hat
Li enpòtan pou distenksyon ant sous lokal kabòn (CO.)2 sekèstre dirèkteman nan atmosfè a oswa kolòn dlo) ak kabòn soti nan lòt zòn (CO2 fiks yon lòt kote nan peyizaj la ki transpòte ak depoze sou sit). Pli lwen, pwojè yo ta dwe kont pou sous enpòtan yo ak lavabo nan CO2 (kabòn), CH4 (metàn), ak N2O (protoksid oksid) akòz aktivite pwojè ak aksyon ki rezilta nan dezòd nan rezèv sediman oswa idroloji modifye ki rezilta nan ki tou pre enfimyè gaz emisyon (flit ekolojik). Pwosedi pou distenksyon ak kontablite pou kabòn otokon ak alochthonous yo bay nan la VCS Methodology pou Tideal Wetland ak Seagrass Restorasyon.
eng
It is important to differentiate between local sources of carbon (CO2 sequestered directly from the atmosphere or water column) and carbon from other areas (CO2 fixed elsewhere in the landscape that is transported and deposited on site). Further, projects should account for significant sources and sinks of CO2 (carbon dioxide), CH4 (methane), and N2O (nitrous oxide) due to project activities and actions that result in disruption of sediment supply or modified hydrology that result in nearby greenhouse gas emissions (ecological leakage). Procedures for distinguishing and accounting for autochthonous and allochthonous carbon are provided within the VCS Methodology for Tidal Wetland and Seagrass Restoration.