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1.
试验了几种抗菌药物对马氏珠母贝幼虫的毒性,结果表明,几种抗菌药物对马氏珠母贝D型幼虫96h半数耐受浓度(96TLM=96LC50)及安全浓度分别为:氯霉素45.4×10-6、4.5×10-6;红霉素53.0×10-6、5.3×10-6;呋喃西林64.1×10-6,6.4×10-6土霉素、百炎净、硫酸链霉素、青霉素G钠均大于100×10-6及10×10-6。但若以幼虫活力、摄食率、日生长率的变化作为观察指标,则这些药物的96TLM及安全浓度分别落在下述区间内:土霉素(38~67)×10-6、(3.8~6.7)×10-6;百炎净(52~67)×10-6、(5.2~6.7)×10-6;硫酸链霉素(25~38)×10-6、(2.5~3.8)×10-6;青霉素G钠仍大于100×10-6及10×10-6。下列药物在一定浓度下对幼虫的生长有明显的促进作用:青霉素G钠,百炎净(13~38)×10-6;呋喃西林13×10-6。  相似文献   

2.
用孔雀绿、福尔马林对罗氏沼虾各期蚤状幼体及仔虾进行急性毒性试验。结果表明,孔雀绿的24hLC50是:蚤状幼体为0.141~0.257×10-6、仔虾为0.271×10-6;48hLC50是:蚤状幼体0.077~0.152×10-6、仔虾为0.174×10-6;安全浓度蚤状幼体为0.007~0.016×10-6、仔虾为0.021×10-6.福尔马林的24hLC50是:蚤状幼体为23,5~51.9×10-6、仔虾为42.6×10-6;48hLC50是:蚤状幼体为14.3~33.6×10-6、仔虾为28.7×10-6;安全浓度蚤状幼体为1.2~4.2×10-6、仔虾为3.9×10-6。  相似文献   

3.
本文研究了鲁米诺-高碘酸钾-钒体系产生化学发光反应,建立了测定痕量钒新的化学发光法。在EDTA为活化剂存在下,方法的检出限为3×19(-9)g/ml,工作曲线响应浓度范围为1×10(-8)~1×10(-6)g/ml,测定5×10(-7)g/ml钒的相对标准偏差为2.5%~3.0%之间。该法有很好的选择性,用于测定岩矿等物料中痕量钒可获得满意结果。  相似文献   

4.
家峪-北五台沟一带太古宙变质岩经过韧性剪切作用。变质岩中石英的应变特征揭示了该韧性剪切带各种因素的量,经分析计算差异应力为σ_1-σ_3=122.87MPa,最大剪切应力为τ_(max)=61.44MPa,剪切带的温度为55O-650℃,剪切带形成深度为18-22km,静压力即围压为450-600MPa,弗林指数K=0.49-0.50.经历三维应变,X轴增加60%,Y轴增加25%,Z轴缩短50%,体积缩小3%,变形强度为R=2.83,应变速率为ε=(4×10 ̄(-9)-4×10 ̄(-10))/s,变形比温度值为T/Tm=0.96-1.13,等效粘滞度为(3.07×10 ̄(10)-3.07×10 ̄(11))MPa/s。石英的应力结构发育。  相似文献   

5.
采用静水生物试验法测定了氟乐灵对斑节对虾卵和幼体的急性毒性。结果表明:氟乐灵对斑节对虾无节幼体、蚤状幼体、糠虾幼体和仔虾的24hLC50/×10-6分别是1.68,0.83,1.84和2.09;48hLC50/×10-6分别是0.76,0.53,1.09和1.51。5.01×10-6氟乐灵浸浴受精卵12h,50%的受精卵可孵化。第22天仔虾用10×10-6以下浓度的氟乐灵浸浴5min,对其存活率无影响。  相似文献   

6.
理塘地区擦岗隆洼岩组硅质岩的 w(SiO2)为81.27%~92.71%,Si/Al比值为11.69~37.22,表明硅质岩的泥质成分相对较多,硅质岩样品的稀土元素总量较低,多 介 于22.61×10-6~41.67×10-6之 间,轻稀土元素富集。硅 质 岩 的 w(V)为10.718×10-6~38.14×10-6,Ti/V 比值为10.5~89.0,与大陆边缘硅质岩相应值相近。对硅质岩岩石学和地球化学的研究表明理塘洋盆于早三叠世就已经进入到洋壳俯冲消减、岛弧发育的活动陆缘演化阶段。   相似文献   

7.
在野外地质工作基础上,运用岩石地球化学方法,通过主量元素、稀土元素和微量元素研究,探讨了水洞岭矿区石英角斑岩的岩石化学特征、形成环境及其与成矿的关系。研究表明:石英角斑岩的w(SiO2)=73.11%~79.30%,w(K2O)=1.20%~5.99%,w(Na2O)=1.57%~4.61%,w(K2O+Na2O)=4.82%~8.67%,Na2O/K2O=0.45~3.49,ACNK=0.99~1.25。稀土元素总量w(ΣREE)=70.19×10-6~198.75×10-6,轻稀土元素富集,重稀土元素亏损,轻重稀土元素分馏明显((La/Yb)N=3.65~8.20),Eu中度至轻度亏损(δEu=0.53~0.96);大离子亲石元素(Rb、Ba、Th、U、K)和 Pb等元素富集,高场强元素(Nb、Ta、Ti、P)和Sr等元素亏损。综合表明水洞岭矿区石英角斑岩形成环境类似于洋壳俯冲成因的火山弧环境。   相似文献   

8.
在水温为21.4℃—31.2℃,盐度为27.2‰—36.3‰的环境条件下,进行了企鹅珍珠贝培育附壳珍珠的研究。经287天的育珠,成活率87.5%。在收获的15个母贝中,植入直径为7~10mm的珠核47粒,佛像模型2个;收获附壳珍珠40颗,佛像2个,留核率达85.7%。其中商品珠35颗,商品珠率为83.3%。在商品珠中,珠色为银白色的16颗,占45.7%;金黄色的16颗(包括1佛像),占45.7%;污斑珠3颗,占8.6%。珍珠直径超过11mm的有5颗,10.0~10.9mm的有19颗,9.0~9.9mm的有9颗,8.0~8.9mm的仅1颗。抽测珍珠5颗,珠层厚度最大者862.5μm,最薄者562.5μm。  相似文献   

9.
为揭示土壤饱和渗透系数的变化规律,在江汉平原杨林尾-陆溪口地区分别采用 Guelph入 渗仪 和 改 进 的 TST-55型土壤渗透仪开展了土壤饱和渗透系数实验。结果表 明:采 用 Guelph入渗法在粉砂质黏壤土中测得冲积物饱和渗透系数相对较大,数量级在10-2 ~10-1之间,最高达到7.50×10-1 m/d,最小为1.40×10-2 m/d;湖积物饱和渗透系数在1.86×10-3 ~4.99×10-2 m/d之间;而残积物的为6.05×10-3 m/d,相对较小;同为粉砂壤 土,相同水位埋深条件下甘蔗地和小麦地(同 为 耕 地)的土壤饱和渗透系数明显比林地的大,这与土壤翻耕及根 系、虫孔发育等有关;在相同水位埋深条件下,粉砂壤土的土壤饱和渗透系数普遍比粉砂质黏壤土的大,主要是因 为粉砂质黏壤土比粉砂壤土的黏粒比重大、孔隙比相对较小的缘故。室内变水头达西法和 Guelph入渗法测得的土壤饱和渗透系数分别介于5.43×10-5 ~2.10×10-3 m/d和1.57×10-3 ~7.50×10-1 m/d之间。室内 变 水 头 达西法所测结果明显偏小,主要原因包括:①Guelph入渗法进行现场原位测试时,土壤有效直径相对于室内变水 头达西法使用的环刀直径要大得多;②室内变水头达西法所用土样为单一岩性,而 Guelph入渗法为原位土层,常 常具有双层或多层结构;③Guelph入渗试验期间恰逢雨季,地下水位埋深小,当支持毛细水带接近地表时,Guelph 入渗试验将受支持毛细水的影响,从而使 Guelph入渗法所测得的结果产生误差。   相似文献   

10.
东昆仑祁漫塔格-都兰成矿带是青海省重要的矽卡岩型铁多金属成矿带,胜利矽卡岩型铁铜矿床位于该成矿带东段,其成矿作用与二长花岗岩密切相关,矿体产于二长花岗岩与大理岩接触带的矽卡岩中。地球化学数据显示,胜利铁铜矿床二长花岗岩w(SiO2)为 71.84% ~74.50%,w(K2O+Na2O)为 8.03% ~8.61%,明 显 富 碱;K2O/Na2O 为 1.28~1.62,相 对 富 钾;A/CNK为0.95~0.98,属于准铝质高钾钙碱性I型花岗岩。岩石总体富集大离子亲石元素 K、Ba、Rb和活泼不相容元 素 Th、U,相对亏损高场强元素 Ta、Nb、P、Ti等。样 品 稀 土 元 素 总 量 w(∑REE)=132.73×10-6~181.36×10-6,(La/Yb)N 为7.40~11.67,δEu为0.67~0.78,稀土元素配分曲线呈右倾型,具有较明显的轻稀土元素富集、重稀土元素亏损的特征,具 Eu负 异 常。二长花岗岩 LA-ICP-MS锆石 U-Pb加权平均年龄为(240.5±2.8)Ma,形成于中三叠世。综合研究表明,二长花岗岩是阿尼玛卿洋盆向北俯冲,致使壳幔岩浆发生混合,后经侵位、结晶分异形成。   相似文献   

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12.
Based on the hydrographic data in austral summer during the 22nd Antarctic Expedition of China(2005/2006),some features can be found about the northern margin of Emery ice shelf as follows.The heat content in the surface layer(0-50 m) at the eastern end and the western end of the ice-shelf margin is much higher than that at the middle.The upper mixing-layer depth and the seasonal thermocline depth at the middle of the ice-shelf northern margin are much shallower than those at the both ends.However there is much less difference between the middle and the ends in the bottom layer.The remote sensing photos show that the inhomogeneity in the surface-layer water is closely related to the spatial distribution of the floes and polynia in the area.  相似文献   

13.
Phylogenetic analysis based on 16S rDNA of 8 strains of cultivable bacteria isolated from Arctic sea-ice was studied.The results showed that strain BJ1 belonged to genus Planococcus,which was a genus of low mole percent G C gram-positive bacteria;strain BJ6 belonged to genus Burkholderia of β-proteobacteria and the rest 6 strain all belonged to γ-proteobacteria,of which strain BJ8 was a species of Pseudoalteromonas,strain BJ2-BJ5 and BJ7 were members of genus Psychrobacter.Phylogenetic analysis also indicated that bacteria of genus Psychrobacter of the isolates formed a relatively independent phylogenetic cluster in comparison with other bacteria belonged to genus Psychrobacter.  相似文献   

14.
正1 Aims and Scope Advances in Polar Science(APS)is an international,peer-reviewed journal jointly sponsored by the Polar Research Institute of China and the Chinese Arctic and Antarctic Administration.APS is a comprchensive academic journal dedicated to presentation of multi-disciplinary achievements in Arctic and Antarctic expeditions and research.Its primary purpose is to publish achievements in fundamental research,applied  相似文献   

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《山地科学学报》2014,(4):I0004-I0009
<正>AIMS AND SCOPE(Editorial Policy)The Journal of Mountain Science(JMS)is devoted to mountains and their surrounding lowlands-ecoregions of particular global importance,with a particular emphasis on the important highlands/mountains in the world,such as the Tibetan Plateau,the Himalayas,the Alps,the Andes,the Rockies and many other mountain ranges of our planet.  相似文献   

17.
<正>The Journal of Mountain Science(JMS),founded in2004,is an international English-language journal on mountain sciences.JMS is supervised by the Chinese Academy of Sciences(CAS),sponsored by the Chengdu Institute of Mountain Hazards and Environment,CAS,published by Science Press China,and distributed by Springer exclusively throughout the world(excluding Mainland China).The JMS is published bimonthly,fulltexted in SpringerLink and CNKI,indexed/abstracted by  相似文献   

18.
Foreword     
正Rapid changes of Arctic sea ice cover have been in the focus of the international climate research community in recent years.Quite a few of nations have completed a large number of related surveys and research projects in the Arctic Ocean.Up to now,China has performed six research cruises to the Arctic Ocean resulting in a significant volume of research output.Improved knowledge on the atmospheree-sea ice-ocean interactions in the Arctic is a  相似文献   

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The GRV 024516 and GRV 024517 meteorite samples collected from Grove Montains,Antactica are ureilite and H5 ordinary chondrite,respectively.Based on the study of mineralogy-petrology,the cosmic-ray exposure ages and gas retention ages of these two meteorites were determinated and calculated.Their cosmic-ray exposure ages are 33.3 Ma,51.7 Ma,and gas retention ages are 1936.8 Ma and 3720 Ma,respectively.The ureilite contains diamond,graphite and amorphous C,which are mainly carrier of noble gases indicating obviously shock metamorphism effects,which induced 40Ar partial loss.The H5 chondrite indicates thermal metamorphism of parent body,its gas retention age fall the range between 3220 Ma and 4510 Ma of the least shocked H5 chondrites  相似文献   

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