Permeability characteristics of lime treated marine clay   总被引：1，自引：0，他引：1  

G. Rajasekaran  S. Narasimha Rao 《Ocean Engineering》2002,29(2):113-127

An attempt has been made to investigate the lime induced permeability changes in the permeability and engineering behavior of different lime column treated soil systems. Lime columns treated marine clay shows an increase in permeability up to a maximum value of 15–18 times that of untreated soil with time. The shear strength of the treated soil systems show an increment up to 8–10 that of untreated soil within a period of 30–45 days curing. In the case of lime injection systems, the permeability has been increased up to 10–15 times that of untreated soil, whereas the strength of the soil has been higher by 8–10 times that of untreated soil. Further, consolidation tests show a reduction in the compressibility up to 1/2–1/3 of original values. The test results revealed that both lime column and injection techniques could be used to improve the behaviour of underwater marine clay deposits.  相似文献   

裙带菜(Undaria pinnitifida)色素蛋白复合物的分离及光谱特性的初步研究   总被引：5，自引：2，他引：5  

刘洪艳  王广策  侯和胜  曾呈奎 《海洋与湖沼》2004,35(3):284-288

以褐藻裙带菜(Undaria pinnatifida)为实验材料，采用蔗糖密度梯度超速离心的方法纯化类囊体膜；以去污剂sDs为增溶剂(SDS：Chl=20：1，4℃增溶20min)，再用蔗糖密度为60％、50％、40％、30％、20％、15％和10％的梯度离心法，从裙带菜中成功地分离出5条含色素的蛋白质复合物带。离心结果显示在离心管顶部没有任何颜色，表明经过SDS增溶没有产生游离色素，纯化的类囊体膜和5条色素条带进行吸收光谱分析，显示了属于叶绿素n(Chl-a)的吸收峰：418、436和667到672nm。叶绿素c(Chl-c)的吸收峰：615和620nm。荧光发射最高峰位于682到690nm的区域。荧光激发光谱显示有Chl-a和Chl-c的激发峰，40％层带所含有的色素复合物只有属于Chl．n的吸收峰。分析结果表明：10％、15％层带所含有的色素复合物是褐藻的捕光色素复合物；20％、30％层带所含有的色素复合物是浅绿色的PSⅡ复合体(仍然含有捕光色素)，40％层带所含有的色素复合物是深绿色PSⅠ复合体，50％层带所含有的色素复合物是没有被增溶的类囊体膜。  相似文献   

Possible evidence for enrichment of trace elements in the hydrous manganese oxide phases of suspended matter from an urbanized embayment     

Richard A. Feely  Gary J. Massoth  Anthony J. Paulson  James F. Gendron 《Estuarine, Coastal and Shelf Science》1983,17(6):693-708

Total and weak-acid-soluble trace elements in suspended matter from the Duwamish River and Elliott Bay were determined from samples collected in February and September 1980. The results indicate that Mn scavenging in the water column is coincident with enrichments of Cr, Ni, Cu, Zn, and Pb in the suspended matter, suggesting a possible enrichment of these trace elements in a hydrous Mn oxide phase. This process occurs primarily in the sub-surface waters of Elliott Bay. Since mass balance calculations show a net export of Mn out of the bay, this mechanism may be an important means of transporting toxic trace metals from polluted estuaries and embayments to cleaner coastal environments.  相似文献   

Geographical and temporal variation in levels of organochlorine contaminants in marine mammals   总被引：1，自引：0，他引：1  

Aguilar A  Borrell A  Reijnders PJ 《Marine environmental research》2002,53(5):425-452

The interpretation of the spatial and temporal patterns of variation in organochlorine concentrations in marine mammal populations is complex because of the lack of wide-scale, long-term surveys. Therefore the results from several surveys must be combined and this causes undesired heterogeneity due to differences in the sampling and analytical techniques used and in the biological characteristics of the individuals sampled. Moreover, information is not homogeneously distributed in either space or in time. Most research is concentrated in western Europe, northern America and certain areas of Asia, while it is extremely limited or non-existent in Africa and most regions of the southern hemisphere. Marine mammals from the temperate fringe of the northern hemisphere, particularly fish-eating species which inhabit the mid-latitudes of Europe and North America, show the greatest organochlorine loads; noteworthy are the extremely high levels found in the Mediterranean Sea and certain locations on the western coasts of the United States. Concentrations in the tropical and equatorial fringe of the northern hemisphere and throughout the southern hemisphere are low or extremely low. The polar regions of both hemispheres showed the lowest concentrations of DDTs and PCBs, although levels of HCHs, chlordanes and HCB were moderate to high in the cold waters of the North Pacific. During recent decades, concentrations have tended to decrease in the regions where pollution was initially high but they have increased in regions located far from the pollution source as a consequence of atmospheric transport and redistribution. It is expected that the Arctic and, to a lesser extent, the Antarctic, will become major sinks for organochlorines in the future; this process may already be significant for some compounds such as HCB and HCHs. Effort should be devoted to both assessment of organochlorine trends in the now highly polluted populations of the temperate fringe of the northern hemisphere and to the implementation of long-term monitoring of marine mammal populations inhabiting polar regions.  相似文献   

白酒中几种含氮杂环化合物     

薛长湖  李兆杰  肖辉  岑雪梅 《中国海洋大学学报(自然科学版)》1994,(3)

实验确定了分析白酒中含氮杂环化合物的最佳条件：含氮杂环化合物在ｐＨ１～２的条件下成盐，酒样浓缩１０倍后以乙醚萃取除去中性杂质和酸性杂质，将样品ｐＨ再调至９，用乙醚萃取后ＫＤ浓缩，取样品进行气相色谱分析。以上述条件测定了茅台酒等６种名酒中的含氮化合物，发现各种酒中均有含氮杂环化合物存在，但因酒型的差别，化合物含量和组成模式相差较大。  相似文献   

季铵盐类化合物灭杀赤潮异弯藻的实验研究   总被引：29，自引：2，他引：29       下载免费PDF全文

曹西华  俞志明 《海洋与湖沼》2003,34(2):201-207

通过对几种不同结构的季铵盐类化合物对赤潮异弯藻的去除效率进行比较，发现具有一定结构的季铵盐类化合物对该种藻具有较强的灭杀去除效果；在相同用量（质量）下，含有一个长碳链的季铵盐化合物的灭杀效果明显高于含有双长链的季铵盐化合物。同时，通过测定十六烷基三甲基溴化铵作用下的赤潮异弯藻的叶绿素含量变化和光合作用强度，并借用透射电镜研究了受肋迫藻细胞的亚显微结构，从而分析了季铵盐类化合物灭杀赤潮生物的原理：季铵盐对赤潮异弯藻的“毒性“主要是由于其强表面活性，易于吸附在藻细胞的磷脂双分子膜结构的表面，从而引起膜结构的破坏和功能的丧失，进而导致细胞死亡。  相似文献   

海产腹足类性畸变现象的形态特征   总被引：19，自引：1，他引：19  

施华宏  黄长江 《台湾海峡》2001,20(4):552-555,T007

本文选取我国东南沿海的重要港口海口、北海、湛江、汕头和厦门港等作为海产腹足类性畸变现象的现场调查区，结果发现有11种海产腹足类存在性畸变。文中对分布广泛、易采集、性畸变现象普遍的疣荔枝螺的性畸变特征的解剖观察结果进行了详细的描述，同时对其他几种海产腹足类性畸变特性作了对比。根据研究结果将疣荔枝螺性畸变雌体的阴茎和输精管的畸变程度划分为5个阶段。  相似文献   

海水中大分子有机质对铂族元素的吸附动力学研究     

刘凯  高学鲁  邢前国  陈夫山 《海洋学报(英文版)》2019,38(8):8-16

Adsorption kinetics of the interaction between Pt, Pd and Rh(defined here as platinum group elements, PGEs)ions and macromolecular organic compounds(MOCs, 10 kDa), including humic acid, carrageenan and bovine serum albumin, and different cutoff fractions of natural organic matter(1 kDa and 3 kDa) obtained from seawater using centrifugal ultrafiltration devices were investigated. For a given element, all the adsorption kinetics did not reach equilibrium except the interaction between Pt and 1 kDa cutoff, and between Pd and humic acid.For all the tested MOCs, the adsorption kinetics could be divided into two stages, a rapid adsorption process in the first 8 h and the desorption stage after the first 8 h until the equilibrium. The change trend of partition coefficient(log_(10)K_d) values with experiment time was consistent with that of the kinetic curves. However, in the interaction between PGE ions and natural dissolved organic matter(NDOM), an obvious difference in the change trends of log_(10)K_d and kinetic curves was observed. It indicated that the partition behavior of PGE ions interacting with NDOM in seawater was a combined effect of different organic constituents. The adsorption and log_(10)K_d of PGEs in the 1 kDa NDOM fraction were higher and more stable than those in the 3 kDa NDOM fraction. The results also indicated that the 1–3 kDa NDOM may dominate the interaction between PGEs ions and NDOM. Moreover, no kinetic model could perfectly simulate the adsorption process. It indicated that the colloidal struction and morphology of MOCs or NDOM in seawater might be inhomogeneous. Hence, the interaction between PGE ions and organic matter in seawater was a complicated process and needs further research.  相似文献   

盐度和腐殖酸共同作用下的长江口泥沙絮凝过程研究   总被引：5，自引：2，他引：3       下载免费PDF全文

刘启贞  李九发  徐灿华  戴志军  李道季 《海洋学报》2008,30(3):140-147

长江河口有机质含量丰富,盐度变化较大,因此研究长江河口以细颗粒泥沙为主的多因子共同作用下的絮凝有助于了解最大浑浊带的形成机制.通过实验研究盐度和腐殖酸共同作用对长江口细颗粒泥沙浊度变化影响的过程,从浊度相对变化率、絮团粒径和电位变化三方面综合分析了其絮凝机理,并且对絮凝体进行了红外和电镜分析,探讨了絮凝体的微观结构.结果表明:(1)随着盐度增大细颗粒泥沙浊度相对变化率逐渐增大,粒径增大,而电位绝对值变小;(2)随着腐殖酸浓度增大细颗粒泥沙浊度相对变化率先略有升高后迅速降低,粒径增大,电位绝对值增大;(3)微观结构的分析表明腐殖酸是以腐殖酸盐的形式包覆在泥沙表面,同时也验证了河口中C-P-OM(C代表黏土,P代表阳离子,OM代表有机化合物)的泥沙絮凝模式.  相似文献   

Organic-Inorganic Interaction Recorded by Polycyclic Aromatic Steranes in Continental Epithermal Ore Deposits     

XU Huiyuan  LIU Quanyou  JIN Zhijun  ZHU Dongy  MENG Qingqiang  LI Pengpeng  ZHU Biqing 《《地质学报》英文版》2023,97(1):327-336

Continental epithermal ore deposits are commonly associated with sedimentary organic matter, oils or solid bitumen. These organics embedded in mineral deposits can convey valuable information of the ore genesis. However, the extent to which the formation of ore minerals was recorded by organic compounds remains largely unknown, as also is how metal-rich ores interfere with the molecular proxies in the temperature regime envisaged for hydrothermal activity. The molecular compositional changes of ...  相似文献