Performance of microbial-induced carbonate precipitation on wind erosion control of sandy soil

被引:122
|
作者
Maleki, M. [1 ]
Ebrahimi, S. [1 ]
Asadzadeh, F. [2 ]
Tabrizi, M. Emami [3 ]
机构
[1] Sahand Univ Technol, Fac Chem Engn, Biotechnol Res Ctr, Tabriz, Iran
[2] Urmia Univ, Fac Agr, Dept Soil Sci, Orumiyeh, Iran
[3] Sahand Univ Technol, Dept Civil Engn, Tabriz, Iran
关键词
Biocement; Microbial-induced carbonate precipitation; Soil treatment; Wind erosion control; Urease; CALCITE; DESERT; IMPROVEMENT; VELOCITIES; PARTICLES; TEMPORARY; CAPTURE; INPUT;
D O I
10.1007/s13762-015-0921-z
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Wind erosion is a serious problem throughout the world which results in soil and environment degradation and air pollution. The main objective of this study was to evaluate feasibility of microbial-induced carbonate precipitation, as a novel soil-strengthening technique, to reduce wind erosion risk of a sandy soil. For this purpose, the erosion of biocemented soil samples was investigated experimentally in a wind tunnel under the condition of wind velocity of 45 km h(-1). The weight loss of treated samples relative to the weight loss of control treatment was 1.29 and 0.16 % for low and high bacterial mix concentrations, respectively, indicating a significant improvement in erosion control in biologically treated samples. The effect of biological treatment on wind erosion control was even superior at the higher velocities. Thereafter, the penetration resistance of the surface layers as a simple index of resistance against wind erosion was measured. Significant improvements in the penetration resistance of the treated soil samples were observed. Although low bacterial mix concentrations did not significantly improve the penetration resistance of the samples, significant improvements in the penetration resistance of the treated soil samples were observed reaching to the highest measured strength (56 kPa) in high bacterial mix concentrations samples. Finally, the morphology of precipitated CaCO3 crystals using scanning electron microscopy and X-ray powder diffraction analysis showed that the CaCO3 was mainly precipitated as vaterite crystals forming point-to-point contacts between the sand granules.
引用
收藏
页码:937 / 944
页数:8
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