Changes in Soil Organic Carbon and Total Nitrogen at a Small Watershed Scale as the Result of Land Use Conversion on the Loess Plateau

Soil organic carbon (SOC) and total nitrogen (total N) are important soil components for agricultural production. Soil quality is related to the total amount of SOC and total N sequestered in the soil. Land use plays a major role in the distribution and amount of SOC and total N. This study analyses...

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Main Authors: Zhijing Xue, Shaoshan An
Format: Article
Language:English
Published: MDPI AG 2018-12-01
Series:Sustainability
Subjects:
Online Access:https://www.mdpi.com/2071-1050/10/12/4757
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spelling doaj-42b15964cf594f2097a68e139249c4fa2020-11-24T23:00:36ZengMDPI AGSustainability2071-10502018-12-011012475710.3390/su10124757su10124757Changes in Soil Organic Carbon and Total Nitrogen at a Small Watershed Scale as the Result of Land Use Conversion on the Loess PlateauZhijing Xue0Shaoshan An1State Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Northwest A&amp;F University, Yangling 712100, Shaanxi, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Northwest A&amp;F University, Yangling 712100, Shaanxi, ChinaSoil organic carbon (SOC) and total nitrogen (total N) are important soil components for agricultural production. Soil quality is related to the total amount of SOC and total N sequestered in the soil. Land use plays a major role in the distribution and amount of SOC and total N. This study analyses the amount of SOC and total N under various land cover types in 1987, 2005 and 2010, and evaluated their storage in land use conversions in a comprehensively managed watershed on the Loess Plateau, China. Results show that concentrations of SOC and total N in shrub land and natural grassland areas were significantly higher than for other land uses (farmland, orchard, abandoned farmland, manmade grassland) while cropland had the lowest concentration. Storage of SOC and total N increased along the revegetation chronosequence. As the storage of SOC in 2005 and 2010, they were 3461.86 &#215; 10<sup>8</sup> and 4504.04 &#215; 10<sup>8</sup> g respectively. Soil organic carbon storage were enhanced one third just during 5 years. The effects of land use on SOC and total N were the most significant in the upper soil layers. The correlation between SOC, total N, and the C/N ratio indicated that the best combination of land uses were natural grassland and shrub land. They efficiently influenced the distribution and storage of SOC and total N, and benefited vegetation restoration.https://www.mdpi.com/2071-1050/10/12/4757vegetation restorationland use conversionsoil organic carbontotal nitrogensoil carbon storageC/N ratio
collection DOAJ
language English
format Article
sources DOAJ
author Zhijing Xue
Shaoshan An
spellingShingle Zhijing Xue
Shaoshan An
Changes in Soil Organic Carbon and Total Nitrogen at a Small Watershed Scale as the Result of Land Use Conversion on the Loess Plateau
Sustainability
vegetation restoration
land use conversion
soil organic carbon
total nitrogen
soil carbon storage
C/N ratio
author_facet Zhijing Xue
Shaoshan An
author_sort Zhijing Xue
title Changes in Soil Organic Carbon and Total Nitrogen at a Small Watershed Scale as the Result of Land Use Conversion on the Loess Plateau
title_short Changes in Soil Organic Carbon and Total Nitrogen at a Small Watershed Scale as the Result of Land Use Conversion on the Loess Plateau
title_full Changes in Soil Organic Carbon and Total Nitrogen at a Small Watershed Scale as the Result of Land Use Conversion on the Loess Plateau
title_fullStr Changes in Soil Organic Carbon and Total Nitrogen at a Small Watershed Scale as the Result of Land Use Conversion on the Loess Plateau
title_full_unstemmed Changes in Soil Organic Carbon and Total Nitrogen at a Small Watershed Scale as the Result of Land Use Conversion on the Loess Plateau
title_sort changes in soil organic carbon and total nitrogen at a small watershed scale as the result of land use conversion on the loess plateau
publisher MDPI AG
series Sustainability
issn 2071-1050
publishDate 2018-12-01
description Soil organic carbon (SOC) and total nitrogen (total N) are important soil components for agricultural production. Soil quality is related to the total amount of SOC and total N sequestered in the soil. Land use plays a major role in the distribution and amount of SOC and total N. This study analyses the amount of SOC and total N under various land cover types in 1987, 2005 and 2010, and evaluated their storage in land use conversions in a comprehensively managed watershed on the Loess Plateau, China. Results show that concentrations of SOC and total N in shrub land and natural grassland areas were significantly higher than for other land uses (farmland, orchard, abandoned farmland, manmade grassland) while cropland had the lowest concentration. Storage of SOC and total N increased along the revegetation chronosequence. As the storage of SOC in 2005 and 2010, they were 3461.86 &#215; 10<sup>8</sup> and 4504.04 &#215; 10<sup>8</sup> g respectively. Soil organic carbon storage were enhanced one third just during 5 years. The effects of land use on SOC and total N were the most significant in the upper soil layers. The correlation between SOC, total N, and the C/N ratio indicated that the best combination of land uses were natural grassland and shrub land. They efficiently influenced the distribution and storage of SOC and total N, and benefited vegetation restoration.
topic vegetation restoration
land use conversion
soil organic carbon
total nitrogen
soil carbon storage
C/N ratio
url https://www.mdpi.com/2071-1050/10/12/4757
work_keys_str_mv AT zhijingxue changesinsoilorganiccarbonandtotalnitrogenatasmallwatershedscaleastheresultoflanduseconversionontheloessplateau
AT shaoshanan changesinsoilorganiccarbonandtotalnitrogenatasmallwatershedscaleastheresultoflanduseconversionontheloessplateau
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