Spatial modelling and drivers of soil organic carbon across successional communities in tropical deciduous forests: insights from Northwest Himalayan foothills

IF 3 4区 环境科学与生态学 Q3 ENVIRONMENTAL SCIENCES Environmental Monitoring and Assessment Pub Date : 2025-04-07 DOI:10.1007/s10661-025-13953-3
Rahul Bodh, Hitendra Padalia, Divesh Pangtey, Kusum Arunachalam, Subrata Nandy, Ishwari Datt Rai
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Abstract

Soil Organic Carbon (SOC), a key component of the global carbon cycle, remains poorly understood with respect to its linkage to ecological succession. The study aimed to unravel SOC dynamics during ecological succession in a tropical deciduous forest in the foothills of the northwest Himalaya (NWH), India. Ecological parameters derived from satellite remote sensing in conjunction with field sampled SOC was used to predict soil organic carbon density (SOCD) employing four techniques viz., multiple linear regression (MLR), random forest (RF), support vector machines (SVM), and extreme gradient boosting (XGBoost). Cross-validation with hundred replications was employed to evaluate the performance of different models. Significant variability in SOCD was observed across the study area varying from 2.7 t/ha to 65.7 t/ha. The RF model with RMSE of 12.17, R2 of 0.81 and mean bias of 0.16 performed best among all the models. Vegetation parameters emerged as primary predictors, with SOC accumulation increasing alongside vegetation succession—from 24.7 t/ha in pioneer stages to 35.9 t/ha in climax community. The mature forests with dense, tall canopies and substantial biomass contribute significantly to soil carbon storage. For the majority of the tree community types, the uncertainty in predicted SOCD remained below 3 t/ha except for the post-climax community (6–9 t/ha) due to high SOCD and moisture. Study stresses on the roles of successional stages in carbon sequestration in tropical deciduous forests, underscore the importance of the protection of these communities to safeguard SOC stocks effectively.

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热带落叶森林演替群落土壤有机碳的空间模拟与驱动因素:来自西北喜马拉雅山麓的见解
土壤有机碳(SOC)是全球碳循环的重要组成部分,但其与生态演替的关系尚不清楚。本研究旨在揭示印度喜马拉雅西北山麓热带落叶森林生态演替过程中的有机碳动态。采用多元线性回归(MLR)、随机森林(RF)、支持向量机(SVM)和极端梯度提升(XGBoost) 4种技术,结合野外土壤有机碳采样,利用卫星遥感生态参数对土壤有机碳密度(SOCD)进行预测。采用100个重复的交叉验证来评价不同模型的性能。在整个研究区域,SOCD的变化幅度从2.7 t/ha到65.7 t/ha不等。其中,射频模型的RMSE为12.17,R2为0.81,平均偏倚为0.16。植被参数是土壤有机碳积累的主要预测因子,土壤有机碳积累随植被演替而增加,从早期的24.7 t/ha增加到顶极群落的35.9 t/ha。茂密、高冠层和丰富生物量的成熟森林对土壤碳储量有显著贡献。除顶极后群落(6 ~ 9 t/ha)外,大多数乔木群落类型的SOCD预测值均低于3 t/ha。研究强调了演替阶段在热带落叶森林固碳中的作用,强调了保护这些群落对有效保护有机碳储量的重要性。
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来源期刊
Environmental Monitoring and Assessment
Environmental Monitoring and Assessment 环境科学-环境科学
CiteScore
4.70
自引率
6.70%
发文量
1000
审稿时长
7.3 months
期刊介绍: Environmental Monitoring and Assessment emphasizes technical developments and data arising from environmental monitoring and assessment, the use of scientific principles in the design of monitoring systems at the local, regional and global scales, and the use of monitoring data in assessing the consequences of natural resource management actions and pollution risks to man and the environment.
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