Specific conductivity in groundwater (DP1.20015.001)
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Specific conductance is a proxy for the level of total dissolved solids of the groundwater as well as related to the redox potential. Conductivity may also be used as a tracer of distinct water masses for understanding flow. NEON measurements of groundwater conductivity at high temporal resolution. Up to eight wells (and as low as three) are available per aquatic site. From NEON groundwater elevation measurements, the magnitude and direction of groundwater flow can be calculated, which may be coupled to better understand the exchange between groundwater and surface water. This data product includes continuous quality-controlled groundwater temperature captured every 5 minute and reported as 5-minute instantaneous measurements and 30-minute averages. Latency: Data collected in any given month are published during the second full week of the following month.
比电导率(Specific Conductance)可作为地下水总溶解固体总量的替代表征指标,同时与氧化还原电位存在关联。电导率(Conductivity)还可作为不同水团的示踪剂,助力解析水文流动过程。NEON以高时间分辨率开展了地下水电导率的监测工作。每个水生监测站点可配备最多8口监测井(最少3口)。依托NEON的地下水位监测数据,可计算地下水径流的幅值与流向,将该结果与其他相关数据联用,可更深入地理解地下水与地表水之间的交换过程。本数据产品包含每5分钟采集、经持续质量控制的地下水温度数据,以5分钟瞬时测量值与30分钟平均值两种形式发布。数据发布延迟:任意自然月采集的数据将于次月的第二个完整工作周内发布。



