Department of Chemical Engineering and Analytical Science, The University of Manchester, Sackville Street, Manchester, M13 9PL, UK.
NILU - Norwegian Institute for Air Research, PO Box 100, Kjeller, 2027, Norway.
Nat Commun. 2021 Nov 18;12(1):6663. doi: 10.1038/s41467-021-26907-3.
Soil salinization has become one of the major environmental and socioeconomic issues globally and this is expected to be exacerbated further with projected climatic change. Determining how climate change influences the dynamics of naturally-occurring soil salinization has scarcely been addressed due to highly complex processes influencing salinization. This paper sets out to address this long-standing challenge by developing data-driven models capable of predicting primary (naturally-occurring) soil salinity and its variations in the world's drylands up to the year 2100 under changing climate. Analysis of the future predictions made here identifies the dryland areas of South America, southern and western Australia, Mexico, southwest United States, and South Africa as the salinization hotspots. Conversely, we project a decrease in the soil salinity of the drylands in the northwest United States, the Horn of Africa, Eastern Europe, Turkmenistan, and west Kazakhstan in response to climate change over the same period.
土壤盐渍化已成为全球主要的环境和社会经济问题之一,预计随着气候变化预测的进一步加剧,这一问题将更加严重。由于影响盐渍化的过程非常复杂,因此几乎没有解决气候变化如何影响自然发生的土壤盐渍化动态的问题。本文旨在通过开发数据驱动的模型来应对这一长期存在的挑战,这些模型能够预测世界旱地中主要(自然发生)土壤盐分及其在不断变化的气候下到 2100 年的变化。对这里进行的未来预测的分析确定了南美洲、澳大利亚南部和西部、墨西哥、美国西南部和南非的旱地为盐渍化热点地区。相反,我们预计在同一时期,由于气候变化,美国西北部、非洲之角、东欧、土库曼斯坦和哈萨克斯坦西部的旱地土壤盐分将会减少。