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[1981年至2002年中国东北森林生态系统碳储量模拟]

[Simulation of carbon stocks of forest ecosystems in Northeast China from 1981 to 2002].

作者信息

Zhao Jun-Fang, Yan Xiao-Dong, Jia Gen-Suo

机构信息

Chinese Academy of Meteorological Sciences, Beijing 100081, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2009 Feb;20(2):241-9.

Abstract

Based on the forest carbon budget model for China FORCCHN, which had been improved through adding variables and modules of precipitation (rainfall and snowfall) intercepted by tree crown and of understory and litter, the spatiotemporal distribution pattern of carbon stocks of forest ecosystems in Northeast China from 1981 to 2002 were simulated. The results showed that from 1981 to 2002, the forest ecosystems in Northeast China played a role of carbon sink, and the total carbon stock was about 12.37 Pg C x a(-1), of which, the stock of vegetation and soil was 4.01 Pg C x a(-1) and 8.36 Pg C x a(-1), respectively. During the study period, the carbon stock of both vegetation and soil all had an increasing trend, and the increase of air temperature contributed more than the change of precipitation. Spatially, the carbon density of vegetation had the characteristics of high in southeast part and low in northwest part, with an average of 10.45 kg C x m(-2). Most of the forest ecosystems in Northeast China had a higher soil carbon density, with a mean value of 21.78 kg C x m(-2) and the maximum in part regions of Daxing'anling, Xiaoxing'anling, and Changbai mountains. The forest area in Northeast China accounted for 31.4% of that in the whole country, possessing an important position in China forest carbon pool. The carbon stock of vegetation and soil in the forests of Northeast China occupied 74.23% and 63.88%, and the carbon density of vegetation and soil was 2.70 and 1.22 times of that in the forests of the whole country, respectively.

摘要

基于通过添加树冠截留降水(降雨和降雪)以及林下植被和凋落物的变量和模块改进后的中国森林碳收支模型FORCCHN,模拟了1981年至2002年中国东北森林生态系统碳储量的时空分布格局。结果表明,1981年至2002年,中国东北森林生态系统发挥了碳汇作用,总碳储量约为12.37 Pg C×a⁻¹,其中植被碳储量和土壤碳储量分别为4.01 Pg C×a⁻¹和8.36 Pg C×a⁻¹。研究期间,植被和土壤的碳储量均呈增加趋势,气温升高的贡献大于降水变化。在空间上,植被碳密度具有东南部高、西北部低的特征,平均值为10.45 kg C×m⁻²。中国东北大部分森林生态系统土壤碳密度较高,平均值为21.78 kg C×m⁻²,在大兴安岭、小兴安岭和长白山部分地区达到最大值。中国东北森林面积占全国森林面积的31.4%,在中国森林碳库中占有重要地位。中国东北森林植被和土壤的碳储量分别占全国森林的74.23%和63.88%,植被和土壤的碳密度分别是全国森林的2.70倍和1.22倍。

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