4.7 Article

Potential Drought Mitigation Through Microbial Induced Calcite Precipitation-MICP

期刊

WATER RESOURCES RESEARCH
卷 57, 期 9, 页码 -

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2020WR029434

关键词

drought mitigation; microbially induced calcite precipitation; soil water evaporation control; clayey soil; soil water retention; soil microstructure

资金

  1. National Key Research and Development Program of China [2019YFC1509902, 2020YFC1808101, 2020YFC1808002]
  2. National Natural Science Foundation of China [41925012, 41902271, 41772280, 42007244]
  3. Fundamental Research Funds for the Central Universities

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Extreme drought events resulting from climate change have led to increased soil water loss through evaporation, prompting the introduction of MICP as an environmentally friendly method for water evaporation suppression. Experimental results demonstrate that MICP can enhance water retention capacity and inter-particle bonding of clayey soils, with key factors such as dense surface crust and calcite crystals contributing to improved soil response under drying conditions. This study improves understanding of soil-atmosphere interactions under MICP treatment and suggests potential applications of bio-mediated technologies for drought mitigation in arid regions.
Extreme drought events occur more frequently due to climate change. Soil water loss through evaporation is therefore significantly intensified. This study introduces an environment-friendly and sustainable bio-mediated technique, known as microbially induced calcite precipitation (MICP), for water evaporation suppression in clayey soils. Through lab-scale evaporation tests, we investigate the effects of cementation solution concentration (0.5, 1.0, and 1.5 mol/L) and MICP treatment procedure (one-phase and two-phase MICP methods) on both macroscale (e.g., water loss, desiccation cracking) and microscale (e.g., microstructure variations) behaviors of soils. Experimental results show that MICP is capable of improving water retention capacity and enhancing the inter-particle bonding of clayey soils. Both water evaporation rate and total water loss decrease with the increasing concentration of cementation solution and the number of MICP treatment cycle. For most testing samples, both one-phase and two-phase MICP treatment methods have a similar influence on soil properties. Further microstructure characterizations reveal four key factors contributing to the improved soil response under drying, including dense surface crust, remediated desiccation cracks, smaller pore size and residual solutes. Dense structure of surface crust suppresses the migration of water vapor into the atmosphere. Calcite crystals tend to reduce the evaporation surface if precipitated within cracks, and clog the movement of pore water if precipitated within the soil pore space. This study is expected to improve the fundamental understanding of soil-atmosphere interactions under MICP treatment and provide insights into the potential application of bio-mediated technologies as a nature-based solution for drought mitigation in arid and semi-arid region.

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