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首页> 外文期刊>Journal of Water Resources and Ocean Science >Analyzing rainfall events and soil characteristics for water resources management in a canal irrigated area
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Analyzing rainfall events and soil characteristics for water resources management in a canal irrigated area

机译:分析降雨事件和土壤特性,以管理运河灌区的水资源

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Rainfall analysis is essential for water resources management and crop planning. An attempt has been made to analyse the rainfall of Daspalla region in Odisha, eastern India for prediction of monsoon and post-monsoon rainfall by using 6 different probability distribution functions, forecasting the probable date of onset and withdrawal of monsoon and finally crop planning for the region. Soil parameters were assessed for head, mid and tail reaches of the command area. Results revealed that, for prediction of monsoon and post-monsoon rainfall, Log Pearson Type-III and Gumbel distribution are found as the best fit probability distribution functions. The earliest and delayed most week of onset of rainy season was 20th SMW (14-20th May) and 25th SMW (18-24th June), respectively. Similarly, the earliest and delayed most week of cessation of rainy season was 39th SMW (24-30th September) and 47th SMW (19-25th November) respectively. The soils have the clay contents ranging from 29.6 to 48.8%. The bulk density ranged from 1.44 to 1.72 Mg.m-3 irrespective of different sites. The saturated hydraulic conductivity decreased significantly with soil depth due to greater clay contents in lower layers; whereas water retention at field capacity and PWP increased significantly with increase in soil depths. Soil organic carbon varied from 0.34 to 0.95%; it was the highest in the surface (0-15 cm) layer and then decreased down to the soil profile. The results of rainfall analyses and soil properties would help in management of rainfall and canal water in an effective way.
机译:降雨分析对于水资源管理和作物计划至关重要。尝试通过使用6种不同的概率分布函数分析印度东部奥里萨邦Dasp​​alla地区的降雨,以预测季风和季风后降雨,预测季风的发作和撤离日期,最后为该季的作物计划地区。评估了指挥区头,中和尾段的土壤参数。结果表明,为了预测季风和季风后降雨,Log Pearson III型和Gu​​mbel分布被认为是最佳拟合概率分布函数。雨季开始的最早和最晚的一周分别是20兆瓦(5月14日至20日)和25兆瓦(6月18日至24日)。同样,最早和最晚的雨季停止时间分别是第39个SMW(9月24日至30日)和第47个SMW(11月19日至25日)。土壤的粘土含量为29.6%至48.8%。堆积密度在1.44至1.72 Mg.m-3之间,与不同位置无关。饱和水力传导率随着土壤深度的增加而显着下降,这是由于下层的粘土含量增加所致。而随着土壤深度的增加,田间持水量和PWP显着增加。土壤有机碳含量从0.34到0.95%不等;它在表层(0-15厘米)最高,然后下降到土壤剖面。降雨分析和土壤特性的结果将有助于有效管理降雨和运河水。

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