模拟深井条件下的PDC钻头破岩试验研究

利用深井破岩试验装置模拟不同井深压力条件下对泥岩进行了ＰＤＣ钻头破岩试验，试验结果表明，随着井深的增加，岩石强度增加，破碎岩石的切削力增加，同时，ＰＤＣ钻头齿形和结构对破岩效率影响较大，因此必须按深井条件和岩石特点进行ＰＤＣ钻头齿形和结构设计，以达到提高机械钻速的目的。     

中国大气水分气候变化研究

该文对我国逐日两次探空资料，经过综合静力学质量控制系统（CHQC）和序列均一性检验后，计算分析了中国大气水分的气候分布特点及近20年来气候变化趋势，讨论了大气水分变化与地面气温、夏季大气水分与我国东部降水异常之间的关系。     

对虾饵料水中稳定性测定方法的研究

对虾饵料水中稳定性,是衡量对虾饵料质量的一个非常重要的指标。本文通过对对虾饵料在海水中损失机理的探讨,提出了一个测定对虾饵料水中稳定性的新方法,并对方法中可能的影响因素进行了研究。经实际应用,本方法6次测定精密度（RSD）为1．24％。     

我国西南地区夏季降水异常与太平洋海温季节演变的关系

根据太平洋（10°S-50°N，120°E-80°W）286个网格点1951-1986年逐月平均海温资料和同期西南地区34个站月平均降水资料1），利用交叉相关场EOF分解考察我国西南地区夏季降水与太平洋海温遥相关的结构;然后通过聚类对西南地区夏季降水分成两种基本型，分别对两种降水型对应的各季海温进行距平和复自然正交（CEOF）的合成分析。结果表明:太平洋中高纬地区和赤道东太平洋海温与我国西南四川、贵州等地存在明显的季节变化遥相关;两种降水型对应的海温异常分布，无论是距平结构还是振荡传播，均有明显的两类相反特征。     

A simulation analysis on pelagic-benthic coupling ecosystem of the northern Jiaozhou Bay, Qingdao, China

INTRODUCTIONWith the development of economy and the exploitation of coastal resources, the coastal en-vironment of the northern part of China was seriously damaged, especially in the Jiaozhou Bay.More attention was paid to this phenomenon. Five comprehensive investigations on theecological dynamics of the Jiaozhou Bay were carried out from March to November of 1995. Theaim is to study the annual variation characteristics of the ecosystem dynamics of the Jiaozhou Bay.Yu Guangyao et al.…     

皱纹盘鲍经诱导后血淋巴中一些因子变化的研究

于１９９５年１１月在山东荣城大鱼岛鲍养养殖厂采集皱纹盘鲍，以大肠杆菌，弧菌为诱导物，将鲍分为三组分别进行注射，在注射后的５，１８，３２，５０ｈ分别取鲍血淋巴，测定其抗菌，溶菌，酚氧化酶和超氧化物歧化酶活力，并研究注射组各项活力的变化规律。实验结果表明，适当的刺激可增加皱纹盘鲍的抗病能力。     

27.3-day and 13.6-day atmospheric tide

An analysis of time variations in the earth's length of day (LOD) for 25 years (1973-1998) versus at- mospheric circulation changes and lunar phase is presented. It is found that, on the average, there is a 27.3-day and 13.6-day period oscillation in global zonal wind speed, atmospheric geopotential height, and LOD following alternating changes in lunar phase. Every 5-9 days (6.8 days on average), the fields of global atmospheric zonal wind and geopotential height and LOD undergo a sudden change in rela- tion to a change in lunar declination. The observed atmospheric oscillation with this time period may be viewed as a type of atmospheric tide. Ten atmospheric tidal cases have been analyzed by comparing changes in LOD, global zonal wind speed and atmospheric geopotential height versus change in lunar declination. Taken together these cases reveal prominent 27.3-day and 13.6-day tides. The lunar forcing on the earth's atmosphere is great and obvious changes occur in global fields of zonal wind speed and atmospheric geopotential height over the equatorial and low latitude areas. The driving force for the 27.3-day and 13.6-day atmospheric tides is the periodic change in lunar forcing during the moon's revolution around the earth. When the moon is located on the celestial equator the lunar declination equals zero and the lunar tidal forcing on the atmosphere reaches its maximum, at this time the global zonal wind speed increases and the earth's rotation rate decreases and LOD increases. Conversely, when the moon reaches its most northern or southern positions the lunar declination is maximized, lunar tidal forcing decreases, global zonal wind speed decreases, earth's rotation rate increases and LOD decreases. 27.3-day and 13.6-day period atmospheric tides deserve deeper study. Lunar tidal forcing should be considered in models of atmospheric circulation and in short and medium range weather forecasting.     

The fragment of Paleo-Tethys ophiolite from central Qiangtang, Tibet:Geochemical evidence of meta-basites in Guoganjianian

N-MORB-type metabasites are discovered in the Guoganjianian area, central Qiangtang, Tibet, which are mainly metagabbro with cumulate structure and metabasalt. The rocks are distributed nearly from west to east unconformably underlying the Wanghuling Group of upper Triassic. On the basis of geo- chemical analysis, we find that the content of SiO2 is 43.03%―53.42%, and TiO2 1%―2.67%, Al2O3 16.75%―21.52%, CaO 7.03%―11.13%, K2O 0.05%―0.38%; the REE pattern is slight depletion or flat, and the trace spider diagram is like that of N-MORB, so we consider that the metabasite was formed under the setting of mid-ocean ridge or adult back-arc basin, and it is the fragment of Paleo-Tethys ophiolite.     

Geochemistry and Sr-Nd isotope characteristics of tonalites in Zêtang, Tibet: New evidence for intra-Tethyan subduction

Tonalites from the island arc rock assemblage in the Zêtang segment of the Yarlung Zangbo suture zone were analyzed for major, trace elements (including REE) and Sr-Nd isotope. The experimental datademonstrate that the tonalites have the adakite-like characteristics, including high SiO2 (58%-63%),Al2O3 (18.4%-22.4%), Sr (810×10-6-940×10-6), Sr/Y (77-106), low HREE (Y=9×10-6-11×10-6, Yb=1×10-6-1.3×10-6), with LREE enrichment and faint Eu positive anomaly. Isr (0.70421-0.70487) is relatively low whereas 143Nd/144Nd (0.512896-0.512929) and εNd(t) values ( 6.7- 7.3) are high. These feainvolvement of a small amount of oceanic sediments. The identification of Z(e)tang adakites, derived from slab melting, presents new evidence for the intra-Tethyan subduction and the previous suggestion about the existence of intra-oceanic island arc within Tethys.     

Multi-year Simulations and Experimental Seasonal Predictions for Rainy Seasons in China by Using a Nested Regional Climate Model （RegCM_NCC）. Part Ⅰ： Sensitivity Study

A modified version of the NCAR/RegCM2 has been developed at the National Climate Center （NCC）, China Meteorological Administration, through a series of sensitivity experiments and multi-year simulations and hindcasts, with a special emphasis on the adequate choice of physical parameterization schemes suitable for the East Asian monsoon climate. This regional climate model is nested with the NCC/IAP （Institute of Atmospheric Physics） T63 coupled GCM to make an experimental seasonal prediction for China and East Asia. The four-year （2001 to 2004） prediction results are encouraging. This paper is the first part of a two-part paper, and it mainly describes the sensitivity study of the physical process paraxneterization represented in the model. The systematic errors produced by the different physical parameterization schemes such as the land surface processes, convective precipitation, cloud-radiation transfer process, boundary layer process and large-scale terrain features have been identified based on multi-year and extreme flooding event simulations. A number of comparative experiments has shown that the mass flux scheme （MFS） and Betts-Miller scheme （BM） for convective precipitation, the LPMI （land surface process model I） and LPMII （land surface process model Ⅱ） for the land surface process, the CCM3 radiation transfer scheme for cloud-radiation transfer processes, the TKE （turbulent kinetic energy） scheme for the boundary layer processes and the topography treatment schemes for the Tibetan Plateau are suitable for simulations and prediction of the East Asia monsoon climate in rainy seasons. Based on the above sensitivity study, a modified version of the RegCM2 （RegCM_NCC） has been set up for climate simulations and seasonal predictions.