Soil hydrological process of microbiotic crusts (MC) has been a most debated problem with so much academic concerns all along.
生物结皮的土壤水文过程一直是学术界比较关注的争议性问题。
In artificial vegetation-fixed sandy dunes, microbiotic crusts always occur with stabilizing of the environmental conditions in vegetation regions.
在沙坡头人工植被固沙区，微生物结皮是伴随着植被区环境的日趋稳定而出现的。
Soil microbiotic crusts are widespread in arid and semiarid regions, they are one of the major components of desert ecosystems, and their importance has been demonstrated by numerous researches.
生物土壤结皮广泛分布在干旱半干旱地区与寒区荒漠，是荒漠生态系统的主要组成和景观特征之一，其重要性已被大量的研究报道所证实。
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