水科学与工程技术2024,Issue(5) :9-11.DOI:10.19733/j.cnki.1672-9900.2024.05.03

基于指示克里格插值方法的土壤轻度盐渍化风险分析

Risk analysis of mild soil salinity based on Indicator Kriging Method

张高鹏 张文聪 张秀红 孙国华 王子茉
水科学与工程技术2024,Issue(5) :9-11.DOI:10.19733/j.cnki.1672-9900.2024.05.03

基于指示克里格插值方法的土壤轻度盐渍化风险分析

Risk analysis of mild soil salinity based on Indicator Kriging Method

张高鹏 1张文聪 1张秀红 2孙国华 3王子茉4
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作者信息

  • 1. 河北水利电力学院水利工程系,河北沧州 061001
  • 2. 河北省沧州市林业有害生物防治检疫站,河北沧州 061001
  • 3. 内蒙古巴彦淖尔市水文水资源勘测中心,内蒙古巴彦淖尔 015000
  • 4. 南开大学哲学院,天津 300071
  • 折叠

摘要

针对河套灌区土壤盐分变异性较高的问题,基于指示克里格插值方法,分析土壤盐渍化的时空风险变化.结果表明:研究区各时期0~100cm 土层土壤均属于轻度盐渍化且呈中等变异性;指示变异函数符合高斯模型且为中等空间自相关性,说明土壤盐分的空间变异是由结构性因素和随机性因素共同引起的.研究区北部轻度盐渍化风险大且分布集中,建议采用水利工程措施为主、农业生物措施为辅的综合治理措施.南部土地利用强度较高,人为农业活动较为频繁,应加强田间管理来防治土壤盐渍化.

Abstract

In response to the high variability of soil salinity in Hetao irrigation area,the indicator Kriging is used to analyze the spatiotemporal risk changes of soil salinization.The results showed that the soil in 0~100cm soil layer of the study area belonged to mild salinity and exhibited moderate variability at different stages;The indication that the variation function conforms to the Gaussian model and has moderate spatial autocorrelation indicates that the spatial variation of soil salinity is caused by both structural and stochastic factors.The risk of mild salinity in the northern part of the study area is high and concentrated.It is recommended to adopt a comprehensive management measure mainly based on water conservancy engineering measures and supplemented by agricultural biological measures.The land use intensity in the southern region is relatively high,and artificial agricultural activities are more frequent.Field management should be strengthened to prevent soil salinity.

关键词

河套灌区/灌排单元/指示克里格/土壤盐渍化

Key words

Hetao Irrigation District/drainage and drainage unit/Indicator Kriging/soil salinity

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基金项目

2024年度沧州市科技创新研究课题(CZKX2024487)

河北水利电力学院基本科研业务费专项资金(SYKY2208)

河北省大学生创新创业训练计划项目(S202310085041)

出版年

2024
水科学与工程技术
河北省水利学会 水利部河北水利水电勘测设计研究院

水科学与工程技术

影响因子:0.334
ISSN:1672-9900
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