首页> 外文期刊>Fresenius environmental bulletin >TEMPORAL AND SPATIAL CHARACTERISTICS OF PHOSPHORUSFRACTIONS UNDER LONG-TERM WASTEWATER IRRIGATION IN TONGLIAO CITY, CHINA
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TEMPORAL AND SPATIAL CHARACTERISTICS OF PHOSPHORUSFRACTIONS UNDER LONG-TERM WASTEWATER IRRIGATION IN TONGLIAO CITY, CHINA

机译:通辽市长期污水灌溉下磷素的时空特征

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The irrigation reuse of municipal and industrial effluents conserves freshwater resources and avoids direct nutrient discharges to surface waters. The sustainability of agricultural reuse programs, however, may be challenged by changes in phosphorus (P) availability. To understand the characteristics of P fractions, 130 soil samples were collected around an irrigation drain in May 2009, at the beginning of the growing season. In the study area, total phosphorus (TP) varied from 302.32 to 716.30 mg/kg, residual P varied from18.21 to 126.08 mg/kg, and Olsen P varied from 0.71 to 90.04 mg/kg. The relative abundance detected for nearly every P fraction followed the order Ca-P>residual P>NaOH-Po≈NaOH-Pi>KCl-P. Although NaOH-Pi and most of the Ca-P fractions contributed markedly to P availability, NaOH-Po and Ca-P contributed more to residual P when different phosphate sources were added to the soil. However, the available P in the studied soils represented only 5.5% of the TP, which was inadequate for the growth and development of crops. The influence of wastewater irrigation differs significantly at different depths. Wastewater irrigation is favorable to the transformation of stable P (NaOH-Po and Ca-P) into available P (NaOH-Pi), and cancause an increase in residual P in the shallow layer (0- 60 cm), as well as an increase in TP in the middle layer (60- 110 cm). However, wastewater and groundwater irrigation is beneficial to the increase in soil P concentration in the deep layer (110-170 cm). These effects may depend on soil properties, water cycles and biological processes, among other factors.
机译:市政和工业废水的灌溉再利用可以节省淡水资源,并避免养分直接排放到地表水中。但是,农业重复利用计划的可持续性可能会受到磷(P)利用率变化的挑战。为了了解P组分的特征,在生长季节开始时,2009年5月在灌溉排水渠附近收集了130个土壤样品。在研究区域,总磷(TP)从302.32到716.30 mg / kg不等,残留磷从18.21到126.08 mg / kg不等,Olsen P从0.71到90.04 mg / kg不等。几乎每个P组分的相对丰度都遵循Ca-P>残留P>NaOH-Po≈NaOH-Pi> KCl-P的顺序。尽管NaOH-Pi和大多数Ca-P组分对磷的有效性有显着贡献,但是当向土壤中添加不同的磷酸盐源时,NaOH-Po和Ca-P对残留磷的贡献更大。但是,研究土壤中的有效磷仅占总磷的5.5%,这不足以满足作物的生长发育。在不同深度,废水灌溉的影响差异很大。废水灌溉有利于将稳定的P(NaOH-Po和Ca-P)转化为有效P(NaOH-Pi),并且可能导致浅层(0-60 cm)中残留的P增加,并且中间层(60-110厘米)的TP增加。但是,废水和地下水灌溉有利于增加深层(110-170 cm)中的土壤P浓度。这些影响可能取决于土壤特性,水循环和生物过程以及其他因素。

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