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可持续农业利用含镭活度升高的天然水源。

Sustainable agricultural use of natural water sources containing elevated radium activity.

机构信息

Southern Arava Research and Development, Hevel-Eilot 88820, Israel.

Radiation Safety Division, Soreq Nuclear Research Center, Yavne 81800, Israel.

出版信息

Chemosphere. 2014 Jun;104:205-11. doi: 10.1016/j.chemosphere.2013.11.020. Epub 2013 Dec 15.

Abstract

Relatively elevated concentrations of naturally occurring radium isotopes ((226)Ra, (228)Ra and (224)Ra) are found in two main aquifers in the arid southern part of Israel, in activity concentrations frequently exceeding the limits set in the drinking water quality regulations. We aimed to explore the environmental implications of using water containing Ra for irrigation. Several crops (cucumbers, melons, radish, lettuce, alfalfa and wheat), grown in weighing lysimeters were irrigated at 3 levels of (226)Ra activity concentration: Low Radium Water (LRW)<0.04 Bq L(-1); High Radium Water (HRW) at 1.8 Bq L(-1) and (3) Radium Enriched Water (REW) at 50 times the concentration in HRW. The HYDRUS 1-D software package was used to simulate the long-term (226)Ra distribution in a soil irrigated with HRW for 15 years. Radium uptake by plants was found to be controlled by its activity in the irrigation water and in the soil solution, the physical properties of the soil and the potential evapotranspiration. The (226)Ra apeared to accumulate mainly in the leaves of crops following the evapotranspiration current, while its accumulation in the edible parts (fruits and roots) was minimal. The simulation of 15 years of crop irrigation by HYDERUS 1-D, showed a low Ra activity concentration in the soil solution of the root zone and a limited downward mobility. It was therefore concluded that the crops investigated in this study can be irrigated with the natural occurring activity concentration of (226)Ra of 0.6-1.6 Bq L(-1). This should be accompanied by a continuous monitoring of radium in the edible parts of the crops.

摘要

在以色列干旱南部的两个主要含水层中,发现了天然镭同位素((226)Ra、(228)Ra 和 (224)Ra)的浓度相对较高,其活度浓度经常超过饮用水质量法规规定的限值。我们旨在探索使用含镭水进行灌溉的环境影响。在称重蒸渗仪中种植的几种作物(黄瓜、甜瓜、萝卜、生菜、紫花苜蓿和小麦)分别用 3 种 (226)Ra 活度浓度的水进行灌溉:低镭水(LRW)<0.04 Bq L(-1);高镭水(HRW)为 1.8 Bq L(-1);富镭水(REW)为 HRW 的 50 倍。使用 HYDRUS 1-D 软件包模拟了用 HRW 灌溉 15 年的土壤中 (226)Ra 的长期分布。发现植物对镭的吸收受灌溉水中镭的活度及其在土壤溶液中的活度、土壤的物理性质和潜在蒸散量的控制。(226)Ra 似乎主要通过蒸腾流积累在作物的叶片中,而其在可食用部分(果实和根)中的积累则很少。HYDERUS 1-D 对 15 年作物灌溉的模拟表明,根区土壤溶液中的镭活度浓度较低,向下迁移能力有限。因此,可以得出结论,本研究中调查的作物可以用 0.6-1.6 Bq L(-1)的天然存在的 (226)Ra 活度浓度进行灌溉。这应伴随着对作物可食用部分中镭的持续监测。

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