首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Potential of fallow chronosequence in shifting cultivation to conserve soil organic carbon in northeast India
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Potential of fallow chronosequence in shifting cultivation to conserve soil organic carbon in northeast India

机译:印度东北地区休耕时空时序的潜力以保护土壤有机碳

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摘要

Secondary forest in shifting cultivation might influence soil organic carbon (SOC) stock. However, information with respect to SOC accumulation or depletion in fallow stand with secondary forest in shifting cultivation is insufficient. We, therefore, undertaken this experiment with the objective to evaluate the impact of secondary forest on SOC stock and its allocation into pools of different oxidizability [very labile (C-VL), labile (C-L), less labile (C-LL) and nonlabile C (C-NL)] along soil depth using three fallow chronosequences of shifting cultivation located in subtropical mid-hills of northeast India. Results showed that SOC content in 0-0.45 m depth increased with age of the fallow stand [the values being 78.4, 91.5 and 102.8 Mg ha(-1) in young (5-9 years), mid-aged (18-20 years) and old (28-33 years) secondary forest, respectively] after land clearing (slashing and burning of forest) and exhaustive cropping (75.9 kg ha(-1)). There was a decrease in SOC content with increasing soil depth, constituting 49.0, 27.8 and 232% of the total (for 0-0.45 m) for 0-0.15,0.15-030 and 0.30-0.45 m, respectively. Among the analyzed C pools C-VL, C-L and C-LL were influenced by the fallow period and the active pools (C-VL + C-L) constituted 65.7% of the SOC. Most of the SOC pools were significantly correlated with each other and with fallow age. Results thus indicate that soil in shifting fallow conserves increasing amount of organic C during regeneration of forest vegetation and majority of the SOC is in active or labile pools of shorter residence time. (C) 2015 Elsevier B.V. All rights reserved.
机译:轮作中的次生林可能会影响土壤有机碳(SOC)储量。但是,关于在轮作中次生林中休耕林中SOC积累或枯竭的信息不足。因此,我们进行此实验的目的是评估次生林对SOC储量的影响及其在不同氧化性[非常不稳定(C-VL),不稳定(CL),较不稳定(C-LL)和非活泼碳(C-NL)],使用位于印度东北部亚热带中部丘陵的三个轮作耕作休耕时间序列。结果表明,0-0.45 m深度的SOC含量随着休耕林的年龄而增加[年轻(5-9岁),中年(18-20岁)的值分别为78.4、91.5和102.8 Mg ha(-1) )和旧的(28-33岁的次生林)],分别进行了土地清理(砍伐和烧毁森林)和详尽的耕作(75.9 kg ha(-1))。 SOC含量随土壤深度的增加而降低,分别为0-0.15、0.15-030和0.30-0.45 m,分别占总数的49.0%,27.8%和232%(对于0-0.45 m)。在分析的C池中,C-VL,C-L和C-LL受休止期的影响,活动池(C-VL + C-L)构成SOC的65.7%。大部分SOC池彼此之间以及与休憩年龄之间存在显着相关性。结果因此表明,休耕的土壤在森林植被更新过程中保留了增加的有机碳,并且大部分SOC处于活动时间或活动时间较短的不稳定池中。 (C)2015 Elsevier B.V.保留所有权利。

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