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首页> 外文期刊>Estuarine Coastal and Shelf Science >Mapping soil carbon stocks in an oceanic mangrove ecosystem in Karimunjawa Islands, Indonesia
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Mapping soil carbon stocks in an oceanic mangrove ecosystem in Karimunjawa Islands, Indonesia

机译:印度尼西亚Karimunjawa群岛海洋红树林生态系统中土壤碳储量的绘图

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Mangrove ecosystems store large amounts of carbon in biomass and sediments. This so called 'blue carbon' that is captured by oceanic and coastal ecosystems plays an important role in climate change mitigation strategies. However, most biomass and carbon measurements have been conducted in coastal and delta mangroves, while oceanic mangroves are still insufficiently researched. In this paper we present results from our research on the Karimunjawa archipelago in the Java Sea north of Central Java, Indonesia, where we measured soil carbon stocks (soil total organic carbon - TOC) of an oceanic mangrove ecosystem. In previous research, we had already analyzed above-ground carbon (AGC) and below-ground biomass carbon (BGBC), so that we are now able to present the total ecosystem carbon stock. We took 35 soil samples along seven transects to analyze the relationship between (a) soil TOC and distance from shoreline, (b) total ecosystem carbon stock (AGC + BGBC + soil TOC) and distance from shoreline, (c) total C of living biomass (AGC + BGBC) and distance from shoreline, as well as (d) soil TOC and living biomass. We took another nine soil samples to analyze the distribution of soil TOC in the soil profile at a greater resolution. Our results show that there is a wide range of soil carbon stocks that varies from 3.3 t C ha(-1) to 366.7 t C ha(-1). On average of the 35 samples soils contribute to 45.5% of the total ecosystem carbon stock. Overall there is no correlation between the analyzed variables. However, there is a correlation between distance from the shoreline and soil carbon stock for the longest transect and a strong relationship between soil depth and soil carbon stock for all samples. Carbon stock per increment decreases with a conspicuous drop at 15 cm.
机译:红树林生态系统在生物质和沉积物中存储大量碳。被海洋和沿海生态系统捕获的所谓的“蓝色碳”在缓解气候变化战略中发挥着重要作用。然而,大多数生物量和碳的测量是在沿海和三角洲的红树林中进行的,而海洋红树林的研究还很不足。在本文中,我们介绍了在印度尼西亚中爪哇省北部爪哇海的Karimunjawa群岛上进行的研究所得的结果,在该群岛中,我们测量了海洋红树林生态系统的土壤碳储量(土壤总有机碳-TOC)。在先前的研究中,我们已经分析了地上碳(AGC)和地下生物质碳(BGBC),因此我们现在能够显示生态系统碳的总储量。我们沿着七个样带抽取了35个土壤样本,分析了(a)土壤TOC与距海岸线的距离,(b)生态系统碳总量(AGC + BGBC +土壤TOC)与距海岸线的距离,(c)生活总C之间的关系。生物量(AGC + BGBC)和距海岸线的距离,以及(d)土壤TOC和生物量。我们还抽取了九个土壤样本,以更高的分辨率分析了土壤中TOC在土壤剖面中的分布。我们的结果表明,土壤碳储量范围很广,从3.3 t C ha(-1)到366.7 t C ha(-1)。在35个样本中,土壤平均占生态系统总碳储量的45.5%。总体而言,分析变量之间没有相关性。但是,对于最长的样带,距海岸线的距离与土壤碳储量之间存在相关性,而对于所有样本而言,土壤深度与土壤碳储量之间存在很强的关系。每次增加的碳储量随着15 cm处的明显下降而减少。

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