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APPLICATION OF BORON ISOTOPE RATIOS FOR IDENTIFYING NITRATE CONTAMINATION SOURCES IN THE GROUNDWATER OF AVRA VALLEY, ARIZONA

机译:硼同位素比值法在亚利桑那州阿弗拉河谷地下水中硝酸盐污染源识别中的应用

摘要

The stable isotopes of the conservative element boron, 11B and 1°B, have beenudemployed as co- migrating isotopic tracers to determine the origin of nitrate observed inudgroundwater from a large capacity (2500 gpm) irrigation well in the Avra Valley ofudsoutheastern Arizona. The isotopic ratios of the conservative element, boron, provided anudidentifying signature for various nitrate rich source waters. Additional chemicaludparameters were also examined to corroborate the isotopic indications.udFindings of this investigation indicate that most of the nitrate observed inudgroundwater from well CMID 18 at the beginning of the 1993 irrigation season was dueudto municipal wastewater contamination. As the irrigation season progressed, an increasingudproportion of nitrate was contributed by irrigation return flow from neighboringudagricultural fields.
机译:ud利用保守元素11B和1°B的稳定同位素作为共迁移同位素示踪剂,以确定在阿夫拉河谷大容量(2500 gpm)灌溉井中地下水中观察到的硝酸盐的来源。 udsoutheastern亚利桑那州。保守元素硼的同位素比为各种富含硝酸盐的源水提供了一个识别特征。 ud研究的结果表明,在1993年灌溉季节开始时,从CMID 18井中地下水中观察到的大部分硝酸盐是由于市政废水污染所致。随着灌溉季节的进行,邻近农业耕地的灌溉回流导致硝酸盐的增加不成比例。

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