Department of Ecology and Environmental Sciences, Pondicherry University, Puducherry, 605014, India.
Environ Monit Assess. 2019 Oct 30;191(11):690. doi: 10.1007/s10661-019-7881-6.
Sequestration of atmospheric carbon-dioxide in biospheric carbon (C) pools is a key strategy towards climate change mitigation. Soil is a huge C reservoir and its storage potential varies greatly with forest types. Therefore, in the present study, the soil organic carbon (SOC) storage pattern was assessed from 70 plots laid at three selected forest types comprising seven study sites at Kanyakumari Wildlife Sanctuary, Western Ghats, India: tropical dry deciduous (TDD I and TDD II), tropical semi-evergreen (TSE I and TSE II) and tropical evergreen forest (TEF I, TEF II and TEF III) at three depths (0-10, 10.1-20 and 20.1-30 cm). Statistical analyses were performed to understand the relationships between SOC stocks with other predictor variables. The SOC stock varied markedly with forest type and site-wise. The SOC ranged from 58 (TEF III) to 123.6 (TDD I) Mg C/ha with a mean of 84.9 ± 4.4 Mg C/ha at 0-30 cm depth. SOC stock decreased, while soil bulk density increased with increase in soil depth. The TDD forest type (115.6 Mg C/ha) stocked the highest SOC compared to TEF (75.1 Mg C/ha) and TSE (68.9 Mg C/ha) forest types. Of the total SOC stock (0-30 cm), 44.2, 32.0 and 23.8% were stored in 0-10, 10.1-20 and 20.1-30 cm respectively in all the forest types. In contrast, litter C stock were high in TEF and TSE forest types and low in TDD forest type. SOC showed significant (P < 0.01) negative relationships with bulk density, litter C, and vegetation attributes. The SOC stock stored in the study sites amount to 212.9 (TEF III) to 453.6 (TDD I) Mg of CO equivalents. The present study reveals that forest type and site characteristics have a profound impact on SOC stock, which would, in turn, exert a great bearing on the ecosystem C cycling. These results would also enhance our ability to evaluate the role of these forest types in soil C sequestration and for developing and validating SOC models for tropical forest ecosystems.
将大气二氧化碳隔离在生物碳 (C) 库中是减缓气候变化的关键策略。土壤是一个巨大的 C 储存库,其储存潜力随森林类型而有很大差异。因此,在本研究中,从 70 个位于印度西高止山脉卡尼亚库马里野生动物保护区三个选定森林类型(热带干旱落叶林(TDD I 和 TDD II)、热带半常绿林(TSE I 和 TSE II)和热带常绿林(TEF I、TEF II 和 TEF III)的七个研究点)的 3 个深度(0-10、10.1-20 和 20.1-30 cm)评估了土壤有机碳 (SOC) 储存模式。进行了统计分析以了解 SOC 储量与其他预测变量之间的关系。SOC 储量随森林类型和地点而有显著差异。SOC 范围从 58(TEF III)到 123.6(TDD I)Mg C/公顷,平均值为 84.9 ± 4.4 Mg C/公顷,深度为 0-30 cm。随着土壤深度的增加,SOC 储量减少,而土壤容重增加。与 TEF(75.1 Mg C/公顷)和 TSE(68.9 Mg C/公顷)森林类型相比,TDD 森林类型(115.6 Mg C/公顷)储存的 SOC 最高。在总 SOC 储量(0-30 cm)中,44.2%、32.0%和 23.8%分别储存在所有森林类型的 0-10、10.1-20 和 20.1-30 cm 中。相比之下,TEF 和 TSE 森林类型的凋落物 C 储量较高,而 TDD 森林类型的凋落物 C 储量较低。SOC 与容重、凋落物 C 和植被属性呈显著(P < 0.01)负相关。研究地点储存的 SOC 储量为 212.9(TEF III)至 453.6(TDD I)Mg CO 当量。本研究表明,森林类型和地点特征对 SOC 储量有深远影响,这反过来又会对生态系统的 C 循环产生重大影响。这些结果还将提高我们评估这些森林类型在土壤 C 固存中的作用以及开发和验证热带森林生态系统 SOC 模型的能力。