巴基斯坦半干旱区不同灌溉方式对盐碱地盐分的响应

Kamran Baksh Soomro, S. Alaghmand, M. M. Shaikh, S. Andriyas, A. Talei
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引用次数: 1

摘要

土壤盐度是半干旱区灌溉种植者面临的一个关键挑战。为了实现盐化,种植者需要有关盐的基础和盐在根区流动过程的信息。土壤盐分可以通过特殊的灌溉耕作方法来管理,包括灌溉计划,使盐通过根区浸出。本研究旨在研究巴基斯坦信德省半干旱地区盐碱地中的盐类运动。本试验于2017年夏季在盐渍化土地上进行,采用灌溉水T1 (7 d灌溉间隔)、T2 (14 d灌溉间隔)和T3 (21 d灌溉间隔)3种处理,灌溉水深度分别为10、9和8 cm。土壤质地为粉质粘壤土,电导率(EC)在7.73 ~ 20.69 dS/m之间。土壤pH值在7.89 ~ 8.04之间。双向方差分析的结果与EC和pH数据的统计检验结果一致,这些数据按天(7、14和21天)和按深度(10、9和8 cm)进行。土壤EC和pH的平均下降在间隔7 d和10cm深度,P<0.05。总的来说,研究结果表明,与14天和21天的灌溉间隔相比,7天的灌溉间隔在土壤剖面的盐淋失方面更有效。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Response of Salts in Saline Soil Using Different Irrigation Scheduling in Semi-Arid Zone of Pakistan
The salinity of soil is a crucial challenge for growers irrigating in semi-arid zones. To accomplish salinity, growers require information about salt's basis and processes of the salt mobility through the root zone. Soil salinity can be managed by exceptional irrigating farming practices including irrigation scheduling to leach down salts through the root zone. This study aimed at examining the salts movement in saline soil in a semi-arid region in Sindh, Pakistan. This field experiment was conducted during the summer of 2017 on a salt-affected land by using three irrigation treatments of canal water including T1 (7 day irrigation interval), T2 (14 day irrigation interval) and T3 (21 days irrigation interval) under 10, 9 and 8 cm depths of irrigation water, respectively. The texture of soil was silty clay loam having an electrical conductivity (EC) ranging from 7.73 to 20.69 dS/m. However, the pH of the soil ranged from 7.89 to 8.04. The findings of a two-way analysis of variance were consistent with the statistical examination of EC and pH data day- wise (7, 14 and 21 days) and depths-wise (10, 9 and 8 cm). Average reductions in the EC and pH of the soil were observed at 7 days interval and 10cm depth at P<0.05. Overall, the findings exhibited that, compared to the 14 and 21 day intervals, a 7 day irrigation interval was more effective in terms of salt leaching from the soil profile.    
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