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1.
对长岛北四岛海洋牧场海域101个表层沉积物和102个表层海水样进行取样调查,开展表层沉积物类型、粒度、表层沉积物和海水重金属等指标分析测试,采用单因子污染指数法、富集系数法和潜在生态危害指数法评价该区表层沉积物潜在生态风险,采用海水水质分类和单因子污染指数法评价表层海水污染情况。表层沉积物结果表明：沉积物为泥质砂质砾、砾质泥质砂、砾质泥、含砾泥质砂、砂、粉砂质砂和砂质粉砂,平均粒径介于2.44~5.44Ф;Hg、Cu、Zn、Pb、Cd、As、Cr、硫化物和石油类都符合第一类标准,属于清洁沉积物;Cr、Cu、Pb、Zn、Cd、Hg和As富集系数均＜1,处于低度污染水平;Cr、Cu、Pb、Zn、Cd、Hg和As单项潜在生态危害系数Eir介于0.56~30.71之间,RI均值为66.27,远低于低度生态危害的划分标准值。表层海水结果表明：21个站位受到Hg污染,略高于第一类标准,满足第二类标准,主要位于研究区西北部、西中部和东北部海域,其余指标均符合规定第一类标准;Hg、Cu和Zn含量处于较清洁环境范围内,As、COD、石油类、Pb、Cr和Cd含量处于自然本底环境。根据海底沉积物和海水分析结果得出,长岛北四岛海域海洋牧场规划区底质和水质环境适宜建设海洋牧场。 相似文献
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《广东海洋大学学报》2017,(4)
于2015年11月和2016年3月调查了较场尾海域海洋环境状况,以海水水质标准、综合污染指数和潜在生态风险指数、目标危险系数来评价较场尾海域海水、沉积物及生物体重金属的污染现状和摄入健康风险。结果表明:两个航次海水均有个别重金属含量超标,其中2015年11月份航次重金属Pb、Hg超标,站位超标率分别为40%和20%,2016年3月份航次重金属Cu、Pb、Hg超标,站位超标率分别为5%、20%和5%,较场尾海域表层海水重金属浓度基本呈现由北向南逐渐递减的趋势;较场尾海域表层沉积物主要受到Cu、Pb、Cr、Hg的污染,其中5站的Cr和15站的Hg均超过海洋沉积物质量二类标准,Cu和Cr的站位超标率为16.7%,Pb和Hg的站位超标率为8.3%,站位综合污染指数以5站6.02为最大,潜在生态风险指数以15站65.14为最大;较场尾附近海域的重金属污染主要来自附近的工业厂区和燃煤电厂;较场尾海域所捕获到的鱼、虾、头足类目标危险系数之和由大到小为:鱼(0.132)头足(0.062)虾(0.012),均不存在人体摄入健康风险。 相似文献
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中山海域浮式试验鱼礁效果研究 总被引：2，自引：0，他引：2
陈丕茂 《广东海洋大学学报》2005,25(3):85-89
广东省中山市所属海域位于珠江口伶仃洋西侧，属热带和亚热带河口浅海区半咸淡水域，是多种海洋生物种类和多种江河生物种类的产卵场所和幼体成长场所。近年来中山海域渔业资源衰退、海洋环境恶化，建设人工鱼礁是恢复渔业资源和修复海洋生态环境的重要措施之一。2002年初至8月，中国水产科学研究院南海水产研究所、 相似文献
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刘思俭 《广东海洋大学学报》1995,(2)
综述了我国及广东省十多年来鱼虾种苗人工放流及人工鱼礁的投放情况，结合广东省广大海区的水温、盐度、ｐＨ值、海流、营养盐含量情况及天然饵料的种类、分布等，提出了除在大亚湾已设置了水产增殖站以外，还应该在广东东部的南澳和西部的湛江各设一个增殖站，会收到更大的效果。人工鱼礁应总结过去投放的经验，加强礁区管理，逐步解决投资与收益的关系问题，并进一步扩大投放人工鱼礁的地点和密度，把广东海区切实建成理想的海洋牧场。 相似文献
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于2005年8月对湛江港附近海域潮间带的海水、表层沉积物和贝类体内的重金属进行了分析,结果表明:海水中的砷优于海水水质Ⅰ类标准,而汞、铜、锌、铅、镉均有不同程度的污染,其中铜、铅、镉污染较为严重,均劣于海水水质Ⅳ类标准;表层沉积物中砷的含量低于全国海岸带背景值,而汞、铜、锌、铅、镉均高于全国海岸带背景值,其标准指数分别为1.35、1.66、1.50、2.08、3.10,汞、铜略高于海洋沉积物质量标准第一类标准,有轻微污染,砷、锌、铅均低于海洋沉积物质量标准第一类标准,未受污染,而镉略高于海洋沉积物质量标准第二类标准,环境受镉污染。各元素在各站点的分布没有规律性。牡蛎和蛤仔体内各重金属含量均优于海洋生物污染评价标准和人体消费卫生标准,其卫生质量良好。 相似文献
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通过对2 131km高分辨率浅地层剖面资料分析和研究,揭示了威海市近海海域浅地层结构特征,分析了海洋灾害地质因素类型及分布特征,并绘制了主要灾害地质因素分布图。威海市近海海域65m以浅地层共分为5层,第一层为全新世泥质楔形体,地层厚度8~15m;第二层为末次盛冰期以来的海侵层,厚度一般小于3m;第三层为MIS2期的陆相沉积层,地层厚度3~8m;第四层为MIS3期的海相沉积层,厚度3~6m;第五层未完全揭示。近海海域灾害地质因素主要包括埋藏下切谷、浅部断层、浅层气、海底沙波沙脊、浅埋起伏基岩等5种类型;埋藏下切谷主要分布在南部海域U3地层单元中;浅部断层主要分布在南部海域水深大于20m的海底堆积平原;浅层气主要分布在北部海域,东部和南部海域面积较小;海底沙波沙脊主要分布在荣成成山头外海海域;浅埋起伏基岩主要分布在基岩海岸和岛屿较近的海域。 相似文献
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采取烟台近岸海域150个海底表层沉积物样品进行Hg,Cu,Pb,Zn,Cd,Cr,As,Ni元素分析。结果显示,烟台市近岸海域重金属主要富集在芝罘湾(Cd,Cu)、龙口(As,Cr,Cu)及海阳东部(Ni,Pb)一带,而莱州、招远及牟平近岸海域重金属含量较低。单因子、内梅罗和潜在生态危害指数评价结果显示,研究区88%海域的沉积物达到一类标准,轻污染区主要分布在芝罘岛北部及龙口市西部,龙口、招远及烟台市近岸沉积物潜在风险中等。 相似文献
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通过对滨州近海海域海底沉积物测试数据及海岸带陆域土壤地球化学分析,对滨州海岸带陆域土壤和海底沉积物中7种重金属(Hg,Cd,Pb,Cu,Zn,Cr,Ni)的空间分布特征进行了研究,并绘制了各指标含量陆海联合分区图。分析结果表明,滨州市海岸带重金属元素含量基本上均低于国标规定的海洋一类沉积物的最高标准,仅有个别元素含量超过一级标准值,表明局部存在一定的重金属污染。从滨州海岸带重金属含量空间分布上来看,除Hg元素外,其余重金属元素含量呈现一定的规律,基本上陆域含量高于海域含量,且大部分元素都呈现出陆域城镇值高,郊区值低的态势。区内化工企业较发达,Ni,Cr属于中度变异区,Cd,Hg,Pb属于高度变异,受人为影响因素较大,考虑区内土壤及海底沉积物重金属富集主要来源于工业"三废"。 相似文献
11.
Qinqin Tang Jinchang Zhang Yingci Feng Jian Li Yantao Yao Jie Sun Wenhuan Zhan 《中国海洋大学学报(英文版)》2018,17(4):763-772
In recent years, infrastructure construction on coral reefs has been increasingly developed. Therefore, the shallow strata stability of coral reefs in the South China Sea should be evaluated. This study aims to investigate the profiles for the shallow strata of coral reefs in the southwest of the Yongshu Reef, particularly in the hydrodynamic marine environment, and to establish a geological model for numerical simulation using Geo-Studio. The shallow strata of the coral reefs include mass gravel, sand gravel, mid-coarse sand, silty sand, fine sand, and reef limestone. The shallow reef slope near the lagoon is similar to a ‘layer cake', in which the side close to the sea is analogous to a ‘block cake'. The simulation results showed that coral reef stability depends on wave loads and earthquake strength and on the physical properties of coral reefs. The factor of safety for the outer reef is greater than 10.0 under static, wave, and seismic conditions; this indicated that the outer reefs were less affected by waves and earthquakes. However, the factor of safety next to the lagoon varied from 0.1 to 5.3. The variation was primarily caused by the thick strata of coral reefs close to the sea(reef limestone, typically with the thickness 10 m and equivalent to a block). The soil and rock layers in the coral reef strata with thicknesses 10 m showed weak engineering geological characteristics. Our findings can provide useful information to future construction projects on coral reefs. 相似文献
12.
Type and evolution of landscapes of Nansha Islands 总被引：1，自引：0，他引：1
赵焕庭 《中国地理科学(英文版)》1998,8(2):144-151
ＴＹＰＥＡＮＤＥＶＯＬＵＴＩＯＮＯＦＬＡＮＤＳＣＡＰＥＳＯＦＮＡＮＳＨＡＩＳＬＡＮＤＳＺｈａｏＨｕａｎｔｉｎｇ（赵焕庭）ＳｏｕｔｈＣｈｉｎａＳｅａＩｎｓｔｉｔｕｔｅｏｆＯｃｅａｎｏｌｏｇｙ,ｔｈｅＣｈｉｎｅｓｅＡｃａｄｅｍｙｏｆＳｃｉｅｎｃｅｓ,Ｇｕ... 相似文献
13.
Zhao Huanting 《中国地理科学(英文版)》1997,8(2):144-151
Landscapes of the Nansha Islands may be divided into five types: tropical marine organism-breeding landscape of reef knoll
like Zengmu Shoal, Wan’an Bank and so on; tropical marine organism-breeding landscape of atoll including all emerged reefs
and most submerged reefs; tropical evergreen arbor-bush forest and phosphorous lime soil landscape of limesand Islets like
Taiping Islet, Nanwei islet and so on; tropical shallow sea marine organism-breeding landscape of southern continental shelf;
tropical oceanic and deep-sea marine organism landscape in middle and north parts of the Nansha Islands area. These five landscape
types may be also summed up as two categories, one is tropical sea landscape including those in shallow and deep sea, the
other is tropical coral reef landscape including those of reef knoll, atoll and limesand islet. This paper outlines the evolutional
model of landscapes of the Nansha Islands. The distribution and evolution of landscape types are related with palaeogeography
and modern environmental conditions. The former shallow sea of the Nansha islands was coastal zone in the Late Pleistocene
epoch. Deep sea is evolved from shallow sea due to long and slow subsidence of crust. Modern coral reefs develop on old reef
top of the Late pleistocene epoch or on baserock of continental shelf in the Holocene due to the rise of sea level in postglacial.
Limesand islet is in the peak of developmental stage. 相似文献
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彼此相邻的海域之间由于用海类型的不同,经常存在相互的干扰和影响。本文以国家海洋功能区划中规定的海洋功能区分类及海洋环境保护要求为基础,设计了用海变化的自动检测方法。根据不同海洋功能分区的海水水质质量的标准建立缓冲区检测算法和历史用海检测算法,缓冲区检测算法用来检测同一时期不同位置的用海是否存在冲突;历史用海检测算法用来检测同一位置不同时期的用海是否存在冲突。在两种检测算法的基础上,利用地理信息系统开发组件实现了对新加入宗海及原宗海用海变更的自动检测功能,并以上海海洋功能区划数据为测试数据,验证了作为海籍空间信息管理系统的核心功能之一,可以实现用海变化的自动检测,满足对宗海空间变化和时间变化的信息化管理。 相似文献
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Based on various patterns of groundwater and their abundance characters in south Liaodong Peninsula, the distribution, stage, pattern and characters of sea water intrusion in the serious sea water intrusion areas are analysed. The reasons to cause sea water intrusion are uneven precipitation, limited recharge of surface water, artificial overpumping, lithology and geological structure. It can provide scientific basis for reasonable utilization of limited water resource in line with the local conditions. 相似文献
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经济的快速发展, 对砂石料的需求巨大, 海砂的开发成为当前的热点。琼州海峡东口海砂资源丰富, 资源潜力概算可达数十亿方。依据前期调查数据, 选取含泥量、含砂量、粒级、海砂厚度、水深和离岸距离6类指标, 采用层次分析法, 构造判断矩阵计算评价因子的权重, 运用ArcGIS空间分析功能进行叠加, 对琼州海峡东口的海砂进行了开发适宜性评价。结果表明: 经计算将研究区分为开发适宜性好、较好、中等、较差、差5个等级, 其中浅滩区域海砂规模大、质量好、水深浅和开采环境影响小, 其开发适宜性最佳。分析了不同的指标对海砂开发适宜性的影响, 在浅滩区, 厚度和含砂量指标贡献较大; 在近岸海湾, 环境影响是主要因子; 在琼州海峡深槽区, 水深条件则成为海砂开发的主要限制条件。根据海砂资源的特点, 建立了以资源自然属性、开发技术条件、生态环境影响和行政管理为主要因子的海砂开发利用适宜性评价体系, 具体工作可选取不同的指标开展评价。研究结果可以为研究区海砂的开发利用和其他区域海砂开发适宜性评价提供参考。 相似文献
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In this study, we used Landsat images and meteorological data to examine the spatiotemporal distribution and variability of sea ice in Jiaozhou Bay(JZB) between 1986 and 2016. The results show that JZB is not always covered by sea ice in winter, but in some extreme cases, sea ice has covered more than one-third of the sea area of the bay. Sea ice in JZB has generally formed between January 1 and February 5, primarily along the coast, and gradually expanding to the central area of the bay. Both meteorological and artificial factors have played important roles in modulating the sea ice distribution. We found sea ice coverage to have been strongly correlated with the accumulated freezing-degree days nine days before the occurrence of sea ice(R2 = 0.767). North-northwest surface winds have dominated the freezing period of sea water in the JZB, and wind speed has exerted a more significant influence on the formation of sea ice when the sea ice coverage has been generally small. Additionally, artificial factors began to affect the expansion of sea ice in JZB since 2007. The construction of the Jiao-Zhou-Bay Bridge(JZBB) is believed to have retarded water flow and reduced the tidal prism, thereby leading to the formation of an ice bridge along the JZBB, which effectively prevents the southward expansion of sea ice. 相似文献
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近年来, 受人类活动和全球变暖的双重影响, 我国南海区域珊瑚礁生态系统退化, 发生白化现象。利用遥感技术监测和掌握珊瑚礁的白化情况, 对南海生态环境的保护和治理具有重大价值。首先通过多期海表温度数据获取珊瑚礁白化预警的区域, 选定西沙群岛永乐环礁中的羚羊礁作为研究对象; 然后, 提出了一种新型的珊瑚礁白化监测模型, 分别采取水深校正、珊瑚礁分类、反射率调整以及阈值选择等方式对2013-2018年的Landsat-8遥感影像开展了多时间序列的珊瑚礁白化监测研究。最终的结果显示, 该模型能够较为准确地获取珊瑚礁白化区域, 为南海珊瑚礁白化现象的长时间序列监测提供依据。 相似文献
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An artificial oyster shell reef was deployed in Rongcheng Bay, East China. However, the effects of this reef on the surrounding macrobenthic communities were unknown. We compared sedimentary factors, macrobenthic biomass, abundance, and community composition and ecological indicators between the reef and non-reef areas over a one year period. The mean values for chlorophyll a （Chl a）, total organic matter （TOM）, total organic carbon （TOC）, and total nitrogen （TN） content in surface sediments in the reef area were slightly higher than those in the non-reef area. The Chl a levels differed significantly between the two areas, but the TOM, TOC, and TN were not significantly different. The abundance of crustaceans was significantly different between the two areas, but the abundance and biomass ofpolychaetes, echinoderms, mollusk did not differ significantly. The permutational multivariate analysis of variance （PERMANOVA） revealed that the macrobenthic community differed significantly through time and analysis of similarity multivariate analyses （ANOSIM） revealed that the macrobenthic community differed significantly in some months. The ecological indicators revealed that the environmental quality of the reef area was slightly better than that of the non-reef area. Overall, our results suggest that the artificial oyster shell reef may change the macrobenthic community and the quality of the environment. Despite the lack of an effect in the short term, long-term monitoring is still needed to evaluate the effects of artificial oyster shell reefs on macrobenthic communities. 相似文献