The carbon cycle of sandy lands in China and its global significance

被引：42

作者：

Qi F. ^{[1
,2
]}

Guoduong C. ^{[1
]}

Masao M. ^{[2
]}

机构：

[1] Lanzhou Institute of Glaciology and Geocryology, Chinese Academy of Sciences

[2] Meteorological Research Institute of Japan, Tsukuba Ibaraki 305

来源：

Climatic Change | 2001年 / 48卷 / 4期

基金：

中国国家自然科学基金;

关键词：

Atmosphere; Organic Carbon; Carbon Content; Soil Layer; Conversion Rate;

D O I：

10.1023/A:1005664307625

中图分类号：

学科分类号：

摘要：

The quantitative C dynamics of desertified lands in Northern China were predicted for the years 2000 and 2030, based on the areas and conversion rates (positive and negative) of desertified lands in the past forty years and organic carbon contents of soils. The top 1.0 m soil layer of natural desertified lands in China contained some 7,841 Tg of organic carbon as of 1992. In China, over the last 40 years, a total of 2,812 Tg of organic carbon was released from desert lands and, in the reverse process about 644 Tg of organic-C were fixed into lands undergoing desertification. Thus, China's desert lands have shown a net release of 2,168 Tg of organic-C over the past 40 years, equivalent to 7,949 Tg of CO2. By the year 2000, the area of desertified lands in China had increased 40,300 km2 and released 368 Tg of organic-C into the atmosphere. By 2030 this area will increase to 249,700 km2 and release about 1,996 Tg of organic-C into the atmosphere. Net releases of 151 Tg and 1,243 Tg of organic-C can be expected by the year 2000 and 2030, respectively. This would be equivalent to a net release of 553 Tg of CO2 by 2000 and 4,558 Tg by 2030. Thus, the organic carbon released through land desertification in China could be an important factor affecting changes in concentrations of greenhouse gases worldwide.

引用

页码：535 / 549

页数：14

共 36 条

[21]

Schlesinger W.H., Soil organic matter: Sources of atmospheric CO2, Role of Terrestrial Vegetation in the Global Carbon Cycle. Measurement by Remote Sensing, pp. 11-127, (1984)

[22]

Schlesinger W.H., Adrienne P.M., Plant-soil interactions in deserts, Biogeochemistry, 42, pp. 169-187, (1998)

[23]

Spain A.V., Influence of environmental conditions and some soil chemical properties on the carbon and nitrogen contents of some tropical Australian rainforest soils, Aust. J. Soil Res., 28, pp. 823-833, (1990)

[24]

Turner D.P., Lee J.J., Koerper G.J., Barker J.R., The forest sector carbon budget of the United States, Carbon Pools and Flux under Alternative Policy Options, (1993)

[25]

Wang B.Z., The situation of observation on global atmospheric CO2 concentration, Geogr. Sci. Progr., 9, pp. 14-20, (1994)

[26]

Wang B.Z., The main progress of studying the greenhouse atmosphere in China, Greenhouse Gases Concentration and Emission Observation and Its Relation Process, pp. 1-5, (1996)

[27]

Watson R.T., Greenhouse gases and aerosols, Climate Change, the IPCC Scientific Assessment, pp. 1-40, (1990)

[28]

Wen Y.P., Xu X.B., Observation and investigation of variability of baseline CO2 concentration over Waliguan Mountain in Qinghai province of China, Acta Meteorol. Sinica, 8, pp. 55-60, (1994)

[29]

Wen Y.P., Xu X.B., Shao Z.Q., Measurement of atmospheric baseline CO2 with a non-ignited infrared analyzer, Quart. J. Appl. Meteorol., 24, pp. 476-480, (1993)

[30]

International Operations Handbook for Measurement of Background Atmospheric Pollution, (1978)

← 1 2 3 4 →