Assessing Soil Organic Carbon Pool for Potential Climate-Change Mitigation in Agricultural Soils-A Case Study Fayoum Depression, Egypt

被引:1
|
作者
Abdellatif, Mostafa A. [1 ]
Hassan, Farag O. [1 ]
Rashed, Heba S. A. [2 ]
El Baroudy, Ahmed A. [3 ]
Mohamed, Elsayed Said [1 ]
Kucher, Dmitry E. [4 ]
Abd-Elmabod, Sameh Kotb [5 ]
Shokr, Mohamed S. [3 ]
Abuzaid, Ahmed S. [2 ]
机构
[1] Natl Author Remote Sensing & Space Sci, Cairo 11843, Egypt
[2] Benha Univ, Fac Agr, Soils & Water Dept, Banha 13518, Egypt
[3] Tanta Univ, Fac Agr, Soil & Water Dept, Tanta 31527, Egypt
[4] Peoples Friendship Univ Russia, RUDN Univ, Inst Environm Engn, Dept Environm Management, 6 Miklukho Maklaya St, Moscow 117198, Russia
[5] Natl Res Ctr NRC, Agr & Biol Res Inst, Soil & Water Use Dept, Cairo 12622, Egypt
关键词
sustainable carbon sequestration; NDVI; land surface temperature (LST); greenhouse gases mitigation; Fayoum depression; LAND-USE; PARTICLE-SIZE; SPATIAL VARIABILITY; CROP PRODUCTION; MATTER; SEQUESTRATION; QUALITY; MANAGEMENT; COMPOST; EROSION;
D O I
10.3390/land12091755
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
It is essential to assess the soil organic carbon pool (SOCP) in dry environments to apply appropriate management techniques that address sustainable development. A significant opportunity for sustaining agricultural output and reducing climate change is the storage of soil organic carbon in agricultural soil. The goal of this study was to measure the spatial variability of SOCP content, and determine the effects of soil texture, changes in land use, and land cover on SOCP in surface soil samples. The study additionally investigated the relationships between SOCP and other characteristics, including the normalized vegetation index (NDVI) and land surface temperature (LST), as well as the effects of increasing soil organic carbon on the amount of greenhouse gases. To accomplish this goal, 45 soil surface samples were collected to a depth of 30 cm at the Fayoum depression in Egypt, and analyzed. The soil samples were representative of various soil textures and land uses. The average SOCP concentration in cultivated regions is 32.1 and in bare soils it is 6.5 Mg ha-1, with areas of 157,112.94 and 16,073.27 ha, respectively. According to variances in soil textures, sandy soils have the lowest SOCP (1.8 Mg ha-1) and clay loam soils have the highest concentrations (49 Mg ha-1). Additionally, fruit-growing regions have the greatest SOCP values and may therefore be better suited for carbon sequestration. The overall average SOCP showed 32.12 Mg C ha-1 for cultivated areas. A rise in arable land was accompanied by a 112,870.09 Mg C rise in SOCP. With an increase in soil organic carbon, stored carbon dioxide emissions (greenhouse gases) would be reduced by 414,233.24 Mg CO2. We should consider improving fertilization, irrigation methods, the use of the multiple cropping index, decreasing desertion rates, appropriate crop rotation, and crop variety selection. The research highlights the significance of expanding cultivated areas towards sustainable carbon sequestration and the climate-change-mitigation potential.
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页数:19
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