欧洲农业土壤中的 - - 大陆范围的来源与沉没 - - 地质视角
Philippe Négrel1, Anna Ladenberger2, Clemens Reimann3
1BRGM, 45060 Orléans, France.
The Science of the total environment
|April 19, 2024
概括
(P) 对于植物和生物的生长至关重要. 土壤P的可用性主要由pH和气候等自然因素控制,人类的影响很难量化.
科学领域:
- 地质化学 地质化学
- 环境科学 环境科学
- 土壤科学 土壤科学
背景情况:
- (P) 是所有生命必需的营养素,对植物和生物体的生长至关重要.
- 尽管地丰富,但由于pH,矿物学和复杂形成等因素,许多土壤缺乏可用的P.
- 有机P形式和人为投入 (肥料) 也影响土壤P动态.
研究的目的:
- 研究欧洲农业土壤中的空间分布和控制因素.
- 评估地质,气候和人为因素对土壤含量的影响.
主要方法:
- 使用X射线光 (XRF) 和热水 (AR) 提取总 (P) 度的分析.
- 利用了来自农业和牧场土壤地化学绘图 (GEMAS) 项目的数据.
- 检查了与欧洲各地的土壤特性,地质和气候有关的P度.
主要成果:
- 总P度 (XRF中位数为786 mg/kg) 略高于AR提取 (中位数为653 mg/kg).
- 在最后一次冰河时期的沙沉积物和石灰质土壤中观察到低度的P.
- 欧洲东北和北北地区的高P值与寒冷,潮湿的气候和富含湿的土壤相关.
结论:
- 大陆范围的P分布主要是由地质和气候因素驱动的.
- 从自然背景水平区分人为P影响仍然具有挑战性.
- 了解这些因素对于管理土壤肥力和环境含量至关重要.
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