Abstract
The quantitative C dynamics of desertifiedlands in Northern China were predicted for the years2000 and 2030, based on the areas and conversion rates(positive and negative) of desertified lands in thepast forty years and organic carbon contents of soils.The top 1.0 m soil layer of natural desertified landsin China contained some 7,841 Tg of organic carbon asof 1992. In China, over the last 40 years, a total of2,812 Tg of organic carbon was released from desertlands and, in the reverse process about 644 Tg oforganic-C were fixed into lands undergoingdesertification. Thus, China's desert lands have showna net release of 2,168 Tg of organic-C over the past40 years, equivalent to 7,949 Tg of CO2. By theyear 2000, the area of desertified lands in China hadincreased 40,300 km2 and released 368 Tg oforganic-C into the atmosphere. By 2030 this area willincrease to 249,700 km2 and release about 1,996 Tg of organic-Cinto the atmosphere. Net releases of151 Tg and 1,243 Tg of organic-C can be expectedby the year 2000 and 2030, respectively. This wouldbe equivalent to a net release of 553 Tg of CO2by 2000 and 4,558 Tg by 2030. Thus, the organiccarbon released through land desertification in Chinacould be an important factor affecting changes inconcentrations of greenhouse gases worldwide.
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Qi, F., Guoduong, C. & Masao, M. The Carbon Cycle of Sandy Lands in China and its GlobalSignificance. Climatic Change 48, 535–549 (2001). https://doi.org/10.1023/A:1005664307625
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DOI: https://doi.org/10.1023/A:1005664307625