首页|基于EM38-MK2大地电导率仪的宁夏青铜峡灌区剖面土壤盐分分布反演研究

基于EM38-MK2大地电导率仪的宁夏青铜峡灌区剖面土壤盐分分布反演研究

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宁夏青铜峡灌区普遍存在的原生和次生盐渍化现象严重制约了农业的可持续发展。为定量分析青铜峡灌区土壤盐分空间分布格局,提出利用EM38-MK2数据预测剖面土层土壤盐分空间分布的最优模型。采用一元线性回归、多元线性回归和逐步回归方法,研究青铜峡灌区EM38-MK2测量数据与剖面土层土壤盐分之间的解译模型。基于该模型,采用回归-克里金插值法探讨灌区剖面土层土壤盐分的空间分布格局。结果表明:①EM38-MK2大地电导率仪对浅层土壤电导率的响应表现出最佳性能,ECh0。75测定模式展现了良好的稳定性;②结合EM38-MK2与SR模型能够有效解析剖面土壤盐分分布;③青铜峡灌区土壤盐分显示出西北和东北区域较高而西部区域较低的空间分布特征,整体处于中度盐渍化水平,特别是在21~40 cm土层中盐分质量比最高,部分区域已达重度盐渍化,水盐迁移及淋洗沉积作用进一步使得该土层盐分显著积聚。
Inversion Study of Soil Salinity Distribution in the Qingtongxia Irrigation District Using EM38-MK2 Electromagnetic Conductivity Meter
The prevalent primary and secondary salinization in the Qingtongxia Irrigation District severely limits the sustainable development of agriculture.This study aims to propose an optimal model using EM38-MK2 data to predict soil salinity in the profile layers and quantitatively analyze the spatial distribution pattern of soil salinity.Univariate linear regression,multivariate linear regression,and stepwise regression methods were employed to investigate the interpretative models between EM38-MK2 measurement data and soil salinity in the profile layers of the Qingtongxia Irrigation District.Based on these models,a regression-kriging interpolation method was utilized to explore the spatial distribution pattern of soil salinity in the profile layers.The results showed that:① The EM38-MK2 electromagnetic conductivity meter demonstrated optimal performance in measuring the electrical conductivity of shallow soil layers,with the ECh0.75 measurement mode demonstrating good stability.② The combination of EM38-MK2 with the SR model effectively elucidated the distribution of soil salinity in the profile.③ Soil salinity in the Qingtongxia Irrigation District displayed a spatial distribution characterized by higher salinity in the northwest and northeast regions,while lower salinity was observed in the western region.The overall salinity level is moderate,particularly in the 21~40 cm soil layer,where the salinity content is highest,and some areas have severe salinization.Water and salt migration,along with leaching and deposition effects,further contribute to significant salt accumulation in this layer.

Qingtongxia Irrigation DistrictsoilsalinityEM38-MK2spatial distribution

宋阿维、刘雨星、高乾程、常凯、王相平、谢文萍、俞烜、姚荣江

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中国科学院南京土壤研究所 土壤与农业可持续发展国家重点实验室,江苏 南京 210008

湖北省十堰市气象局,湖北 十堰 442000

长江大学 农学院,湖北 荆州 434025

扬州大学 环境科学与工程学院,江苏 扬州 225001

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青铜峡灌区 土壤 盐分 EM38-MK2 空间分布

2024

农业科学研究
宁夏大学

农业科学研究

影响因子:0.671
ISSN:1673-0747
年,卷(期):2024.45(4)