Komal Qasim, S. Ali Shah, S. A. Soomro, A. G. Siyal, Irfan Ahmed
{"title":"EFFECT OF SALINE AND NON-SALINE WATER ON OKRA CROP PRODUCTION","authors":"Komal Qasim, S. Ali Shah, S. A. Soomro, A. G. Siyal, Irfan Ahmed","doi":"10.26480/bdwre.01.2021.24.29","DOIUrl":null,"url":null,"abstract":"Under the situation of acute water crises and the regular or occasional use of marginal to saline groundwater by the farming community to cultivate the crops, the research needs to be conducted on the use of marginal to saline groundwater based on the guidelines and strategies for the effective use be developed. In context of this, the experiment was conducted at the field research station of the laboratory of the Department of Land and Water Management (LWM) Faculty of Agricultural Engineering (FAE), Sindh Agriculture University (SAU) Tandojam during the year 2019. The experiment was arranged in a completely randomized design with three treatments of varying water qualities with three replications were deployed. The treatments were: W1 = non-Saline water (canal water) E.C= 1.0 dS m-1, W2 = Saline water (groundwater) EC= 4 dS/m-1and W3= Saline water (groundwater) EC= 6 dS/m-1. Okra crop was grown on ridges. The results showed that the soil EC decreased 0.76 dS/m-1 under T1, and increased 0.83 and 1.33 dS/m-1 under T2 and T3, respectively. The soil pH decreased by 0.29, 0.43, and 0.44 under T1, T2, and T3. The soil Mg increased 21.57, 22.11, and 27.03; soil SAR increased 6.15, 7.82, and 8.91; and soil ESP increased 6.51, 8.61, and 10.33 under T1, T2, and T3, respectively. The soil Ca decreased 1.34 under T1 treatment; and increased 0.30 and 10.28 under T2 and T3, respectively. The maximum yield of 18500 kg ha-1 was found with T1 followed by 17391 kg ha-1 with T2 and the lowest yield of 16836 kg ha-1 was found with T3. The highest water productivity of 1.91 kg m-3 was found with T1 treatment followed by 1.79 kg m-3 with T2 treatment and the lowest water productivity of 1.73 kg m-3 was found with T3 treatment.","PeriodicalId":141870,"journal":{"name":"Big Data in Water Resources Engineering (BDWRE)","volume":"143 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-09-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Big Data in Water Resources Engineering (BDWRE)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.26480/bdwre.01.2021.24.29","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
Under the situation of acute water crises and the regular or occasional use of marginal to saline groundwater by the farming community to cultivate the crops, the research needs to be conducted on the use of marginal to saline groundwater based on the guidelines and strategies for the effective use be developed. In context of this, the experiment was conducted at the field research station of the laboratory of the Department of Land and Water Management (LWM) Faculty of Agricultural Engineering (FAE), Sindh Agriculture University (SAU) Tandojam during the year 2019. The experiment was arranged in a completely randomized design with three treatments of varying water qualities with three replications were deployed. The treatments were: W1 = non-Saline water (canal water) E.C= 1.0 dS m-1, W2 = Saline water (groundwater) EC= 4 dS/m-1and W3= Saline water (groundwater) EC= 6 dS/m-1. Okra crop was grown on ridges. The results showed that the soil EC decreased 0.76 dS/m-1 under T1, and increased 0.83 and 1.33 dS/m-1 under T2 and T3, respectively. The soil pH decreased by 0.29, 0.43, and 0.44 under T1, T2, and T3. The soil Mg increased 21.57, 22.11, and 27.03; soil SAR increased 6.15, 7.82, and 8.91; and soil ESP increased 6.51, 8.61, and 10.33 under T1, T2, and T3, respectively. The soil Ca decreased 1.34 under T1 treatment; and increased 0.30 and 10.28 under T2 and T3, respectively. The maximum yield of 18500 kg ha-1 was found with T1 followed by 17391 kg ha-1 with T2 and the lowest yield of 16836 kg ha-1 was found with T3. The highest water productivity of 1.91 kg m-3 was found with T1 treatment followed by 1.79 kg m-3 with T2 treatment and the lowest water productivity of 1.73 kg m-3 was found with T3 treatment.
在水资源危机严重、农业社区经常或不定期使用边际含盐地下水进行作物种植的情况下,需要对边际含盐地下水的利用进行研究,并制定有效利用的指导方针和策略。在此背景下,该实验于2019年在信德省农业大学(SAU)坦多贾姆农业工程学院(FAE)土地和水管理系(LWM)实验室的实地研究站进行。试验采用完全随机设计,设置3个不同水质处理,重复3次。处理方法:W1 =非咸水(运河水)EC= 1.0 dS - m-1, W2 =咸水(地下水)EC= 4 dS/m-1, W3=咸水(地下水)EC= 6 dS/m-1。秋葵种植在山脊上。结果表明:土壤EC在T1处理下降低0.76 dS/m-1,在T2和T3处理下分别增加0.83和1.33 dS/m-1;在T1、T2和T3处理下,土壤pH分别降低0.29、0.43和0.44。土壤Mg分别增加21.57、22.11和27.03;土壤SAR分别增加6.15、7.82和8.91;土壤ESP分别增加6.51、8.61和10.33。T1处理下土壤Ca降低1.34;T2和T3分别增加0.30和10.28。T1的产量最高可达18500 kg ha-1,其次是T2的17391 kg ha-1, T3的产量最低为16836 kg ha-1。T1处理的水分生产力最高,为1.91 kg m-3, T2处理次之,为1.79 kg m-3, T3处理的水分生产力最低,为1.73 kg m-3。