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喜马拉雅山麓14年生竹林下不稳定和稳定碳组分的积累

Build-up of labile, non-labile carbon fractions under fourteen-year-old bamboo plantations in the Himalayan foothills.

作者信息

Kaushal Rajesh, Tewari Salil, Thapliyal Shanker Dutt, Kumar Amit, Roy Trisha, Islam Sadikul, Lepcha S T S, Durai Jayaraman

机构信息

ICAR-Indian Institute of Soil and Water Conservation, 218 Kaulagarh Road, Dehradun, India.

G.B. Pant University of Agriculture and Technology, Pantnagar, India.

出版信息

Heliyon. 2021 Aug 21;7(8):e07850. doi: 10.1016/j.heliyon.2021.e07850. eCollection 2021 Aug.

DOI:10.1016/j.heliyon.2021.e07850
PMID:34485734
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8405993/
Abstract

Carbon fractions under different bamboo species ., and were evaluated to understand the potential of these different bamboo species in soil rehabilitation in Himalayan foothills. The highest accumulation of the different carbon fractions likes very labile (6.12 mg g), less labile (2.55 mg g) and non-labile (11.40 mg g) was observed under while highest labile fraction (3.17 mg g) was recorded under . The highest active (8.85 mg g) and passive pool (13.95 mg g) were recorded under . Higher carbon management index (CMI) was obtained under (186.04) which was comparable with (182.66) and (179.24). Among all the six species, had the highest buildup of active and passive pool in both the soil depths. Bamboo plantations irrespective of the different species helped in enhancing the SOC fraction and enhanced C buildup in the soil in comparison to the open fallow land and holds potential in combating the problems of land degradation and soil rehabilitation.

摘要

对不同竹种(分别为……和……)下的碳组分进行了评估,以了解这些不同竹种在喜马拉雅山麓土壤修复中的潜力。在……下观察到不同碳组分(如非常不稳定的碳组分(6.12毫克/克)、较不稳定的碳组分(2.55毫克/克)和非不稳定的碳组分(11.40毫克/克))的最高积累量,而在……下记录到最高的不稳定碳组分(3.17毫克/克)。在……下记录到最高的活性碳库(8.85毫克/克)和惰性碳库(13.95毫克/克)。在……下获得了较高的碳管理指数(CMI)(186.04),这与……(182.66)和……(179.24)相当。在所有六个竹种中,……在两个土壤深度的活性碳库和惰性碳库积累量最高。与撂荒地相比,无论何种竹种的竹林都有助于提高土壤有机碳组分,并增强土壤中的碳积累,在应对土地退化和土壤修复问题方面具有潜力。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e39b/8405993/1a3188f58399/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e39b/8405993/ec02e1076c04/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e39b/8405993/cd4c78e5dc77/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e39b/8405993/5b64891230b5/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e39b/8405993/1a3188f58399/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e39b/8405993/ec02e1076c04/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e39b/8405993/cd4c78e5dc77/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e39b/8405993/5b64891230b5/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e39b/8405993/1a3188f58399/gr4.jpg

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Carbon Balance Manag. 2018 Feb 12;13(1):4. doi: 10.1186/s13021-018-0091-7.
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