Soil Properties Study for the Western Side of Kut City, Iraq

Noor Hmood, M. Shamkhi
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Abstract

Soil properties checks and classification are an important part of any engineering project as they directly affect buildings as well as agriculture and others. The research aims to create an integrated database for soil properties in the study area, which is the western side of the city of Kut, to know its relationship to groundwater in the region. Laboratory tests were conducted for five soil samples from the Bar Drilling sites to monitor the movement of groundwater in the area. Soil samples were taken when drilling and upon reaching the groundwater level, which was approximately 6 meters sieve analysis, hydrometer, specific gravity, and hydraulic conductivity were also conducted, as well as the content of chlorides and sulfates in the soil was calculated.  For classifying testure of the soil, the triangle of US agriculture department was utilized, soil can be divided into groups by this triangle based on clay, silt and sand proportion.  Results of examination of soil texture  showed that the soil in the first was Clay loam and the second point was Silty Clay loam and in the third point, it was sandy clay loam, while in the fourth point it was silty clay loam and it was in the fifth point silt loam As shown in Table 1. The specific gravity was measured in the field, and the lowest value was 2.65 in the third well, while the highest value was 2.70 in the fifth well. The hydraulic conductivity of the five well points was calculated and was close to each other and considered as an average value of hydraulic conductivity equal to 0.013522. The content of chlorides and sulfates in the soil was calculated due to its importance in knowing the chemical properties. The results showed that the value of the chlorides ranged between (0.154 - 1.72) %, while the values of the sulfate content in the soil ranged between (0.930 - 3.11) %.
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伊拉克库特市西部土壤性质研究
土壤性质检查和分类是任何工程项目的重要组成部分,因为它们直接影响到建筑物以及农业和其他方面。这项研究的目的是在库特市西侧的研究区域建立一个土壤特性的综合数据库,以了解其与该地区地下水的关系。为监测该地区地下水的移动情况,对从沙洲钻探地点采集的5个土壤样本进行了实验室测试。钻孔时和到达地下水位时取土样,约6米进行筛析、比重计、比重、导水率等,并计算土壤中氯化物和硫酸盐的含量。为了对土壤进行分类,使用了美国农业部的三角形,根据粘土、粉砂和砂土的比例,可以将土壤分成不同的组。土壤质地检测结果显示,第1点为粘壤土,第2点为粉质粘壤土,第3点为砂质粘壤土,第4点为粉质粘壤土,第5点为粉质壤土,如表1所示。现场测量比重,第三口井比重最小,为2.65,第五口井比重最大,为2.70。计算了5个井点的水力导电性,它们的导电性比较接近,取平均值0.013522。计算土壤中氯化物和硫酸盐的含量,因为它对了解土壤的化学性质很重要。结果表明,土壤中氯化物含量在(0.154 ~ 1.72)%之间,硫酸盐含量在(0.930 ~ 3.11)%之间。
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