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Dynamics of nitrogen, phosphorus, algal biomass, and suspended solids in an artificial lentic ecosystem and significant implications of regional hydrology on trophic status

机译:人工晶状体生态系统中氮,磷,藻类生物量和悬浮固体的动态以及区域水文学对营养状况的重大影响

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Chemical and biological parameters were analyzed to examine how regional hydrological fluctuations influence water quality of a artificial lentic ecosystem over a two-year period. The intensity of seasonal monsoon rain accounted for most of annual inflow and discharge and influenced flow pathway (interflow vs. overflow), resulting in a modification of chemical and biological conditions. Sharp contrasting interannual hydrology of intense vs. weak monsoon occurred during the study. The intense monsoon disrupted thermal stratification and resulted in ionic dilution, high TP and high inorganic solids (NVSS) in the headwater reach. The variation of NVSS accounted 75% of TP variation (slope = 4.14, p < 0.01, n = 48). Regression analysis of residual chlorophyll-a (Chl) versus flushing rate indicated that short hydraulic retention time and high mineral turbidity affected algal growth in the headwater reach during summer monsoon. In contrast, severe drought during weak monsoon produced strong thermal stratification, low inorganic solids, high total dissolved solids (TDS), and low TP in the entire system. In addition, Chl concentrations were controlled by phosphorus. Based on the physical, chemical and biological parameters, riverine conditions, dominated during the intense monsoon, but lacustrine conditions were evident during the weak monsoon. The interannual dynamics suggest that monsoon seasonality is considered the main forcing factor regulating overall functions and processes of the waterbody and this characteristic has an important implication to eutrophication of the system.
机译:分析了化学和生物学参数,以检查区域水文波动如何影响两年内人工透镜体生态系统的水质。季风雨的强度占年度流入和排放量的大部分,并影响了流动路径(内流与溢流),从而改变了化学和生物条件。在研究期间,强烈季风与弱季风形成鲜明对比的年际水文。强烈的季风破坏了热分层,导致源头河段离子稀释,高TP和高无机固体(NVSS)。 NVSS的变化占TP变化的75%(斜率= 4.14,p <0.01,n = 48)。残留叶绿素-α(Chl)与冲洗速率之间的回归分析表明,夏季季风期间较短的水力停留时间和较高的矿物浊度会影响源头河段藻类的生长。相反,在弱季风期间的严重干旱会导致整个系统强烈的热分层,低的无机固体,高的总溶解固体(TDS)和低的TP。另外,Chl浓度由磷控制。根据物理,化学和生物学参数,在强季风期间,河流条件占主导地位,但在弱季风期间,湖泊条件明显。年际动力学表明季风季节被认为是调节水体整体功能和过程的主要推动因素,这一特征对系统的富营养化具有重要意义。

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