, Iss 11314, p 11314 (2021)
institution DOAJ
collection DOAJ
language EN
topic cultivated land
soil erosion
SOC losses
land use policy
black soil region
Medicine
R
spellingShingle cultivated land
soil erosion
SOC losses
land use policy
black soil region
Medicine
R
Haiyan Fang
Changes in Cultivated Land Area and Associated Soil and SOC Losses in Northeastern China: The Role of Land Use Policies
description Land use policy is the driving factor influencing land use; however, little research has been conducted to identify the role of agricultural policy in influencing land cultivation and associated soil and soil organic carbon (SOC) losses. The aims of this study were to explore temporal changes in cultivated land, soil erosion, and SOC loss and to identify the role of land use policy. The present study was conducted using the revised universal soil loss equation by integrating remote sensing images from 1980, 1990, 2000, and 2017. The study found that cultivated land areas increased from 275.11 thousand km<sup>2</sup> in 1980, to 300.03 thousand km<sup>2</sup> in 2000, and to 344.16 thousand km<sup>2</sup> in 2010, and then decreased by 326.94 thousand km<sup>2</sup>. The mean soil loss rates changed from 590.66 t·km<sup>−2</sup>·yr<sup>−1</sup> in 1980 to 634.25 t·km<sup>−2</sup>·yr<sup>−1</sup> in 2010, and then decreased to 495.66 t·km<sup>−2</sup>·yr<sup>−1</sup> in 2017. Soil loss rate increased with increasing slope gradient. The changes in SOC loss rates demonstrated the same pattern as that of soil loss, with the largest loss rate of 728.27 kg·km<sup>−2</sup>·yr<sup>−1</sup>. These changes can be explained by changed land use policy and population growth. In future land use management, reasonable implementation of soil conservation measures should be undertaken to reduce soil and SOC losses in the black soil region of northeastern China.
format article
author Haiyan Fang
author_facet Haiyan Fang
author_sort Haiyan Fang
title Changes in Cultivated Land Area and Associated Soil and SOC Losses in Northeastern China: The Role of Land Use Policies
title_short Changes in Cultivated Land Area and Associated Soil and SOC Losses in Northeastern China: The Role of Land Use Policies
title_full Changes in Cultivated Land Area and Associated Soil and SOC Losses in Northeastern China: The Role of Land Use Policies
title_fullStr Changes in Cultivated Land Area and Associated Soil and SOC Losses in Northeastern China: The Role of Land Use Policies
title_full_unstemmed Changes in Cultivated Land Area and Associated Soil and SOC Losses in Northeastern China: The Role of Land Use Policies
title_sort changes in cultivated land area and associated soil and soc losses in northeastern china: the role of land use policies
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/667b26aa72c641d48eca47932fd525bf
work_keys_str_mv AT haiyanfang changesincultivatedlandareaandassociatedsoilandsoclossesinnortheasternchinatheroleoflandusepolicies
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