南海中部海水化学要素研究：Ⅰ.水文,生物对溶解...     

吕荣辉  杨嘉东 《海洋通报》1990,9(3):29-36

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南极夏季沿海海藻Phaeocystis Pouchetii繁殖...     

杨和福 《南极研究》1990,2(4):45-49

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盐生植物     

Yens.  NP 鲁晓云 《世界沙漠研究》1990,(3):31-35

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显生宙海水成分、碳酸盐沉积和生物演化系统研究进展   总被引：6，自引：2，他引：6  

颜佳新  伍明 《地质科技情报》2006,25(3):1-7

简述了显生宙海水成分演化的特征、识别标志和成因解释模型以及存在的问题和今后研究的方向.不同时期海水的成分的差异,特别是海水的x(Mg)/x(Ca)值,导致了文石海、方解石海时期的碳酸盐沉积和早期成岩作用均存在差异,甚至影响了盆地深部成岩流体的特征.显生宙海生生物的演替和盛衰,特别是简单生物(如钙藻和海绵)和高产率生物(如造礁生物和碳酸盐沉积物主要生产者),明显体现了海水的x(Mg)/x(Ca)值周期性变化对海生生物的影响.这种影响也同样体现在古生代末期的生物大绝灭及随后的生物复苏样式上,在生物更替事件研究中应引起重视.因此,生物与环境的协同演化研究必须从地球系统科学的角度展开.  相似文献   

Seasonal Phase-Locking of Peak Events in the Eastern Indian Ocean     

Qin ZHANG  Song YANG 《大气科学进展》2007,24(5):781-798

The sea surface temperature （SST） anomaly of the eastern Indian Ocean （EIO） exhibits cold anomalies in the boreal summer or fall during E1 Nino development years and warm anomalies in winter or spring following the E1 Nino events. There also tend to be warm anomalies in the boreal summer or fall during La Nina development years and cold anomalies in winter or spring following the La Nina events. The seasonal phase-locking of SST change in the EIO associated with E1 Nino/Southern Oscillation is linked to the variability of convection over the maritime continent, which induces an atmospheric Rossby wave over the EIO. Local air-sea interaction exerts different effects on SST anomalies, depending on the relationship between the Rossby wave and the mean flow related to the seasonal migration of the buffer zone, which shifts across the equator between summer and winter. The summer cold events start with cooling in the Timor Sea, together with increasing easterly flow along the equator. Negative SST anomalies develop near Sumatra, through the interaction between the atmospheric Rossby wave and the underneath sea surface. These SST anomalies are also contributed to by the increased upwelling of the mixed layer and the equatorward temperature advection in the boreal fall. As the buffer zone shifts across the equator towards boreal winter, the anomalous easterly flow tends to weaken the mean flow near the equator, and the EIO SST increases due to the reduction of latent heat flux from the sea surface. As a result, wintertime SST anomalies appear with a uniform and nearly basin-wide pattern beneath the easterly anomalies. These SST anomalies are also caused by the increase in solar radiation associated with the anticyclonic atmospheric Rossby wave over the EIO. Similarly, the physical processes of the summer warm events, which are followed by wintertime cold SST anomalies, can be explained by the changes in atmospheric and oceanic fields with opposite signs to those anomalies described above.  相似文献   

前言     

牟光迅 《华南地震》2006,26(1):1-1

1605年7月13日海南琼山发生7.5级强震,造成东寨港一带陆陷成海,72个村庄被海水淹没,万顷良田变沧海,各类建筑物倒毁殆尽,3300余人死亡。此次地震震中烈度Ⅹ度强,是迄今为止华南地区毁坏性最大的地震,留下了中国唯一陆陷成海的古地震遗址,形成了世界罕见的大规模“海底村庄”景观。2004年12月26日在印尼苏门答腊西北近海发生8.7级地震引发的海啸波及了亚洲和非洲至少10个国家和地区,近30万人死亡,造成了人类历史上空前的灾难和数百亿美元的经济损失。随着社会的进步、经济的快速发展,工业化、城镇化进程的不断加快,地震灾害对社会的经济影响…  相似文献   

水介质中多金属海水矿瘤砷吸附的研究     

S.Maity  S.Chakravarty  S.Bhattacharjee  B.C. Roy  赵玉军 《水文地质工程地质技术方法动态》2006,(4):28-37

本文详细报告了水介质中多金属海水矿瘤吸附砷（Ⅲ）和砷（Ⅴ）的研究结果。海水矿瘤的元素成分主要由铁、锰、硅（含有微量铝）、铜、钴和镍。海水矿瘤对砷（Ⅴ）的吸附取决于水介质的pH值，而砷（Ⅲ）的吸附不受水介质pH值的影响。砷吸附数据大体上符合兰米尔（Langmuir）等温线。砷（Ⅲ）和砷（Ⅴ）的动力学数据满足一种假定的二级动力学模型。海水矿瘤去除砷的效果取决于砷的初始浓度。当水介质中砷（Ⅲ）的初始浓度为0．34mg／L或砷（Ⅴ）的初始浓度为0．78mg／L时，海水矿瘤的最佳剂量为0．74mg／g。砷（Ⅲ）的吸附一般取决于离子环境。除PO4^3-以外，砷（Ⅲ）的吸附不受阴离子的影响，但受阳离子的影响显著。另一方面，砷（Ⅴ）的吸附受阴离子的影响显著，但不受阳离子的影响。试验结果表明，海水矿瘤吸附的砷（Ⅲ）主要为内部结核复合物，而吸附的砷（Ⅴ）为部分内部结核和部分外部结核复合物。当水介质的pH值为2-10时，吸附的砷（Ⅲ）和砷（Ⅴ）的解吸附较小。当水介质的pH值为6或更高时，海水矿瘤能被用于吸附地下水中的砷（Ⅲ）和砷（Ⅴ）物种。海水矿瘤被成功地用于去除采于印度西孟加拉邦的6种受砷污染地下水样中的砷（6种地下水样中砷的浓度范围为0．04-0．18mg／L）。  相似文献   

Major ions characteristics in a disturbed aquifer of an oceanic island——Sipadan, Malaysia     

Mohd Harun Abdullah Baba musta Mazlin Mokhtar Ahmad Zaharin Aris 《中国地球化学学报》2006,25(B08):151-152

The Sipadan island is the only oceanic island found in Malaysia, and is popularly known for its beautiful corals and diving activities. The aquifer of the island is affected by seawater intrusion associated with groundwater exploitation. Geologically, the aquifer is composed of several series of Quaternary bioherm facies, and its recharge merely depends on rainfall. This research attempts to understand the chemical changes of the groundwater attributed to the salinization processes based on major ion composition （Ca^2＋, Mg^2＋, Na^＋, K^＋, HCO, SO, Cl^-）. The initial assessments were done in years 1993 - 1994, followed by subsequent assessment in years 2004-2005. Methods of analyses were adopted from APHA （1995）. The hydrogeochemical saturation indices （SI） were computed using the PHREEQC program in order to assess the state of equilibrium between groundwater and the minerals present. The results of analyses indicated that the groundwater has been highly enriched in Na^＋, SO and CI, reflecting an encroachment of saline water into the aquifer. The groundwater facies can be classified as sodium chloride （Na-Cl） water type. There are positive correlations （moderate to strong）, except HCO3^-, between the studied parameters. The weak and inconsistent correlation of HCO3^- with the cations and anions related to dissolved salts suggests that saltwater intrusion has an insignificant impact on the chemistry of HCO3^- in the groundwater. Strong correlations （r 〉0.70） exist among the major elements （Na^＋, Mg^2＋, K^＋, Cl^- and SO4^-） and salinity （EC）. These relationships clearly identify the main elements contributing to the groundwater salinity and their tendency to depict a similar trend of salinization pattern. Chloride has a major influence on the salinity of groundwater based on the positive and strong correlation that exist between Cl^- and EC （r=0.97）.  相似文献   

西北太平洋MD06-3054孔浮游有孔虫表层海水温度估算     

仇晓华  南青云  唐正  李铁刚  陈双喜 《海洋地质与第四纪地质》2011,(3):61-68

在古海洋学研究中,常用浮游有孔虫来恢复表层海水温度(SST),然而基于浮游有孔虫恢复SST的这些方法之间存在一定的差异.为了说明各方法的特点,在浮游有孔虫鉴定和浮游有孔虫表层种Globigerinoides ruber Mg/Ca比值测试的基础上,分别利用转换函数FP12-E,现代类比(Modern Analog Te...  相似文献   

海水化学需氧量烘箱加热测定方法的研究   总被引：1，自引：0，他引：1  

沈加正  侯沙沙  刘鹰  罗荣强 《海洋科学》2011,35(8):1-4

在海水化学需氧量(COD)测定中, 利用烘箱代替海洋监测规范中的电炉对样品进行加热; 探讨了烘箱加热测定法所需的加热条件及其测定范围, 并通过实际水样测定了解此法的精确度和准确度。结果表明, 烘箱加热测定法具有与海洋监测规范方法同等水平的精确度和准确度, 并且在大批量样品测定中具有省时、省电、省力的优点, 具有较好的应用价值。  相似文献