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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >GEMAS: Spatial distribution of the pH of European agricultural and grazing land soil
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GEMAS: Spatial distribution of the pH of European agricultural and grazing land soil

机译:GEMAS:欧洲农业和牧场土壤pH值的空间分布

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摘要

During 2008 the GEochemical Mapping of Agricultural Soils (GEMAS) project collected 2108 agricultural (ploughed soil, Ap horizon, 0–20 cm) and 2023 grazing land soil samples (Gr, 0–10 cm) evenly spread over 33 European countries and covering an area of 5.6 million km~2. The pH of all samples was determined by one single laboratory applying a 0.01 M CaCl_2 extraction, and following a strict quality-control procedure. The resulting pH-value distributions for European Ap and Gr soil are both bimodal. Broad acidic modes, with pH between 4 and 6, and sharp alkaline modes, with pH between 7 and 8 due to the Ca~(2+) buffer system, are clearly separated. The European median pH is 5.8 for the GEMAS Ap soil samples and 5.5 for the GEMAS Gr soil samples. According to the pH distribution maps, Europe is separated into two main zones: northern Europe with generally lower pH values (Ap: 5.2, Gr: 4.8), dominated by acidic soils occurring in Fennoscandia, and southern Europe with higher pH values (Ap: 6.3, Gr: 5.9), dominated by carbonate rich soils. The separation line coincides with the southern border of the sediments of the last glaciation. The dominant factors controlling pH at the European scale are thus geology (crystalline bedrock) in combination with climate (temperature and precipitation). The GEMAS pH maps mainly reflect the natural site conditions on the European scale, whilst anthropogenic impact is hardly detectable. The GEMAS results provide a unique set of homogenous and spatially representative soil pH data for the continent. The data set defines a dependable continental-scale background, and offers the possibility to calibrate studies on more detailed scales.
机译:在2008年,农业土壤地球化学制图项目(GEMAS)收集了2108份农业土壤(耕地,Ap地平线,0–20厘米)和2023牧场土壤样本(Gr,0–10厘米),平均分布在33个欧洲国家,覆盖了面积560万公里〜2。所有样品的pH值均由一个实验室采用0.01 M CaCl_2萃取,并遵循严格的质量控制程序确定。欧洲Ap和Gr土壤的pH值分布均为双峰。由于Ca〜(2+)缓冲系统,pH值介于4至6的宽酸性模式和pH值介于7至8的尖锐碱性模式被清楚地分离了。 GEMAS Ap土壤样品的欧洲pH中值为5.8,GEMAS Gr土壤样品的欧洲pH为5.5。根据pH分布图,欧洲分为两个主要区域:pH值通常较低的北欧(Ap:5.2,Gr:4.8),以芬诺斯堪的亚州的酸性土壤为主,而pH值较高的欧洲南部(Ap: 6.3,Gr:5.9),以富含碳酸盐的土壤为主。分隔线与最后一次冰川沉积的南部边界重合。因此,在欧洲范围内控制pH值的主要因素是地质(晶体基岩)与气候(温度和降水)的组合。 GEMAS pH图主要反映了欧洲范围内的自然地点条件,而人为的影响几乎无法检测到。 GEMAS结果为该大陆提供了一组独特的,均一的,具有空间代表性的土壤pH数据。数据集定义了可靠的大陆尺度背景,并提供了在更详细尺度上校准研究的可能性。

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