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天文轨道周期及火山活动对中上扬子区晚奥陶世-早志留世有机碳聚集的影响 被引量:12
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作者 张喜 张廷山 +6 位作者 赵晓明 祝海华 MIHAI Emilian Popa 陈雷 雍锦杰 肖强 李红佼 《石油勘探与开发》 SCIE EI CAS CSCD 北大核心 2021年第4期732-744,共13页
基于野外露头资料,通过旋回地层学、地球化学等分析方法,运用有机碳同位素组成及化学风化指标数据序列,滤波输出记录在沉积物中的天文轨道参数,探讨天文轨道周期变化及火山活动对中上扬子区晚奥陶世—早志留世有机碳聚集的影响。研究表... 基于野外露头资料,通过旋回地层学、地球化学等分析方法,运用有机碳同位素组成及化学风化指标数据序列,滤波输出记录在沉积物中的天文轨道参数,探讨天文轨道周期变化及火山活动对中上扬子区晚奥陶世—早志留世有机碳聚集的影响。研究表明,天文轨道周期驱动下的气候变化控制不同级次海平面波动,斜率周期调制的气候变化驱动海洋温盐循环,将位于高纬度区营养物质向中低纬度区转移,温盐循环是低纬度扬子区海洋生产力的主要动力。赫南特晚期海洋生产力指标Ba/Al及Ni/Al值显示,火山活动对海洋生产力贡献有限,对有机碳保存效率有显著影响;古海洋氧化还原环境指标Th/U、V/Cr及V/(V+Ni)值显示,火山活动与古海洋含氧量有显著关系,火山活动通过调节大洋含氧量来控制有机碳的保存效率,不同地区火山活动强度的差异是有机碳差异保存的重要因素。天文轨道周期驱动的有机碳输入动力及火山活动影响有机碳保存效率,二者耦合控制中上扬子区有机碳聚集。图10参74。 展开更多
关键词 旋回地层学 有机碳聚集 化学风化指标 温盐循环 火山活动 上奥陶统五峰组 下志留统龙马溪组
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黑海全新世腐泥中的有机碳聚集
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作者 S.E.Calvert 周立君 《海洋地质动态》 1998年第9期14-16,共3页
黑海被认为是全新世典型的缺氧盆地(Glenn和Arthur,1984)。因为缺氧环境促进沉积有机物质的优先贮存。这个沉积环境被用作地质记录中富含有机沉积物的聚集作用的现代模拟(Woolnough,1937)。黑海现代... 黑海被认为是全新世典型的缺氧盆地(Glenn和Arthur,1984)。因为缺氧环境促进沉积有机物质的优先贮存。这个沉积环境被用作地质记录中富含有机沉积物的聚集作用的现代模拟(Woolnough,1937)。黑海现代沉积物中有机碳的聚集速率与其有相同... 展开更多
关键词 黑海 全新世 腐泥 有机碳聚集 沉积物
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Role of Organic Matter and Carbonates in Soil Aggregation Estimated Using Laser Diffractometry 被引量:17
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作者 I.VIRTO N.GARTZIA-BENGOETXEA O.FERNANDEZ-UGALDE 《Pedosphere》 SCIE CAS CSCD 2011年第5期566-572,共7页
>Aggregation in many soils in semi-arid land is affected by their high carbonate contents.The presence of lithogenic and/or primary carbonates can also inffuence the role of soil organic matter(SOM) in aggregation.... >Aggregation in many soils in semi-arid land is affected by their high carbonate contents.The presence of lithogenic and/or primary carbonates can also inffuence the role of soil organic matter(SOM) in aggregation.The role of carbonates and SOM in aggregation was evaluated by comparing the grain-size distribution in two carbonate-rich soils(15% and 30% carbonates) under conventional tillage after different disaggregating treatments.We also compared the effect of no-tillage and conventional tillage on the role of these two aggregating agents in the soil with 30% of carbonates.Soil samples were treated as four different ways:shaking with water(control),adding hydrochloric acid(HCl) to remove carbonates,adding hydrogen peroxide(H2O2) to remove organic matter,and consecutive removal of carbonates and organic matter(HCl + H2O2),and then analyzed by laser diffraction grain-sizing.The results showed that different contributions of carbonates and SOM to aggregate formation and stability depended not only on their natural proportion,but also on the soil type,as expressed by the major role of carbonates in aggregation in the 15% carbonate-rich soil,with a greater SOC-to-SIC(soil organic C to soil inorganic C) ratio than the 30% carbonate-rich soil.The increased organic matter stocks under no-tillage could moderate the role of carbonates in aggregation in a given soil,which meant that no-tillage could affect the organic and the inorganic C cycles in the soil.In conclusion,the relative role of carbonates and SOM in aggregation could alter the aggregates hierarchy in carbonate-rich soils. 展开更多
关键词 aggregate stabilization conventional tillage grain-size distribution NO-TILLAGE semi-arid land
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