Preliminary study on carbon fluxes from land change in a subtropical watershed of China

Ye Shen, Jinliang Huang, Hongyou Hu
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Abstract

This study represents a watershed-scale study of C fluxes from land change in the Jiulong River watershed, a subtropical watershed in Southeast China. Land-cover maps of woodland, cropland, orchard, built-up, water, and barren from 1986, 1996, 2002, 2007, 2010 were produced using a combination of unsupervised classification and spatial reclassification based on manual on-screen digitizing. Intensity analysis was then used to identify the dominant and systematic transitions. C fluxes from land change over three decades of imagery were estimated from the transitions among woodland, cropland, built and orchard for each time period. C accumulation and losses from terrestrial biomass are derived from observed changes in land cover. The ecological method used in this study considered that the amount of C emitted to the atmosphere is a function of the amount of C stored in terrestrial vegetation and the areal extent of each land-use category, combined with key terms of biomass, annual carbon gain, and burning efficiency. The results indicate that the trend of LUCC in Jiulong River watershed can produce a considerable potential of function as an important Carbon sink in south-eastern China, the net amount of carbon stored can be 4.50×104 t, 1.86×105 t, 9.21×105 t, 1.35×105 t for 1986–1996, 1996–2002, 2002–2007, and 2007–2010, respectively. The findings of this study enable us to gain a broad understanding of watershed-scale C fluxes from land change in a subtropical watershed of China.
中国亚热带流域土地变化碳通量的初步研究
本文对中国东南亚热带九龙江流域土地变化引起的碳通量进行了流域尺度的研究。采用无监督分类和基于人工屏幕数字化的空间再分类相结合的方法,制作了1986年、1996年、2002年、2007年、2010年的林地、农田、果园、建成区、水域和荒地土地覆盖图。然后使用强度分析来确定主导和系统的转变。根据每个时期林地、农田、建筑和果园之间的转换,估算了30年影像中土地变化带来的碳通量。陆地生物量的碳积累和损失来源于观测到的土地覆盖变化。本研究采用的生态学方法认为,向大气排放的碳量是陆地植被中储存的碳量和每个土地利用类别的面积范围的函数,并结合生物量、年碳增益和燃烧效率等关键术语。结果表明,九龙江流域土地利用变化趋势具有作为中国东南地区重要碳汇的潜力,1986-1996年、1996-2002年、2002-2007年和2007-2010年的净碳储量分别为4.50×104 t、1.86×105 t、9.21×105 t、1.35×105 t。本研究结果使我们对中国亚热带流域土地变化引起的流域尺度碳通量有了更广泛的认识。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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