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991.
根据现场调查和室内试验工作, 计算珠江口水域浮游植物有效光合作用水体体积, 同时研究浮游动物摄食行为对磷再生的补偿作用, 进而对该水域磷的生物利用状况进行初步评估。分析珠江口2002—2003年的数据发现, 珠江口水域浮游植物有效进行光合作用水体的体积存在季节性变化, 枯水期约为9.7×104m3, 而丰水期约为6.6×104m3。该水域总初级生产量在枯水期约为36kg.d-1, 在丰水期约为31kg.d-1, 呈现枯水期大于丰水期的特点。浮游动物的摄食作用可促进水体中磷的再生, 这部分磷可满足浮游植物生长对磷需求的1.5%—15.6%, 并呈现丰水期大于枯水期的特点。浮游动物摄食作用直接释放的量远大于其自身生理周转释放的量。 相似文献
992.
"红肉病"文蛤(Meretrix meretrix Linnaeus)中发现的3种病毒样颗粒 总被引:3,自引:1,他引:3
本文报道了在患“红肉病”文蛤组织中发现的 3种病毒样颗粒。 1种主要存在于鳃上皮下的结缔组织中 ,呈球形或椭球形 ,大小 (5 0~ 6 0 ) nm× (5 0~ 110 ) nm,无囊膜包裹。另 1种为球形 ,直径 16 0~ 180 nm,有囊膜 ,存在于外套膜上皮细胞及结缔组织细胞质中。第 3种存在于消化盲囊上皮细胞质内 ,为无囊膜包裹的球形病毒样颗粒 ,直径为 5 0~ 80 nm。 相似文献
993.
994.
基于GIS的长江三峡库区滑坡影响因子分析 总被引:11,自引:1,他引:10
利用GIS技术和统计方法,对三峡库区选定的研究区域(面积4539km2)滑坡空间分布和地形、地质等滑坡内部因子之间相关性进行统计计算。在建立地质、地形数据库等滑坡因子空间数据库和滑坡空间分布数据库(数据比例尺均为1∶10000)基础上,从地形数据库提取25m分辨率DEM,再派生出高程、高差、坡度、坡向、平面曲率、剖面曲率等地形影响因子;从地质数据库提取地层和岩性组合影响因子。将各个定性的因子按一定规则进行重分类、转换为25m分辨率的栅格数据格式,在GIS中进行地图代数运算、统计计算滑坡和各影响因子相关性。结果表明,滑坡分布和Q4、J1x,J1z、S岩性岩组;90m以下、90~135m和135~175m三个高程带;15~20m局部高差;10°~25°坡度;北、南和西北方向及-1~1曲率范围等影响因子相关性等级都大于1,为滑坡发生的主要影响因子类属。研究的结果是进行滑坡易发性评价的基础,可以指导库区滑坡灾害管理、土地利用等。 相似文献
995.
研究了湛江东海岛3种不同养殖模式虾池弧菌对抗菌药物的耐药性,并对虾池水域环境的水温、盐度、DO、pH、叶绿素a、DOC、无机氮、无机磷、硅酸盐、细菌总数和弧菌数量变化进行了监测和评价。结果表明,调查的三个虾池的弧菌对万古霉素产生耐药性,高位新池和传统精养池的弧菌对利福平产生耐药性,对其他抗菌药尚未形成耐性,3个虾池的弧菌对恩诺沙星和氯霉素高度敏感,传统精养池和天然虾池的弧菌对复方新诺明、庆大霉素、TMP和环丙沙星高度敏感;在水平差异上,高位新池的弧菌比传统精养池和天然虾池对12种抗菌药更具耐药性,同时多重耐药菌株在高位新池中出现,可能与虾苗来源和配合饲料中添加了抗菌药物有关。水质监测结果表明,养殖过程中,虾池水域环境逐渐富营养化,无机氮和Chla超过富营养化阈值,细菌总数增加;两个精养池的水体富营养化程度高于天然虾池;调查期间的弧菌数量在对虾发病的感染剂量阈值范围之内,尚无弧菌病害发生的潜在危险。 相似文献
996.
WANG Liang SHENG Jinyu 《中国海洋大学学报(英文版)》2005,4(4):349-356
An advanced ocean observatory has been established in Lunenburg Bay of Nova Scotia, Canada as part of an interdisciplinary research project of marine environmental prediction. The development of a high-resolution coastal circulation model is one of important components of the observatory. The model horizontal resolution is 60m and the vertical resolution is about 1 m. The coastal circulation model is used to simulate the semi-diurnal tidal circulation and associated nonlinear dynamics with the M2 forcing specified at the model open boundaries. The model is also used to simulate the storm-induced circulation in the bay during Hurricane Juan in September 2003, with the model forcing to be the combination of tides and remotely generated waves specified at the model open boundaries and wind stress applied at the sea surface. The model results demonstrate strong interactions between the local wind stress, tidal forcing, and remotely generated waves during this period. Comparison of model results with the surface elevation and current observations demonstrates that the coastal circulation model has reasonable skills in simulating the tidal and storm-induced circulation in the bay. 相似文献
997.
998.
In this paper, an arbitrary Lagrangian–Eulerian (ALE) method is generalized to solve consolidation problems involving large deformation. Special issues such as pore‐water pressure convection, permeability and void ratio updates due to rotation and convection, mesh refinement and equilibrium checks are discussed. A simple and effective mesh refinement scheme is presented for the ALE method. The ALE method as well as an updated‐Lagrangian method is then used to solve some classical consolidation problems involving large deformations with different constitutive laws. The results clearly show the advantage and efficiency of the ALE method for these examples. Copyright © 2007 John Wiley & Sons, Ltd. 相似文献
999.
Assessing pollutions of soil and plant by municipal waste dump 总被引:1,自引:0,他引:1
Changli Liu Yun Zhang Feng’e Zhang Sheng Zhang Miying Yin Hao Ye Hongbing Hou Hua Dong Ming Zhang Jianmei Jiang Lixin Pei 《Environmental Geology》2007,52(4):641-651
Research is few in the literature regarding the investigation and assessment of pollutions of soil and plant by municipal
waste dumps. Based upon previous work in seven waste dumping sites (nonsanitary landfills) in Beijing, Shanghai and Shijiazhuang,
this study expounds the investigation and assessment method and report major pollutants. Using relative background values,
this study assesses soil pollution degree in the seven dumping sites. Preliminary conclusions are: (1) pollution degrees are
moderate or heavy; (2) pollution distance by domestic waste that is dumped on a plane ground is 85 m; (3) the horizontal transport
distance of pollutants might be up to 120 m if waste leachates are directly connected with water in saturated soils; (4) vertical
transport depth is about 3 m in unsaturated silty clayey soils. Furthermore, using relative background values and hygiene
standards of food and vegetable this study assesses the pollutions of different parts of reed, sorghum, watermelon and sweet-melon.
It is found: (1) in comparison with the relative background values in a large distance to the waste dumping sites, domestic
wastes have polluted the roots and stems of reed and sorghum, whereas fine coal ash has polluted the leaves, rattans and fruits
of watermelon and sweet-melon; (2) domestic wastes and fine coal ash have heavily polluted the edible parts of sorghum, water
melon and sweet-melon. As, Hg, Pb and F have far exceeded standard values, e.g., Hg has exceeded the standard value by up
to 650–1,700 times and Cd by 120–275 times, and the comprehensive pollution index is up to 192.9–369.7; (3) the polluted sorghum,
watermelon and sweet-melon are inedible. 相似文献
1000.
Since the Xingtai (邢台) earthquake in 1966,China Earthquake Administration has carried out a survey campaign along more than thirty deep seismic sounding (DSS) profiles altogether about twenty thousand kilometers long in North China to study the velocity structure of the crust and the upper mantle in this region,and has obtained a great number of research findings. However,these researches have not provided a 3D velocity structure model of the crust of North China and cannot provide seismic evidence for the study of the deep tectonic characteristics of the crust of the whole region. Hence,based on the information from the published data of the DSS profiles,we have chosen 14 profiles to obtain a 3D velocity structure model of North China using the vectorization function of the GIS software (Arc/Info) and the Kriging data gridding method. With this velocity structure model,we have drawn the following conclusions: (1) The P-wave velocity of the uppermost crust of North China changes dramatically,exhibiting a complicated velocity structure in plane view. It can be divided into three velocity zones mainly trending towards north-west. In the research area,the lowest-velocity zones lie in the Haihe (海河) plain and Bohai (渤海) Bay. Although the geological structure of the sedimentary overburden in the study area is somewhat inherited by the upper crust,there are still several differences between them. (2) Generally,the P-wave velocity of the crust increases with depth in the study area,but there still exists local velocity reversion. In the east,low-velocity anomalies of the Haihe plain gradually disappear with increasing depth,and the Shanxi (山西) graben in the west is mainly characterized by relatively low velocity anomalies. Bounded by the Taihang (太行) Mountains,the eastern and western parts differ in structural trend of stratum above the crystalline basement. The structural trend of the Huanghuaihai (黄淮海) block in the east is mainly north-east,while that of the Shanxi block and the eastern edge of the Ordos block is mainly north-west. (3) According to the morphological features of Moho,the crust of the study area can be divided into six blocks. In the Shanxi block,Moho apppears like a nearly south-north trending depression belt with a large crustal thickness. In the southern edge of the Inner Mongolia block and the south of the Yanshan (燕山) block,the Moho exhibits a feature of fold belt,trending nearly towards east-west. In the eastern edge of the Ordos block,the structure of Moho is relatively complex,presenting a pattern of fold trending nearly towards north-west with alternating convexes and concaves. Beneath the Huanghuaihai block,the middle and northern parts of the North China rift zone,the Moho is the shallowest in the entire region,with alternating uplifts and depressions in its shape. For the anteclise zone in the west of Shandong (山东) Province,the Moho is discontinuous for the fault depression extending in the north-west direction along Zaozhuang (枣庄) -Qufu (曲阜). 相似文献