Zamanian Kazem, Taghizadeh-Mehrjardi Ruhollah, Tao Jingjing, Fan Lichao, Raza Sajjad, Guggenberger Georg, Kuzyakov Yakov
Institute of Soil Science, Leibniz University of Hannover, Herrenhäuser Str. 2, 30419 Hannover, Germany; School of Geographical Sciences, Nanjing University of Information, Science and Technology, Nanjing 210044, China.
Faculty of Agriculture and Natural Resources, Ardakan University, Ardakan, Iran.
Sci Total Environ. 2024 May 10;924:171631. doi: 10.1016/j.scitotenv.2024.171631. Epub 2024 Mar 11.
Soil acidification is an ongoing problem in intensively cultivated croplands due to inefficient and excessive nitrogen (N) fertilization. We collected high-resolution data comprising 19,969 topsoil (0-20 cm) samples from the Land Use and Coverage Area frame Survey (LUCAS) of the European commission in 2009 to assess the impact of N fertilization on buffering substances such as carbonates and base cations. We have only considered the impacts of mineral fertilizers from the total added N, and a N use efficiency of 60 %. Nitrogen fertilization adds annually 6.1 × 10 kmol H to European croplands, leading to annual loss of 6.1 × 10 kg CaCO. Assuming similar acidification during the next 50 years, soil carbonates will be completely removed from 3.4 × 10 ha of European croplands. In carbonate-free soils, annual loss of 2.1 × 10 kmol of basic cations will lead to strong acidification of at least 2.6 million ha of European croplands within the next 50 years. Inorganic carbon and basic cation losses at such rapid scale tremendously drop the nutrient status and production potential of croplands. Soil liming to ameliorate acidity increases pH only temporarily and with additional financial and environmental costs. Only the direct loss of soil carbonate stocks and compensation of carbonate-related CO correspond to about 1.5 % of the proposed budget of the European commission for 2023. Thus, controlling and decreasing soil acidification is crucial to avoid degradation of agricultural soils, which can be done by adopting best management practices and increasing nutrient use efficiency. Regular screening or monitoring of carbonate and base cations contents, especially for soils, where the carbonate stocks are at critical levels, are urgently necessary.
由于氮肥施用效率低下且过量,土壤酸化是集约化农田中一个持续存在的问题。我们收集了高分辨率数据,这些数据包括2009年欧盟委员会土地利用和覆盖面积框架调查(LUCAS)中的19969个表层土壤(0 - 20厘米)样本,以评估氮肥对碳酸盐和碱金属阳离子等缓冲物质的影响。我们仅考虑了矿物肥料中总添加氮的影响,以及60%的氮利用效率。氮肥每年向欧洲农田添加6.1×10千摩尔氢离子,导致每年损失6.1×10千克碳酸钙。假设在未来50年内酸化情况相似,欧洲3.4×10公顷农田中的土壤碳酸盐将被完全去除。在无碳酸盐土壤中,每年损失2.1×10千摩尔的碱金属阳离子将导致在未来50年内至少260万公顷的欧洲农田发生强烈酸化。如此快速的无机碳和碱金属阳离子损失极大地降低了农田的养分状况和生产潜力。通过土壤施用石灰来改善酸度只能暂时提高pH值,且会带来额外的经济和环境成本。仅土壤碳酸盐储量的直接损失以及与碳酸盐相关的二氧化碳补偿就约占欧盟委员会2023年拟议预算的1.5%。因此,控制和减少土壤酸化对于避免农业土壤退化至关重要,这可以通过采用最佳管理措施和提高养分利用效率来实现。迫切需要定期筛选或监测碳酸盐和碱金属阳离子含量,特别是对于碳酸盐储量处于临界水平的土壤。