Temporal and Spatial Variations in Soil Elemental Stoichiometry Coupled with Alterations in Agricultural Land Use Types in the Taihu Lake Basin

Soil elemental stoichiometry, expressed as the ratios of carbon (C), nitrogen (N), and phosphorus (P), regulates the biogeochemical processes of elements in terrestrial ecosystems. Generally, the soil C:N:P stoichiometry characteristics of agricultural ecosystems may be different from those of natur...

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Main Authors: Chonggang Liu, Jiangye Li, Wei Sun, Yan Gao, Zhuyun Yu, Yue Dong, Pingxing Li
Format: Article
Language:English
Published: MDPI AG 2023-02-01
Series:Agriculture
Subjects:
Online Access:https://www.mdpi.com/2077-0472/13/2/484
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author Chonggang Liu
Jiangye Li
Wei Sun
Yan Gao
Zhuyun Yu
Yue Dong
Pingxing Li
author_facet Chonggang Liu
Jiangye Li
Wei Sun
Yan Gao
Zhuyun Yu
Yue Dong
Pingxing Li
author_sort Chonggang Liu
collection DOAJ
description Soil elemental stoichiometry, expressed as the ratios of carbon (C), nitrogen (N), and phosphorus (P), regulates the biogeochemical processes of elements in terrestrial ecosystems. Generally, the soil C:N:P stoichiometry characteristics of agricultural ecosystems may be different from those of natural ecosystems, with distinct temporal and spatial variations along with the alterations of agricultural land use types (LUTs). The balance of soil C, N, and P reflected by their stoichiometry is primarily important to microbial activity and sustainable agricultural development. However, information on soil stoichiometric changes after long-term alterations in land use is still lacking. We characterized the temporal and spatial changes in soil elemental stoichiometry coupled with alterations in agricultural LUTs in the Taihu Lake basin. By using the ArcGIS method and meta-data analysis, our results showed that the C:N, C:P, and N:P ratios of agricultural soil in the Taihu Lake basin were much lower than the well-constrained values based on samples from forest, shrubland, and grassland at a global scale. Generally, these elemental ratios in soils increased from the 1980s to the 2000s, after experiencing changes from agricultural to other land use. The soil C:N:P stoichiometry may have maintained the increasing trend according to the meta-data analysis from the 341 peer-reviewed publications since 2010. Nevertheless, different regions showed inconsistent change patterns, with the Tianmu Mountain area surrounding the downstream of the Taihu Lake basin experiencing a reduction in those ratios. The changes in LUTs and their corresponding management practices were the major drivers shaping the spatial and temporal distributions of soil C:N, C:P, and N:P. Paddy soil generally achieved higher C sequestration potential due to more straw input and a more rapid transfer of straw C into soil C in the upstream of the Taihu Lake basin than other land use types. These results provide valuable information for the agricultural system of intensive cultivation on how their soil elemental stoichiometry characteristics vary temporally and spatially due to the alteration of agricultural land use types.
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spelling doaj.art-dfe97a6f6058456dab01757f7e53c3362023-11-16T18:31:52ZengMDPI AGAgriculture2077-04722023-02-0113248410.3390/agriculture13020484Temporal and Spatial Variations in Soil Elemental Stoichiometry Coupled with Alterations in Agricultural Land Use Types in the Taihu Lake BasinChonggang Liu0Jiangye Li1Wei Sun2Yan Gao3Zhuyun Yu4Yue Dong5Pingxing Li6Nanjing Institute of Geography & Limnology, Chinese Academy of Sciences, Nanjing 210008, ChinaInstitute of Agricultural Resources and Environment, Jiangsu Academy of Agricultural Sciences, Nanjing 210014, ChinaNanjing Institute of Geography & Limnology, Chinese Academy of Sciences, Nanjing 210008, ChinaInstitute of Agricultural Resources and Environment, Jiangsu Academy of Agricultural Sciences, Nanjing 210014, ChinaHebei Province Key Laboratory of Wetland Ecology and Conservation, Hengshui University, Hengshui 053000, ChinaScientific Research Base Administration Office, Jiangsu Academy of Agricultural Sciences, Nanjing 210014, ChinaNanjing Institute of Geography & Limnology, Chinese Academy of Sciences, Nanjing 210008, ChinaSoil elemental stoichiometry, expressed as the ratios of carbon (C), nitrogen (N), and phosphorus (P), regulates the biogeochemical processes of elements in terrestrial ecosystems. Generally, the soil C:N:P stoichiometry characteristics of agricultural ecosystems may be different from those of natural ecosystems, with distinct temporal and spatial variations along with the alterations of agricultural land use types (LUTs). The balance of soil C, N, and P reflected by their stoichiometry is primarily important to microbial activity and sustainable agricultural development. However, information on soil stoichiometric changes after long-term alterations in land use is still lacking. We characterized the temporal and spatial changes in soil elemental stoichiometry coupled with alterations in agricultural LUTs in the Taihu Lake basin. By using the ArcGIS method and meta-data analysis, our results showed that the C:N, C:P, and N:P ratios of agricultural soil in the Taihu Lake basin were much lower than the well-constrained values based on samples from forest, shrubland, and grassland at a global scale. Generally, these elemental ratios in soils increased from the 1980s to the 2000s, after experiencing changes from agricultural to other land use. The soil C:N:P stoichiometry may have maintained the increasing trend according to the meta-data analysis from the 341 peer-reviewed publications since 2010. Nevertheless, different regions showed inconsistent change patterns, with the Tianmu Mountain area surrounding the downstream of the Taihu Lake basin experiencing a reduction in those ratios. The changes in LUTs and their corresponding management practices were the major drivers shaping the spatial and temporal distributions of soil C:N, C:P, and N:P. Paddy soil generally achieved higher C sequestration potential due to more straw input and a more rapid transfer of straw C into soil C in the upstream of the Taihu Lake basin than other land use types. These results provide valuable information for the agricultural system of intensive cultivation on how their soil elemental stoichiometry characteristics vary temporally and spatially due to the alteration of agricultural land use types.https://www.mdpi.com/2077-0472/13/2/484temporal-spatial distributionsC:N:P stoichiometry characteristicsland use type changessustainable agricultural developmentC sequestration
spellingShingle Chonggang Liu
Jiangye Li
Wei Sun
Yan Gao
Zhuyun Yu
Yue Dong
Pingxing Li
Temporal and Spatial Variations in Soil Elemental Stoichiometry Coupled with Alterations in Agricultural Land Use Types in the Taihu Lake Basin
Agriculture
temporal-spatial distributions
C:N:P stoichiometry characteristics
land use type changes
sustainable agricultural development
C sequestration
title Temporal and Spatial Variations in Soil Elemental Stoichiometry Coupled with Alterations in Agricultural Land Use Types in the Taihu Lake Basin
title_full Temporal and Spatial Variations in Soil Elemental Stoichiometry Coupled with Alterations in Agricultural Land Use Types in the Taihu Lake Basin
title_fullStr Temporal and Spatial Variations in Soil Elemental Stoichiometry Coupled with Alterations in Agricultural Land Use Types in the Taihu Lake Basin
title_full_unstemmed Temporal and Spatial Variations in Soil Elemental Stoichiometry Coupled with Alterations in Agricultural Land Use Types in the Taihu Lake Basin
title_short Temporal and Spatial Variations in Soil Elemental Stoichiometry Coupled with Alterations in Agricultural Land Use Types in the Taihu Lake Basin
title_sort temporal and spatial variations in soil elemental stoichiometry coupled with alterations in agricultural land use types in the taihu lake basin
topic temporal-spatial distributions
C:N:P stoichiometry characteristics
land use type changes
sustainable agricultural development
C sequestration
url https://www.mdpi.com/2077-0472/13/2/484
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