青海省湖竹县土壤有机质和全氮空间变异特征及其影响因素

Bicheng Zhang, Lele Niu, Tianzhong Jia, X. Yu, D. She
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引用次数: 4

摘要

青藏高原土壤有机质(SOM)和土壤全氮(STN)是一个值得关注的问题。本研究分析了青藏高原土壤有机质和土壤氮的空间分布特征,并确定了影响因子,为青藏高原耕地保护和可持续农业战略的制定提供依据。在青海省呼竹县0 ~ 20 cm土层共采集土壤样品120份。采用传统的统计学和地统计学方法分析了SOM和STN的空间分布;利用地理探测器(GeoDetector)探索影响空间变异的因素。SOM和STN浓度分别为6.92 ~ 44.57和0.52 ~ 2.54 g/kg。Cokriging插值图显示,研究区SOM和STN浓度具有相似的空间分布格局,从东北向西南递减。GeoDetector结果显示,土壤类型、年累积降水量和海拔高度是影响土壤有机质和地表氮空间变异的主要因子,其解释能力在38.4% ~ 59.5%之间。双因子交互作用增强了SOM和STN空间变异的解释力。研究结果可为保护性耕作和精准农业提供参考。
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Spatial variability of soil organic matter and total nitrogen and the influencing factors in Huzhu County of Qinghai Province, China
ABSTRACT The soil organic matter (SOM) and soil total nitrogen (STN) is a significant concern in Qinghai–Tibet Plateau, China. This study analysed the spatial distribution of SOM and STN and determined their influencing factors to support the conservation of cultivated soil and development of sustainable agricultural strategies in the Plateau. In total, 120 soil samples were collected from the 0–20-cm soil layer in Huzhu County, Qinghai Province. Traditional statistical and geostatistical methods were used to analyse the spatial distribution of SOM and STN; a geographical detector (GeoDetector)was used to explore the factors influencing the spatial variation. The SOM and STN concentrations were 6.92–44.57 and 0.52–2.54 g/kg, respectively. The Cokriging interpolation map showed a similar spatial distribution pattern for SOM and STN concentrations, which decreased from the northeast to southwest directions in the study area. GeoDetector results revealed that the three primary factors influencing the spatial variability of SOM and STN were soil type, annual accumulated precipitation and elevation, with their explanatory power ranging between 38.4% and 59.5%. Two-factor interactions enhanced the explanatory power of the spatial variability of SOM and STN. The research results provide a reference for conservation tillage and precision agriculture.
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