首页> 外文期刊>Journal of the American Water Resources Association >Aquatic Plant and Dissolved Oxygen Changes in a Reference-Condition Prairie Stream Subjected to Experimental Nutrient Enrichments
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Aquatic Plant and Dissolved Oxygen Changes in a Reference-Condition Prairie Stream Subjected to Experimental Nutrient Enrichments

机译:参考营养条件下草原水流中水生植物和溶解氧的变化

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Effects of controlled nutrient additions on a prairie stream were studied using a before-after-control-impact paired design. The site is in a reference condition with low soluble nitrate (NO3) and phosphate (soluble reactive phosphorus [SRP]) in summer (3 mu g NO3-N/L, 4 mu g SRP/L). Nutrients were added to two reaches over the growing season at two levels (Low Dose - 39 mu g NO3-N/L and 4.4 SRP/L; High Dose - 119 mu g NO3-N/L and 15.6 mu g SRP/L). Continuously measured dissolved oxygen (DO) and changes in aquatic flora were compared to an upstream Control. Enrichment led microalgae and filamentous algae to increase in density, areal coverage, and thickness, and the magnitude of the changes were largely concordant with dosing (more in the High Dose); algal growth also suppressed macrophytes in the High Dose. Enrichment caused significant increases in diel DO swings whose magnitudes were consistent with dosing level. In the High Dose, benthic algae flourished in the growing season and then senesced en masse in fall. The decomposing algae led DO to crash (ca. 0 mg/L on the bottom), but DO impacts were out-of-sync with peak algal growth and photosynthesis, which occurred weeks earlier. This finding provides a plausible explanation as to why high DO delta in streams impacts aquatic life even when concurrently measured DO is not low. When DO crashed, DO was longitudinally patchy, some areas having low DO near the bottom, others near saturation. Geomorphology and exposure to wind may have caused this pattern.
机译:使用控制前-影响-后配对设计研究了受控营养物添加对草原河流的影响。在夏季,该站点处于参考状态,硝酸盐(NO3)和磷酸盐(可溶性反应性磷[SRP])低(3μg NO3-N / L,4μgSRP / L)。在生长季的两个阶段将营养添加到两个水平(低剂量-39μgNO3-N / L和4.4 SRP / L;高剂量-119μgNO3-N / L和15.6μgSRP / L) 。将连续测量的溶解氧(DO)和水生植物群落的变化与上游对照进行比较。富集导致微藻和丝状藻的密度,面积覆盖率和厚度增加,并且变化的幅度在很大程度上与剂量一致(大剂量时更多);藻类生长也抑制了大剂量的大型植物。浓缩导致diel DO摆动幅度显着增加,其幅度与剂量水平一致。在高剂量下,底栖藻类在生长期旺盛,然后在秋季大幅度降低。分解的藻类导致DO崩溃(底部约0 mg / L),但DO的影响与藻类生长和光合作用的峰值(几周前发生)不同步。这一发现提供了一个合理的解释,即即使同时测量的DO不低,河流中的高DO增量也会影响水生生物。当溶解氧崩溃时,溶解氧在纵向上是零散的,一些区域的底部附近溶解氧较低,另一些区域则接近饱和。地貌和暴露于风中可能导致了这种模式。

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