Spatio-Temporal Variations in Soil pH and Aluminum Toxicity in Sub-Saharan African Croplands (1980–2050)

Author:

Uwiragiye Yves123,Khalaf Qahtan Abdul Wahid4,Ali Hayssam M.5ORCID,Ngaba Mbezele Junior Yannick13ORCID,Yang Mingxia13,Elrys Ahmed S.678,Chen Zhujun13,Zhou Jianbin13ORCID

Affiliation:

1. College of Natural Resources and Environment, Northwest A&F University, Yangling 712100, China

2. Department of Agriculture, Faculty of Agriculture, Environmental Management and Renewable Energy, University of Technology and Arts of Byumba, Byumba P.O. Box 25, Rwanda

3. Key Laboratory of Plant Nutrition and the Agri-Environment in Northwest China, Ministry of Agriculture, Yangling 712100, China

4. Department of Medical Laboratory Techniques, College of Medical Technology, Al-Kitab University, Kirkuk 36001, Iraq

5. Department of Botany and Microbiology, College of Science, King Saud University, Riyadh 11451, Saudi Arabia

6. Soil Science Department, Faculty of Agriculture, Zagazig University, Zagazig 44511, Egypt

7. College of Tropical Crops, Hainan University, Haikou 570228, China

8. Liebig Centre for Agroecology and Climate Impact Research, Justus Liebig University, 35390 Giessen, Germany

Abstract

Soil acidity threatens food production in the tropics. The effect of increasing ammonium-based fertilizer (INF) on soil pH was assessed in sub-Saharan Africa (SSA). A total of 9043 soil data from Africa soil information services, past INF use, and two future scenarios of INF use (business as usual (BAU) and equitable diet (EqD)) were used to determine soil pH variations from 1980 to 2022 and to predict soil PH variations from 2022 to 2050. Random forest and extreme gradient boosting algorithms and soil-forming factor covariates were used for the spatio-temporal soil pH predictions. Topsoil acidification was shown to be significant, with mean annual decrements of 0.014, 0.024, and 0.048 from 1980 to 2022, 2022 to 2050 (BAU), and 2022 to 2050 (EqD), respectively. Over the past 42 years, croplands with soil pH < 6.5 have declined significantly, and soil acidification is predicted to become severe by 2050 in the BAU and EqD scenarios. This was indicated by a predicted 3% increase in croplands at risk of aluminum toxicity (soil pH < 5.5) from 66 × 106 ha in 2022 to 78.5 × 106 ha in 2050. The drivers of the spatial variations in the soil pH between 1980 and 2050 were the MAP, basic cation, clay content, SOC, and nitrogen fertilizers. The evaluation metrics of the 10-fold cross-validation showed that the root mean squared errors (RMSEs) of the soil pH from 1980 to 2022, as well as the predicted soil PH from 2022 to 2050 (BAU) and 2022 to 2050 (EqD), were 0.53 pH units, 0.54 pH units, and 0.56 pH units, respectively, with coefficients of determination (R2) of 0.63, 0.64, and 0.66. The findings of this study can be used for the establishment of management strategies for increasing INF use in acidic soils.

Funder

Researchers Supporting Project number

King Saud University, Riyadh, Saudi Arabia, the National Natural Science Foundation of China

National Key R. & D Program of China

111 Project

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

Reference72 articles.

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