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首页> 外文期刊>Water, Air, and Soil Pollution >STABLE ISOTOPE AND CHLORIDE, BORON STUDY FOR TRACING SOURCES OF BORON CONTAMINATION IN GROUNDWATER: BORON CONTENTS IN FRESH AND THERMAL WATER IN DIFFERENT AREAS IN GREECE
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STABLE ISOTOPE AND CHLORIDE, BORON STUDY FOR TRACING SOURCES OF BORON CONTAMINATION IN GROUNDWATER: BORON CONTENTS IN FRESH AND THERMAL WATER IN DIFFERENT AREAS IN GREECE

机译:同位素和氯化物的稳定硼研究跟踪地下水中硼污染的来源:希腊不同地区的新鲜水和热水中的硼含量

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Boron is biologically an essential element but is toxic at high concentrations to plants (above approximately 1 mg/L in irrigation water) and probably to humans: The EU Drinking Water Directive fixes a threshold of 1 mg/L and the World Health Organisation (WHO) set a recommended limit at 0.3 mg/L now increased to 0.5 mg/L. Because of this potential toxicity and the need of implementation of EU regulation on national level, the study of the boron levels in both ground- and surface water is of great significance for water management. In Greece, a significant number of thermal, mineral and superficial water springs are found especially in Northern Greece, that present high boron values rendering such water unacceptable according to the European standards. Nevertheless, such ground waters or borehole water with high temperature and high boron content are used for irrigation and drinking purposes, and could therefore have an antagonistic effect on crop yield and health. In order to study the boron contamination and to elucidate the origin of B, we collected a number of hot and fresh water all over Greece. In all the water sampled, the boron concentration exceeds the limit of 0.3 mg/L, which is the former recommended WHO limit. Moreover, in the irrigation water examined, the boron concentration exceeds the value of 0.75 mg/L, which is the limit for sensitive plants (for plants of moderate and plants of high tolerance, these values vary between 0.75-3 and > 3 mg/L respectively). In all cases, eleyated boron could be attributed to natural sources, geothermal activity and/or seawater intrusion into the aquifers. This finding has important implications for water management: In a setting of high natural geochemical background values, source control of the pollution is not possible and water managers have to cope with a local to regional geochemical anomaly that implies boron specific water treatment or mixing with unpolluted resources to bring concentrations down.
机译:硼是生物学上必不可少的元素,但在高浓度下对植物(在灌溉水中约1 mg / L以上)和对人类有毒:欧盟饮用水指令将阈值设定为1 mg / L,世界卫生组织(世卫组织) )将建议极限值从现在的0.3 mg / L提高到0.5 mg / L。由于这种潜在的毒性以及需要在国家一级执行欧盟法规的要求,因此研究地下水和地表水中的硼含量对水管理具有重要意义。在希腊,特别是在希腊北部,发现了大量的温泉,矿泉和浅水泉水,这些泉水具有很高的硼值,根据欧洲标准,这种水是不可接受的。然而,这种高温或高硼含量的地下水或井孔水被用于灌溉和饮用目的,因此可能对作物的产量和健康产生不利影响。为了研究硼污染并阐明B的来源,我们在希腊各地收集了许多热水和淡水。在所有采样的水中,硼浓度都超过了0.3 mg / L的限值,这是以前建议的WHO限值。此外,在所检查的灌溉水中,硼浓度超过0.75 mg / L的值,这是敏感植物的极限(对于中度植物和高耐受性植物,这些值在0.75-3和> 3 mg / L之间变化L分别)。在所有情况下,硼的散发都可以归因于自然资源,地热活动和/或海水侵入含水层。这一发现对水管理具有重要意义:在自然地球化学背景值很高的情况下,不可能对污染源进行控制,水管理者必须应对局部到区域地球化学异常,这意味着需要对硼进行特殊的水处理或与未污染的水混合。资源以降低集中度。

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