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Effect of Irrigation Water Quality on the Leaching and Desorption of Phosphorous from Soil

机译:灌溉水质对土壤中磷的淋溶与解吸的影响

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Knowledge of the rate of decrease of nutrients from soils resulting from poor water quality application is essential for long-term planning of crop production while minimizing the impact on groundwater quality. In this study, we examined the effect of Ca2+ concentration of irrigation water on phosphorus (P) leaching and kinetic release in columns of sandy soil. Phosphorous sorption in the presence of CaCl2 solutions with Ca2+ concentrations of 3, 5, 10, and 15 mM CaCl2 was determined to understand the transport and leaching of P in the sandy soil. The geochemical Visual MINTEQ was used to calculate saturation indices. A considerable number of leachate samples contained P at concentrations that could cause eutrophication. Total P leached from soil due to application of different CaCl2 solutions ranged from 1.7 to 1.8 kg ha(-1) after 20 pore volumes had passed through the soil. Comparison of the leaching experiments results with the kinetic desorption data indicated that leaching removed on average 50 times less P than cumulative P desorbed by successive extractions with different CaCl2 solutions. Leaching in presence of different CaCl2 solutions was controlled by rate-limited dissolution of calcium hydroxyappatite and beta-tricalcium phosphate.
机译:认识到因水质不佳而导致土壤养分减少的速率对于长期计划农作物生产同时最小化对地下水质量的影响至关重要。在这项研究中,我们研究了灌溉水中Ca2 +浓度对沙质土壤中磷(P)淋溶和动力学释放的影响。确定存在于CaCl2溶液中的Ca2 +浓度分别为3、5、10和15 mM CaCl2时的磷吸附,以了解P在沙质土壤中的运输和浸出。地球化学Visual MINTEQ用于计算饱和度指数。大量渗滤液样品中的P含量可能导致富营养化。在20个孔体积穿过土壤后,由于施用不同的CaCl2溶液而从土壤中浸出的总磷在1.7至1.8 kg ha(-1)之间。浸出实验结果与动力学解吸数据的比较表明,浸出所除去的P平均比用不同CaCl2溶液连续萃取所解吸的累积P少50倍。在不同CaCl2溶液存在下的浸出是通过限制羟基磷灰石钙和β-磷酸三钙的速率限制溶解来控制的。

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