土壤有机碳(soc):一个评估人为和自然胁迫程度的指标

Joystu Dutta, K. Banerjee, Sangita Agarwal, A. Mitra
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引用次数: 3

摘要

在所有类型的生态系统中,地球的碳收支是由土壤隔间调节的。2017年11月,我们在以红树林为主的印度孙德尔本斯和高度城市化的加尔各答进行了一阶soc分析,目的是确定土壤中有机碳的自然和人为贡献。我们还试图分析这两个显著不同的生态系统间soc的空间差异。加尔各答的soc平均值(2.06%)高于孙德尔本斯(1.25%)。加尔各答与孙德尔本斯的社会生态系统空间差异显著(p < 0.05),这可能与人为压力有关,其中加尔各答的人为压力更大。南北加尔各答的soc空间差异显著(p < 0.05),主要是由于北部排水系统的效率和南部城市边界扩张的程度。在孙德班三角洲复合体中,侵蚀等自然现象似乎是土壤碳动力学领域的决定性因素。对包括加尔各答在内的世界上所有主要城市进行soc分析,对于了解城市土壤的固碳潜力至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil Organic Carbon (soc): A Proxy to Assess the Degree of Anthropogenic and Natural Stress
The carbon budget of planet earth is regulated by the soil compartment in all types of ecosystems. We conducted a first order analysis of soc in November 2017 both in the mangrove dominated Indian Sundarbans and the highly urbanized city of Kolkata with the aim of identifying the natural and anthropogenic contributions of organic carbon in soil. We also attempted to analyze the spatial variation of soc between these two significantly different ecosystems. We observed a comparatively higher mean value of soc in Kolkata (2.06%) than in the Sundarbans (1.25%). The significant spatial variation in soc between Kolkata and the Sundarbans (p < 0.05) may be attributed to anthropogenic stress, which is of greater magnitude in the city of Kolkata. The significant spatial variation in soc between north and south Kolkata (p < 0.05) is due to the efficiency of the drainage system in the north and the magnitude of city limit expansion in the south. In the Sundarban deltaic complex, a natural phenomenon like erosion seems to be a determining factor in the domain of soil carbon dynamics. soc analyses of all major metropolises around the world, of which Kolkata is one, are essential to understand the carbon sequestration potential of urban soils.
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