Soil organic carbon dynamics in the agricultural soils of Bangladesh following more than 20 years of land use intensification

被引:21
作者
Uddin, M. J. [1 ,2 ]
Hooda, Peter S. [1 ]
Mohiuddin, A. S. M. [2 ]
Haque, M. Ershadul [3 ]
Smith, Mike [4 ]
Waller, Martyn [1 ]
Biswas, Jayanta Kumar [5 ]
机构
[1] Kingston Univ London, Sch Engn & Environm, Kingston Upon Thames, Surrey, England
[2] Univ Dhaka, Dept Soil Water & Environm, Dhaka, Bangladesh
[3] Univ Dhaka, Dept Stat, Dhaka, Bangladesh
[4] Ulster Univ, Sch Geog & Environm Sci, Coleraine, Londonderry, North Ireland
[5] Univ Kalyani, Dept Ecol Studies, Kalyani, W Bengal, India
关键词
Cropping intensity; Land types; Soil management practices; Food security; INDO-GANGETIC PLAINS; NITROGEN-FERTILIZATION; CROPPING SYSTEMS; RICE; SEQUESTRATION; STORAGE; MATTER; MANAGEMENT; IMPACTS; PRODUCTIVITY;
D O I
10.1016/j.jenvman.2021.114427
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Soil organic carbon (SOC) is a key soil quality indicator, as it is a source and storage of plant nutrients and plays a vital role in soil fertility and productivity maintenance. Intensification of agriculture is known to cause SOC decline; however, much of the evidence stems from field-scale experimental trials. The primary aim of this study is to investigate how more than 20 years of agricultural land use intensification in Bangladesh has influenced SOC levels at landscape levels. This was achieved by revisiting in 2012 four sub-sites from the Brahmaputra and Ganges alluviums which were previously sampled (1989-92) by the Soil Resource Development Institute and collecting 190 new samples. These were located at different elevations and subjected to differing amounts of inundation. The SOC was determined using the same method, potassium dichromate wet oxidation, used in the 1989-92 campaign. A comparison of the SOC in the 2012 samples with their historic levels (1989-92) revealed that overall SOC declined significantly across both alluviums as well at their four sub-sites. Further analysis, however, showed that SOC has declined more at higher sites. The higher sites are inundated to a limited level, which makes them suitable for growing multiple crops. Among the land types considered here, the low land sites (because of their topographical position) remain inundated for a greater part of the year, allowing a maximum of only one crop of submerged rice. As a result of reduced biomass decomposition due to anaerobic conditions when inundated, and lower land use/cropping intensity, SOC accretion has occurred in the lower land sites. The SOC levels in South Asian countries are inherently low and agricultural land use intensification fuelled by growing food production demand is causing further SOC loss, which has the potential to jeopardise food security and increase the environmental impact of agriculture.
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页数:10
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