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Spatial patterns of soil stoichiometry and their responses to land use in a desertified area

A case study of China's Horqin Sandy Land

Bibliographic Data

ID21648686
AuthorsWenjie Cao (0009-0007-1224-3367, Northwest Institute of Eco‐Environment and Resources Chinese Academy of Sciences Lanzhou China), Yuqiang Li (0000-0001-5264-8122, Northwest Institute of Eco‐Environment and Resources Chinese Academy of Sciences Lanzhou China, corresponding author), Yun Chen (0000-0001-5123-1624, Northwest Institute of Eco‐Environment and Resources Chinese Academy of Sciences Lanzhou China), Yinping Chen (School of Environmental and Municipal Engineering Lanzhou Jiaotong University Lanzhou China), Xuyang Wang (0009-0001-6609-4463, Northwest Institute of Eco‐Environment and Resources Chinese Academy of Sciences Lanzhou China)
Year2024
Volume35
Issue1
Pages350-359
Publication date2024-01-15
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueLand Degradation and Development (JOURNAL)
Journal identifiersISSN: 1085-3278 • E-ISSN: 1099-145X
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ldr.4920
OpenAlexW4386994531
LanguageEN
Citations received1
References cited37

Ecological stoichiometry facilitates the understanding of biogeochemical cycles by studying the balance among multiple elements in ecosystems. However, the spatial patterns of soil stoichiometry and their responses to land use in desertified land are unclear. In this study, we selected 525 sample points to collect topsoil (0–20 cm) samples throughout China's Horqin Sandy Land and measured soil organic carbon (SOC), total nitrogen (TN), and total phosphorus (TP). We then calculated stoichiometric ratios (C:N:P). SOC (8.7 g kg −1 ), TN (0.9 g kg −1 ), and TP (0.3 g kg −1 ) were lower in this region than in Chinese and global terrestrial ecosystems due to aeolian desertification. SOC, TN, C:P, and N:P were significantly ( p p > 0.05) among grassland, woodland, and cropland because of the strong coupling relationship between SOC and TN. The values of SOC, TN, TP, C:P, and N:P in the Horqin Sandy Land were high in the north (dominated by mountain woodland and grassland) and were low in the south (dominated by desertified land). SOC, TN, and TP contents and C:N:P ratios were mainly affected by mean annual temperature (29.6%), land use (11.5%), and bulk density (11.4%) through their influence on soil microbial metabolism, litter and nutrient input, and soil structure, respectively. The results provide information on the overall changes in soil stoichiometry in the Horqin Sandy Land and its responses to land‐use changes, and can therefore guide ecological restoration in semiarid regions affected by desertification in the modern context of climate change

Agronomy · Biogeochemical cycle · Biology · Ecosystem · Geography · Grassland · Land use · Soil carbon · Soil water · Topsoil · Woodland · Ecology and Vegetation Dynamics Studies · Environmental Science · Plant Water Relations and Carbon Dynamics · Soil Carbon and Nitrogen Dynamics · Ecology · Forestry · Soil Science

  • Characteristics and Drivers of Soil Ecological Stoichiometry in Saline–Alkali Areas of Western Jilin Province, Northeast China

    Open Access•Yuefen Li, Jingfa Zhong et al.•Land Degradation and Development•2024

  • Soil structure and management

    Open Access•C J Bronick, Rattan Lal•Geoderma•2005

Unique citing works1
Citations per year0,5
Citation span2024 - 2024 (1)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 1

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