超轻油页岩渣陶粒的研制与生产工艺方案设计   总被引：2，自引：1，他引：1  

邓家平  张明华  李泽林  刘冰杰  李巍巍  曹重仪 《吉林大学学报(地球科学版)》2006,36(6):1031-1035

吉林省桦甸市、农安县油页岩资源丰富。以桦甸市示范电厂油页岩渣为主要原料,用新的烧胀试验方法开展了超轻陶粒的研制,采用自制的新试验装置,烧制出的陶粒接近实际陶粒回转窑水平,并可专门烧制小颗粒陶砂,可比现有烧胀试验方法工作效率提高约50倍;并以国产陶粒设备,提出拟建年产20 万m³陶粒工厂工艺方案设计,对窑炉两端的余热利用提出了可行方案。油页岩渣SiO₂,Al₂O₃,R₂O含量适中,特别是含碳非常少,可以人为地调整发泡剂的用量而控制陶粒的密度,使在1 030～1 100℃范围内烧制出300～500 kg/m³级陶粒或陶砂。  相似文献   

基于ArcGIS模型构建器处理1∶5000专题地理信息数据的方法     

张忠斌 《吉林地质》2020,39(1):100-103

在基于ArcGIS模型处理1∶5000专题地理信息数据过程中,数据的批量面擦除、批量数据整合和裁切、数据属性一致性检查、数据格式转换到外业调绘平板是生产过程中遇到的主要问题,为了提高作业效率,利用ArcGIS模型构建器对专题地理数据处理程序进行了研究。本文详细介绍了主要程序的关键技术和在实际应用中取得的较好效果。  相似文献   

The Control of the Spatial and Temporal Differential Evolution of Boundary Faults on Faulted Basins     

Yuhu Liu  Chunhui Cao  Ruilei Li  Jianfeng Zhu  Wen Xu  Lan Huang  Ying Luan 《地球科学进展》2020,35(1):79-87

The boundary faults of faulted basins generally have segmental growth characteristics. Quantitative analysis of fault growth processes and combined models is of great significance for basin formation and evolution and hydrocarbon accumulation. Taking the Fulongquan fault depression in the southern part of the Songliao Basin as an example, using the 3D seismic data and using the fault-displacement length analysis method, the segmental growth and evolution process of the boundary fault is systematically studied, and the control effect of the spatial and temporal differential evolution of boundary faults on faulted basins is analyzed. The study shows that the segmental growth control of the boundary fault of Fulongquan fault depression forms a series of semi-mantle shoals; the sedimentary center of the Shahezi-Yingcheng fault is controlled to migrate from south to north; The slanting and thrusting activities control the height of the anticline trap; the transformation of the boundary fault property controls the evolution of the basin's tectonic pattern from the tandem semi-mantle to the faulted anticline.  相似文献   

Coupling relationship between reservoir diagenesis and hydrocarbon accumulation in Lower Cretaceous Yingcheng Formation of Dongling,Changling fault depression,Songliao Basin,Northeast China     

《China Geology》2020,3(2):247-261

The Lower Cretaceous Yingcheng Formation in the southern Songliao Basin is the typical tight oil sandstone in China. In order to better predict the petrophysical properties of the tight sandstone reservoirs in the Lower Cretaceous Yingcheng Formation, Songliao Basin, Northeast China, the diagenesis and porosity evolution was investigated using a suite of petrographic and geochemical techniques including thin section analysis, scanning electron microscopy, mercury intrusion and fluid inclusion analysis, on a set of selected tight sandstone samples. Combined with the histories of burial evolution, organic matter thermal evolution and hydrocarbon charge, the matching relationship between reservoir porosity evolution and hydrocarbon accumulation history is analyzed. The result showed that the tight sandstone reservoirs characterized of being controlled by deposition, predominated by compaction, improved by dissolution and enhanced by cementation. The hydrocarbon accumulation period was investigated using a suite of hydrocarbon generation and expulsion history, microfluorescence determination and temperature measurement technology. According to the homogenization temperature of the inclusions and the history of burial evolution, Yingcheng Formation has mainly two phases hydrocarbon accumulation. The first phase of oil and gas is charged before the reservoir is tightened, the oil and gas generated by Shahezi source rocks enter the sand body of Yingcheng Formation, influenced by the carrying capability of sand conducting layer, oil and gas is mainly conducted by the better properties and higher connectivity sand body and enriched in the east, which belongs to the type of densification after hydrocarbon accumulation. The second phase of oil and gas charge after densification, which belongs to the type of densification before the hydrocarbon accumulation.  相似文献   

区域农业景观生态风险评价初步构想   总被引：16，自引：0，他引：16  

张学林  王金达  张博  洪梅 《地球科学进展》2000,15(6):712-716

区域农业景观生态风险评价研究是适应当前区域农业可持续发展的需要而产生的。我国区域农业景观类型多种多样,十分复杂。且有农业生态环境恶化、土壤污染加剧、水体污染日趋严重等环境问题,为了解决这些问题,保护环境,保护人类健康,提出了区域农业景观生态风险评价研究的框架和方法以及今后的发展前景。  相似文献   

长岭断陷东岭鼻状构造带沙河子组烃源岩特征及评价     

刘曼丽  高福红  徐文 《世界地质》2016,35(1):184-190

为确定东岭鼻状构造带沙河子组烃源岩的发育程度,本文应用有机地球化学分析方法,对沙河子组的暗色泥岩进行了有机质丰度、类型和成熟度的研究。研究结果显示:有机碳平均含量为2.21%,生烃潜量平均值为9.13 mg/g,氯仿沥青"A"含量0.5%,总烃含量500×10~(-6),说明沙河子组暗色泥岩有机质丰度较高;有机显微组分中惰质组分含量较低,"壳质组+腐泥组"相对含量远远高于镜质组和惰质组。T_(max)为446℃~462℃,结合T_(max)与氢指数和降解指数的关系,指示有机质干酪根类型以II1~I型为主;镜质体反射率(Ro)为0.56%~0.71%,处于低成熟-成熟阶段。综合分析认为沙河子组烃源岩有机质丰度高,有机质类型好,有机质成熟度处于低成熟-成熟阶段,属于中等-好的烃源岩,以生油为主。东岭断鼻构造带沙河子组具有较大的勘探潜力。  相似文献   

梨树断陷苏家屯油田成藏主控因素及富集规律     

曲前中 《世界地质》2016,35(3):785-788

结合梨树断陷苏家屯地区油气藏的空间分布特征,深入研究了烃源岩条件、圈闭条件、输导条件及保存条件等方面对油气成藏的控制作用。研究表明:构造、沉积演化特征控制了优质源、储的空间分布;构造背景结合不同输导条件控制了优势运移方向,同时导致不同构造位置的圈闭的含油气性差异明显;多种差异聚集模式共同作用导致圈闭分段捕获、保存油气,控制了油气平面富集程度。  相似文献   

东北高空湿度变化特征及其与地面气温和降水的关系   总被引：2，自引：0，他引：2  

刘玉英  李宇凡  谢今范  张红 《地理科学》2016,36(4):628-636

利用1971~2005年探空和地面观测资料,详细分析了东北地区高空比湿和相对湿度的时空变化特征,并探讨了比湿和相对湿度与地面气温、降水量的关系。结果表明：东北地区比湿空间分布主要受到水汽来源的影响,地面由东南向西北递减,高空由南向北递减;相对湿度受水汽、海拔高度和纬度的共同影响,地面和对流层下层由南向北先减后增,对流层中层由南向北递增,赤峰向通辽延伸的西南-东北向干舌地面最明显,随高度增加逐渐减弱。1971~2005年,东北地区比湿从地面到高空均为增加趋势,对流层中下层的增加趋势更加显著;相对湿度在地面呈显著减小趋势,对流层中层呈显著增加趋势。大气比湿与地面气温在年、季尺度上存在一致的显著正相关关系,大气相对湿度与地面气温在季节尺度上存在显著负相关关系;对流层中下层相对湿度与降水量相关最显著;地面气温升高对东北气候趋于干旱化起了重要作用,高空相对湿度增加有利于降水增加,气温与比湿的相互消长,影响了气候的干、湿变化。  相似文献   

基于重组降水集合预报的洪水概率预报   总被引：2，自引：2，他引：0       下载免费PDF全文

赵琳娜  刘莹  包红军  王彬雁  白雪梅  李潇濛  杨瑞雯  李依瞳 《应用气象学报》2017,28(5):544-554

采用条件亚正态模型方法,生成了具有包含不同可能性的降水集合预报。为了保持各子流域降水集合预报变量之间的空间相关性,采用集合预报重组方法对降水集合预报进行重新排列。使用重组后的降水集合预报驱动水文模型,实现了淮河上游大坡岭-息县、淮河上游息县-王家坝和汝河-洪河上游3个子流域的12次洪水过程的洪水概率预报,并对1988年9月7日和1991年7月31日两次洪水概率预报进行个例分析。结果表明:相对于单一确定性预报,通过条件亚正态分布模型生成降水集合预报后,再经过Schaake洗牌法空间相关性重新组合的降水集合预报,捕捉洪峰出现时间和流量的能力更强。对洪水概率预报来说,降水概率预报更能达到对未来的水文事件进行最大可能估计的目的,并尽可能综合了降水预报不确定性因素,同时也说明维持变量原有的空间相关特征对于降水概率预报具有重要意义。  相似文献   

Advance in Application of Regional Climate Models in China     

ZHANG Wei YAN Minhua CHEN Panqin XU Helan 《中国地理科学(英文版)》2008,18(1):93-100

Regional climate models have become the powerful tools for simulating regional climate and its change process and have been widely used in China. Using regional climate models, some research results have been obtained on the following aspects： 1） the numerical simulation of East Asian monsoon climate, including exceptional monsoon precipitation, summer precipitation distribution, East Asian circulation, multi-year climate average condition, summer rain belt and so on; 2） the simulation of arid climate of the western China, including thermal effect of the Qinghal-Tibet Plateau, the plateau precipitation in the Qilian Mountains; and the impacts of greenhouse effects （CO2 doubling） upon climate in the western China; and 3） the simulation of the climate effect of underlying surface changes, including the effect of soil on climate formation, the influence of terrain on precipitation, the effect of regional soil degradation on regional climate, the effect of various underlying surfaces on regional climate, the effect of land-sea contrast on the climate formulation, the influence of snow cover over the plateau regions on the regional climate, the effect of vegetation changes on the regional climate, etc. In the process of application of regional climate models, the preferences of the models are improved so that better simulation results are gotten. At last, some suggestions are made about the application of regional climate models in regional climate research in the future.  相似文献