欢迎访问《应用生态学报》官方网站,今天是 分享到:

应用生态学报

• 研究报告 • 上一篇    下一篇

利用1∶5万土壤数据库估算浙江省土壤有机碳密度及储量

支俊俊1,荆长伟1,张操1,吴嘉平1**,倪治华2,陈红金2,徐进2   

  1. 1浙江大学环境与资源学院, 杭州 310058; 2浙江省土肥站, 杭州 310009)
  • 出版日期:2013-03-18 发布日期:2013-03-18

Estimation of soil organic carbon density and storage in Zhejiang Province of East China by using 1:50000 soil database.

ZHI Jun-jun1, JING Chang-wei1, ZHANG Cao1, WU Jia-ping1, NI Zhi-hua2, CHEN Hong-jin2, XU Jin2   

  1. (1College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China; 2Zhejiang Provincial Station of Soils and Fertilizers, Hangzhou 310009, China)
  • Online:2013-03-18 Published:2013-03-18

摘要:

土壤有机碳库作为陆地生态系统中重要的碳库之一,对于温室效应和全球变化研究具有重要意义.利用浙江省1∶5万土壤数据库,对浙江省277个土种0~100 cm土层的有机碳密度进行估算,分析了全省土壤有机碳密度和储量,以及各主要土壤类型有机碳密度和分布.结果表明: 浙江省土壤有机碳密度值主要集中在5~10 kg·m-2;山香灰土有机碳密度最高,为52.80 kg·m-2,清水砂最低,为1.82 kg·m-2;红壤和水稻土土类土壤有机碳储量最大,两者之和占浙江省土壤有机碳总储量的63.8%;浙江省土壤总面积为100784.19 km2,土壤有机碳储量为875.42×106 t,土壤有机碳平均密度为8.69 kg·m-2.通过叠加数字高程模型分析,发现土壤有机碳密度随高程、坡度和坡向的变化均呈现明显的变化趋势.
 

Abstract: As an important component of the carbon pool of terrestrial ecosystem, soil carbon pool plays a key role in the studies of greenhouse effect and global change. By using a 1:50000 soil database, the organic carbon density in the 0-100 cm layer of 277 soil species in Zhejiang Province was estimated, and the soil organic carbon (SOC) density and storage in the whole Province as well as the spatial distribution of the SOC density and storage in the main soil types of the Province were analyzed. In the whole Province, the SOC density ranged from 5 kg·m-2 to 10 kg·m-2. Among the main soil types in the Province, humic mountain yellow soil had the highest SOC density (52.80 kg·m-2), whereas fluvio-sand ridge soil had the lowest one (1.82 kg·m-2). Red soil and paddy soil had the largest SOC storages, with the sum accounting for 63.8% of the total SOC storage in the Province. The total area of the soils in the Province was 100784.19 km2, the estimated SOC storage was 875.42×106 t, and the estimated SOC density was averagely 8.69 kg·m-2. The analysis with the superposition digital elevation model showed that the SOC density presented an obvious variation trend with the changes of elevation, slope gradient, and aspect.