Impact of reclaimed water irrigation on soil salinity, hydraulic conductivity, cation exchange capacity and macro-nutrients

S. A. Alkhamisi, M. Al-Wardy, Mushtaque Ahmed, S. Prathapar
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引用次数: 3

Abstract

Field studies were conducted at Agriculture Research Center, Oman during the year 2010/2011 to monitor the impact of reclaimed water irrigation on soil physical and chemical properties after wheat, cowpea and maize cultivation (in rotation). Three different water sources (Groundwater (GW), desalinized water (DW), and Reclaimed Water (RW)) were used as the treatments in Randomized Completely Block Design (RCBD) with 3 blocks (replicates). Samples were taken from four depths (30, 45, 60 and 90 cm) after harvesting time of the three crops. Soil salinity (ECe) in all soil depths decreased with time. Organic carbon did not show significant difference between harvest timings of wheat and cowpea. Organic carbon increased with time in soil irrigated with reclaimed water. The saturated hydraulic conductivity of the soil, Ksat didn’t show significant difference among the water types and their interaction with soil depths. Total nitrogen was the highest after cowpea harvest in reclaimed water irrigation. The soil phosphorus and potassium were not affected by any of the three water irrigation types. The highest concentrations of phosphorus and potassium were found to be in the upper soil layers. Overall, no adverse impacts of reclaimed water irrigation were observed after growing three crops of rotation.
再生水灌溉对土壤盐分、导电性、阳离子交换量和常量养分的影响
2010/2011年度在阿曼农业研究中心进行了实地研究,监测再生水灌溉对小麦、豇豆和玉米轮作后土壤理化性质的影响。采用随机完全区组设计(RCBD),采用地下水(GW)、淡化水(DW)和再生水(RW) 3种不同水源作为处理,3个区组(重复)。在三种作物收获后,分别从30、45、60和90 cm四个深度取样。各土层深度土壤盐度(ECe)随时间的增加而降低。有机碳在小麦和豇豆收获期间无显著差异。再生水灌溉土壤有机碳随时间增加而增加。土壤饱和水导率Ksat在不同水类型及其与土壤深度的相互作用中无显著差异。再生水灌溉中,总氮在豇豆收获后最高。三种灌溉方式对土壤磷、钾均无显著影响。磷和钾的最高浓度在土壤的上层。总体而言,3季轮作后再生水灌溉无不良影响。
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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