Ontogeny of the lymphoid organs of Japanese flounder, Paralichthys olivaceus     

Liu Yun  Jiang Guoliang  Zhang Shicui 《中国海洋大学学报(英文版)》2004,3(2):161-165

Histological study on the ontogeny of the lymphoid organs, kidney, thymus and spleen of Japanese flounder, Paralichthys olivaceus, from hatching to 40 d was carried out. The pronephric kidney duct appeared early in hatching although the primordial haemopoietic stem cells were observed within a week after hatching. The spleen was first seen after 8d of hatching. The thymus appeared after 15d, situated near the pronephric kidney. Small lymphoid cells appeared during the later phase of the post-larval stage in the sequence of thymus, kidney and spleen. During the 40d of observations, there were no distinct inner or outer zones in thymus and no red or white pulp in spleen. These results suggest that the nonspecific defense immune system plays a very important role in the early larval stage of Japanese flounder.  相似文献   

形变大地测量学的进展、问题与地震预报   总被引：12，自引：7，他引：5  

周硕愚  吴云  李正媛  杜瑞林 《大地测量与地球动力学》2004,24(4):95-101

简要概括了形变大地测量学的革命性进展，研讨了它的科学特色、功能和定义以及对地球科学和防灾减灾的推动。形变大地测量学有助于从根本上击破多年来制约地震预报的“瓶颈”，但也存在不少急待解决的问题。着重研讨了在21世纪前10年，形变大地测量学如何依托多年的学科积累并充分受益于人造卫星和数字化等新技术，开展创新性研究和试验以推进地震预报。为此，对当前的研究工作提出了12条科学技术途径。最后对学科名称提出了建议。  相似文献   

THE EFFECT OF DRAINAGE ON CHEMICALELEMENTS CONTENT OF MARSH     

ZHANG Yun  LU Xian-guo 《中国地理科学(英文版)》2001,11(1):76-79

I INTRODUCTIONWetland has very important effect on retainingwater and against drought, regUlating climate, controlling soil erosion and so on ac. Today men often attachimportance to economic effect of wetland reclamation,but neglect and destroy other functions and effectswhich result in blind wetland development, a lot ofwetland degeneration. The area of freshwater wetland inthe 1950s was 134 x 10'ha, but in the 1970s 70% hadchanged into farmland (MITSCH, 1993). The area ofwetland in d…  相似文献   

INVERSE DDA OF A SYSTEM OF BLOCKS IN SPHERE COORDINATES     

Wu Yun  Wang Hui  Zhou Shuoyu  Shi Shunying 《大地测量与地球动力学》2003,23(Z1)

1　IntroductionDiscontinuousDeformationAnalysis(DDA)developedbyShiin 1 980’s[1 ,2 ] maybeusedtocalculatethedeformationanddisplacementsinamulti blocksystemandtoanalyzetherelationbe tweenforcesanddisplacementsinthesystem .Ifthesurveydisplacementofeverypointordirectionisknown,alldisplacementsanddeformationsofblocks,eventheglide ,theclosureandthestretchoftheboundary planeofblocks ,canbecalculated .TheresultisoptimallyfittedaccordingtotheLeastSquarePrinciple.DDAismainlyusedinrockblockssystems…  相似文献   

Reference models of sunspot chromospheres     

H. S. Yun  H. A. Beebe 《Astrophysics and Space Science》1986,118(1-2):173-175

Recent observational and theoretical studies of the structure of umbral chromosphres have led us to propose new models of the region. We combine space and ground based determinations of the densitytemperature structure of the transition region with existing Caii H, K, and IR triplet spectral data to establish relatively high density, gradient models of the sunspot chromosphere.Avrett in 1981 presented theSunspot Sunspot Model which can be characterized as a physically extended, low density, plateau model. However, in a similar study, the authors (Beebeet al., 1982) pointed out that the relatively high transition region pressures derived from space observations indeed are required to reproduce high resolution Caii spectral features. Studies of the umbral chromosphere as a resonant cavity for slow-mode magneto-acoustic waves producing umbral oscillations (Zhugzhdaet al., 1984) also lead to atmospheres of relatively small physical thickness, thus higher densities.Paper presented at the IAU Third Asian-Pacific Regional Meeting, held in Kyoto, Japan, between 30 September–6 October, 1984.  相似文献   

火试金法测定铜精矿中金含量结果的不确定度评定   总被引：2，自引：0，他引：2  

江水英  肖化云  吴声东  吴波  秦云和 《岩矿测试》2008,27(4):299-301

对火试金法测定铜精矿中金含量的结果进行不确定度评定。分析了铜精矿样品称量、铜精矿样品的不均匀性和配料处理,以及金粒称量等因素对金含量测量结果不确定度的影响,并得出火试金法测量铜精矿中金含量的扩展不确定度。  相似文献   

祁连山不同植被类型对积雪消融的影响   总被引：7，自引：1，他引：6  

车宗玺  金铭  张学龙  张虎  牛云  董晓丽 《冰川冻土》2008,30(3):392-397

为研究祁连山植被对积雪消融的影响, 利用人工调查积雪深度逐日变化量和积雪盖度变化, 并结合空气雪面感热通量(SH)观测, 对祁连山水源林生态站排露沟流域海拔2 600～2 700 m青海云杉林、灌丛林、林缘、阳坡草地在2003-2007年的积雪消融进行了研究, 每年的观测从10月降雪开始到翌年5月积雪消融完结束, 共获取数据134 400个. 结果表明: 当SH<0时, 积雪消融停止;当SH>0时, 积雪消融开始;植被可以减缓积雪消融速率, 有植被的地方消融速率减慢, 反之则加快;不同植被消融速率大小顺序为草地>林缘>灌木林>乔木林;同一植被、不同坡向消融速率不同, 半阳坡云杉林＞半阴坡云杉林＞阴坡云杉林. 积雪含水率随气温升高而增大, 1月融化积雪占整个积雪的5%, 2月增大到28%, 大量积雪在3月消融, 占55%. 从坡位看, 下坡消融速率最大;在一个垂直带上, 低海拔消融速率大于高海拔. 温度是影响积雪消融的主要因子, 积雪消融速率随温度升高而增大, 反之则减小.  相似文献   

河南省洛宁县寨凹钼矿床流体包裹体研究及矿床成因   总被引：10，自引：0，他引：10  

邓小华陈衍景  姚军明李文博李 诺王 运糜 梅张 颖 《中国地质》2008,35(6):1250-1266

寨凹钼矿床位于华北克拉通南缘的熊耳地体．矿床定位受马超营断裂带的次级断裂控制,矿体呈脉状贼存于太华超群石板沟组黑云角闪斜长片麻岩中。成矿过程包括3个阶段：石英-辉钼矿阶段（I）、石英-多金属硫化物阶段（Ⅱ）、石英-碳酸盐阶段（Ⅲ）,其中,I阶段为主成矿阶段。寨凹钼矿床可见2类流体包裹体,即水溶液型和含子晶包裹体;激光拉曼指示包裹体成分主要为H2O。从早到晚,流体包裹体均一温度从I阶段100～260℃,经Ⅱ阶段110～160℃．变化为Ⅲ阶段120—180℃．矿床总体属于低温热液矿床：流体包裹体盐度从I阶段的2～25wt％NaCl．eqv演化至Ⅱ阶段的6—30wt％NaCl．eqv．然后降为Ⅲ阶段的7～25wt％NaCl．eqv。I阶段均一温度范围宽广、流体包裹体盐度由双峰式演化为单峰式以及包裹体温度-盐度双变图的负相关性指示了流体混合是主要的成矿机制。寨凹钼矿流体包裹体以高密度、高盐度的低温低压流体为特征,是含CaCl,流体参与成矿的结果,热的岩浆流体与冷的含CaCl,的卤水的混合．导致了辉钼矿的沉淀。寨凹钼矿床地质和流体包裹体特征与侵入岩相关的成矿系统一致．指示其成因类型为与侵入岩有关的钼矿床．  相似文献   

ADCM测流数据后处理探索     

许云 《水文》2008,28(6)

声学多普勒剖面测流(ADCP-Acoustic Doppler Current Profilers)是当今水文领域进行流量测验的新技术.声学多普勒流速仪ADCM(ADCM-Acoustic Doppler Current Meter)用于对水文站点的流量测验,可以实现流速信息采集的自动化,但对收集到信息的后处理提出了新的要求.本文旨在探索采用自主开发程序的方式,建立声学多普勒流速仪速度、断面特性、水位等数据序列的数学模型,进而实现ADCM洲流数据快速后处理.  相似文献   

真空堆载联合预压加固软基中孔隙水压力消散规律研究   总被引：1，自引：0，他引：1  

刘运涛  张云  蒲晓芳  高倚山  孙亚哲 《水文地质工程地质》2008,35(2):71-75

通过实测资料分析了真空堆载联合预压中不同深度的孔隙水压力、超孔隙水压力、相对超孔隙水压力随时间的变化规律,并对孔压变化的原因进行了微观解释。结果表明:(1)处理区外侧,孔压变化主要由地下水位下降引起,受真空影响较小;(2)在处理区内,孔压变化受真空负压、土体渗透性和堆载荷载的影响。真空作用下的渗流是孔压消散的主要方式,土体渗透性的强弱影响着孔压消散的速度,消散的孔压转化成有效应力,促使土颗粒移动,对孔隙水产生挤压,这使孔压消散呈脉动性特征。  相似文献