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采用多指标方法追踪脆弱冲积系统中的氮循环:以克罗地亚瓦拉日丁冲积含水层为例。

Tracking the nitrogen cycle in a vulnerable alluvial system using a multi proxy approach: Case study Varaždin alluvial aquifer, Croatia.

机构信息

Croatian Geological Survey, Milana Sachsa 2, 10 000 Zagreb, Croatia.

Ruđer Bošković Institute, Bijenička cesta 54, 10 000 Zagreb, Croatia.

出版信息

Sci Total Environ. 2022 Dec 20;853:158632. doi: 10.1016/j.scitotenv.2022.158632. Epub 2022 Sep 7.

Abstract

At high concentrations nitrate is considered a serious environmental pollutant which degrades the quality of ground and surface waters. Such high nitrate concentrations (>50 mg NO/L) have been observed for decades in the alluvial aquifer in the Varaždin region of Croatia. Here we employ a novel cross disciplinary approach (dual isotopes, chemical, bacteria diversity and mixing modelling) to determine sources of nitrate and processes that can influence nitrate concentration within this vulnerable alluvial aquifer. Ten groundwater wells were sampled across the region and in different hydrological conditions for basic chemical, stable isotopes (δO-HO, δH-HO, δN-NO and δO-NO), and bacterial diversity analyses. In addition, solid samples, i.e. soil samples and fertilizers were collected and analysed for bulk δN. The primary nitrate sources were manure, sewage, soil organic N, and ammonia fertilizers, however we observe no clear evidence to indicate that synthetic fertilizers are a major contributor to groundwater nitrate concentrations. Whilst denitrification was observed in the parts of the study area with dissolved oxygen (DO) deficiency, i.e. anoxic conditions, nitrification has been identified as the major process responsible for nitrate behaviour within the aquifer system. Our results will facilitate the creation of a conceptual model of nitrate behaviour in the study area and from this, a numerical groundwater nitrate transport model. These data, understanding of nitrate dynamics and subsequent models will be critical for future sustainable water and agricultural management of the study area.

摘要

在高浓度下,硝酸盐被认为是一种严重的环境污染物,会降低地下水和地表水的质量。几十年来,克罗地亚瓦拉日丁地区的冲积含水层中一直存在如此高浓度的硝酸盐(>50mgNO/L)。在这里,我们采用一种新的跨学科方法(双重同位素、化学、细菌多样性和混合模型)来确定硝酸盐的来源以及可能影响该脆弱冲积含水层中硝酸盐浓度的过程。在该地区不同水文条件下,对 10 口地下水井进行了基本化学、稳定同位素(δO-HO、δH-HO、δN-NO 和 δO-NO)和细菌多样性分析的采样。此外,还收集和分析了固体样品,即土壤样品和肥料的总氮(δN)。主要的硝酸盐来源是粪肥、污水、土壤有机氮和氨肥,但我们没有明确的证据表明合成肥料是地下水硝酸盐浓度的主要来源。虽然在缺氧(即无氧条件)的研究区部分观察到反硝化作用,但硝化作用已被确定为含水层系统中硝酸盐行为的主要过程。我们的研究结果将有助于在研究区域内创建硝酸盐行为的概念模型,并由此建立一个地下水硝酸盐输运模型。这些数据、对硝酸盐动态的了解以及随后的模型将对该研究区域未来的可持续水资源和农业管理至关重要。

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