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Study of Soil Microbiological Character at Different Altitudes in the Region of Dry and Hot River Valley

机译:干热河谷地区不同海拔高度土壤微生物学特征研究

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In this paper, soils at various altitudes in the lower reaches of the Jinshajiang River, Ningnan County, Sichuan Province, China, were selected to study the variation in characteristics of soil enzymes and soil microbial biomass and their activities at different altitudes. By laboratory testing, statistical analysis and correlation analysis, results indicated that in the dry-hot river valley region, the altitude has a significant impact on the soil microbial characteristics, including soil enzyme activities, microbial biomass, soil basal respiration intensity and substrate-induced respiration intensity (SIR). The major indicators of soil enzymes and microbial biomass exhibit an evident linear increasing trend with the rise in altitude. Soil enzymes and microbial biomass and their activities increase gradually with the reduction in dry-hot wind impact at altitudes ranging from 705-1005 m; thereafter, these indicators tend to be stable as a whole, as the altitude continues to rise and the impact of the dry-hot wind lessens. Under wet-dry cycling conditions, the main soil microbial characteristics, including soil enzyme activities, microbial biomass, soil basal respiration intensity and SIR, display an evident dry-wet seasonal change following a similar law of change; that is, the soil enzymes and microbial biomass and their activities in the dry season are significantly lower than are those in the wet season. The metabolic quotient (qCO2) in the dry season initially falls, then rises and, finally tends to be stable with the rise in altitude, whereas, in the wet season, there is no significant change in qCO2 with altitude. Further analysis shows that soil enzyme indicators, enzyme activities, soil microbial biomass and its activities in both dry and wet seasons have relatively strong correlations with soil physical and chemical properties, and, thus, can act as the indicators for soil fertility assessment. Therefore, the dry-hot wind is one of the major factors that impact soil enzymes and microbial biomass and their activities in the dry-hot river valley region along the Jinshajiang River. Technical measures should be taken, so far as is possible, during the ecological restoration to reduce the stress effects of the dry-hot wind on soil and vegetation and, thus, to promote sustainable development of regional ecological construction.
机译:本文选择了四川省宁南县金沙江下游不同海拔高度的土壤,研究了不同海拔高度土壤酶和微生物生物量的变化特征及其活性。通过实验室测试,统计分析和相关分析,结果表明,在干热河谷地区,海拔高度对土壤微生物特征有重要影响,包括土壤酶活性,微生物生物量,土壤基础呼吸强度和基质诱导呼吸强度(SIR)。土壤酶和微生物量的主要指标随着海拔的升高呈明显的线性增加趋势。随着海拔705-1005 m的干热风影响的减小,土壤酶和微生物生物量及其活性逐渐增加。此后,随着海拔的持续升高和干热风的影响减小,这些指标总体上趋于稳定。在干湿循环条件下,土壤微生物的主要特征,包括土壤酶活性,微生物生物量,土壤基础呼吸强度和SIR,遵循相似的变化规律,表现出明显的干湿季节性变化。也就是说,旱季的土壤酶和微生物生物量及其活性明显低于雨季。干旱季节的代谢商(qCO2)最初下降,然后上升,最终随着海拔的升高趋于稳定,而在潮湿季节,qCO2随海拔高度没有明显变化。进一步分析表明,旱季和湿季土壤酶指标,酶活性,土壤微生物量及其活性与土壤理化性质具有较强的相关性,可作为土壤肥力评估的指标。因此,干热风是影响金沙江干热河谷地区土壤酶和微生物生物量及其活动的主要因素之一。在生态恢复过程中应尽可能采取技术措施,以减少干热风对土壤和植被的压力影响,从而促进区域生态建设的可持续发展。

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