库水位变化对边坡稳定性影响的有限元模拟

在假定坡体孔隙水水位为水平线且不考虑渗透作用影响的基础上，基于强度折减有限元法分析了水位上升及下降速度对边坡稳定性的影响。对比计算表明，在库水位骤降或陡升条件下，相同库水位对应的边坡安全系数基本上均小于库水位缓慢变化情况下的安全系数。故在实际工程中，无论是排水还是蓄水，都应尽量保持水位缓慢变化，以使边坡处于相对较安全的状态。     

南海北部陆缘晚期油气成藏机理及动力学过程

总结了南海北部陆缘晚期(或浅层)油气藏的勘探技术和方法,指出晚期油气成藏具有海底麻坑、气烟囱、"地震模糊带"和"亮点"等地震异常特征,从地化特征上可划分为浅层生物气、成熟—高成熟热解气和高含CO₂热解气等3种油气成藏类型.在研究新构造运动表现形式的基础上,分析了逆断层、正断层和底辟—走滑断层3个断层活动区的晚期油气成藏机理,指出断层晚期活动和后期快速沉降促进了油气的运移和再分配,晚期油气成藏主要沿莺歌海盆地莺东斜坡带、东方—乐东区和沿琼东南盆地二号断裂带及珠江口盆地坳陷边缘斜坡带等分布,有利于油气和天然气水合物的勘探.      

基于WebGIS的防汛信息服务系统的构建

在充分分析防汛信息服务系统功能需求、特点的基础上,提出了基于WebGIS的防汛信息服务系统B/S多层体系结构的设计方案;描述了防汛信息服务系统的网络拓扑结构设计;重点阐述了基于Java自主开发WebGIS平台的方法;借鉴R树及四叉树索引特点,提出了优化系统性能的空间数据组织与检索方法,并将此方法应用在防汛信息服务系统中。最后,对基于GIS的防汛信息服务系统进行了展望。     

MIKEII 软件系统在穆棱河流域面源污染估算中的应用

穆棱河流域面源污染入河量调查和估算采用了MIKEII软件系统，根据水质、水量实测数据，在参数率定和模型验证的基础上．对穆棱河部分河段的水质进行模拟，拟合出面源入河量和年内分布。经验证计算结果较其他方法更合理可靠。     

高含蜡石蜡乳状液的研制及影响因素探讨

以石蜡为主要原料,采用剂在油中法制备了石蜡乳状液.考察了乳化剂类型和用量、乳化水用量、乳化温度、乳化时间、搅拌速度对石蜡乳化效果的影响.结果表明,复配乳化剂优于单一乳化剂,且复配-Ⅱ型乳化剂效果最好.并确定了最佳乳化工艺条件:复配-Ⅱ型乳化剂用量10%,乳化水用量65%～70%,乳化温度90℃,乳化时间30min,搅拌速度1000r/min.在此条件下,石蜡乳状液蜡含量为30%～35%,具有较好的稳定性和分散性.     

氮气氛下LTCC基板Cu共烧金属化研究

从PMMA型LTCC素坯膜的制备和PMMA的排胶机理两方面，研究了LTCC基板Cu共烧金属化。结果表明，采用PMMA作为粘结剂的流延浆料具有剪切变稀行为，所得的流延坯膜微观组织均匀，叠压后坯体内部无分层现象。热失重、差热和傅立叶红外光谱联用分析结果表明高纯N2气氛中PMMA以解聚机理热解，热解后释放的主要产物为丙烯酸甲酯。在高纯N2气氛中LTCC与Cu共烧后Cu金属化膜平整、致密，连通良好。经测试，基板表面Cu导体方阻小于5mΩ/□。     

几种过渡金属化合物对沥青的催化氧化

以铁、钴、锰等过渡佥属的化合物作为催化剂，对沥青催化氧化。根据沥青的延度、针入度和软化点的变化．研究催化剂的种类和催化剂的加入量对沥青氧化的影响。     

KINETICS OF HYDROCARBON GAS GENERATION FROM MARINE KEROGEN AND OIL: IMPLICATIONS FOR THE ORIGIN OF NATURAL GASES IN THE HETIANHE GASFIELD, TARIM BASIN, NW CHINA

In this paper we derive kinetic parameters for the generation of gaseous hydrocarbons (C_1‐5) and methane (C₁) from closed‐system laboratory pyrolysis of selected samples of marine kerogen and oil from the SW Tarim Basin. The activation energy distributions for the generation of both C_1‐5 (Ea = 59‐72kcal, A = 1.0×10¹⁴ s^?1) and C₁ (Ea = 61‐78kcal, A = 6.06×10¹⁴ s^?1) hydrocarbons from the marine oil are narrower than those for the generation of these hydrocarbons from marine kerogen (Ea = 50‐74kcal, A = 1.0×10¹⁴ s^?1 for C_1‐5; and Ea = 48‐72kcal, A=3.9×10¹³ s^?1 for C₁, respectively). Using these kinetic parameters, both the yields and timings of C_1‐5 and C₁ hydrocarbons generated from Cambrian source rocks and from in‐reservoir cracking of oil in Ordovician strata were predicted for selected wells along a north‐south profile in the SW of the basin. Thermodynamic conditions for the cracking of oil and kerogen were modelled within the context of the geological framework. It is suggested that marine kerogen began to crack at temperatures of around 120°C (or 0.8 %Ro) and entered the gas window at 138°C (or 1.05 %Ro); whereas the marine oil began to crack at about 140 °C (or 1.1 %Ro) and entered the gas window at 158 °C (or 1.6%Ro). The main geological controls identified for gas accumulations in the Bachu Arch (Southwest Depression, SW Tarim Basin) include the remaining gas potential following Caledonian uplift; oil trapping and preservation in basal Ordovician strata; the extent of breaching of Ordovician reservoirs; and whether reservoir burial depths are sufficiently deep for oil cracking to have occurred. In the Maigaiti Slope and Southwest Depression, the timing of gas generation was later than that in the Bachu Arch, with much higher yields and generation rates, and hence better prospects for gas exploration. It appears from the gas generation kinetics that the primary source for the gases in the Hetianhe gasfield was the Southwest Depression.     

ASON在当前应用中存在的问题及分析

对ASON在当前应用中可能碰到的几个问题进行了分析，并提出了看法。