淮安市土壤pH时空变化特征及影响因素
作者:
作者单位:

(江苏省地质调查研究院,自然资源部国土(耕地)生态监测与修复工程技术创新中心,江苏 南京 210018)

作者简介:

李文婷(1990-),硕士,工程师,主要从事土壤地球化学调查。E-mail:958151585@qq.com。

基金项目:

基金项目:江苏省地质勘查专项基金项目(苏财建[2018]96号);江苏省地质勘查基金项目(苏财资环[2022]27号);江苏省自然资源科研课题(2024012)。


Spatiotemporal variation characteristics and influencing factors of soil pH in Huai’an city
Author:
Affiliation:

(Geological Survey of Jiangsu Province,Technology Innovation Center of Ecological Monitoring & Restoration Project on Land(Arable),Ministry of Natural Resources,Nanjing Jiangsu 210018)

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    摘要:

    对淮安市2004、2019年土壤地球化学调查数据进行分析,深入探讨土壤pH空间变异特征及其影响因素。结果表明,2019年研究区土壤pH值范围是4.66~9.46,均值为7.95,整体表现为南低北高,变异系数为0.095,属于弱空间变异性。地统计学分析结果表明,2004、2019年研究区土壤pH的变异函数的最优理论模型均为指数模型,块金系数分别为0.283和0.352,表明受人为因素和结构性因素共同影响,土壤pH值具有中等程度的空间相关性,冷热点分析结果显示,2019年较2004年土壤pH高值区明显增多,土壤pH低值区范围进一步扩大,空间集聚分布更显著。相关分析表明,研究区土壤pH值空间变异的主要控制因素为地貌类型和土壤类型,分别能独立解释研究区40.9%和21.7%的土壤pH值空间变异。此外,土壤pH与钙含量呈显著正相关,与氮、硫、有机质含量呈显著负相关。近15年来研究区黄泛区土壤出现轻微碱化现象,洪泽湖泛滥平原区、里下河浅洼平原区土壤出现酸化现象,需要采取相应措施,调控土壤pH。

    Abstract:

    The geochemistry survey analysis was conducted on the soil samples from the Huai’an city in the years of 2004 and 2019,to explore the spatial variation characteristics and influencing factors of soil pH. The results showed that the soil pH value ranged from 4.66 to 9.46 in the study area in 2019,with an average of 7.95. The overall performance was low in the south and high in the north,the coefficient of variation is 0.095,indicating weak spatial variability. The geostatistical analysis results indicated that the optimal theoretical models for the variation function of soil pH were both exponential models in the study area in 2004 and 2019,with block gold coefficients of 0.283 and 0.352,respectively,it indicated that soil pH values had a moderate spatial correlation due to the combined influence of human and structural factors. The analysis results of cold and hot spots showed that,in 2019,there was a significant increase in areas with high soil pH values compared to 2004,and the range of areas with low soil pH values further expanded,with more significant spatial clustering distribution. Correlation analysis showed that the main controlling factors for the spatial variation of soil pH values in the study area were geomorphic type and soil type,which could independently explain 40.9% and 21.7% of the spatial variation of soil pH values in the study area,respectively. In addition,soil pH was significantly positively correlated with calcium content,and significantly negatively correlated with nitrogen,sulfur,and organic matter content. In the past 15 years,the soil of the Yellow River floodplain in the research area has slightly alkalized,and the soil of the Hongze Lake floodplain and low-lying plain area of Lixia River has slightly acidified. Corresponding measures need to be taken to regulate the soil pH.

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李文婷,黄顺生,许伟伟,任静华,崔晓丹,刘玮晶.淮安市土壤pH时空变化特征及影响因素[J].中国土壤与肥料,2025,(1):1-14.

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  • 收稿日期:2024-06-25
  • 录用日期:2024-08-10
  • 在线发布日期: 2025-03-21
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