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Effect of tree roots on water infiltration rate into the soil

机译:树根对水分渗入土壤的影响

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To study the effect of tree roots on increasing water infiltration in soil and also to determine and assess the coefficients of different infiltration models, some infiltration tests were performed in three tree plantation areas in Badjgah, Fars province with different soil textures (clay loam for pear plantation, sandy loam for grape plantation, loamy sand for pine trees). In each plantation, four double rings were installed, whereas two double rings were placed under the tree in two sides of the tree truck with 50 cm distance and the other two double rings were placed on open space between the trees. Vertical infiltration of water into the soil was measured and the coefficients of five models of infiltration (i.e. Kostiakov, Kostiakov-Lewis, Philip, Soil Conservation Service (SCS) and Horton) were assessed. Furthermore, soil texture and initial soil water content were determined in these points. Results showed that all models accurately fitted to the measured values. The infiltration rate under the trees was higher than those between the trees due to the occurrence of roots and root channels that improved the rate of infiltration of water into the soil. The 180-minute infiltration under the trees increased 69% and 354% in loamy sand and clay loam, respectively compared with those on open space between the trees.
机译:为了研究树根对增加土壤水分入渗的影响以及确定和评估不同入渗模型的系数,在法斯省巴德加的三个具有不同土壤质地的人工林中进行了一些入渗试验(梨壤土)人工林,葡萄种植用沙质壤土,松树种植用沙质壤土)。在每个种植园中,都安装了四个双环,而两个双环则被放置在树车的两侧,距树木50厘米(50厘米),另外两个双环被放置在树木之间的空地上。测量了水在土壤中的垂直渗透,并评估了五个渗透模型(即Kostiakov,Kostiakov-Lewis,Philip,土壤保护局(SCS)和Horton)的系数。此外,在这些点上确定了土壤质地和初始土壤含水量。结果表明,所有模型均准确地符合测量值。树木和树木之间的入渗率高于树木之间,这是由于根部和根部通道的出现提高了水对土壤的入渗率。与两棵树之间的空地相比,在壤土下180分钟的渗透率在壤土和壤土中分别增加了69%和354%。

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