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The spatial distribution of soil organic carbon in tidal wetland soils of the continental United States

机译:美国大陆潮湿地土壤有机碳的空间分布

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Tidal wetlands contain large reservoirs of carbon in their soils and can sequester carbon dioxide (CO2) at a greater rate per unit area than nearly any other ecosystem. The spatial distribution of this carbon influences climate and wetland policy. To assist with international accords such as the Paris Climate Agreement, national-level assessments such as the United States (U.S.) National Greenhouse Gas Inventory, and regional, state, local, and project-level evaluation of CO2 sequestration credits, we developed a geodatabase (CoBluCarb) and high-resolution maps of soil organic carbon (SOC) distribution by linking National Wetlands Inventory data with the U.S. Soil Survey Geographic Database. For over 600,000 wetlands, the total carbon stock and organic carbon density was calculated at 5-cm vertical resolution from 0 to 300 cm of depth. Across the continental United States, there are 1,153-1,359 Tg of SOC in the upper 0-100 cm of soils across a total of 24945.9 km(2) of tidal wetland area, twice as much carbon as the most recent national estimate. Approximately 75% of this carbon was found in estuarine emergent wetlands with freshwater tidal wetlands holding about 19%. The greatest pool of SOC was found within the Atchafalaya/Vermilion Bay complex in Louisiana, containing about 10% of the U.S. total. The average density across all tidal wetlands was 0.071 g cm(-3) across 0-15 cm, 0.055 g cm(-3) across 0-100 cm, and 0.040 g cm(-3) at the 100 cm depth. There is inherent variability between and within individual wetlands; however, we conclude that it is possible to use standardized values at a range of 0-100 cm of the soil profile, to provide first-order quantification and to evaluate future changes in carbon stocks in response to environmental perturbations. This Tier 2-oriented carbon stock assessment provides a scientific method that can be copied by other nations in support of international requirements.
机译:潮湿地含有土壤中的大量碳储存,可以以比几乎任何其他生态系统更大的速率释放二氧化碳(CO2)。这种碳的空间分布影响了气候和湿地政策。协助国际协议,如巴黎气候协议,美国(美国)国家温室气体库存等国家级评估,以及地区,州,地方和项目级别评估二氧化碳封存信用,我们开发了一个地理数据库(CoBlucarb)和土壤有机碳(SoC)分布的高分辨率地图通过将国家湿地与美国土壤调查地理数据库联系起来。对于超过60,000次湿地,总碳储备和有机碳密度以5cm的垂直分辨率计算为0至300cm的深度。在美国大陆,在潮湿地区共24945.9公里(2)个潮汐地区,有1,153-1,359吨SOC,遍布潮湿地区的两倍,碳的两倍是最近的国家估计。在河口涌动湿地中发现大约75%的碳,淡水潮湿地持有约19%。在路易斯安那州的阿特希非拉亚/朱梅里昂湾综合体中找到了最大的SoC池,占美国总共约10%。在100cm深度下,在0-100cm,0.055g cm(-3)上的所有潮汐湿地的平均密度为0.071g cm(-3),在100cm深度下为0.040g cm(-3)。各个湿地之间的固有变异性;然而,我们得出结论,可以在0-100厘米的土壤轮廓范围内使用标准值,以提供一定量级的量化,并评估碳储存的未来变化以应对环境扰动。这款导向的面向2级碳股票评估提供了一种科学方法,可以由其他国家复制,以支持国际要求。

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