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Prediction and validation of soil electromagnetic characteristics for application in landmine detection

机译:地雷探测中土壤电磁特性的预测与验证

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Factors controlling the distribution and intensity of soil magnetic susceptibility (MS) and electrical conductivity (EC) were investigated. The purpose was to determine the factors to be considered in predicting MS and EC characteristics of soils in landmine-affected areas and in developing effective landmine detection systems and strategies. Results indicate that knowledge of bedrock geology, soil weathering and transportation (wind and water) history is essential to predict soil MS and EC characteristics. These factors determine the distribution, concentration and mineral type (e.g., ferromagnetic and clay minerals) in soil. For example, fluctuating water tables in tropical climates could produce soils rich in ferromagnetic minerals at the surface, even though their source (bedrock) may have low iron content. Also, subsequent weathering may change these minerals to high or low MS values. Although high clay concentrations homogeneously distributed may not produce high soil EC values, a low clay content concentrated in a single layer may produce extremely high EC values. These suggest that bedrock geology, agricultural soil, air photo and airborne geophysical survey maps can be used for predicting soil MS and EC characteristics of landmine-affected areas. Laboratory and surficial geophysical surveys are techniques for use in validation.
机译:研究了控制土壤磁化率(MS)和电导率(EC)的分布和强度的因素。目的是确定在预测受地雷影响地区土壤的MS和EC特性以及开发有效的地雷探测系统和策略时应考虑的因素。结果表明,基岩地质,土壤风化和运输(风和水)的历史知识对于预测土壤的MS和EC特性至关重要。这些因素决定了土壤中的分布,浓度和矿物质类型(例如铁磁和粘土矿物质)。例如,在热带气候下,地下水位的波动可能会在地表产生富含铁磁性矿物的土壤,即使其来源(基岩)的铁含量可能较低。同样,随后的风化可能会将这些矿物质改变为高或低的MS值。尽管均匀分布的高粘土浓度可能不会产生较高的土壤EC值,但浓缩在单层中的低粘土含量可能会产生极高的EC值。这些表明,基岩地质,农业土壤,航空照片和航空地球物理勘测图可用于预测受地雷影响地区的土壤MS和EC特征。实验室和表面地球物理勘测是用于验证的技术。

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