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    题名 作者 年代 出处 被引量
1郾城郝家台遗址的发掘显示文摘郝家台遗址位于河南省漯河市偃城县东3公里石槽赵村东北的台地上。南去1公里为漯河市,沙河在遗址南1公里处由西向东流去,京广铁路从遗址的西南部穿过(图一)。遗址平面呈椭圆形,东西长260、南北宽250米,遗址总面积65000平方米。遗址高出附近地面2—3米,海拔62.1米。郝家台俗称“磕脚台”,其上原有“裴晋公庙”,HPAI and Yancheng County Memorial Hall of Xu Shen, 1992华夏考古1992,,3:57
2A numerical study of the South China Sea deep circulation and its relation to the Luzon Strait transport显示文摘A fine-resolution MOM code is used to study the South China Sea basin-scale circulation and its relation to the mass transport through the Luzon Strait. The modal domain includes the South China Sea, part of the East China Sea, and part of the Philippine Sea so that the currents in the vicinity of the Luzon Strait are free to evolve. In addition, all channels between the South China ,Sea and the Indonesian seas are closed so that the focus is on the Luzon Strait transport. The model is driven by specified Philippine Sea currents and by surface heat and salt flux conditions. For simplicity, no windstress is applied at the surface.The simulated Luzon Strait transport and the South China Sea circulation feature a sandwich vertical structure from the surface to the bottom. The Philippine Sea water is simulated to enter the South China Sea at the surface and in the deep ocean and is carried to the southern basin by western boundary currents. At the intermediate depth, the net Luzon Strait transport is out of the South China Sea and is fed by a western boundary current flowing to the north at the base of the thermocline. Corresponding to the western boundary currents, the basin circulation of the South China Sea is cyclonic gyres at the surface and in the abyss but an anti-cyclonic gyre at the intermediate depth. The vorticity balance of the gyre circulation is between the vortex stretching and the meridional change of the planetary vorticity.Based on these facts, it is hypothesized that the Luzon Strait transports are determined by the diapycnal mixing inside the entire South China Sea. The South China Sea plays the role of a 'mixing mill' that mixes the surface and deep waters to return them to the Luzon Strait at the intermediate depth. The gyre structures are consistent with the Stommel and Arons theory (1960), which suggests that the mixlng-induced circulation inside the South China Sea should be cyclonic gyres at the surface and at the bottom but an anti-cyclonic gyre at the intermediate depth. The simulated gyre circulation at the intermediate depth has been confirmed by the dynamic height calculation based on the Levitns hydrography data.The sandwich transports in the Luzon Strait are consistent with recent hydrographic, al observations.Model results suggest that the Kuroshio tends to form a loop current in the northeastern South China Sea. The simulated Kuroshio Loop Current is generated by the pressure head at the Pacific side of the Luzon Strait and is enhanced by theβ- plane effects. The β- plane appears to be of paramount importance to the South China Sea circulation and to the Luzon Strait translports. Without theβ-plane, the Luzon Strait transports would be greatly reduced and the South China Sea circulation would be complete-ly different.Yuan Dongliang1. Goddard Earth Science and Technology Center, University of Maryland, Baltimore County Code 971, Laboratory for Hydrospheric Processes, NASA/Goddard Space Flight Center, Greenbelt, MD 20771, USA 2002Acta Oceanologica Sinica2002,21,2:37
3浙江绍兴印山大墓发掘简报显示文摘印山大墓位于浙江省绍兴县城西南,是春秋晚期越王的陵墓。该墓的墓圹和墓道总长达100米,是在印山之巅的岩石中凿出,上堆筑高大的封土墩,四周围绕印山开挖长方形的壕沟,构成8500平方米的陵园。印山大墓墓室用加工规整的巨大方木构筑,室内髹漆,横截面呈等腰三角形,形成长达34.8米、高约5米的长条形木屋,分为前中后三室。中室顺置的一长6米余的独木棺,采用一大型圆木一剖为二,再经掏挖而成。该墓虽早年被盗,随葬品较少,但其规模庞大,结构奇特,是我国近年来重大考古发现之一。据研究,该墓就是史书上记载的“木客大冢”,墓主应是越王勾践之父允常。本期刊发了印山大墓的发掘简报。The Institute of Archaeology of Zhejiang Province CPAM of Shaoxing County 1999文物1999,,11:24
4Estimate of Methane Emission from Rice Paddy Fieldsin Taihn Region, China显示文摘EstimateofMethaneEmissionfromRicePaddyFieldsinTaihnRegion,ChinaCAIZU-CONG;XUHUA;ZHANGHAN-HUI;andJINJI-SHENG(InstituteofSoilSc...CAI ZU-CONG XU HUA ZHANG HAN-HUI and JIN JI-SHENG(Institute of Soil Science, Chinese Academy of Sciences, P. O. Box 821, Nanjing 210008 ( China)Agricultural Extension Station of Wuxian County, Suzhou 215007 (China)) 1994Pedosphere1994,4,4:22
5河北省永年县何庄遗址发掘报告显示文摘何庄遗址位于河北省永年县临沼关西南约15公里的何庄北,北临通天河,西面是起伏的丘陵地带,东面约1公里处为北两岗水库(图一)。何庄遗址是1987年永年县文物保管所在文物普查中发现的,面积约3万平方米。由于当地农民烧砖取土,对遗址的破坏非常严重,因此,1988年8月9日至9月12日,邯郸地区文物保管所和永年县文物保管所联合对该遗址进行了抢救性发掘,开挖5×5米探方13个,面积325平方米。Handan Prefectural Office for the Preservation of Ancient Monuments and Yongnian County Office for the Preservation of Ancient Monuments, 1992华夏考古1992,,4:21
6The Zoulang Nanshan Caledonian Subduct ion Complex in the Northern Qilian Mountains and Its Dynamics显示文摘The front of the Zoulang Nanshan Caledonian volcanic island arc zone in the northern Qilian Mountains is a forearc accretionary terrane, composed of multiple accretionary volcanic island arcs, flysch accretionary wedges,high-pressure metamorphosed detachment zones and remnants of ophiolites. It resulted from the northeastward subduction of the Early Palaeozoic Qilan oceanic crust beneath the Alxa block. High-pressure metamorphism, which occurred during the subduction, progressed through three stages: the initial stage of medium T-high P,the main stage of temperature decrease and pressure increase, and the lag stage of pressure decrease and temperature increase. Finally the paper presents a retrotrench subduction dynamic model indicative of northward subduction of the central Qilian block and southward accretion of the Alxa block during the period of 450-500 Ma.Xu Zhiqin, Xu Huifen, Zhang Jianxin, Li Haibing, Zhu Zhizhi, Qu Jingchuan,Institute of Geology, Chinese Academy of Geological Sciences, BeijingChen Daizhang, Chen Jinlu, China University of Geosciences, Beijingand Yang KaichunNo. 2 Q ilian Geological Party, Bureau of Geology and Mineral Resources of Q inghai Province, Q ilian County, Q inghai 1994Acta Geologica Sinica(English Edition)1994,68,3:19
7Ecological niche suitability model with an application in Taojiang land use planning显示文摘EcologicalnichesuitabilitymodelwithanapplicationinTaojianglanduseplanningOuyangZhiyun;WeismanJason;WangRusong(ResearchCenterf...Ouyang Zhiyun Weisman Jason Wang Rusong(Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences , Beijing 100085, China) Fu Guinan (Taojiang County Land Bureau, Hunan Province, China) 1994Journal of Environmental Sciences1994,6,4:17
8淅川县和尚岭春秋楚墓的发掘显示文摘和尚岭墓地位于淅川县城南约50公里丹江口水库西岸的龙山脚下,仓房乡陈庄行政村东沟村东南1公里处,西去0.4公里为下寺楚墓群(图一)。1989年,丹江口水库水位下降,和尚岭楚墓被盗。淅川县公安局在仓房乡党委、县文管会的协助下,对盗墓活动进行严厉打击,并收缴了一部分文物,其中有铜编钟、铜方壶、铜簋、铜鼎等。1990年2月28日,河南省文物研究所与南阳地区文物研究所、淅川县博物馆组成考古队,前往抢救性发掘。发掘工作从3月2日开始,至3月19日结束。这次共发掘清理古墓葬4座,其中2座为春秋楚墓,2座为汉墓。现将2座楚墓的发掘情况简报如下。两座楚墓(编号 HXHM 1、HXHM 2)HPAI,Nanyeng Prefectural Antiquities Institute and Xichuan County Museum, 1992华夏考古1992,,3:15
9河南杞县朱岗遗址试掘报告显示文摘一、遗址概况和发掘方法杞县位于豫东西部,东距商丘约90公里,西距郑州约120公里。其地北依黄河,南临涡水,《禹贡》豫州之域,商周杞国旧地,今属开封市辖区。由于历史时期河、济泛滥,这一带的古文化遗址也屡遭湮没,淤土广厚,曾长期被视为无古可考或有古难觅之地,以往尚未进行过任何早期遗址的发掘工作。为了填补这一空白。Archaeology Speciality of Zhengzhou University,Kaifeng Municipal Museum and Qixian County office for the Preservation of Ancient Monuments, 1992华夏考古1992,,1:13
10Upper Devonian and Lower Carboniferous Sequence Stratigraphy of South China显示文摘In South China four depositional sequences are recognized in the upper part of Upper Devonian and Tournaisian. They are named SQ0 SQ1, SQ2 and SQ3 in ascending order. SQ0 is Strunian (uppermost Devonian), and the other three Tournaisian in age. These four depositional sequences appear to correlate fairly well with the four sequence recognized in Europe, North America and other areas. This may suggest that these sequences are synchronous depos- its resulted from the eustatic changes. The present study on sequence stratigraphy, biostratigraphy and event stratigraphy indicates that in neritic facies areas of South China, the Devonian-Carboniferous boundary, matching the boundary between Siphonodella praesulcata zone and S. sulcata zone in pelagic facies areas, is not only higher than the top of the Cystophrentis zone, but also higher than the top of the Devonian-Carboniferous boundary event bed. In neritic facies areas, the Devonian-Carbonifrerous boundary is marked by the most distinct transgressive surface within the Cystophrentiseudouralina interval zone, i. e. at the base of the TST of the SQ1. This boundary coincides with the top surface of the event bed resulted from the eustatic fall, and approximately corresponds to the basal part of Rseudouralina assemblage zone.Wang Xunlian Li Shilong (Department of Geology and Mineral Resources, China University of Geosciences, Beijing 100083) Wang Yue (Mineral Office of Dushan County, Dushan 558200) 1996Journal of Earth Science1996,15,1:12
11金坛南宋周瑀墓显示文摘南宋周(王禹)墓在金坛县茅麓公社向阳大队,位于镇江地区金坛和句容县交界的茅山东麓黑龙岗东向坡上,东距金坛县城三十公里。一九七五年七月发现。这座墓的形制和随葬器物与过去发现的一般南宋墓没有什么区别,所不同的是,在这墓中发现了一份牒文抄件(图版壹),大量的衣物丝织品,以及一具保存完好的墓主尸体。The Chengkiang Municipal Museum and CPAM, Chin-t’an County 1977考古学报1977,,1:12
121991年河南罗山考古主要收获显示文摘1991年,为探讨淮河流域古代文化面貌及与周邻文化相互作用这一学术课题,我们对淮河上游信阳地区信阳、罗山、光山、潢川、息县、淮滨、固始等七县的古代文化遗址进行了调查,同时对罗山天湖商周墓地、李上湾、擂台子遗址进行了小面积的发掘。现以罗山县为重点,将此次调查与发掘的主要收获报告如下。罗山县位于信阳地区中部偏西,商代晚期这里为息族方国领地,春秋时又有息、江等小方国,战国时为楚所统一。这里地处秦岭——淮河南北自然地理分界地带。HPAI,Xinyang Prefectural CPAM and Luoshan County CPAM, 1992华夏考古1992,,3:11
13THE CASE STUDY ON THE EFFECT OF CO_2 IN CAVE ATMOSPHERE ON STABILITY OF SPELEOTHEM SCENERY IN YAOLIN CAVE, ZHEJIANG PROVINCE, CHINA显示文摘Because of the development of tourist activities and the facilities in the show cave, the closed system of show cave has been changed into the complicated open system. The great number of the visitors and the landscape lights give great deal of thermoenergy to the show cave system, especially the high intensive lights make the temperature nearby goes up very fast and reduce the humidity. After the visitors leaving and the lights switching off, the temperature goes down and humidity increases even upto saturation, the condensation taken place. In the dry seasons, the cave humidity is relative low, even down to 40 50 percent. The administrations of show cave rushes the water to clean the touristic trails and keep the high humidity as to protect the cave environment. Under the function of artificial readjustment, the humidity of Yaolin cave atmosphere reaches to 97-100 percent throughtout the year.Song Linhua Yang Jingrong Lin Junshu Group of Karstology and Speleology, Institute of Geography, CAS, Beijing 100101 People’s Republic of ChinaWang Laihong Administration of Yaolin Cave, Tonglu County, Zhejiang Province, 311500 People’s Republic 1997Journal of Geographical Sciences1997,7,3:8
14河南永城芒山西汉梁国王陵的调查显示文摘芒山位于河南永城县东北30余公里处,面积20余平方公里,王引河从其西部流过(图一)。芒山是芒砀山、保安山、僖山、黄土山、铁角山、夫子山等山的总称。古时亦称砀山,《说文解字》“砀,文石也”。因此山出文石(制作砚台的石料)而得名。这里地处豫、皖交界,素有“豫东门户”之称,为历史上的豫东重镇所在。HPAI and Yongcheng County CPAM, 1992华夏考古1992,,3:7
15Estimation on the Total Quantity of Biomass Energy and Its Environmental Benefit Analysis in Shandong Province显示文摘[Objective] The aim was to estimate the total quantity of biomass energy and analyze its environmental benefit in Shandong Province.[Method] Based on the data from the statistics yearbook of Shandong Province in 2010,the total quantity of biomass resources and biomass energy in Shandong Province in 2009 was estimated,and its environmental benefit was analyzed.[Result] Biomass resources in Shandong Province mainly refer to crop residues,forest residues,grassland changed from degraded land.If degraded land became grassland,the total quantity of biomass resources and biomass energy in Shandong Province in 2009 was 182.808 8 million tons and 2.68×1015 kJ respectively.Meanwhile,the reduction of total emission of CO2,SO2 and nitrogen oxides was up to 241.265 million tons,and the reduced emission of SO2 accounted for 48.9% of annual SO2 emission in Shandong in 2009.Planting energy crops plays important roles in the development of new energy sources,reduction of greenhouse gas emission and environmental protection.[Conclusion] The study could provide theoretical foundations for the establishment of energy policy and study on development strategy of biomass energy in Shandong Province.ZHENG Yan-lin1,2,LI Fu-li3,LIU Fang4 1.College of Science,Shandong University of Science and Technology,Qingdao 266510,China 2.College of Environmental Science and Engineering,Ocean University of China,Qingdao 266101,China 3.Qingdao Institute of Bioenergy and Bioprocess Technology,Chinese Academy of Sciences,Qingdao 266101,China 4.Animal Husbandry and Veterinary Bureau of Wenshang County,Jining 272500,China 2011Meteorological and Environmental Research2011,2,7:6
16不同类型水库引种斜颌鲴试验小结显示文摘斜颌鲴在我县桃园河水库已形成了一个自然种群,占该水库渔获物总重量的8%,有相当大的经济价值。1973年起湖北省水生生物研究所与桃园河水库管理处协作对斜颌鲴的生物学,人工繁殖技术和苗种培育进行了研究,了解到斜颌鲴以腐植质,有机碎屑及底生藻类为食,可以充分利用水体的饵料资源。Bureau of Water Utilization and Electric Power,Sui County,Hupei Province 1977水生生物学集刊1977,6,2:6
17Treatment of rotaviral gastroenteritis with Qiwei Baizhu powder显示文摘AIM To observe the effects of Qiwei Baizhu Powder ( QWBZP) on rotaviral gastroenteritis in children and in animal models.``METHODS Enrolled patients were divided into two groups, and one group was treated with oral rehydration solution(ORS) and the other treated with oral liquid of QWBZP. Neonate mice were orally infected with 50 μLrotavirus suspension (4 × l0s PFU/mL) and treated with ORS or oral liquid of QWBZP, respectively.``RESULTS Eighty-three cases of rotaviral gastroenteritis treated with QWBZP revealed a better efficacy than that treated with ORS (x2 - 10.8T, P<0.05). The contents of sodium and glucose as well as number of patients with positive human rotavirus antigen in stool in QWBZP group were all less than that in ORS group. In animal models,QWBZP was found effective in treating rotavirus gastroenteritis in neonate NIH mice, as compared with control groups. In QWBZP group, the mortality of infected mice was decreased by 73.3%, the body weight of infected mice was increased, the contents of sodium and glucose as well as number of mice with positive rotavirus antigen in feces were significantly reduced, and the pathological changes such as damage of small intestinal mucosa and villi were also obviously alleviated.``CONCLUSION QWBZP has effects on improving the absorptive function of small intestine, shortening the duration of diarrhea and rotavirus shedding from stool and alleviating the pathological changes of small intestine induced by rotavirus.Shuang-Teng He~1 Fei-Zhou He~2 Can-Rong Wu~3 Shun-Xiang Li~2 Wei-Xin Liu~4 Yong-Fang Yang~2 Shi-Sheng Jiang~2 Gang He~1 1 Institute of Combined Traditional Chinese and Western Medicine,Xiangya Hospital,Hunan Medical University,Changsha,410008,China2 Hunan Province Academy of Traditional Chinese Medicine,Changsha 410006,China3 Department of Microbiology,Hunan College of Traditional Chinese Medicine,Changsha 410007,China4 Department of Pediatrics,The Second Hospital of Shuangfeng County,Hunan Province,411700,China 2001World Journal of Gastroenterology2001,7,5:6
18河南淅川大石头山楚墓发掘报告显示文摘一、地理位置及概况大石头山位于淅川县仓房乡沿江村北,距淅川县城约80公里(图一)。山头北高南低,呈西北东南走向,西邻淅川县林场刘裴沟分场山林,位于丹江水库区内(当蓄水量至海拔150米时,整个山头都被库水淹没。而水位降至135米时,全部山头则露出水面),东、南、北三面环水,只有西部可路通林场。以此向南5公里内为徐家岭、和尚岭及下寺春秋楚墓群。这里因库水冲刷,大部分墓口表土被库水冲走,其中有一部分墓已冲刷到底部。HPAI and Xichuan County Museum 1993华夏考古1993,,3:5
19河南省陕县化纤厂宋墓发掘简报显示文摘1987年4月,三门峡市文物工作队在配合河南省陕县化纤厂基建时,与陕县文物管理委员会联合清理了三座古墓葬,现将这次发掘整理的结果简介如下: 三座墓葬形制相似,均由墓道、墓门、甬道和墓室四部分构成。为系统起见,下面分别介绍。一、一号墓 1.墓葬形制一号墓坐北朝南,方向175°,阶梯式墓道,由10级生土台阶构成,长2.44米。SMAT and Shaanxian County CPAM (Commission of the Preservation of Ancient Monuments) 1993华夏考古1993,,4:4
20阜新程沟辽墓清理简报显示文摘The tomb lies 3 kilometre from the east of Cheng Gou village of Mantang hong Town of Zhang Wu County of Fuxin city. A farmer of the village found the top of the windward side of the tomb 0. 5 metre under the surface of the ground when he built a wau in 1982. Fuxin Cultrural Relics Office, Archaeological Team. and Zhang Wu Cultrural Relics office rescued and ercavated.The tomb is a single room tomb which is made of long and square bricks. The tomb is 2. 6 metet long and 2.5 mere wide. There are deceased frescoes around the coffin platform, a skeleon ornamented with copper wire-weaving net was kept very well. The things left behind by the deceased are as follows: glazed bowl 、gilded cop per ornament、jade bird and amber decorative bead.The inferences of the time of the Liao tomb in Cheng Gou is the later period of liao Dynasty. The status of the host of the tomb is common aristocrat according to archaeological materials. and document(Relics Management Institute of Zhangwu County and Museum of Fuxin City ) 1998北方文物1998,,2:4
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