Estimations of soil metal accumulation or leaching potentials under climate change scenarios: the example of copper on a European scale

IF 5.8 2区 农林科学 Q1 SOIL SCIENCE
Soil Pub Date : 2024-06-06 DOI:10.5194/soil-10-367-2024
Laura Sereni, Julie-Maï Paris, Isabelle Lamy, Bertrand Guenet
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引用次数: 0

Abstract

Abstract. Contaminant inputs to soil are highly dependent on anthropogenic activities, while contaminant retention, mobility, and availability are highly dependent on soil properties. The knowledge of partitioning between soil solid and solution phases is necessary to estimate whether deposited amounts of contaminants will be either transported with runoff or accumulated. Besides, runoff is expected to change during the next century due to changes in climate and in rainfall patterns. In this study, we aimed to estimate at the European scale the areas with a potential risk due to contaminant leaching (LP). We also defined, in the same way, the surface areas where limited copper (Cu) leaching occurred, leading to potential accumulation (AP) areas. We focused on Cu widely used in agriculture either in a mineral form or in association with organic fertilizers, resulting in high spatial variations in the deposited and incorporated amounts in soils, as well as in European policies of application. We developed a method using both Cu partition coefficients (Kf) between total and dissolved Cu forms and runoff simulation results for historical and future climates. The calculation of Kf with pedo-transfer functions allowed us to avoid any uncertainties due to past management or future depositions that may affect total Cu concentrations. Areas with a high potential risk of leaching or of accumulation were estimated over the 21st century by comparing Kf and runoff to their respective European medians. Thus, at three distinct times, we considered a grid cell to be at risk of LP if its Kf was low compared to the European median and if its runoff was high compared to the European median of the time. Similarly, a grid cell was considered to be at risk of AP if its Kf was high and its runoff was low compared to its respective European median of the time. To deal with uncertainties in climate change scenarios and the associated model prediction, we performed our study with two atmospheric greenhouse gas representative concentration pathways (RCPs), defined according to climate change associated with a large set of socio-economic scenarios found in the literature. We used two land surface models (ORCHIDEE and LPJmL, given soil hydrologic properties) and two global circulation models (ESM2m and CM5a, given rainfall forecasts). Our results show that, for historical scenarios, 6.4 ± 0.1 % (median, median deviation) and 6.7 ± 1.1 % of the grid cells of the European land surfaces experience LP and AP, respectively. Interestingly, we simulate a constant surface area with LP and AP for around 13 % of the grid cells, which is consistent with an increase in AP and a decrease in LP. Despite large variations in LP and AP extents, depending on the land surface model used for estimations, the two trends were more pronounced with RCP 6.0 than with RCP 2.6, highlighting the global risk of combined climate change and contamination and the need for more local and seasonal assessments. Results are discussed to highlight the points requiring improvement to refine predictions.
气候变化情景下的土壤金属积累或浸出潜力估算:以欧洲范围内的铜为例
摘要。污染物对土壤的输入在很大程度上取决于人为活动,而污染物的滞留性、流动性和可用性则在很大程度上取决于土壤特性。要估计沉积的污染物是随径流迁移还是累积,就必须了解土壤固相和溶相之间的分配情况。此外,由于气候和降雨模式的变化,预计下个世纪的径流也会发生变化。在这项研究中,我们旨在估算欧洲范围内因污染物沥滤(LP)而存在潜在风险的区域。我们还以同样的方式确定了发生有限铜(Cu)沥滤的地表区域,从而确定了潜在累积(AP)区域。我们重点研究了以矿物形式或与有机肥料结合的形式广泛用于农业的铜,这导致土壤中的沉积量和结合量以及欧洲的施用政策存在很大的空间差异。我们利用总铜和溶解铜之间的分配系数(Kf)以及历史和未来气候条件下的径流模拟结果,开发了一种方法。通过脚步转移函数计算 Kf,我们避免了因过去的管理或未来的沉积而可能影响总铜浓度的任何不确定性。通过将 Kf 和径流与各自的欧洲中位数进行比较,估算出 21 世纪潜在浸出或累积风险较高的地区。因此,在三个不同的时间段,如果一个网格单元的 Kf 低于欧洲中位数,而径流又高于当时的欧洲中位数,我们就认为该网格单元存在低浓度沥滤风险。同样,如果一个网格单元的 Kf 值较高,且其径流量与当时的欧洲中位数相比较低,则该网格单元被视为面临 AP 风险。为了应对气候变化情景和相关模型预测的不确定性,我们采用了两种大气温室气体代表性浓度路径(RCPs)进行研究。我们使用了两个地表模型(ORCHIDEE 和 LPJmL,考虑土壤水文特性)和两个全球环流模型(ESM2m 和 CM5a,考虑降雨预测)。我们的结果表明,在历史情景下,欧洲陆地表面分别有 6.4 ± 0.1 %(中位数,中位偏差)和 6.7 ± 1.1 % 的网格单元经历 LP 和 AP。有趣的是,我们模拟了约 13% 的网格单元具有 LP 和 AP 的恒定表面积,这与 AP 的增加和 LP 的减少相一致。尽管根据估算所用的地表模型,LP 和 AP 的范围存在很大差异,但 RCP 6.0 的两种趋势比 RCP 2.6 更为明显,这凸显了气候变化和污染共同带来的全球风险,以及进行更多地方和季节性评估的必要性。对结果进行了讨论,以突出需要改进的地方,从而完善预测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Soil
Soil Agricultural and Biological Sciences-Soil Science
CiteScore
10.80
自引率
2.90%
发文量
44
审稿时长
30 weeks
期刊介绍: SOIL is an international scientific journal dedicated to the publication and discussion of high-quality research in the field of soil system sciences. SOIL is at the interface between the atmosphere, lithosphere, hydrosphere, and biosphere. SOIL publishes scientific research that contributes to understanding the soil system and its interaction with humans and the entire Earth system. The scope of the journal includes all topics that fall within the study of soil science as a discipline, with an emphasis on studies that integrate soil science with other sciences (hydrology, agronomy, socio-economics, health sciences, atmospheric sciences, etc.).
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