A Laboratory Watershed Model to Study the Effect of Rainfall Intensity and Soil Surface Slope on Surface Runoff Rate of Karbala Desert Soil

Q3 Earth and Planetary Sciences
Ayoob Al-Janabi, Riyadh Al-Saadi, Husam Alwan
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Abstract

Precipitation generating surface runoff is very important in various water resources development and management activities such as flood control and management, irrigation scheduling, irrigation design, and drainage networks. The aim of this study is to indicate the effect of rainfall intensity and soil surface slope on the surface runoff rate of Karbala desert soil. This study was conducted on the soil of the Karbala desert in Iraq, located between the provinces of Karbala and Najaf, extended from the longitude 32o44'186'' E and latitude 44o100'960''N. In this study, a laboratory watershed model was designed and constructed to be used to examine surface runoff of the Karbala desert soil and other hydrological properties, under the influence of different precipitation intensities (1.83 cm/min, 1.67 cm/min, 0.9 cm/min, and 0.64 cm/min) and different slopes of the soil surface (0.0 %, 2.0 %, 3.3 %, and 6.7 %). A Gene Expression Programming model was used to develop an equation of the surface runoff rate for the Karbala desert soil. The results showed that the rate of surface runoff increased with increasing rainfall intensity. The highest surface runoff rate of 101.53 cm/hr was obtained when the rainfall intensity was 1.83 cm/min, while at the rainfall intensity of 0.64 cm/min, the highest value of surface runoff rate of 31.17 cm/hr was obtained. The results also showed that the slope of the soil surface has a clear effect on the surface runoff rates. The highest value of surface runoff rate of 96.82 cm/hr was obtained when the slope of the soil surface was 0.0%, while at the slope of the soil surface of 6.7%, the highest value of surface runoff rate of 101.53 cm/hr was obtained. According to the simulation results, the surface runoff rate equation created using the Gene Expression Programming model did a great job of predicting the Karbala desert soil surface runoff, with a coefficient of determination R2 equal to 0.8812 for training and 0.8155 for testing.
研究降雨强度和土壤表面坡度对卡尔巴拉沙漠土壤地表径流速率影响的实验室流域模型
降水产生的地表径流在防洪管理、灌溉调度、灌溉设计和排水管网等各种水资源开发和管理活动中非常重要。本研究旨在说明降雨强度和土壤表面坡度对卡尔巴拉沙漠土壤地表径流率的影响。本研究的对象是伊拉克卡尔巴拉沙漠的土壤,位于卡尔巴拉省和纳杰夫省之间,东经 32o44'186'',北纬 44o100'960''。本研究设计并构建了一个实验室流域模型,用于研究卡尔巴拉沙漠土壤在不同降水强度(1.83 厘米/分钟、1.67 厘米/分钟、0.9 厘米/分钟和 0.64 厘米/分钟)和不同土壤表面坡度(0.0%、2.0%、3.3% 和 6.7%)影响下的地表径流及其他水文特性。使用基因表达编程模型为卡尔巴拉沙漠土壤建立了地表径流速率方程。结果表明,地表径流量随着降雨强度的增加而增加。降雨强度为 1.83 厘米/分钟时,地表径流率最高,为 101.53 厘米/小时;降雨强度为 0.64 厘米/分钟时,地表径流率最高,为 31.17 厘米/小时。结果还表明,土壤表面的坡度对地表径流率有明显的影响。当土壤表面坡度为 0.0% 时,地表径流速率的最高值为 96.82 厘米/小时;当土壤表面坡度为 6.7% 时,地表径流速率的最高值为 101.53 厘米/小时。根据模拟结果,利用基因表达编程模型创建的地表径流率方程在预测卡尔巴拉沙漠土壤地表径流方面表现出色,训练和测试的判定系数 R2 分别为 0.8812 和 0.8155。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Iraqi Geological Journal
Iraqi Geological Journal Earth and Planetary Sciences-Geology
CiteScore
1.80
自引率
0.00%
发文量
152
审稿时长
7 weeks
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