{"title":"中国亚热带流域土地变化碳通量的初步研究","authors":"Ye Shen, Jinliang Huang, Hongyou Hu","doi":"10.1109/EORSA.2012.6261167","DOIUrl":null,"url":null,"abstract":"This study represents a watershed-scale study of C fluxes from land change in the Jiulong River watershed, a subtropical watershed in Southeast China. Land-cover maps of woodland, cropland, orchard, built-up, water, and barren from 1986, 1996, 2002, 2007, 2010 were produced using a combination of unsupervised classification and spatial reclassification based on manual on-screen digitizing. Intensity analysis was then used to identify the dominant and systematic transitions. C fluxes from land change over three decades of imagery were estimated from the transitions among woodland, cropland, built and orchard for each time period. C accumulation and losses from terrestrial biomass are derived from observed changes in land cover. The ecological method used in this study considered that the amount of C emitted to the atmosphere is a function of the amount of C stored in terrestrial vegetation and the areal extent of each land-use category, combined with key terms of biomass, annual carbon gain, and burning efficiency. The results indicate that the trend of LUCC in Jiulong River watershed can produce a considerable potential of function as an important Carbon sink in south-eastern China, the net amount of carbon stored can be 4.50×104 t, 1.86×105 t, 9.21×105 t, 1.35×105 t for 1986–1996, 1996–2002, 2002–2007, and 2007–2010, respectively. The findings of this study enable us to gain a broad understanding of watershed-scale C fluxes from land change in a subtropical watershed of China.","PeriodicalId":132133,"journal":{"name":"2012 Second International Workshop on Earth Observation and Remote Sensing Applications","volume":"16 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2012-06-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Preliminary study on carbon fluxes from land change in a subtropical watershed of China\",\"authors\":\"Ye Shen, Jinliang Huang, Hongyou Hu\",\"doi\":\"10.1109/EORSA.2012.6261167\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"This study represents a watershed-scale study of C fluxes from land change in the Jiulong River watershed, a subtropical watershed in Southeast China. Land-cover maps of woodland, cropland, orchard, built-up, water, and barren from 1986, 1996, 2002, 2007, 2010 were produced using a combination of unsupervised classification and spatial reclassification based on manual on-screen digitizing. Intensity analysis was then used to identify the dominant and systematic transitions. C fluxes from land change over three decades of imagery were estimated from the transitions among woodland, cropland, built and orchard for each time period. C accumulation and losses from terrestrial biomass are derived from observed changes in land cover. The ecological method used in this study considered that the amount of C emitted to the atmosphere is a function of the amount of C stored in terrestrial vegetation and the areal extent of each land-use category, combined with key terms of biomass, annual carbon gain, and burning efficiency. The results indicate that the trend of LUCC in Jiulong River watershed can produce a considerable potential of function as an important Carbon sink in south-eastern China, the net amount of carbon stored can be 4.50×104 t, 1.86×105 t, 9.21×105 t, 1.35×105 t for 1986–1996, 1996–2002, 2002–2007, and 2007–2010, respectively. The findings of this study enable us to gain a broad understanding of watershed-scale C fluxes from land change in a subtropical watershed of China.\",\"PeriodicalId\":132133,\"journal\":{\"name\":\"2012 Second International Workshop on Earth Observation and Remote Sensing Applications\",\"volume\":\"16 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2012-06-08\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"2012 Second International Workshop on Earth Observation and Remote Sensing Applications\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/EORSA.2012.6261167\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"2012 Second International Workshop on Earth Observation and Remote Sensing Applications","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/EORSA.2012.6261167","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Preliminary study on carbon fluxes from land change in a subtropical watershed of China
This study represents a watershed-scale study of C fluxes from land change in the Jiulong River watershed, a subtropical watershed in Southeast China. Land-cover maps of woodland, cropland, orchard, built-up, water, and barren from 1986, 1996, 2002, 2007, 2010 were produced using a combination of unsupervised classification and spatial reclassification based on manual on-screen digitizing. Intensity analysis was then used to identify the dominant and systematic transitions. C fluxes from land change over three decades of imagery were estimated from the transitions among woodland, cropland, built and orchard for each time period. C accumulation and losses from terrestrial biomass are derived from observed changes in land cover. The ecological method used in this study considered that the amount of C emitted to the atmosphere is a function of the amount of C stored in terrestrial vegetation and the areal extent of each land-use category, combined with key terms of biomass, annual carbon gain, and burning efficiency. The results indicate that the trend of LUCC in Jiulong River watershed can produce a considerable potential of function as an important Carbon sink in south-eastern China, the net amount of carbon stored can be 4.50×104 t, 1.86×105 t, 9.21×105 t, 1.35×105 t for 1986–1996, 1996–2002, 2002–2007, and 2007–2010, respectively. The findings of this study enable us to gain a broad understanding of watershed-scale C fluxes from land change in a subtropical watershed of China.