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首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Effects of snowfall depth on soil physical-chemical properties and soil microbial biomass in moss-dominated crusts in the Gurbantunggut Desert, Northern China
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Effects of snowfall depth on soil physical-chemical properties and soil microbial biomass in moss-dominated crusts in the Gurbantunggut Desert, Northern China

机译:降雪深度对北方Gurbantunggut沙漠中苔藓主导地壳中土壤物理化学性质及土壤微生物生物量的影响

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摘要

Winter snowfall is an important source of moisture that may influence the growth and development of biological soil crusts (BSCs) in temperate desert regions of China. Yet there is still limited empirical knowledge about the effect of snowfall on BSCs. In this study, moss crusts from the Gurbantunggut Desert were exposed to five snow depths to evaluate how snowfall affected the physical-chemical properties (pH; electric conductivity, EC; soil organic carbon, SOC; total nitrogen, TN; available nitrogen, AN; available phosphorus, AP; available potassium, AK) and microbial biomass (soil microbial biomass carbon, SMBC; soil microbial biomass nitrogen, SMBN; soil microbial biomass phosphorus, SMBP) of soil in the BSCs, before (in October 2016: representing three consecutive years of snow manipulation) and after winter (in April 2017). Results showed that the soil water content increased significantly as snowfall depth increased (p & 0.05) in October 2016 and April 2017. Most of the soil physical-chemical features (EC, SOC, TN, AN, AP, and AK) and microbial biomass (SMBC and SMBN) showed an increase with an increase of snowfall depth after three consecutive years of snow manipulation. Moreover, for most experimental treatments, after a winter of melting snow (in April 2017) most of the soil properties were significantly higher (p & 0.05) than found in October 2016. Together, these results showed that the dynamics of soil nutrients and microbial biomass in moss BSCs were affected by snowfall depth in Gurbantunggut Desert. Different snowfall depths can have different effects on the dynamics of soil nutrients and microbial biomass of moss crusts, an impact that may alter the future growth and development of BSCs. Thus, we suggest that the potential influence of snowfall depth on soil nutrients and microbial biomass dynamics in BSCs require consideration when discussing the effects of moisture on ecological functions of BSCs in arid and semi-arid regions.
机译:冬季降雪是影响我国温带沙漠地区生物土壤结皮生长发育的重要水分来源。然而,关于降雪对平衡计分卡影响的经验知识仍然有限。在这项研究中,将古尔班通古特沙漠的苔藓结皮暴露在五个积雪深度,以评估降雪如何影响物理化学性质(pH;电导率,EC;土壤有机碳,SOC;全氮,TN;有效氮,AN;有效磷,AP;有效钾,AK)和微生物生物量(土壤微生物生物量碳,SMBC;土壤微生物生物量氮,SMBN;土壤微生物生物量磷,SMBP)在冬季(2017年4月)之前(2016年10月:代表连续三年的降雪)和之后的BSC中的土壤。结果表明,2016年10月和2017年4月,随着降雪深度的增加,土壤含水量显著增加(p;0.05)。在连续三年的降雪处理后,大多数土壤物理化学特征(EC、SOC、TN、AN、AP和AK)和微生物生物量(SMBC和SMBN)都随着降雪深度的增加而增加。此外,对于大多数试验处理而言,在冬季冰雪融化(2017年4月)后,大多数土壤性质显著高于2016年10月的水平(p;0.05)。总之,这些结果表明,在古尔班通古特沙漠,土壤养分和苔藓生物量的动态受降雪深度的影响。不同的降雪深度会对土壤养分和苔藓结皮微生物生物量的动态产生不同的影响,这种影响可能会改变BSC未来的生长和发展。因此,我们建议,在讨论干旱和半干旱地区水分对BSC生态功能的影响时,需要考虑降雪深度对BSC中土壤养分和微生物生物量动态的潜在影响。

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