辽宁西部沿海地区土壤碳库构成及变化规律研究  

COMPOSITIONS AND VARIATION RULE OF SOIL CARBON POOL IN THE COASTAL AREA OF WESTERN LIAONING PROVINCE

作　　者：王诚煜 李玉超 关旭 王毅 韩岩宏 于跃 杨兵兵 WANG Cheng-yu;LI Yu-chao;GUAN Xu;WANG Yi;HAN Yan-hong;YU Yue;YANG Bing-bing(Liaoning Institute of Geology and Mineral Survey Co.,Ltd.,Shenyang 110032,China)

机构地区：[1]辽宁省地质矿产调查院有限责任公司,辽宁沈阳110032

出　　处：《地质与资源》2021年第2期173-185,135,共14页Geology and Resources

基　　金：中国地质调查局“辽宁西部沿海经济带1∶25万土地质量地球化学调查”项目(DD20160316-1).

摘　　要：基于辽宁西部沿海地区多目标地球化学调查获得的表层和深层土壤碳含量数据,计算了研究区表层(0~20 cm)、中层(0~100 cm)和深层(0~180 cm)的土壤碳密度及储量,探讨了不同分类单元的土壤碳库构成特征及固碳潜力,并对近40年来土壤有机碳变化规律进行研究.结果显示:1)研究区土壤碳库构成以有机碳为主,无机碳储量随深度增加有所增大.表层、中层和深层土壤有机碳密度分别为2.14、7.59和11.27 kg/m^(2),低于全国多目标调查区平均值和环渤海地区.2)不同分类单元土壤碳库构成具有一定差异:表层土壤元古宇和中生界单元的碳密度较大,而中层和深层表现为古生界土壤碳密度较大;山地土壤碳密度大于丘陵和平原;褐土土壤碳密度最高,潮土最低;林草地土壤碳密度最高,耕地和园地较低.3)研究区表层、中层和深层固碳潜力分别为33.91、103.32和129.37 Mt,其中有机碳的固碳潜力大于无机碳.4)近40年间,土壤有机碳总体呈增加态势,其中,耕地和园地的表层土壤总体表现为碳源效应,释放有机碳量0.29 Mt.棕壤分布区和林地分布区对土壤有机碳的输入贡献最大.Based on the surface and deep soil carbon content data obtained from multi-objective geochemical survey in the coastal area of western Liaoning Province,the paper calculates the soil carbon density and storage in surface(0-20 cm),middle(0-100 cm)and deep(0-180 cm)layers of the study area,and discusses the compositions of soil carbon pool(SCP)and carbon sequestration potential(CSP)in terms of classification,as well as the variation rule of soil organic carbon(SOC)in the last 40 years.The results show that the SCP is dominated by organic carbon,while the inorganic carbon storage increases with depth,with the soil organic carbon density(SOCD)of 2.14,7.59 and 11.27 kg/m^(2) for surface,middle and deep layers respectively,lower than the average of national multi-objective survey areas and circum-Bohai Sea area.The compositions of SCP vary in different classifications as follows:The carbon density of Proterozoic and Mesozoic units is high in surface layer,while that of Paleozoic unit is high in middle and deep layers;The soil carbon density of mountain is higher than that of hills and plain by landforms,the highest in cinnamon soil and the lowest in moisture soil by soil types,the highest in forest and grass lands and lower in cultivated land and garden by land use types.The CSPs of surface,middle and deep soils are 33.91,103.32 and 129.37 Mt,respectively,with CSP of organic carbon higher than that of inorganic carbon.The SOC was increasing generally in the last 40 years,among which the surface soil of cultivated land and garden showed carbon source effect,releasing 0.29 Mt of SOC.The distribution of brown soil and forest land contributes the most to the input of SOC.

关 键 词：土壤碳库 土壤碳储量 土壤碳密度 固碳潜力 沿海地区 辽宁省 

分 类 号：S153.6[农业科学—土壤学]