浙江北部沿海婆罗囊螺（Retusa borneensis)生态敏感因子的筛选研究   总被引：4，自引：0，他引：4  

王志铮  史海东  张义浩  严世强 《海洋与湖沼》2004,35(5):432-437

根据 2 0 0 1年 4月— 2 0 0 2年 9月间对浙江北部沿海婆罗囊螺资源生态调查与实验生态观察、生物学特性研究、敏感药物选择与区域应用实验所获资料 ,以婆罗囊螺繁殖盛期优势群体与同时期滩涂养殖主要经济种类泥螺、彩虹明樱蛤优势群体间生态耐受特性比较为基础 ,通过建立基于利比希最小因子定律和谢尔福德耐受性定律基础之上的婆罗囊螺生态敏感因子确定方法 ,对婆罗囊螺生态敏感因子及其敏感度指数进行定量分析研究。结果表明 ,婆罗囊螺6h内温度、盐度及酸碱度的最大生态幅分别为 0— 40℃、5— 65和 3.92— 9.5 ,最适生态幅分别为温度 1 0— 30℃、盐度 1 7— 35和酸碱度 5 .5— 9.5 ;各实验动物对温度、盐度及酸碱度的生态敏感度指数分别为 :婆罗囊螺呈酸碱度 >温度 >盐度 ,泥螺呈温度 =盐度 >酸碱度 ,彩虹明樱蛤则表现为温度≈酸碱度≈盐度 ;各实验生物间对温度、盐度及酸碱度生态敏感度指数分别表现为 ,温度呈彩虹明樱蛤≈婆罗囊螺 >泥螺 ,盐度呈泥螺 >彩虹明樱蛤≈婆罗囊螺 ,酸碱度呈婆罗囊螺 >泥螺 >彩虹明樱蛤。在讨论并设定酸碱度作为婆罗囊螺生态敏感因子的同时 ,为不影响涂泥底质安全 ,保证泥螺和彩虹明樱蛤的正常存活 ,确定酸碱度对婆罗囊螺的有效作用水平为 9.5— 1 0。  相似文献   

大亚湾海域溶解游离氨基酸及其与环境的关系   总被引：4，自引：0，他引：4  

郑爱榕  沈海维  李文权  詹力扬 《海洋科学》2001,25(10):43-47

对大亚湾海域溶解游离氨基酸(DFAA)的分布特征及其影响因素进行了研究。现场采样调查分别于1995年5月、11月和2000年4月进行。结果表明 :(1)大亚湾海域DFAA的含量较高 ,在0.69～4.73μmol/L之间 ,平均2.16±0.87μmol/L,可能主要源于较为旺盛的生物活动 ;(2)DFAA含量在海域的平面分布变化较大 ,垂直分布和季节及年变化不明显 ;(3)DFAA与海水中的DOC呈正相关、与叶绿素呈负相关关系 ,与TIN的相关性则呈季节变化 ,生物效应可能是影响该海域DFAA含量的主要因素。  相似文献   

Analysis of influencing factors on fine sediment flocculation in the Changjiang Estuary   总被引：1，自引：0，他引：1  

Jiang Guojun  Yao Yanming  Tang Ziwen 《海洋学报(英文版)》2002,21(3):385-394

Based on the test data in dynamic water and static water, the main factors, which influence the fine sediment flocculation, are analyzed with a gray model method of correlation theory. It is shown that the main influencing factors are water temperature, settling time, salinity, grain size, sediment concentration and current velocity according to the correlation coefficients. Among them, the salinity and the sediment grain size are critical type influencing factors (CrTIF); the settling time, the sediment concentration and the velocity are continuous type influencing factors (CoTIF); and the water temperature has the characteristics of both. When the critical values of CrTIF are reached or exceeded, the fine sediments will be flocculated, but values of CrTIF will not influence the settlement strength of floes. The influence of CoTIF is continuous. The values of the CoTIF will not only influence the occurrence of flocculation but also the settlement strength of the floes.  相似文献   

Recent changes of Shandong sandy coast and in fluence of human activities     

Wu Sangyun  Wang Wenhai 《海洋学报(英文版)》1997,16(4):505-515

Ｒｅｃｅｎｔ　ｃｈａｎｇｅｓ　ｏｆ　Ｓｈａｎｄｏｎｇ　ｓａｎｄｙ　ｃｏａｓｔ　ａｎｄ　ｉｎ　ｆｌｅｎｃｅ　ｏｆ　ｈｕｍａｎ　ａｃｔｉｖｉｔｉｅｓTXＲｅｃｅｎｔｃｈａｎｇｅｓｏｆＳｈａｎｄｏｎｇｓａｎｄｙｃｏａｓｔａｎｄｉｎｆｌｕｅｎｃｅｏｆｈｕｍａｎ...  相似文献   

Effects of Meteorological Factors on Toxic Red Tide Events in Sabah, Malaysia     

Gires Usup  Yu Kim Lung 《Marine Ecology》1991,12(4):331-339

Abstract. Red tides of the toxic dinoflagellate Pyrodinium bahamense var. compressum have occurred almost annually since 1976 in the coastal waters of the west coast of Sabah, Malaysia. Field obSérvations have indicated that the timings of these outbreaks could be linked to meteorological forcings. All the red tides have occurred during either the northeast or southwest monsoon periods. Matching of red tide outbreaks with total monthly rainfall, monthly-averaged index of wind-induced surface water mixing, and monthly-averaged upwelling index for the period from 1975 to 1989 failed to show any definite pattern. However, more red tide events occurred in months with high mixing index values. The absence of definable patterns could be due to the use of monthly, rather than daily, values in the calculations.  相似文献   

Spartina anglica eradication experiment and in situ monitoring assess structuring strength of habitat complexity on marine macrofauna at high tidal level     

Maud Cottet  Xavier de Montaudouin  Hugues Blanchet  Pascal Lebleu 《Estuarine, Coastal and Shelf Science》2007,71(3-4):629-640

The cordgrass Spartina anglica is an introduced species that tends to invade sheltered sand and mudflats, at the upper low marsh level. In Arcachon Bay, a lagoon in South West of France, the cordgrass can also replace Zostera noltii beds. The consequence of cordgrass presence on macrobenthic fauna was estimated and compared to adjacent habitats (bare sands, Z. noltii sea grass beds) during one year. The communities of the three habitats were characterised by low species richness, low abundance and biomass (when Hydrobia ulvae, 90% of abundance, is not considered) and high seasonal stability. The infaunal assemblages were particularly homogeneous between habitats without any characteristic species.Cordgrass eradication experiments were performed and zoobenthic recolonisation was observed the following year. Modifications in benthic fauna were observed on epifauna only.These results highlight the limited structuring effect of habitat heterogeneity at high tidal levels and in soft-bottom sediments where desiccation becomes the dominant factor determining infauna community structure.  相似文献   

大亚湾海域沉积物中的硝化与反硝化作用   总被引：3，自引：0，他引：3       下载免费PDF全文

徐继荣  王友绍  殷建平  孙翠慈  张凤琴  王清吉  何磊  董俊德 《海洋与湖沼》2007,38(3):206-211

2004年1、4、8、10月在大亚湾海域的4个站点采用自行设计和制作的无扰动沉积物采样器采集沉积物样品,通过使用AIT技术(乙炔同时抑制硝化与反硝化作用),进行实验室同步恒温受控模拟培养实验,并同时测定沉积物上覆水的温度、盐度、DO和pH值,沉积物的Eh值和有机质含量,间隙水的NO3-、NO2-和NH4 浓度,研究沉积物中的硝化与反硝化速率及其影响因素。结果显示大亚湾沉积物的硝化速率范围为[(0.00—4.68)±0.87]μmol/(m2·h);反硝化速率范围[(0.00—2.88)±0.41]μmol/(m2·h);硝化与反硝化作用之间存在耦合,比例范围为0%—100%。沉积物的硝化、反硝化速率和耦合比例与上覆水的温度、DO含量,及沉积物中的有机质含量和Eh值密切相关,人类活动对沉积物的硝化与反硝化作用有明显的影响。  相似文献   

加强海洋灾害地质学研究,减少海洋工程灾害   总被引：3，自引：1，他引：3  

黄庆福  阎军  林国军  董太禄  江荣华 《海洋地质与第四纪地质》1993,13(4):99-103

随着我国近海油气资源的开发及海洋工程的需要,海洋灾害地质学这一边缘学科正在我国兴起和迅速发展。本文对这一学科的研究对象、研究领域以及灾害地质因素分类进行了概述,并对海洋灾害地质学的特点与应用前景,进行了初步总结,最后对该学科的发展方向提出了积极建议。  相似文献   

Spatio-temporal variability of surface soil water content and its influencing factors in a desert area,China     

Pingping Zhang 《水文科学杂志》2013,58(1):96-110

Abstract

Knowledge of the variability of soil water content (SWC) in space and time plays a key role in hydrological and climatic modelling. However, limited attention has been given to arid regions. The focus of this study was to investigate the spatio-temporal variability of surface soil (0–6 cm) water content and to identify its controlling factors in a region of the Gobi Desert (40 km²). The standard deviation of SWC decreased logarithmically as mean water content decreased, and the coefficient of variation of SWC exhibited a convex upward pattern. The spatial variability of SWC also increased with the size of the investigated area. The spatial dependence of SWC changed over time, with stronger patterns of spatial organization in drier and wetter conditions of soil wetness and stochastic patterns in moderate soil water conditions. The dominant factors regulating the variability of SWC changed from combinations of soil and topographical properties (bulk density, clay content and relative elevation) in wet conditions to combinations of soil and vegetation properties (bulk density, clay content and shrub coverage) in dry conditions. This study has important implications for the assessment of soil quality and the sustainability of land management in arid regions.  相似文献   

Qualitative and quantitative characterization of a transitional shale reservoir: A case study from the Upper Carboniferous Taiyuan shale in the eastern uplift of Liaohe Depression,China     

《Marine and Petroleum Geology》2017

The paper takes the Upper Carboniferous Taiyuan shale in eastern uplift of Liaohe depression as an example to qualitatively and quantitatively characterize the transitional (coal-associated coastal swamp) shale reservoir. Focused Ion Beam Scanning Electron Microscope (FIB-SEM), nano-CT, helium pycnometry, high-pressure mercury intrusion and low-pressure gas (N₂ & CO₂) adsorption for eight shale samples were taken to investigate the pore structures. Four types of pores, i.e., organic matter (OM) pores, interparticle (InterP) pores, intraparticle (IntraP) pores and micro-fractures are identified in the shale reservoir. Among them, intraP pores and micro-fractures are the major pore types. Slit-shaped pores are the major shape in the pore system, and the connectivity of the pore-throat system is interpreted to be moderate, which is subordinate to marine shale. The porosity from three dimension (3D) reconstruction of SEM images is lower than the porosity of helium pycnometry, while the porosity trend of the above two methods is the same. Combination of mercury intrusion and gas absorption reveals that nanometer-scale pores provide the main storage space, accounting for 87.16% of the pore volume and 99.85% of the surface area. Micropores contribute 34.74% of the total pore volume and 74.92% of the total pore surface area; and mesopores account for 48.27% of the total pore volume and 24.93% of the total pore surface area; and macropores contribute 16.99% of the total pore volume and 0.15% of the total pore surface area. Pores with a diameter of less than 10 nm contribute the most to the pore volume and the surface area, accounting for 70.29% and 97.70%, respectively. Based on single factor analysis, clay minerals are positively related to the volume and surface area of micropores, mesopores and macropores, which finally control the free gas in pores and adsorbed gas content on surface area. Unlike marine shale, TOC contributes little to the development of micropores. Brittle minerals inhibit pore development of Taiyuan shale, which proves the influence of clay minerals in the pore system.  相似文献