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首页> 外文期刊>Eurasian Soil Science >Soil carbon stocks along an altitudinal gradient in different land-use categories in Lesser Himalayan foothills of Kashmir
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Soil carbon stocks along an altitudinal gradient in different land-use categories in Lesser Himalayan foothills of Kashmir

机译:在克什米尔较小的喜马拉雅山麓的不同土地使用类别沿着一直梯度的土壤碳股

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摘要

The carbon sequestration potential of soils plays an important role in mitigating the effect of climate change, because soils serve as sinks for atmospheric carbon. The present study was conducted to estimate the carbon stocks and their variation with altitudinal gradient in the Lesser Himalayan foothills of Kashmir. The carbon stocks were estimated in different land use categories, namely: closed canopy forests, open forests, disturbed forests, and agricultural lands within the altitudinal range from 900 to 2500 m. The soil carbon content was determined by the Walkley-Black titration method. The average soil carbon stock was found to be 2.59 kg m(-2). The average soil carbon stocks in closed canopy forests, open forests, and disturbed forests were 3.39, 2.06, and 2.86 kg m(-2), respectively. The average soil carbon stock in the agricultural soils was 2.03 kg m(-2). The carbon stocks showed a significant decreasing trend with the altitudinal gradient with maximum values of 4.13 kg m(-2) at 900-1200 m a.s.l. and minimum value of 1.55 kg m(-2) at 2100(-2)400 m a.s.l. The agricultural soil showed the least carbon content values indicating negative impacts of soil plowing, overgrazing, and soil degradation. Lower carbon values at higher altitudes attest to the immature character of forest stands, as well as to degradation due to immense fuel wood extraction, timber extraction, and harsh climatic conditions. The study indicates that immediate attention is required for the conservation of rapidly declining carbon stocks in agricultural soils, as well as in the soils of higher altitudes.
机译:土壤的碳封存潜力在减轻气候变化的影响方面发挥着重要作用,因为土壤用作大气碳的水槽。进行本研究以估算克什米尔较小的喜马拉雅山麓的碳储存及其与高原梯度的变化。碳股在不同的土地使用类别中估计,即:封闭的冠层森林,开放森林,森林和农业土地,从900到2500米。土壤碳含量由伴游 - 黑色滴定法测定。发现平均土壤碳股票为2.59千克M(-2)。封闭树冠森林,开放林和干扰森林的平均土壤碳股分别为3.39,2.06和2.86千克M(-2)。农业土壤中的平均土壤碳股为2.03千克(-2)。碳股显示出显着降低的趋势与高度梯度,最大值为4.13千米(-2),900-1200米A.L.最低值为1.55千克M(-2),在2100(-2)400 m A.L.农业土壤显示出碳含量值最少,表明土壤耕作,过度覆盖和土壤退化的负面影响。较高海拔碳值以较高的碳值证明森林的未成熟特征,以及由于巨大的燃料木材提取,木材提取和恶劣气候条件而降解。该研究表明,在农业土壤中迅速下降的碳储存以及更高海拔的土壤,需要立即关注。

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