{"title":"Biomass and Carbon Stock Estimation of Udawattakele Forest Reserve in Kandy District of Sri Lanka","authors":"A. Abeysekara, S. Yatigammana, K. T. Premakantha","doi":"10.31357/JTFE.V8I2.3760","DOIUrl":null,"url":null,"abstract":"Carbon dioxide has gained lot of attention in recent past as a greenhouse gas, and therefore it has a potential to affect the climate pattern of the world. Several anthropogenic activities are known to be responsible for the increased level of carbon in the atmosphere and disruption of the global carbon cycle. However, nature has its own mechanism of sequestering and storing the carbon in its “reservoirs”. Forest has the ability to sequester carbon in their biomass and reduce the rate of increase of atmospheric carbon dioxide. The carbon sequestered in the forest trees are mostly referred to as the biomass of a tree or a forest. It has been identified five carbon pools of the terrestrial ecosystem, involving biomass. The study was designed to estimate biomass stock and then the carbon stock of the Udawattakele Forest Reserve (7°17'58 \"N, 80°38'20’’E) in Kandy, Sri Lanka. Allometric equations were used to calculate biomass of trees. The total biomass stock was estimated to be 9475.56 t ha-1 (Mega gram-Mg) and the total carbon stock was estimated to be 4,453.55 t ha-1 (Mg) in the Udawattakele Forest Reserve (UFR). This amount is equivalent to 16,344.52 Mg of carbon dioxide in the atmosphere. UFR holds a moderate amount of biomass/carbon stock and the total carbon density of natural forest and plantations was found to be 36.55 Mg ha-1 and 44.89 Mg ha-1 respectively.","PeriodicalId":30404,"journal":{"name":"Journal of Tropical Forestry and Environment","volume":"35 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2019-01-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"5","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Tropical Forestry and Environment","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.31357/JTFE.V8I2.3760","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 5
Abstract
Carbon dioxide has gained lot of attention in recent past as a greenhouse gas, and therefore it has a potential to affect the climate pattern of the world. Several anthropogenic activities are known to be responsible for the increased level of carbon in the atmosphere and disruption of the global carbon cycle. However, nature has its own mechanism of sequestering and storing the carbon in its “reservoirs”. Forest has the ability to sequester carbon in their biomass and reduce the rate of increase of atmospheric carbon dioxide. The carbon sequestered in the forest trees are mostly referred to as the biomass of a tree or a forest. It has been identified five carbon pools of the terrestrial ecosystem, involving biomass. The study was designed to estimate biomass stock and then the carbon stock of the Udawattakele Forest Reserve (7°17'58 "N, 80°38'20’’E) in Kandy, Sri Lanka. Allometric equations were used to calculate biomass of trees. The total biomass stock was estimated to be 9475.56 t ha-1 (Mega gram-Mg) and the total carbon stock was estimated to be 4,453.55 t ha-1 (Mg) in the Udawattakele Forest Reserve (UFR). This amount is equivalent to 16,344.52 Mg of carbon dioxide in the atmosphere. UFR holds a moderate amount of biomass/carbon stock and the total carbon density of natural forest and plantations was found to be 36.55 Mg ha-1 and 44.89 Mg ha-1 respectively.
近年来,二氧化碳作为一种温室气体受到了广泛关注,因此它有可能影响世界的气候模式。已知若干人为活动对大气中碳含量的增加和全球碳循环的破坏负有责任。然而,大自然有它自己的机制来隔离和储存碳在它的“水库”中。森林有能力将碳封存在其生物量中,并降低大气中二氧化碳的增加速度。森林树木所吸收的碳通常被称为树木或森林的生物量。它已经确定了陆地生态系统的五个碳库,包括生物量。本研究旨在估算斯里兰卡康提市Udawattakele森林保护区(7°17′58”N, 80°38′20”E)的生物量和碳储量。利用异速生长方程计算树木生物量。Udawattakele森林保护区生物量总储量为9475.56 t ha-1 (Mega g -Mg),碳总储量为4453.55 t ha-1 (Mg)。这相当于大气中16344.52毫克的二氧化碳。天然林和人工林的总碳密度分别为36.55 Mg ha-1和44.89 Mg ha-1。