广东雷州半岛火山岩二氧化碳矿化封存潜力评估     

李鹏春  江静练  程锦辉  赵明辉 《高校地质学报》2023,29(1):76-84

火山岩的矿物固碳作用为减少大气中的二氧化碳(CO₂)提供了一种永久性的封存解决方案,是一种经济、安全的碳捕集封存(CCS)方式。中国火山岩分布广泛,但对火山岩固碳潜力的研究还很欠缺。文章选择广东省雷州半岛火山岩为研究区,利用MapGis软件,建立雷州半岛火山岩厚度分布的矢量地理信息数据库,插值得到三维网格化数据体;基于火山岩矿化封存机制和CO₂矿化封存潜力评估方法,对雷州半岛火山岩CO₂理论矿化封存潜力进行了计算。结果表明,雷州半岛火山岩总面积约3940 km²,总体积约257 km3,CO₂理论矿化封存量在19～459亿吨之间。其中以雷南火山岩区潜力最大,理论封存量为13～326亿吨;其次为雷北遂溪县以东、湛江市西部区域的火山岩区,理论封存量为2～56亿吨;东海岛区域火山岩,理论矿化封存量虽然不大(1.5～35亿吨),但因其与周边工业排放源较近,具有较好的源汇匹配条件,具备CCS潜力。研究结果不仅对于优选封存CO₂火山岩储集区带提供重要依据,同时为未来开...  相似文献   

页岩层系不同岩矿组合试样渗透率变化规律差异及其机理分析     

尚春江  康永尚  袁晓蔷  邓泽  赵群  王红岩 《地质论评》2023,69(6):2023060006-2023060006

页岩地层垂向岩矿组合变化大,页岩气开采需要对储层进行大规模人工水力压裂改造。笔者等基于样品的全岩X-射线衍射分析,通过对不同岩矿组合的3块页岩试样进行流—固耦合物理模拟实验,获得了3点认识,反映了不同岩矿成分的页岩在不同条件微裂缝与渗透率的变化特征,以及碳酸盐矿物含量高时的影响。这一实验对于研究页岩储层在压裂过程中的变化具有探索性,对于页岩气生产具有重要的参考意义。  相似文献   

南海神狐海域水合物一维速度结构研究： 基于中—低饱和度水合物区的约束     

柳雷锋  夏少红  方允鑫  林霖  范朝焰  孙金龙  赵芳 《高校地质学报》2022,28(3):424-439

高精度OBS探测作为目前研究水合物的常用技术手段,可以获取水合物矿体精细速度结构,在研究天然气水合物饱和度、水合物资源的预测与开发等方面具有重要指导意义。然而正演模拟OBS速度结构是繁琐漫长的过程,构建合理的初始模型是后续精细结构快速成像的重要前提。本研究基于全球18个已探明地震波速度的水合物区,分析了水合物矿体内纵波速度的共性特征和影响因素,拟合了水合物矿体带纵波速度与海水深度、沉积物厚度的经验公式。综合经验公式、OBS数据与多道地震剖面,建立了神狐水合物区横向均匀初始模型,并通过射线追踪与走时拟合模拟了神狐海域的一维纵波速度结构。结果表明,神狐水合物矿体带具有高纵波速度(1.83~1.92 km/s）,游离气层具有低P波速度（1.60~1.70 km/s）,此外,基于全球的水合物速度经验公式对神狐海域速度结构模拟具有重要参考意义,有望为获取神狐海域二维/三维精确速度结构提供可靠的初始模型,进而指导水合物精细勘察与资源评估。  相似文献   

Lake level changes of Nam Co since 25 ka as revealed by OSL dating of paleo-shorelines     

《Quaternary Geochronology》2022

Many lakes in the Tibetan Plateau (TP) experienced dramatic lake level changes in the late Quaternary, as suggested by well-preserved paleo-shorelines up to ∼200 m above present lake levels. These relic shorelines provide direct geomorphic record to reconstruct past lake level fluctuation history and water volume changes, linked closely to variations in paleo-climatic controls including Asian monsoon, westerlies and glacial meltwater. In this study, 27 near-shore sediment samples from three of eight paleo-shorelines at north of Nam Co were dated by Optically Stimulated Luminescence (OSL) technique, using coarse grains of quartz and potassium feldspar.Our results indicate that: 1) S1 is the highest/most developed shoreline (+26 m). Sediment from upper part of S1 has a consistent age of ∼25 ka (nine samples from 3 gullies), suggesting a high lake level of Nam Co occurred around 25 ka. An overflow point west of Nam Co has a close elevation to that of S1 and thus limits the presence of higher lake levels; 2) sediment profile from the slightly lower S2 (+22 m) contains two parts, silty sand (6.9–8.9 ka) at the bottom and shoreline deposits atop (∼2.3 ka), suggesting Nam Co maintained a relative high lake level in the early Holocene and such lake level occurred again at about 3.0–2.0 ka; 3) In contrast to the swift variations of monsoon precipitation and glacial meltwater in the late Quaternary, water level of Nam Co remained relatively stable during the period from ∼25 ka to about early Holocene (from +26 m to +22 m), implying a continuous outflowing stage and lake infill constantly exceeds evaporation; 4) S5 (+11 m) has an age of 0.7–1.4 ka. Nam Co showed a much accelerated pace of shrinkage since about 2.0 ka in the late Holocene in roughly two steps: it dropped from +22 m to +11 m from ∼2.0 ka to 1.4 ka, and subsequently dropped another 11 m after 0.7 ka.  相似文献   

东印度洋水体输运的季节变化及相关盐度变化     

L. A. A. N. Wickramasinghe  王卫强  刘雨  M. K. Abeyratne  W. C. Hemamali  K. B. S. S. J. Ekanayake 《南京气象学院学报》2020,12(4):472-482

利用20年（1992-2012年）的ECCO2模式模拟数据,主要研究了东印度洋（EIO）水体输运的季节变化.在EIO选取3个断面,分别为赤道、80°E和6°N.研究结果表明,跨赤道和80°E的季节输运主体部分大致相补偿.跨赤道的大部分水体输运局限在上层100 m,80°E的水体输运具有复杂结构,与显著的季风流、Wyrtki Jets（WJs）、赤道潜流（EUC）等有关.6°N上层水体净输运较小,但存在较强的边界流和相对较弱的内区流.纬向流的显著变化发生在80°E.在季风盛行季节,由于WJs减弱,赤道附近的水体输运以西向的梯度流为主,上层100 m的其余区域则主要受季风流控制.同样,由于EUC减弱,西向的梯度流与次表层东向的EUC之间也存在转换.在季风转换季节,季风流减弱,WJs与EUC分别在上层100 m和次表层占主导地位.此外,本研究还讨论了与季风流、WJs和EUC相关的盐水和暖水交换,有助于了解研究区域内温度和盐度的水平和垂直结构.  相似文献   

7–4: Kupferschiefer Copper Deposits of SW Poland: Lubin-Sieroszowice District: Lat. 51°35′ N,Long. 16°6′ E     

《Ore Geology Reviews》2006,28(1-4):271

  相似文献   

海底热流长期观测系统研制进展     

杨小秋  曾信  石红才  于传海  施小斌  郭兴伟  王迎春  任自强  邵佳  许鹤华  卫小冬  陈顺  赵鹏  庞忠和 《地球物理学报》2022,65(2):427-447

浅海和俯冲海沟等海域,不仅是矿产和油气资源主潜力区,也是构造地震频发区,其浅表热流和深部温度信息对于了解板块俯冲和岩浆活动等过程至关重要.这些区域浅层地温场和热流场受到底水温度波动(BTV)强烈扰动,其背景热流需由长期观测来获取.在全面分析了国内外海底热流长期观测技术特点后,我们提出了系缆式海底热流长期观测方案,201...  相似文献   

Tectonics of the offshore Red River Fault recorded in the junction of the Yinggehai and Qiongdongnan Basins     

Lei  Chao  Ren  Jianye  Pei  Jianxiang  Liu  Bowen  Zuo  Xiang  Liu  Jiaao  Zhu  Shiguo 《中国科学:地球科学(英文版)》2021,64(11):1893-1908

Science China Earth Sciences - The Red River Fault, which originated from the southeastern margin of the Tibetan Plateau, has a great significance for obtaining a further understanding of the...  相似文献   

Water Policy Supplement 2nd World Water Forum: Session Reports: Rapporteur: F.R.Rijsberman     

《Water Policy》2001

  相似文献   

Sediment-water exchange of Mn,Fe, Ni and Zn in Galveston Bay,Texas     

《Marine Chemistry》2001,73(3-4):215-231

In-situ benthic flux studies were conducted at three stations in Upper Galveston Bay twice during March 1996 to directly measure release rates of dissolved Mn, Fe, Ni and Zn from the sediments. Results showed reproducible increases with time in both replicate light and light–dark benthic chambers, resulting in average fluxes of −1200±780, −17±12, −1.6±0.6 and −2.4±0.79 μmol m⁻² day⁻¹ for Mn, Fe, Ni and Zn, respectively. Sediment cores collected during 1994–1996 showed that surficial pore water concentrations were elevated compared to overlying water column concentrations, suggesting diffusive release from the sediments. Diffusive flux estimates of Mn and Zn agreed in direction with chamber fluxes measured on the same date, but only accounted for 5–38% of the measured flux. Diffusive fluxes of Fe agreed with measured fluxes at the near Trinity River station but overestimated actual release in the mid and outer Trinity Bay regions, possibly due to inaccurate determination of the Fe pore water gradients or rapid oxidation processes in the overlying water at these stations.In general, measured fluxes of Mn and Ni were higher in the mid Trinity Bay region and suggested a mechanism for the elevated trace metal concentrations previously reported for this region of Galveston Bay. However, the fluxes of Fe were highest in close proximity to the Trinity River, supporting the elevated Fe concentrations measured in this region during this and other studies, and decreased towards middle and outer Trinity Bay. Trace metal turnover times were between 0.1 and 1.2 days for Mn, between 1.3 and 4.6 days for Fe, and between 27 and 100 days for Ni and 12–20 days Zn, and were considerably shorter than the average Trinity Bay water residence time (1.5 years) for this period. Comparing area averaged benthic inputs to Trinity River inputs shows the sediments to be a significant source of trace metals to Galveston Bay. However, while benthic inputs of trace metals were measured, water column concentrations remained low despite rapid turnover times for Mn and Fe, suggesting removal of these metals from the water column after release from the sediments.  相似文献