Studies on Rainfall-Runoff Relationship for Assessment of Rainwater Harvesting Potential under Marathwada Region

Ananya Mishra, M. Pendke, B. Bhuibhar, K. Dakhore, U. Khodke, D. Waskar
{"title":"Studies on Rainfall-Runoff Relationship for Assessment of Rainwater Harvesting Potential under Marathwada Region","authors":"Ananya Mishra, M. Pendke, B. Bhuibhar, K. Dakhore, U. Khodke, D. Waskar","doi":"10.56228/jart.2022.47308","DOIUrl":null,"url":null,"abstract":"The rainfall available in the watershed is key factor for determining the availability of water to fulfill the different demand mainly for agriculture, hydropower water supply, industry, etc. A watershed is that contributes runoff water to a common point Runoff is one of the important hydrologic variables used in most of the water resource applications. Runoff is the total surface flow from a given drainage area. Rainfall duration, intensity and aerial distribution influence the rate and volume of runoff. Watershed characteristics such as slope, shape and size, cover of soil and duration of rainfall have a direct effect on the peak flow and volume of runoff from any area (Chandler and Walker, 1998). Rainfall and runoff are significant constitute the sources of water for recharge of ground water in the watershed. Estimation of runoff in a watershed is very important to manage the water resources efficiently. Most of the part of the Marathwada region is comes under assured rainfall zone. The region receives mean annual rainfall of 880 mm. Rainfall in uncertain and erratic in this region and sometimes suffers from severe droughts. The rainfall data for Aurangabad, Parbhani and Nanded stations were collected from the Agro-meteorological station under VNMKV, Parbhani. Runoff was estimated using SCS curve number method considering the all parameters like soil type, vegetation etc. The rainfall runoff relationship was worked out for further planning of small water harvesting structures like farm ponds. The runoff potential for Aurangabad, Parbhani and Nanded station is found to be 20.07 %, 28.31 % and 31.69 % respectively, indicating a good scope for rainwater harvesting and thereby, many more rainwater harvesting structures can be constructed based on site specific conditions. A relation between rainfall and runoff for Aurangabad, Parbhani and Nanded stations were worked out as Y = 0.301X - 55.711 ( R2 value - 0.75), Y = 0.4043X - 88.882 (R2 value - 0.8687) and Y = 0.6018X - 209.2 (R2 value -0.9575) respectively. The linear rainfall-runoff relation obtained can be used for finding out runoff corresponding to any rainfall occurring in the area. The rainfall runoff relationship will be useful for determination of rainwater harvesting potential and its reuse for enhancing production potential of various rainfed crops.","PeriodicalId":418512,"journal":{"name":"Journal of Agriculture Research and Technology","volume":"5 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Agriculture Research and Technology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.56228/jart.2022.47308","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

The rainfall available in the watershed is key factor for determining the availability of water to fulfill the different demand mainly for agriculture, hydropower water supply, industry, etc. A watershed is that contributes runoff water to a common point Runoff is one of the important hydrologic variables used in most of the water resource applications. Runoff is the total surface flow from a given drainage area. Rainfall duration, intensity and aerial distribution influence the rate and volume of runoff. Watershed characteristics such as slope, shape and size, cover of soil and duration of rainfall have a direct effect on the peak flow and volume of runoff from any area (Chandler and Walker, 1998). Rainfall and runoff are significant constitute the sources of water for recharge of ground water in the watershed. Estimation of runoff in a watershed is very important to manage the water resources efficiently. Most of the part of the Marathwada region is comes under assured rainfall zone. The region receives mean annual rainfall of 880 mm. Rainfall in uncertain and erratic in this region and sometimes suffers from severe droughts. The rainfall data for Aurangabad, Parbhani and Nanded stations were collected from the Agro-meteorological station under VNMKV, Parbhani. Runoff was estimated using SCS curve number method considering the all parameters like soil type, vegetation etc. The rainfall runoff relationship was worked out for further planning of small water harvesting structures like farm ponds. The runoff potential for Aurangabad, Parbhani and Nanded station is found to be 20.07 %, 28.31 % and 31.69 % respectively, indicating a good scope for rainwater harvesting and thereby, many more rainwater harvesting structures can be constructed based on site specific conditions. A relation between rainfall and runoff for Aurangabad, Parbhani and Nanded stations were worked out as Y = 0.301X - 55.711 ( R2 value - 0.75), Y = 0.4043X - 88.882 (R2 value - 0.8687) and Y = 0.6018X - 209.2 (R2 value -0.9575) respectively. The linear rainfall-runoff relation obtained can be used for finding out runoff corresponding to any rainfall occurring in the area. The rainfall runoff relationship will be useful for determination of rainwater harvesting potential and its reuse for enhancing production potential of various rainfed crops.
马拉特瓦达地区雨水收集潜力评价的雨量-径流关系研究
流域可利用的降雨量是决定流域能否满足农业、水电、工业等不同用水需求的关键因素。流域是向一个共同点提供径流的地方。径流是大多数水资源应用中使用的重要水文变量之一。径流量是指来自某一流域的总地表流量。降雨的持续时间、强度和空中分布影响径流的速率和体积。斜坡、形状和大小、土壤覆盖和降雨持续时间等流域特征对任何地区的峰值流量和径流量都有直接影响(Chandler和Walker, 1998)。降雨和径流是流域地下水补给的重要水源。流域径流量估算对有效管理水资源具有重要意义。马拉特瓦达地区的大部分地区都处于降雨保证区。该地区年平均降雨量为880毫米。这个地区的降雨不稳定、不稳定,有时还会发生严重的干旱。奥兰加巴德站、帕尔巴尼站和南兰德站的降雨数据来自帕尔巴尼VNMKV农业气象站。综合考虑土壤类型、植被等参数,采用SCS曲线数法估算径流。研究了降雨径流关系,为进一步规划小型集水结构(如农场池塘)提供了依据。奥兰加巴德站、帕尔巴尼站和南兰德站的径流量分别为20.07%、28.31%和31.69%,具有较好的集雨空间,可根据场址具体情况建设更多集雨设施。奥兰加巴德站、帕尔巴尼站和南兰德站降雨与径流的关系分别为Y = 0.301X - 55.711 (R2值- 0.75)、Y = 0.4043X - 88.882 (R2值- 0.8687)和Y = 0.6018X - 209.2 (R2值-0.9575)。得到的降雨-径流线性关系可用于计算该地区任何降雨所对应的径流量。降雨径流关系将有助于确定雨水收集潜力及其再利用,以提高各种雨养作物的生产潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信