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Estimating the full greenhouse gas emissions offset potential and profile between rehabilitating and established mangroves

机译:估算恢复和建立红树林之间的全温室气体排放抵消潜力和外形

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Mangrove forests are extremely productive, with rates of growth rivaling some terrestrial tropical rainforests. However, our understanding of the full suite of processes underpinning carbon exchange with the atmosphere and near shore-waters, the allocation of carbon in mangroves, and fluxes of non-CO2 greenhouse gases (GHGs) are limited to a handful of studies. This constrains the scientific basis from which to advocate for greater support for and investment in mangrove restoration and conservation. Improving understanding is urgently needed given the on-going landuse pressures mangrove forests face, particularly throughout much of Southeast Asia. The current study reduces uncertainties by providing a holistic synthesis of the net potential GHG mitigation benefits resulting from rehabilitating mangroves and established forests. Rehabilitating sites from two contrasting locations representative of high (Tiwoho) and low (Tanakeke) productivity systems on the island of Sulawesi (Indonesia) were used as case studies to compare against established mangroves. A carbon budget, allocation and pathways model was developed to account for inputs (carbon sequestration) and outputs (GHG emissions of CO2, N2O and CH4) to estimate Net Ecosystem Production (NEP) and Net Ecosystem Carbon Balance (NECB). Our results indicate that while Tiwoho's rehabilitating sites and established mangroves represent a significant carbon sink (-10.6 +/- 0.9 Mg CO(2)e ha(-1) y(-1) and 16.1 Mg CO(2)e ha(-1) y(-1) respectively), the low productivity of Tanakeke has resulted in minimal reductions to date (0.7 +/- 0.3 Mg CO(2)e ha(-1) y(-1)). Including NEP from mangrove-allied primary producer communities (e.g. benthic algae) and the portion of dissolved inorganic carbon exported from mangroves (EXDIC) that remainswithin the water column may drive overall removals considerably upwards in established forests to 37.2 Mg CO(2)e ha(-1) y(-1). These values are higher than terrestrial forests and strengthen the evidence base needed to underpin the use of forest carbon financing mechanisms for mangrove restoration. (c) 2019 Elsevier B.V. All rights reserved.
机译:红树林森林非常富有成效,具有成长率媲美一些陆地热带雨林。然而,我们对与大气和岸边的碳交换碳交换的全套流程的理解,红树林中的碳分配以及非二氧化碳温室气体(GHGS)的分配限于少数研究。这限制了科学依据,倡导加强红树林恢复和保护的更多支持和投资。促进了改善的理解,迫切需要,因为正在进行的土地用地的红树林面对,特别是在东南亚的大部分地区。目前的研究通过提供恢复红树林和已建立的森林产生的净潜在温室气体缓解益处的整体综合来减少不确定性。从苏拉威病(印度尼西亚)岛上的高(Tiwoho)和低(Tanakeke)生产率系统的两个染色地点的恢复遗址被用作与既定红树林相比的案例研究。开发了碳预算,分配和途径模型,以考虑输入(碳封存)和输出(CO2,N2O和CH4的温室气体排放),以估算净生态系统生产(NEP)和净生态系统碳平衡(NECB)。我们的结果表明,虽然Tiwoho的康复部位和建立的红树林代表了一个重要的碳汇(-10.6 +/- 0.9mg CO(2)E ha(-1)y(-1)和16.1mg CO(2)E ha( - 1)y(-1)分别),丹丹的低生产率导致迄今为止的减少(0.7 +/- 0.3mg CO(2)E ha(-1)y(-1))。包括来自红树林盟友的初级生产国(例如底栖藻类)的NEP和从红树林出口的溶解无机碳(EXDIC)的部分,该部分在水柱中可以在既定的森林中大大向上推动总体去除,以37.2毫克CO(2)E HA (-1)y(-1)。这些价值观高于地面森林,并加强了支撑使用森林碳融资机制的红树林恢复所需的证据基础。 (c)2019 Elsevier B.v.保留所有权利。

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