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Erwin E. Van Nieuwenhuyse Jacqueline D. LaPerriere 《Journal of the American Water Resources Association》1986,22(1):91-99
ABSTRACT: Turbidity, total residues, settleable solids, vertical light extinction, and primary production were measured in mined and unmined streams located in the interior highlands of Alaska. Undisturbed streams had low turbidities (< 1 NTU), total residue concentrations averaging 120 mg 1?1, and undetectable settleable solids. During active mining, turbidity, total residues, and settleable solids levels in a moderately mined stream averaged 170 NTU, 201 mg 1?1, and < 0.1 ml 1?1, respectively. In a heavily mined stream, turbidity and total residues were two orders of magnitude higher than in unmined streams and settleable solids nearly always exceeded 0.2 ml 1?1. Vertical extinction coefficients and turbidity were positively correlated. In undisturbed streams gross primary productivity (g-O2m?2d?1) ranged from 0.20 shortly after spring breakup to a maximum of 1.20 in early fall. Productivity in the moderately mined stream was reduced by 50 percent while photosynthetic efficiency doubled. Primary production was undetectable in a heavily mined stream. Maximum standing crops of periphyton measured as chlorophyll a occurred in fall in an undisturbed stream after 13 weeks of exposure and ranged from 4.5 to 11.8 mg-chl a m?2. The highest chlorophyll a densities recorded in the moderately mined stream was 3.8 mg m?2, and no chlorophyl a was detected in the heavily mined stream. 相似文献
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黄河口水动力作用的最显著特点是径流方向(WE)和潮流方向(SN)近于垂直。这一特点有利于三角洲的横向扩展[1],但另一方面,由于沿岸流异常发育,加快了河口沉积速度,促进了拦门沙的发育,使河口处的河床抬高,泄流不畅,不利于黄河口外水下河道的自然下切延伸,最终诱发改道。米草生态工程可以通过防止泥沙沿岸搬运,降低海水含沙量,从而降低拦门沙的发育速度,保护黄河水下河道,最终起到降低河口变动频率,防治黄河改道的作用。 相似文献