马来西亚的“黑水”:追踪从泥炭沼泽森林到海洋的水质

K. Irvine, S. Vermette, F. Mustafa
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引用次数: 17

摘要

在马来西亚雪兰莪州的腾吉河系统中,纵向水质趋势进行了评估,因为水从泥炭沼泽森林流过不同的农业用地,最后通过城市地区进入马六甲海峡。从泥炭沼泽森林排出的水由于其有机含量和溶解氧、pH值、大肠杆菌、钙、硝酸盐和氨的含量低而呈深色。泥炭沼泽森林水系的水温具有正常的日变化规律,溶解氧数据没有明显的日变化规律。从泥炭森林水体(0菌落/100 mL)到农业区(100- 2000菌落/100 mL)和城市地区(7100菌落/100 mL),大肠杆菌水平单调增加,pH值也沿同一连续体增加。从泥炭沼泽森林到农业区溶解氧增加,但在腾吉河受城市影响的河段溶解氧较低。
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The “black waters” of Malaysia: Tracking water quality from the peat swamp forest to the sea
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 urban-impacted reach of the Tengi River.
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