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101.
Uptake and release of ship-borne ballast water is a major factor contributing to introductions of aquatic phytoplankton and invasive macroinvertebrates. Some invasive unicellular algae can cause harmful algal blooms and produce toxins that build up in food chains. Moreover, to date, few studies have compared the efficacy of ballast water treatments against different life history phases of aquatic macroinvertebrates. In the present study, the unicellular green alga Dunaliella tertiolecta, and three discrete life history phases of the brine shrimp Artemia salina, were independently used as model organisms to study the efficacy of sonication as well as the advanced oxidants, hydrogen peroxide and ozone, as potential ballast water treatments. Algal cells and brine shrimp cysts, nauplii, and adults were subjected to individual and combined treatments of sonication and advanced oxidants. Combined rather than individual treatments consistently yielded the highest levels of mortality in algal cells (100% over a 2 min exposure) and in brine shrimp (100% and 95% for larvae and adults, respectively, over a 2 min exposure). In contrast, mortality levels in brine shrimp cysts (66% over 2 min; increased to 92% over a 20 min exposure) were moderately high but consistently lower than that detected for larval or adult shrimp. Our results indicate that a combination of sonication and advanced chemical oxidants may be a promising method to eradicate aquatic unicellular algae and macroinvertebrates in ballast water.  相似文献   
102.
亚洲东部存在一个巨大的三角形地震构造区域,大体上,喜马拉雅山脉、帕米尔—天山—阿尔泰山—贝加尔和东经105°线是它的3个边界,主要覆盖中国和蒙古国西部众多高原、山脉及山间盆地。三角区内现今构造活动和地震广泛强烈,地壳破碎,显示不均匀的块体边界和块内变形;区外基本上是稳定的刚性陆块,地震很少,变形较弱,处于整体缓慢运动之中。这个宽阔的板内变形区起源于印度、菲律宾海—西太平洋和欧亚三大板块之间的动力作用以及深部地幔流的影响。向北快速运动的印度次大陆已近水平地插入到西藏板块下,沿喜马拉雅弧产生多种运动和变形,并向亚洲内部远距离地扩散。沿东经95°~100°,向北的地壳运动向东和东南方向偏转,阻截了喜马拉雅弧东端的北向运动;而在喜马拉雅弧西端,帕米尔继续向北挤进中亚,受天山—阿尔泰山—贝加尔一线西北側稳定地壳的限制,扩散的变形被中国、蒙古、俄罗斯边境地区一系列EW向和NW向的老断层吸收并在它们的西端终止。菲律宾海—西太平洋向欧亚大陆的消减-俯冲导致沿海沟-岛弧的漫长而狭窄的地震带,但对亚洲大陆的水平挤压较小,未能阻挡亚洲大陆东部向东移动。其部分原因可能是俯冲板片受到来自欧亚大陆下的ES向地幔流的推挤,这个ES向地幔流与来自印度下面的N向地幔流在西藏中部汇合并向东偏转,在大尺度上与GPS观测到的地表移动图像一致。  相似文献   
103.
东亚与全球地震分布分析   总被引:1,自引:0,他引:1       下载免费PDF全文
现代地震学是一门年轻的学科,但人类对地震现象的观察、记录和思索已有数千年历史。特别是在中国,很早就有灾害性地震的详细历史记载。最近40多年,我国、东亚及世界其他大陆地区的多次大地震的发生,推动了地震构造研究的发展,加深了对地震分布规律性及其地球动力环境的认识。从地质背景和发生机制看,全球地震构造可分为三大类:第一是太平洋海底地壳与陆缘地壳浅、中、深俯冲构成的地震带;第二是南半球离散地壳块体对北半球大地块边缘碰撞浅俯冲带;第三是全球三大洋脊张裂转换构造带。地球北半部内陆的中纬度地带有4个多震密布区,它们都处于N25°~55°的纬向大陆带内,与大陆会聚所造成的陆内变形有关。4个多震密布区的东半部则是相对少震区,显示出相对稳定的地壳结构。全球表壳GPS矢量场和北南两个极区各有不同,北半球欧亚大陆是向北呈弓字形运动;南半球是南美、非洲、阿拉伯、印度、澳大利亚等5块离散的大陆块,除南美大陆,其他4块大陆都是向NE和NNE方向运动。这4块大陆都是依次运动加速,澳大利亚陆块运动最快,向NNE方向约10 cm/a;同时从南太平洋南部沿NWW方向左型转换断层的运动也是高速的,这两个方向运动的交叉相碰,现已处在全球最为强烈的地震活动区域。北冰洋内群岛GPS站点向阿留申岛弧推进;南极冰陆的9个GPS站点则呈现旋扭状彼此相差约90°,可能表明北/南半球彼此有明显的1/4左右表壳的扭动。从卫星重力数据推测的地球的形状、全球热流的和地内热散失量的分布、地球磁场的西漂以及大地震引起的地球振荡特征等证据推测,地球的内部结构具有一定程度的非对称性和非均匀性,它们对全球板块运动、板块变形以及大地震的空间分布可能有一定的控制作用。  相似文献   
104.
2004年12月26日印度尼西亚西北近海8.7级大地震,是一次浅源的海沟俯冲型板间地震。震中位于印尼-美拉尼西亚板块边界构造带的西北端,2004年沿该带发生的8次M≥7地震显示总体由东向西迁移的特征,表明它们具有相互联系的统一动力过程。这些板间地震的发生与该地处于几个板块汇聚地带和较大的板块运动速率有关,它们导致了强烈而复杂的构造变形和构造活动。印度洋-澳大利亚板块向东南亚陆块的低角度俯冲,在俯冲带浅部形成积累应变能的巨大闭锁区,它的突然破裂和大尺度滑动是造成印尼8.7级大地震的直接原因  相似文献   
105.
Ecotoxicological studies, using the tropical marine diatom, Nitzschia closterium (72-h growth rate), were undertaken to assess potential issues relating to the discharge from an alumina refinery in northern Australia. The studies assessed: (i) the species’ upper thermal tolerance; (ii) the effects of three signature metals, aluminium (Al), vanadium (V) and gallium (Ga) (at 32 °C); and (iii) the effects of wastewater (at 27 and 32 °C). The critical thermal maximum and median inhibition temperature for N. closterium were 32.7 °C and 33.1 °C, respectively. Single metal toxicity tests found that N. closterium was more sensitive to Al compared to Ga and V, with IC50s (95% confidence limits) of 190 (140-280), 19,640 (11,600-25,200) and 42,000 (32,770-56,000) μg L−1, respectively. The undiluted wastewater samples were of low toxicity to N. closterium (IC50s > 100% wastewater). Environmental chemistry data suggested that the key metals and discharge are a very low risk to this species.  相似文献   
106.
To prevent grounding of ships and collisions between ships in shallow coastal waters, an underwater data collection and communication network (ACME) using underwater sounds to encode and transmit data is currently under development. Marine mammals might be affected by ACME sounds since they may use sound of a similar frequency (around 12 kHz) for communication, orientation, and prey location. If marine mammals tend to avoid the vicinity of the acoustic transmitters, they may be kept away from ecologically important areas by ACME sounds. One marine mammal species that may be affected in the North Sea is the harbour seal (Phoca vitulina). No information is available on the effects of ACME-like sounds on harbour seals, so this study was carried out as part of an environmental impact assessment program. Nine captive harbour seals were subjected to four sound types, three of which may be used in the underwater acoustic data communication network. The effect of each sound was judged by comparing the animals' location in a pool during test periods to that during baseline periods, during which no sound was produced. Each of the four sounds could be made into a deterrent by increasing its amplitude. The seals reacted by swimming away from the sound source. The sound pressure level (SPL) at the acoustic discomfort threshold was established for each of the four sounds. The acoustic discomfort threshold is defined as the boundary between the areas that the animals generally occupied during the transmission of the sounds and the areas that they generally did not enter during transmission. The SPLs at the acoustic discomfort thresholds were similar for each of the sounds (107 dB re 1 microPa). Based on this discomfort threshold SPL, discomfort zones at sea for several source levels (130-180 dB re 1 microPa) of the sounds were calculated, using a guideline sound propagation model for shallow water. The discomfort zone is defined as the area around a sound source that harbour seals are expected to avoid. The definition of the discomfort zone is based on behavioural discomfort, and does not necessarily coincide with the physical discomfort zone. Based on these results, source levels can be selected that have an acceptable effect on harbour seals in particular areas. The discomfort zone of a communication sound depends on the sound, the source level, and the propagation characteristics of the area in which the sound system is operational. The source level of the communication system should be adapted to each area (taking into account the width of a sea arm, the local sound propagation, and the importance of an area to the affected species). The discomfort zone should not coincide with ecologically important areas (for instance resting, breeding, suckling, and feeding areas), or routes between these areas.  相似文献   
107.
The filtration process of Sabella spallanzanii Gmelin on bacterial community was studied in a coastal area of the Northern Ionian Sea (Mediterranean Sea) at three sites, S. Vito, Lido Gandoli and Lido Silvana, where some specimens of S. spallanzanii were transplanted. Analyses were performed both on water and worm samples. A total of six microbial groups were examined: culturable heterotrophic bacteria, total culturable bacteria at 37 degrees C, culturable vibrios, total and fecal coliforms and fecal streptococci. The bacterial densities were usually orders of magnitude higher in the worm homogenates than in the corresponding seawater and the highest values were observed in August. The ability of S. spallanzanii to accumulate the microbial pollution indicators suggests this species can be employed as a bioindicator for monitoring water quality. Moreover, the accumulation capability of S. spallanzanii for specific micro-organisms provides a potential role in sewage bioremediation.  相似文献   
108.
测定俯冲带全新世地震的一种新方法是将地面穿透雷达,振动取芯和加速同谱测定年龄的结果综合起来,用于研究华盛顿西南威拉帕湾以西的沙堤岬年龄。  相似文献   
109.
110.
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