马来西亚霹雳州武吉美拉水库悬浮泥沙和磷收支及营养状况

Sumayyah Aimi Mohd Najib, W. Ismail, M. Omar
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引用次数: 6

摘要

武吉美拉水库(BMR)是马来西亚51个水库之一。BMR是最古老的水库,建于20世纪初,最初用于储存灌溉用水,但现在它的功能也包括防洪和供水。目前,上游流域的土地利用变化和周边活动将侵蚀物质和化学物质带入水库,对水库构成了威胁。随着水库沉积和富营养化的加速,悬浮沉积物以及进入BMR的养分通量对水库的威胁越来越大。本文讨论了2008年3月至2009年4月开展的BMR研究,以评估南池湖的水质状况,并确定了南池湖的沉积物和总磷(TP)流入量。据估计,大约2,900 t年−1的悬浮泥沙通量来自北池湖(18%),12,900 t年−1来自库劳河主要入口(占BMR总输入的82%)。在这些总泥沙输入(近15,800 t)中,约有5,600 t(36%)的总泥沙流入被截留在BMR中。TP年流入量约为18.8 t,约7 t(37%)被困在储层中。BMR中沉积物和总磷的储存量影响湖泊的水质,因此湖泊的平均营养状态为富营养化(TSI为54.4),与高生产力相关。水库输沙量的增加影响了水库容量,雨季水库下游洪水频发,富营养化导致湖泊水质恶化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Suspended sediment and phosphorus budget and trophic status of Bukit Merah Reservoir, Perak, Malaysia
Abstract Bukit Merah Reservoir (BMR) is one of the 51 impoundments in Malaysia. BMR is the oldest reservoir built in the early 1900s originally to store water for irrigation, but nowadays its functions include also flood control and water supply. Nowadays, it is threatened by land use change in the upper catchments and surrounding activities, which feeding eroded material and chemicals into the reservoir. Suspended sediment, as well as, nutrient fluxes into BMR are becoming an increasing threat to the reservoir, as its sedimentation and eutrophication accelerate. This paper discusses our study on the BMR carried out between March 2008 and April 2009 to assess the water quality status, and to determine the sediment and Total Phosphorus (TP) influx into the south pool lake. An estimated amount of suspended sediment fluxes of about 2,900 t year−1 came from the north pool lake (18%) and 12,900 t year−1 from the main Kurau River inlet (82% of the total input to the BMR). Of these total sediment input (nearly 15,800 t) about 5,600 t (36%) of the total sediment influx was trapped in the BMR. TP influx was about 18.8 t year−1 and about 7 t (37%) was trapped in the reservoir. The amount sediment and TP stored in the BMR affect the water quality of the lake, therefore the mean trophic state of the lake is eutrophic (TSI of 54.4) related to high productivity. Increasing sediment input into the reservoir has affected the reservoir volume and frequent flooding down-stream of the reservoir during rainy seasons, while eutrophication has caused the lake water quality deterioration.
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