水资源保护
水資源保護
수자원보호
WATER RESOURCES PROTECTION
2013年
6期
80-84
,共5页
水资源调度%水利分片%调度方案优化%上海市
水資源調度%水利分片%調度方案優化%上海市
수자원조도%수리분편%조도방안우화%상해시
water resources scheduling%water conservancy regionalization%scheduling scheme optimization%Shanghai City
为提高水资源调度改善水质效果,利用黄浦江水系、崇明岛河网水量水质模型,在分析评估上海市水资源调度现状效果的基础上,从引排水口门配置、水闸开启方式、水位控制条件等方面考虑,研究分片水资源调度优化方案。通过引排水量大小、水质改善效果等多方案分析比较,提出了分片水资源调度优化方案。结果表明:分片COD平均浓度改善3.1%~16.9%;分片NH3-N平均浓度改善3.4%~28.1%。 COD浓度为:劣吁类水的河网面积减少37.1%,Ⅲ类水的河网面积增加33.4%;NH3-N浓度为劣吁类水的河网面积减少9.4%,Ⅳ~Ⅲ类水的河网面积增加25.9%~31.0%。
為提高水資源調度改善水質效果,利用黃浦江水繫、崇明島河網水量水質模型,在分析評估上海市水資源調度現狀效果的基礎上,從引排水口門配置、水閘開啟方式、水位控製條件等方麵攷慮,研究分片水資源調度優化方案。通過引排水量大小、水質改善效果等多方案分析比較,提齣瞭分片水資源調度優化方案。結果錶明:分片COD平均濃度改善3.1%~16.9%;分片NH3-N平均濃度改善3.4%~28.1%。 COD濃度為:劣籲類水的河網麵積減少37.1%,Ⅲ類水的河網麵積增加33.4%;NH3-N濃度為劣籲類水的河網麵積減少9.4%,Ⅳ~Ⅲ類水的河網麵積增加25.9%~31.0%。
위제고수자원조도개선수질효과,이용황포강수계、숭명도하망수량수질모형,재분석평고상해시수자원조도현상효과적기출상,종인배수구문배치、수갑개계방식、수위공제조건등방면고필,연구분편수자원조도우화방안。통과인배수량대소、수질개선효과등다방안분석비교,제출료분편수자원조도우화방안。결과표명:분편COD평균농도개선3.1%~16.9%;분편NH3-N평균농도개선3.4%~28.1%。 COD농도위:렬우류수적하망면적감소37.1%,Ⅲ류수적하망면적증가33.4%;NH3-N농도위렬우류수적하망면적감소9.4%,Ⅳ~Ⅲ류수적하망면적증가25.9%~31.0%。
In order to improve water quality through water resources scheduling, the river network quantity and quality models of the Huangpu River network and the Chongming Island river network were used in this study. Based on the analysis and assessment of current effects of water resources scheduling in Shanghai City, the optimization schemes of water resources regionalization scheduling were studied, considering the configuration of diversion and drainage water gates, the opening and closing of water gates, and the water level controlling conditions. Through comparison of different schemes with different amounts of water diversion and drainage, and different water quality improvement effects, optimized water resources regionalization scheduling schemes were established and their effects were identified. The results show that, using the optimized schemes, the concentration of COD decreased by 3.1% to 16.9% on average, and the concentration of NH3-N decreased by 3.4% to 28.1%on average. The river network area where the concentration of COD was inferior to class V decreased by 37.1%, and the area where the concentration of COD was at class III increased by 33.4%. The river network area where the concentration of NH3-N was inferior to class V decreased by 9.4%, and the area where the concentration of NH3-N was between class III and IV increased by 25.9 % to 31.0%.