A New Method base on Water Drive Curve for Determining the Reasonable Injection-Production Ratio for High Water-Cut Oilfield

<正>The Injection-production Ratio plays a very important role in the high water cut stage in oilfield development.If the Injection-production Ratio is unreasonable,this will result in serials problems,such as sever water breakthrough in high permeable layers,decrease on the water injection effectiveness and water sweep efficiency,serious depletion     

Effects of tropical cyclones on large-scale circulation and ocean heat transport in the South China Sea

In this study, we investigate the influence of tropical cyclones (TCs) on large-scale circulation and ocean heat transport in the South China Sea (SCS) by using an ocean general circulation model at a 1/8° resolution during 2000–2008. The model uses a data assimilation system to assimilate observations in order to improve the representation of SCS circulation. The results reveal an unexpected deep SCS circulation anomaly induced by TCs, which suggests that effects of TC can penetrate deeper into the ocean. This deep effect may result from the near inertial oscillations excited by TCs. The inertial oscillations can propagate downward to the oceanic interior. The analyses confirm that TCs have two effects on ocean heat transport of the SCS. Firstly, the wind stress curl induced by TCs affects the structure of SCS circulation, and then changes heat transport. Secondly, TCs pump surface heat downward to the thermocline, increasing the heat injection from the atmosphere to the ocean. Two effects together amplify the outflow of the surface heat southward away the SCS through the Mindoro and Karimata Straits. The TC-induced heat transports through the Mindoro, Balabac and Karimata Straits account for 20 % of the total heat transport through three straits. An implication of this study is that ocean models need to simulate the TC effect on heat transport in order to correctly evaluate the role of the SCS through flow in regulating upper ocean circulation and climate in the Indonesian maritime continent and its adjacent regions.     

Responses of foraminiferal isotopic variations at ODP Site 1143 in the southern South China Sea to orbital forcing

The foraminiferal δ ¹⁸O and δ ¹³C records for the past 5 Ma at ODP Site 1143 reveal the linear responses of the Plio-Pleistocene climatic changes in the southern South China Sea to orbital forcing at the obliquity and precession bands. The phase of the δ ¹⁸O variations with the orbital forcing is opposite to that of the δ ¹³C, which may be caused by the frequent El Niño events from the equatorial Pacific. The amplification of the Northern Hemisphere Ice Sheet at ñ3.3 Ma probably affected the development of the 100-ka climatic cycles. Its further spreading may spur the 100-ka climatic cycle to become the dominant cycle in the late Pleistocene. The “Mid- Pleistocene Transition” event has localized influence on the isotopic variations in the southern South China Sea. The foraminiferal δ ¹³C records for the past 5 Ma at Site 1143 are highly coherent with the orbital forcing at the long eccentricity band, and lead the δ ¹⁸O records at the shorter eccentricity band, highlighting the importance of the carbon cycle in the global climate change.     

Ecological adaptation strategies of annual plants in artificial vegetation-stabilized sand dune in Shapotou Region

Taking annual plant Eragrostis poaeides in the artificial vegetation-stabilized sand dune in the Shapotou Experimental Research Station as example, study has been done on the adaptation strategies of annual plants to random environment through fixed quadrat observations of population changes and fixed plant determinations of individual growth, seed germination, population dynamics, spatial distribution pattern of population, competition and regulation. During the growing season, the survival rate of annual plants depends on the precipitation intensity and precipitation duration which activate the germination of seeds. The optimal germination strategy of annual plants in this habitat during the growing season appears as continuous germination under suitable conditions. Such continuous germination is an adaptive characteristic of annual plants to random environment. In addition, the variation processes of population size and regulation mechanism of E. poaeoides are studied. Statistical results of natural population in four consecutive years show that water condition in the habitat is the leading factor affecting the population dynamics of E. poaeoides. During the establishment period E. poaeoides had a higher death rate, but in the middle to later period they could survive stably. Due to the limitation of soil moisture, the competition among individuals for water inevitably led to self-thinning phenomena. Under very arid condition, the survival curve of annual herbs entirely appears as Deevey III type (C type), but under relatively adequate precipitation condition, the survival curve appears as intermediate type. The strategy of life history obviously appears as r-strategy. Plant species of r-strategy often occurs in the early succession stage of the communities. In the relatively adequate and evenly-distributed rainfall years, E. poaeoides population exhibited a density-dependent, i. e., survival rate increased with decrease in population density. The main pattern to regulate the population number for the intraspecific competition is to regulate the highly variable initial density into a final density with narrow variation range.     

“8.19”西北东部大到暴雨诊断分析和数值模拟

利用MICAPS系统T213资料、NCEP再分析资料及实况观测资料，对2004年8月19日发生在西北地区东部的暴雨天气过程的大尺度环流背景和物理量场进行分析发现：这次暴雨天气过程中西太平洋副热带高压有一次明显的西伸，是一次较典型的副高西北侧西南气流型暴雨。降水水汽主要来自南海和孟加拉湾，中低层的水汽输送十分充沛，并在甘肃河东和宁夏形成辐合。运用三重嵌套的中尺度数值预报模式MM5，对这次暴雨过程进行了两种方案的高分辨率数值模拟，结果表明，运用四维资料同化后的方案在形势和降水预报方面优于未进行资料同化的方案。     

Chemostratigraphy and lithological characters of Neoproterozoic cap carbonates from the Kuruktag Mountain, Xinjiang, western China

The Neoproterozoic Era includes some of the most largest ice ages in the geological history. The exact number of glaciations is unknown, though there were at least two events of global glaciation. Neoproterozoic glacial deposits in the Kuruktag Mountain, Xinjiang, western China have proven that there had occurred three discrete Neoproterozoic glaciations. Diamictite units occurred in the Bayisi, Tereeken, and Hankalchough formations, carbonate units were recognized among the diamictites and immediately overlied the Bayisi, Tereeken and Hankalchough diamictites. Carbonates at the top of the Bayisi Formation are characterized by the dolo-sility stones with negative δ13C values ranging from -4.10‰ to -8.17‰ (PDB), comparable to the Sturtian cap carbonates that overlie the Sturtian glacial deposits from other Neoproterozoic sequences. Carbonates overlying the Tereeken Formation are characterized by the pinkish cap dolostones (ca. 10 m thick) with negative δ13C values ranging from -2.58‰ to -4.77‰ (PDB), comparable to the Marinoan cap carbonates. The cap is also characterized by tepee-like structures, barite precipitates and pseudomorphous aragonite crystal fan limestones. Carbonates at the top of the Hankalchough Formation are characterized by subaerial exposure crust (vadose pisolite structure, calcareous crust structure) dolostones with negative δ13C values ranging from -4.56‰ to -11.45‰ (PDB) and the calcareous crust dolostones, implying that the Hankalchough cap carbonates differ from either the Sturtian or Marinoan cap carbonates in sedimentary environment and carbon isotopic composition. In addition, it is suggested the Hankalchough glaciation belongs to a terrestrial glaciation and it is the third largest glaciation during the Neoproterozoic period on the Tarim platform.     

Oxygen isotope stratigraphy and events in the northern South China Sea during the last 6 million years

Based on the stable isotopic analysis of more than 1000 samples of planktonic and benthic foraminifers from ODP Site 1148 in the northern South China Sea (SCS), the oxygen isotope stratigraphy has been applied to the last 3 million years for the first time in the SCS. Furthermore, the paleoceanographic changes in the northern SCS during the last 6 million years have been unraveled. The benthic foraminiferal δ¹⁸O record shows that before δ3.1 Ma the SCS was much more influenced by the warm intermediate water of the Pacific. The remarkable decrease in the deepwater temperature of the SCS during the period of 3.1-2.5 Ma demonstrates the formation of the Northern Hemisphere ice-sheet. However, the several sea surface temperature (SST) reductions during the early and middle Pliocene, reflected by the planktonic foraminiferal δ¹⁸O, might be related to the ice-sheet growth in the Antarctic region. Only those stepwise and irreversible SST reductions during the period of δ2.2-0.9 Ma could be related to the formation and growth of the Northern Hemisphere ice-sheet.     

新型城镇化与非正规就业：规模、格局及社会融合

中国城镇化由偏重数量转向更加注重质量的新型城镇化,促进农村转移人口市民化、提高就业质量成为城镇化发展的重要目标,疫情影响下非正规就业问题更为突出。论文从新型城镇化与非正规就业的关系出发阐释非正规就业人口的历史产生和发展要求,基于人口普查和《中国劳动力动态调查》测度了中国城镇非正规就业的规模和格局特征,总结了非正规就业者当前面临的社会融合难题,并提出发展思路和路径。结果发现：① 城镇化与非正规就业之间关系密切,非正规就业为城镇化过程中农村转移人口提供大量就业机会,缓解了城镇就业压力。以人为本的新型城镇化需要关注非正规就业模式,以促进农业转移人口市民化和社会融合。② 经多源数据估算,中国城镇非正规就业占城镇总就业的33.2%~44.7%,就业人数达1.38亿~1.55亿,以隐性就业部分为主。在空间分布上总体呈现东、中、西逐渐减少的特征;在雇佣类型上以从事各类非正规工作的被雇型就业为主;行业结构主要集中在批发和零售贸易及餐饮业,居民服务、修理和其他服务业与制造业等。③ 非正规就业者主要面临职业困境、户籍限制、公共服务差距、风险应对能力弱等问题,需要通过完善就业服务体系等改革,提升就业质量,推动市民化和社会融合。     

长三角城市群城镇化与生态环境质量优化研究

以2003—2016年的长三角城市群26个城市为研究对象,分析长三角城镇化和生态环境的时空变化特征,运用STIRPAT模型探讨城镇化对生态环境影响。结果表明:① 2003—2016年,长三角城镇化与生态环境质量均有提升,且城镇化水平的地区差异大于生态环境质量。长三角形成以上海、南京和杭州为中心的城镇化水平高值集聚,生态环境质量整体提升明显且空间差异小。② 长三角城镇化明显改善本城市生态环境质量,对相邻城市的生态环境质量有一定的负面影响。对本城市而言,多维的城镇化从人口、经济、土地、社会层面疏解生态环境压力,加强生态环境治理,优化提升生态环境质量。以人口集聚和结构优化为特征的人口城镇化,促进消耗集中、排放集中,提升了资源使用效率和污染治理效率。以产业集聚和经济发展为特征的经济城镇化,通过产业集中布局和创造经济效益,在资源配置和污染治理上发挥集聚效应,并为生态环境改善提供资金支持。对相邻城市而言,城市的城镇化“虹吸效应”大于“扩散效应”,城市的产业转型和环境规制会使污染向相邻城市转移,从而对相邻城市生态环境质量有一定的负面影响。