Analysis of Soil Carbon, Nitrogen and Phosphorus Storage and Sequestration Effects in Alpine Grassland with Different Degradation Levels in Maqu County, China

IF 1.4 4区 农林科学 Q4 SOIL SCIENCE Eurasian Soil Science Pub Date : 2024-02-20 DOI:10.1134/s1064229323602846
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Abstract

Soil nutrient storage and sequestration effects are closely related to the stability of alpine grassland ecosystems, and the study of soil nutrient storage and sequestration effects in alpine grasslands with different degradation levels is of great significance to the recovery of alpine grassland vegetation. On this basis, four alpine grasslands with different degrees of degradation (non-degraded, lightly degraded, moderately degraded, and heavily degraded) were selected in Maqu County, Gannan, and soil samples were collected from 0–10, 10–20, 20–40, and 40–60 cm, respectively, and analyzed for nutrients in terms of storage and sequestration effects. The results showed that soil water content decreased with increasing degradation, while soil pH, bulk density, and conductivity tended to increase. The storage and sequestration effects of soil organic carbon decreased with increasing degradation. And the storage and sequestration effects of soil total nitrogen and total phosphorus were smallest for moderately degraded soils in the 10–60 cm soil layer. Soil water content and soil bulk density were co-influences on soil organic carbon, total nitrogen, and total phosphorus storage. For the soil organic carbon sequestration effect, soil total nitrogen sequestration effect and soil pH were the two most important influencing factors, and the soil total nitrogen and total phosphorus sequestration effect were greatly influenced by soil organic carbon sequestration effect. In addition, soil bulk density was also the main influencing factor of soil total nitrogen sequestration effect, and the impact of soil total nitrogen sequestration on soil total phosphorus sequestration was also greatly influenced.

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中国玛曲县不同退化程度高寒草地土壤碳、氮、磷储存与封存效应分析
摘要 土壤养分贮存与固碳效应与高寒草地生态系统的稳定性密切相关,研究不同退化程度高寒草地的土壤养分贮存与固碳效应对高寒草地植被恢复具有重要意义。在此基础上,在甘南玛曲县选取了4片不同退化程度(未退化、轻度退化、中度退化、重度退化)的高寒草地,分别采集了0-10、10-20、20-40、40-60 cm的土壤样品,并从贮存和固碳效应的角度对土壤养分进行了分析。结果表明,土壤含水量随着降解程度的增加而降低,而土壤 pH 值、容重和电导率则呈上升趋势。土壤有机碳的储存和固碳效应随着降解程度的增加而降低。在 10-60 厘米土层的中度退化土壤中,土壤全氮和全磷的储存和固碳效应最小。土壤含水量和土壤容重对土壤有机碳、全氮和全磷的储存有共同影响。对于土壤有机碳的固碳效果而言,土壤全氮的固碳效果和土壤 pH 值是两个最重要的影响因素,而土壤全氮和全磷的固碳效果受土壤有机碳固碳效果的影响较大。此外,土壤容重也是土壤全氮固碳效应的主要影响因素,土壤全氮固碳效应对土壤全磷固碳效应的影响也很大。
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来源期刊
Eurasian Soil Science
Eurasian Soil Science 农林科学-土壤科学
CiteScore
2.70
自引率
35.70%
发文量
137
审稿时长
12-24 weeks
期刊介绍: Eurasian Soil Science publishes original research papers on global and regional studies discussing both theoretical and experimental problems of genesis, geography, physics, chemistry, biology, fertility, management, conservation, and remediation of soils. Special sections are devoted to current news in the life of the International and Russian soil science societies and to the history of soil sciences. Since 2000, the journal Agricultural Chemistry, the English version of the journal of the Russian Academy of Sciences Agrokhimiya, has been merged into the journal Eurasian Soil Science and is no longer published as a separate title.
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