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Comparative Analysis of Water Quality between the Runoff Entrance and Middle of Recycling Irrigation Reservoirs

机译:径流入口与循环灌溉水库中段水质的比较分析。

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Recycling irrigation reservoirs (RIRs) are an emerging aquatic ecosystem of critical importance, for conserving and protecting increasingly scarce water resources. Here, we compare water quality between runoff entrance and middle of four RIRs in nurseries in Virginia (VA) and Maryland (MD). Surface water temperature (T) and oxidation-reduction potential (ORP) were lower in the middle than at the entrance, while the trend was opposite for dissolved oxygen (DO), pH and chlorophyll a (Chla). The magnitude of these differences between the entrance and middle decreased with increasing depth. These differences were magnified by water stratification from April to October. Minimum differences were observed for electrical conductivity (EC), total dissolved solids (TDS) and turbidity (TUR). Cluster analyses were performed on water quality difference data to evaluate whether the differences vary with respect to reservoirs. Two clusters were formed with one consisting primarily of VA reservoirs, and the other consisting mostly of MD reservoirs in both years. Water quality in the middle and at the entrance of RIRs was expected to vary greatly because of runoff inflow. The two-point water quality differences observed here, although statistically significant, are not large enough to cause significant impact on crop health and productivity for most water quality parameters except pH. Additional analysis of outlet data shows that the range and magnitude of water quality difference between the middle and the outlet are comparable to those between the middle and entrance of RIRs. These results indicate that monitoring at a single point is sufficient to obtain reliable water quality estimates for most water quality parameters in RIRs except pH. This is important when considering the cost of labor and equipment necessary for documenting water quality in agricultural production systems. However, additional pH measurements are still necessary to make practical water quality management decisions.
机译:循环灌溉水库(RIR)是一种新兴的水生生态系统,对于保护和保护日益稀缺的水资源至关重要。在这里,我们比较了弗吉尼亚(VA)和马里兰(MD)苗圃的径流入口与四个RIR中间的水质。中间的地表水温度(T)和氧化还原电位(ORP)低于入口处,而溶解氧(DO),pH和叶绿素a(Chla)的趋势相反。这些入口和中间之间的差异的大小随深度的增加而减小。从4月到10月,水分层将这些差异放大了。观察到电导率(EC),总溶解固体(TDS)和浊度(TUR)的最小差异。对水质差异数据进行了聚类分析,以评估差异是否随水库而变化。在这两年中,形成了两个集群,其中一个主要由VA储层组成,另一个主要由MD储层组成。由于径流的流入,RIRs中部和入口处的水质预计会有很大变化。此处观察到的两点水质差异尽管具有统计学意义,但对于除pH值以外的大多数水质参数而言,不足以对作物健康和生产力造成重大影响。出口数据的进一步分析表明,中间和出口之间水质差异的范围和大小与RIR的中间和入口之间的水质差异可比。这些结果表明,在单个点进行监视足以获得RIR中除pH以外的大多数水质参数的可靠水质估计。在考虑记录农业生产系统中水质所需的劳力和设备成本时,这一点很重要。但是,仍然需要进行额外的pH值测量才能做出实际的水质管理决策。

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