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首页> 外文期刊>Estuaries and Coasts >Peat Formation Processes Through the Millennia in Tidal Marshes of the Sacramento–San Joaquin Delta, California, USA
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Peat Formation Processes Through the Millennia in Tidal Marshes of the Sacramento–San Joaquin Delta, California, USA

机译:美国加利福尼亚州萨克拉曼多-圣华金河三角洲潮汐沼泽中的泥炭形成过程经过千年。

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The purpose of this study was to determine peat formation processes throughout the millennia in four tidal marshes in the Sacramento–San Joaquin Delta. Peat cores collected at each site were analyzed for bulk density, loss on ignition, and percent organic carbon. Core data and spline fit age–depth models were used to estimate inorganic sedimentation, organic accumulation, and carbon sequestration rates in the marshes. Bulk density and percent organic matter content of peat fluctuated through time at all sites, suggesting that peat formation processes are dynamic and responsive to watershed conditions. The balance between inorganic sedimentation and organic accumulation at the sites also varied through time, indicating that marshes may rely more strongly on either inorganic or organic matter for peat formation at particular times in their existence. Mean carbon sequestration rates found in this study (0.38–0.79 Mg C ha−1 year−1) were similar to other long-term estimates for temperate peatlands.
机译:这项研究的目的是确定萨克拉曼多-圣华金河三角洲四个潮汐沼泽中整个千年的泥炭形成过程。分析在每个位置收集的泥炭芯的堆积密度,灼烧损失和有机碳百分比。核心数据和样条拟合年龄深度模型用于估算沼泽中的无机沉降,有机积累和碳固存速率。在所有地点,泥炭的堆积密度和有机质百分比随时间波动,这表明泥炭形成过程是动态的,并且对分水岭条件有反应。地点处的无机沉积和有机积累之间的平衡也随时间变化,这表明沼泽可能在存在的特定时间更强烈地依赖于无机或有机物质形成泥炭。在这项研究中发现的平均碳固存率(0.38–0.79 Mg C ha-1 year-1 )与温带泥炭地的其他长期估计值相似。

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