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The #x201C;black waters#x201D; of Malaysia: Tracking water quality from the peat swamp forest to the sea

机译:马来西亚的“黑水域”:跟踪泥炭沼泽森林到海的水质

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Longitudinal water quality trends were assessed in the Tengi River system, Selangor State, Malaysia, as the water moved from a peat swamp forest, through different agricultural land uses, and finally through an urban area to the Straits of Malacca. Water draining from the peat swamp forest was dark in color due to its organic content and low in dissolved oxygen, pH, E. coli, calcium, nitrate, and ammonia. The normal diurnal pattern for water temperature was observed for the peat swamp forest drainage, but no diurnal pattern was evident in the dissolved oxygen data. The E. coli levels increased monotonically from the peat forest waters (0 colonies/100 mL) through the agricultural areas (100–2,000 colonies/100 mL) and the urban area (7,100 colonies/100 mL), and similarly pH increased along the same continuum. Dissolved oxygen increased from the peat swamp forest through the agricultural areas, but was lower in the urbanimpacted reach of the Tengi River.
机译:纵向水质趋势在腾河制度,马来西亚雪兰莪州的雪兰莪州,因为水从泥炭沼泽森林移动,通过不同的农业用地使用,最后通过城市地区到马六甲海峡。由于其有机含量和低于溶解的氧,pH,大肠杆菌,钙,硝酸盐和氨,因此从泥炭沼泽森林中排出的水是暗的。对于泥炭沼泽森林引流,观察到水温的正常昼夜图案,但在溶解的氧数据中没有昼夜模式明显。通过农业区域(100-2,000个菌落/ 100毫升)和城区(7,100块菌落/ 100mL)单调的大肠杆菌水平从泥炭林水(0个菌落/ 100毫升)单调增加,并类似地沿着相同的连续体。溶解氧通过农业领域从泥炭沼泽森林增加,但在腾都河的Urbanvicted Reach较低。

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