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首页> 外文期刊>Environmental earth sciences >Did Tsunami tremor jolt microbial biomass and their activities in soils? A case study in Andaman Island, India
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Did Tsunami tremor jolt microbial biomass and their activities in soils? A case study in Andaman Island, India

机译:海啸是否会震动土壤中的微生物量及其活动?印度安达曼岛的个案研究

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The nature of selected soil-chemical and microbial properties influenced by tsunami affected and non-affected areas along the border areas of the alluvial Andaman Island in India were investigated. Soils of these areas have turned saline and saline-sodic due to the ingression of sea water. The electrical conductivity of the saturation extract of the surface soil varied from 11.2 to 23.8 dS m~(-1) in 2005, and it was decreased to 0.8-10.3 dS m~(-1) in 2006 due to the heavy rain in the following year after the tsunami. Soil quality indicators, like microbial biomass C, microbial metabolic quotient, microbial respiration quotient and fluorescein diacetate hydrolyzing activity, decreased in the tsunami affected soil in 2005, but slightly increased in 2006. All microbial parameters were significantly negatively correlated with the electrical conductivity, sodium absorption ratio and exchangeable sodium percentage. Suppression of microbial biomass and their activities in the soils due to the increased-salinity is of great agronomic significance and needs suitable intervention for sustainable crop production. Significant differences were found in soil-chemical and microbial characteristics between tsunami affected and non-affected areas. Hierarchical clustering algorithm on the basis of different soil-chemical and microbial characteristics revealed that there is significant difference in grouping between tsunami affected and non-affected zones. From this study, it can be concluded that the sea water ingression detrimentally influenced the microbial properties of tsunami affected soil.
机译:考察了印度安达曼岛冲积河沿岸地区受海啸影响和未受影响地区影响的某些土壤化学和微生物特性的性质。由于海水的入侵,这些地区的土壤已变成盐渍和盐渍钠盐。 2005年表层土壤饱和浸出液的电导率从11.2 dS m〜(-1)变化到23.8 dS m〜(-1),2006年由于大雨降到0.8-10.3 dS m〜(-1)。海啸过后的第二年。受海啸影响的土壤中,微生物生物量碳,微生物代谢商,微生物呼吸商和荧光素二乙酸酯水解活性等土壤质量指标在2005年有所下降,但在2006年有所增加。所有微生物参数均与电导率,钠含量呈显着负相关。吸收率和可交换钠百分比。由于盐度增加,抑制土壤中的微生物生物量及其活动具有重要的农艺意义,需要对作物的可持续生产进行适当的干预。在受海啸影响的地区和未受灾的地区之间,土壤化学和微生物特征存在显着差异。基于不同土壤化学和微生物特征的分层聚类算法表明,受海啸影响的地区与未受灾的地区之间的分组存在显着差异。从这项研究中可以得出结论,海水入侵有害地影响了受海啸影响的土壤的微生物特性。

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