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控制排水条件下排水沟中磷素浓度衰减规律研究

he attenuation law of the P content and weight under controlled drainage in drain ditch

中文摘要英文摘要

摘要:磷素是湖泊水体富营养化的限制性因子,稻田排水是磷素损失的主要途径。本文通过试验分析了在控制排水条件下,排水沟中磷素浓度的衰减规律及不同形态磷素组分随时间的变化规律;分析了排水沟不同深度水层中磷素存在形态及其衰减规律。结果表明,控制排水条件下控制稻田排水在沟中滞蓄3-5天,对磷有较好的去除效果,磷素的损失以可溶磷为主;排水沟中磷素浓度与深度正相关并且随滞蓄时间延长可溶磷所占比例增大;可溶磷DP占总磷TP的比例与水层深度负相关。

Phosphorus plays a key role in lake eutrophication. Rice fields drainage is the main way of phosphorus loss. The Attenuationlaw of the P content and weight and the change law of different forms of phosphorus varying with time were analyzed. The exsisting form and the attenuation law of Phosphorus at different water layers were also studied. The results showed that, storing rice fields drainage in drain ditch for 3 to 5 days can achieve very good effect to remove Phosphorus. Water_soluble phosphates was the main loss. It also showed that there was a positive correlation between the P content and weight and depth. the rate of the water_soluble phosphates is increased with the passage of time.the rate of water_soluble phosphates was negatively correlated with water depth.

张晓柳

农业科学研究环境污染、环境污染防治

控制排水排水沟

controlled drainagephosphorusdrain ditch

张晓柳.控制排水条件下排水沟中磷素浓度衰减规律研究[EB/OL].(2009-12-23)[2025-08-02].http://www.paper.edu.cn/releasepaper/content/200912-879.点此复制

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