Climate Change and Soil Dynamics: A Crop Modelling Approach

被引:1
|
作者
Wimalasiri, Eranga M. [1 ]
Sirishantha, Deshani [1 ]
Karunadhipathi, U. L. [2 ]
Ampitiyawatta, Asanga D. [1 ]
Muttil, Nitin [3 ,4 ]
Rathnayake, Upaka [5 ]
机构
[1] Sabaragamuwa Univ Sri Lanka, Fac Agr Sci, Dept Export Agr, Belihuloya 70140, Sri Lanka
[2] Univ Peradeniya, Postgrad Inst Agr, Peradeniya 20400, Sri Lanka
[3] Victoria Univ, Coll Sport Hlth & Engn, Melbourne, Vic 8001, Australia
[4] Victoria Univ, Inst Sustainable Ind & Liveable Cities, Melbourne, Vic 8001, Australia
[5] Atlantic Technol Univ, Fac Engn & Design, Dept Civil Engn & Construct, Ash Lane, Sligo F91YW50, Ireland
关键词
agri-environmental modelling; APSIM; crop nutrition; food security; nutrient cycling; ORGANIC-CARBON; NITROGEN; IMPACTS; WATER; RICE;
D O I
10.3390/soilsystems7040082
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The impact of global climate change is a challenge to the sustainability of many ecosystems, including soil systems. However, the performance of soil properties under future climate was rarely assessed. Therefore, this study was carried out to evaluate selected soil processes under climate change using an agri-environmental modeling approach to Sri Lanka. The Agricultural Production Systems Simulator (APSIM) model was used to simulate soil and plant-related processes using recent past (1990-2019) and future (2041-2070) climates. Future climate data were obtained for a regional climate model (RCM) under representative concentrations pathway 4.5 scenarios. Rainfalls are going to be decreased in all the tested locations under future climate scenarios while the maximum temperature showcased rises. According to simulated results, the average yield reduction under climate change was 7.4%. The simulated nitrogen content in the storage organs of paddy declined in the locations (by 6.4-25.5%) as a reason for climate change. In general, extractable soil water relative to the permanent wilting point (total available water), infiltration, and biomass carbon lost to the atmosphere decreased while soil temperature increased in the future climate. This modeling approach provides a primary-level prediction of soil dynamics under climate change, which needs to be tested using fieldwork.
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页数:17
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