
| Title | Ambient Groundwater Quality in the Moxee Valley Surficial Aquifer, Yakima County, January-June 2006 | |||
| Month-Year Published | May 2007 | |||
| Online Availability |
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| Short Description |
During 2006, the Department of Ecology′s Environmental Assessment Program conducted a screening-level evaluation of ambient groundwater quality conditions in the Moxee Valley, which lies just east of the city of Yakima. During the study, 26 broadly distributed domestic wells were sampled twice for commonly regulated drinking water parameters including nutrients and bacteria, as well as selected general chemistry parameters and metals. This report documents the study findings. (Also see abstract below) | |||
| Publication Number | 07-03-023 | |||
| Author(s) | Sinclair, K. and T. Roberts | |||
| Print Availability | ||||
| Number of pages | 46 pp. | |||
| Keywords | aquifer, environmental, groundwater, water, wells | |||
| Subject Waterbodies |
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| Related Publications | Title | Relationship | ||
| Quality Assurance Project Plan: Assessment of Ambient Groundwater Quality Conditions in the Surficial Unconsolidated Sedimentary Aquifer of the Moxee Valley, Yakima County, Washington | similar topic | |||
| Abstract | Long Description |
During January and June 2006, the Washington State Department of Ecology conducted a screening-level assessment of groundwater quality in the Moxee Valley. The valley lies just east of the city of Yakima in south-central Washington. For this study, 26 broadly distributed domestic wells were sampled for field parameters, common nutrients, bacteria, and selected metals. Concentrations of nitrate-N were found to be higher than the 10 mg/L federal drinking water standard in three wells. Five wells exceeded the primary standard for total coliform. The highest nitrate-N concentrations (up to 18.2 mg/L) occurred in the lower valley near Moxee City where wells generally exhibited elevated concentrations of total persulfate nitrogen, total phosphorus, total dissolved solids, and conductivity, but little measurable iron or manganese. By contrast, wells in the upper valley contained elevated concentrations of iron and manganese, but little, if any, measurable nitrate-N or total persulfate nitrogen. Wells in the upper valley also exhibited generally lower total phosphorus, chloride, total dissolved solids, and conductivity values than did wells in the lower valley. |
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