迟缓爱德华氏菌基因组fosmid文库的构建、opp基因簇的克隆及aroA基因缺失突变株的构建

本研究构建了迟缓爱德华氏菌(Edwardsiella tarda)LSE40 基因组fosmid文库，该文库共包含2 500个克隆，插入片段平均大小为33.6kb���文库总容量约84Mb���覆盖E.tarda LSE40基因组（按5Mb���算）超过16倍。随机挑取1 000个fosmid克隆进行双末端测序共得到1 741条高质量的序列，序列平均长度546 bp，全长949 997bp，约为E.tarda基因组的19％。将这些序列提交到KEGG自动注释服务器KAAS对所得序列进行代谢途径分析，得到E.tarda LSE40的KO (KEGG Orthology) 注释。分析结果表明，与代谢途径相关的基因有932条序列，与环境信息处理相关基因283条，与遗传信息处理相关基因220条，与细胞进程和人类疾病相关的基因分别为64条和16条。同时将序列进行BlastX，按照微生物致病性共同主题找到61个毒力相关基因。Fosmid文库的建立和部分基因组序列的生物信息学分析为进一步研究E.tarda LSE40的致病机制、代谢机制和生理生态机制提供了丰富的物质基础。 通过比较基因组的方法，从E.tarda LSE40 fosmid文库克隆到编码寡肽透过酶的opp基因簇，该基因簇全长6 741bp，含有5个ORF，依次编码OppA-B-C-D-F 5个蛋白；位于oppA和oppB���间隔区和oppF之后的非编码区各有一个茎环结构，推测分别为oppA和opp基因簇的转录终止子。以细菌OppA的保守结构域SBP_bac_5构建系统发生树，结果显示E.tarda LSE40与同属细菌E.ictaluri的亲缘关系最近，与肠杆菌科细菌的亲缘关系较近，与革兰氏阳性细菌的亲缘关系较远，表明OppA的SBP_bac_5结构域可作为细菌分类鉴定的依据。 从E.tarda LSE40 fosmid文库克隆aroA基因全序列，该序列全长1 287bp，编码428个氨基酸，与鲶鱼爱德华氏菌(E. ictaluri)氨基酸相似性在94%，与其他肠杆菌科菌如Escherichia coli和Yersinia enterocolitica相似性在73%-74%。通过In-frame deletion构建了E.tarda LSE40 aroA缺失突变株。与野生型相比，aroA突变株的半数致死量LD50提高了62倍。在牙鲆接种~106cfu/ml的E.tarda细菌时，接种野生型细菌的牙鲆在6天内全部死亡，濒死鱼的细菌数达7.97×108cfu/ 100mg；而接种aroA突变株的牙鲆没有出现死亡，28天后检测不到细菌的存在。实验结果为进一步评价aroA突变株作为减毒活疫苗打下了基础。

模拟增温对短穗兔耳草生长特征的影响

[目的]探讨短穗兔耳草个体对模拟增温的响应。[方法]采用国际冻原计划（ITEX）模拟增温对植物影响的研究方法,将温棚从小到大的顺序依次设为A、B���C、D、E5个温度梯度,分析不同温度梯度下短穗兔耳草个体生长特征的变化,研究模拟增温对短穗兔耳草生长特征的影响。[结果]随着温棚直径的减小,温度（地表温度和土壤温长）逐渐升高。与对照相比,A、B���C、D、E5个处理分别提高了2.68、1.57、1.20、1.07和0.69℃（地表气温）,1.74、1.06、0.80、0.60和0.30℃（土壤温度）。短穗兔耳草从对照至A温室随着温度的升高,叶片数、叶片高度逐渐增加,而匍匐茎逐渐减少。[结论]叶片数变化与温度（地表温度和地温）呈正相关关系,增温促进了短穗兔耳草的营养生长,抑制了它的克隆繁殖能力。

青海果洛黄河源区高寒草甸CO_2释放速率研究

以青海果洛黄河源区高寒退化草甸生态系统为对象,应用静态密闭箱-气相色谱法对高寒退化草甸生态系统CO_2释放进行了初步研究.结果表明:所选4种不同退化程度高寒草甸,即未退化草甸(A)、轻度退化草甸(B)、中度退化草甸(C)和重度退化草甸(D),其CO_2释放速率有明显的日变化特征,日最大排放速率在15:00-17:00左右出现,最低值出现于清晨7:00-9:00左右,释放白天大于夜晚;(2)CO_2释放速率具有明显的季节性变化特征,生长期CO_2释放速率明显高于枯黄期,8月为CO_2释放高峰期,1月或2月为CO_2释放低谷期;(3)CO_2释放速率的日变化主要受地表温度和5cm地温制约,季节动态与5cm地温呈显著正相关关系(P＜0.01),本研究为进一步进行高寒退化草甸生态系统源江效应的准确估测提供科学依据.

模拟增温效应对黑褐苔草（Carex alrofusca）生长特征的影响

在典型矮蒿草草甸上,按大小梯度设置温棚（由小到大依次为A、B���C、D、E）进行模拟增温效应对黑褐苔草（Carex alrofusca）的分蘖数、叶片数和高度影响的研究.结果表明：温度（地表温度和地温）随温室的减小而升高,其中,温室A内地表温度和地温最高,比对照分别提高了2.35℃和2.13℃.温室D的分蘖数增幅最大,温室D与温室A间分蘖数变异达到显著水平（P〈0.05）,温室A至D中黑褐苔草的分蘖数变异随温度的升高而降低,并与温度呈负相关关系（P地表〈0.05;P地温〈0.01）;叶片数的变化趋势与分蘖数基本一致;黑褐苔草平均高度随温度的增加而升高,温室A与对照间达到极显著水平（P〈0.01）,各处理黑褐苔草高度与温度呈正相关且达到极显著水平（P〈0.01）.

大鼠血浆中痕量氨基酸的柱前衍生-高效液相色谱串联质谱测定

以1,2-苯并-3,4-二氢咔唑-9-乙基氯甲酸酯(BCEOC)作为柱前荧光衍生试剂,在Hypersil BDS C18 (4.6 ×200 mm, 5 μm)反相色谱柱上,荧光检测波长为390 nm(激发波长为333 nm),采用梯度洗脱实现了20种氨基酸标准品衍生物的分离检测.20种组分的线性范围为51.6 fmol～105.6 pmol,线性回归系数均大于0.9995;检出限为6.3～177.6 fmol (S/N=3:1).经柱后串联质谱电喷雾电离源(ESI Source)实现了各组分的质谱鉴定,并以酪氨酸(Tyr)衍生物为例进行了质谱裂解机理解析.对A、B���C三组(A:安静对照组;B:运动力竭即刻组;C:力竭恢复12 h 组) 24只大鼠血浆中氨基酸的定量测定结果表明,运动力竭即刻较安静状态大鼠血浆氨基酸含量明显增加;力竭恢复12 h 后血浆氨基酸水平基本恢复到运动前状态.方法的灵敏度高、重现性好,为大鼠血浆中氨基酸的测定提供了一种新方法

青海油菜蜂花粉酶解破壁前后营养成分的比较

对青海油菜蜂花粉及生物酶解破壁花粉的营养成分进行了分析和比较。结果表明，花粉经酶解破壁后，粗蛋白、粗脂肪、还原糖、核酸、总黄酮、灰份、多数氨基酸、维生素（A、B���C和K）及黄酮类化合物（原青花素、芦丁、槲皮素、异鼠李索）的含量得到了明显提高，而K、Na、Ca、Mg、Fe、Zn、Cu、Cr、Cd、Ni、Mn等矿质元素的含量无明显变化。青海油菜花粉经破壁后更有利于营养成分和活性成分的释放。

模拟增温效应对矮嵩草生长特征的影响

基于国际冻原计划(ITEX)模拟增温效应对植物影响的研究方法,将温棚按从小到大的顺序设为A、B���C、D、E 5个梯度水平,研究了矮嵩草(Kobresia humilis)植株的分蘖数、叶片数、高度、生物量以及重要值对温度升高的响应.结果表明:温度(地表温度和地温)随温棚的减小而升高,最高的A温棚内地表温度和地温分别比对照提高2.35℃和2.13℃;分蘖数在E温棚中增加最多,且分别与B���A温棚间差异分别达到显著水平和极显著水平,A～E温棚间分蘖数的变化与棚内温度呈负相关,且与地温呈显著相关;叶片数的变化趋势与分蘖数一致, A～E温棚间叶片数与温度呈极显著负相关;叶片高度随温度的增加而升高,A温棚极显著高于E温棚和对照,处理间叶片高度变化与温度呈极显著正相关;生物量、重要值与温度呈显著负相关.

高寒牧区三种豆科牧草与燕麦混播的试验研究

在中国科学院海北高寒草甸生态系统开放实验站进行的燕麦与箭舌豌豆、红豆草、毛苕子3 种豆科牧草混播栽培的试验研究, 采用正交设计及极差分析方法对混播组合作择优评判。结果表明: 红豆草在年均温-1. 7 ℃, ≥5 ℃积温1 000 ℃, 海拔3 200 m 的高寒地区可与燕麦建立一年生混播割草地。其产量水平高于毛苕子与燕麦混播的草地而与箭舌豌豆与燕麦混播的草地相当。对豆科牧草种(A )、混作方式(B)、混播总密度(C) 和混播比例(D) 4 个因素进行择优组合可提高单位面积牧草产量。4 种试验因素对混播草地牧草产量的效应大小依次为C> A > D> B���本试验最优组合为5 号组合(A 2B2C3D1)。

论世界芨芨草属（禾本科）的地理分布

本文详细讨论了世界芨芨草属的地理分布等问题。1.全世界芨芨草属共有23种1变种,分为5个组。本文对它们进行了系统介绍。2.属的地理分布,最北为北纬62°(羽茅、毛颖芨芨草),最南为北纬26°(林阴芨芨草)。就海拔而论,分布最低的海拔记录为120m(雀麦芨芨草),分布最高的海拔记录为4600m(干生芨芨草和藏芨芨草)。3.本文讨论了芨芨草属5个组(芨芨草组,钝基草组,直芒草组,新芨芨草组,拟芨芨草组)的系统位置，和每个组包括的种类及5个组的分布格局。4.根据塔赫他间世界植物区系区划，统计了每个区的种数，明显看出伊朗-土兰种类（18/24）是第一位，东亚区（14/24）居第二位。中国有17种，横断山脉地区、华北地区和唐古特地区种数最丰富（10种和9种）。5.研究结果表明：（A）从种的分布格局分析可见，横断山脉地区北部、唐古特地区东部和华北地区西部的交汇地是芨芨草属分布中心。（B���根据芨芨草属形态特征演化趋势分析和地史学资料推断横断山脉地区北部是芨芨草属的起源地。（C）有三条路线向外散布：a)从横断山脉地区向西沿喜马拉雅山脉，经克什米尔地区抵达地中海和中欧；b)从横断山脉向西北经祁连山、天山、塔里木盆地西侧山地，抵吉尔吉斯斯坦伊塞克湖；c)由横断山脉向东北经甘肃、宁夏、陕西、山西、河北和东北，抵达西伯利亚，东达勘察加半岛，西至鄂毕河上游，并经白令海峡陆桥分布到美国内华达山脉和落基山山脉。（D）该属植物集中分布于北半球半湿润、半干旱和干旱地区，以及极端干旱的荒漠区山地。植物的形成、发展和生态适应与气候相联系，并经过长期的适应和进化，塑造了一系列中生、旱中生的形态-生态特征和生活型。

Mitochondrial and chloroplast phylogeography of Picea crassifolia Kom. (Pinaceae) in the Qinghai-Tibetan Plateau and adjacent highlands

The disjunct distribution of forests in the Qinghai-Tibetan Plateau (QTP) and adjacent Helan Shan and Daqing Shan highlands provides an excellent model to examine vegetation shifts, glacial refugia and gene flow of key species in this complex landscape region in response to past climatic oscillations and human disturbance. In this study, we examined maternally inherited mitochondrial DNA (nad1 intron b/c and nad5 intron 1) and paternally inherited chloroplast DNA (trnC-trnD) sequence variation within a dominant forest species, Picea crassifolia Kom. We recovered nine mitotypes and two chlorotypes in a survey of 442 individuals from 32 populations sampled throughout the species' range. Significant mitochondrial DNA population subdivision was detected (G(ST) = 0.512; N-ST = 0.679), suggesting low levels of recurrent gene flow through seeds among populations and significant phylogeographical structure (N-ST > GST, P < 0.05). Plateau haplotypes differed in sequence from those in the adjacent highlands, suggesting a long period of allopatric fragmentation between the species in the two regions and the presence of independent refugia in each region during Quaternary glaciations. On the QTP platform, all but one of the disjunct populations surveyed were fixed for the same mitotype, while most populations at the plateau edge contained more than one haplotype with the mitotype that was fixed in plateau platform populations always present at high frequency. This distribution pattern suggests that present-day disjunct populations on the QTP platform experienced a common recolonization history. The same phylogeographical pattern, however, was not detected for paternally inherited chloroplast DNA haplotypes. Two chlorotypes were distributed throughout the range of the species with little geographical population differentiation (G(ST) = N-ST = 0.093). This provides evidence for highly efficient pollen-mediated gene flow among isolated forest patches, both within and between the QTP and adjacent highland populations. A lack of isolation to pollen-mediated gene flow between forests on the QTP and adjacent highlands is surprising given that the Tengger Desert has been a geographical barrier between these two regions for approximately the last 1.8 million years.

Effect of annual weeds on the growth of perennial grass mixtures in the alpine region of the Qinghai-Tibetan Plateau

In the alpine region of the Tibetan Plateau, five perennial grass cultivars, Bromus inermis (B), Elymus nutans (E), Clinelymus nutans (C), Agropyron cristatum (A), and Poa crymophila (P) were combined into nine communities with different compositions and ratios, B+C, E+A, B+E+A, E+B+C,C+E+A,B+E+C+A,B+C+A+P,B+E+A+P and E+C+A+P. Each combination was sown in six 10 X 10 m plots with three hand-weeded plots and three natural-growing plots in a completely randomised design in 1998. A field experiment studied the performance of these perennial grass combinations under the competitive interference of annual weeds in 3 consecutive years from 1998 to 2000. The results showed that annual weeds occupied more space and suppressed the growth of the grasses due to earlier germination and quicker growth in the establishment year, but this pattern changed in the second and third years. Leaf area indexes (LAIs) of grasses were greatly decreased by the competitive interference of weeds, and the negative effect of weeds on LAIs of grasses declined and stabilised in the second and third years. E+B+C, B+E+C+A, and B+E+A+P possessed relatively higher LAIs (P < 0.05) among all grass combinations and their LAIs were close to five when the competitive interference of weeds was removed. Grasses were competitively inferior to weeds in the establishment year, although their competitive ability (aggressivities) increased throughout the growing season. In the second and third years, grasses were competitively superior to weeds, and their competitive ability decreased from May until August and increased in September. Dry matter (DM) yields of grasses were reduced by 29.8-74.1% in the establishment year, 11.0-64.9% in the second year, and 16.0-55.8% in the third year by the competitive interference of weeds. B+E+C+A and B+E+A+P can produce around 14 t/ha of DM yields, significantly higher (P < 0.05) than the production of the other grass combinations in the second and third years after the competitive interference of weeds was removed. It was preliminarily concluded that removal of competitive interference of weeds increased the LAIs of all grass swards and improved the light interception of grasses, thus promoting the production of perennial grass pastures. The germination stage of the grasses in the establishment year was the critical period for weeding and suppression of weeds should occur at an early stage of plant growth. The grass combinations of B+E+C+A and B+E+A+P were productive and can be extensively established in the alpine regions of the Tibetan Plateau. Two or three growing seasons will be needed before determining success of establishment of grass mixtures under the alpine conditions of the Tibetan Plateau.

CIMS中车间控制器软件开发

“CIMS中车间控制器软件开发”来源于国家863高技术计划，它是“CIMS系统技术集成开发环境”的一个重要组成部分，也是柔性制造系统多级管理和控制”的主要部分之一，作者完成了车间控制器的一项十分重要而又非常复杂的工作－制定短期生产计划（包括车间级任务的时间分解和空间分见（单元重构））。1. 根据时间分解要求，针对具有异步特征的车间级任务，本文提出一种有效的启发式方式－TD法。通过TD法，可望将整个计划期内具有异步特征的总任务分解成为多个时间段内呈同步特征的子任务。2. 根据空间分解要求和CIMS特点，针对具有同步特征的子任务，本文提出“成组－平衡－再成组”思想及相应的方法－G-B-C法。通过G-B-C法，可以综合解决负荷平衡问题和机器／工作成组问题，从而，为虚拟单元控制器的实现开辟了一条道路。3. 软件开发文中所提方法均已在PC机上用C语言实现，实验证明，本文所提思想和方法是可行的，有效的。

胜坨油田注聚后油藏动态模型及剩余油分布

The topic of Dynamic reservoir model and the distribution of remaining oil after polymer injection of Shengtuo oilfield is a front problem of "the 11th Five-Year Plan" scientific and technological disciplines of Sinopec Corporation. Reservoirs in study area is distributary channel sandstone. After 34 years of water-injection exploitation and 7 years of polymer injection pilot experiments, a highly complex heterogeneous dynamic evolution has been occurred in macro and micro parameters of reservoir model, together with its flow field. Therefore, it’s essential to construct completed reservoir dynamic model for a successfully prediction of the distribution of remaining oil. With a comprehensive application of multidisciplinary theory and technique, using a variety of data and information to maximize the use of computer technology, combining a static and dynamic, macro and micro and 1~4D integration, the research reveals main features, evolution and mechanism, types of geological disasters and their destructivity of reservoir flow field, the macro field, the micro field, the flow field and reservoir development hydrodynamic geological function in different development periods after a long term of polymer injection in Es2 in Shengtuo oilfield. The principle innovation achievements obtained are: 1. Established A, B, C, D four flow units in target formations, revealed the various features and distribution of flow units. 2. Stated environmental pollution and geological disasters induced during oilfield exploitation in study area, and also explained their formation mechanism, controlling factors, destructivity and approaches to disaster reduction. 3. Established dynamic evolution of the macro parameter model, micro-matrix field, pore network field, clay minerals field, seepage dynamic evolution model of six different exploitation stages in study area, also revealed reservoir flow evolution, the law of evolution mechanism after polymer injection. 4. Established macro and micro distribution model of remaining oil after three mining polymer injection during different water cut periods in study area, revealed the formation mechanism and distribution of remaining oil. 5. Established remaining oilforecasting model in study area, and forecasted the formation and distribution of remaining oil in the following six years. 6. It is proposed that reservoir fluid dynamic geological processes are major driving forces for the evolution of different water cut periods, reservoir macro field after the polymer injection and micro seepage field. 7. Established a dynamic reservoir model, proposed matching theory, methods and technology for the description of the remaining oil characterization and prediction, which can deepen the theory and techniques of continental rift basin development geology. Key words: Polymer reservoir; Geological disasters; Dynamic model; Residual oil forecast

通过第一性原理计算研究内地核的结构与成分

The determination of the composition and structure of the Earth’s inner core has long been the major subject in the study of the Earth’s deep interior. It’s widely believed that the Earth’s core is formed by iron with a fraction of nickel. However, light elements must exist in the inner core because the earth core is less dense than pure iron-nickel alloy (~2-3% in the solid inner core and ~6-7% in the liquid outer core). The questions are what and how much light element is there in the iron-nickel alloy. Besides the composition, the crystal structure of the iron with or without light element is also not well known. According to the seismological observations, the sound waves propagate 3-4% faster along the spin axis than in the equatorial plane. That means the inner core is anisotropic. The densest structure of iron-nickel alloy should be h.c.p structure under the very high pressures. However, the h,c,p structure does not propagate waves anisotropic ally. Then what is the structure of the iron-nickel alloy or the iron-nickle-light element alloy. In this study, we tried to predict the composition and the structure of the inner core through ab initio calculation of the Gibbs free energy, which is a function of internal energy, density and entropy. We conclude that the h.c.p structure is more stable than the b.c.c structure under high pressure and 0 K, but with the increase of temperature, the free energy of the b.c.c structure is decreasing much faster than the h.c.p structure caused by the vibration of the atomics, so the b.c.c structure is more stable at high temperatures. With the addition of light elements (S or Si or both), the free energy of b.c.c. decreases even faster, about 3at% of Si not only explains why the inner core is about 2-3 % lighter than the iron-nickle alloy, but also reasons why the inner core is anisotropic, since the b.c.c. structure becomes more stable than the h.c.p structure at 5500-6000K and b.c.c. is anisotropic in propagating seismic waves. Therefore, we infer that the inner core of the earth is formed by b.c.c iron and a fraction of nickel plus ~3at.% Si, with a temperature higher than 5500K, which is consistent with the studies from other approaches.

济阳-昌潍坳陷火成岩油气藏体系形成机理和分布规律研究

Jiyang & Changwei depressions are two neighboring depressions in Bahai Bay Basin, the famous oil rich basin in East China. The exploration activities in the past 40 years has proved that, within the basins, there exists not only plentiful sandstone hydrocarbon reservoirs (conventional), but also abundant special reservoirs as igneous rock, mudstone and conglomerate ones which have been knowing as the unconventional in the past, and with the prospecting activity is getting more and more detailed, the unconventional reservoirs are also getting more and more important for further resources, among which, the igneous lithological reservoir be of significance as a new research and exploration area. The purpose of this paper is, with the historical researches and data as base, the System Theory, Practice Theory and Modern Comprehensive Petroleum Geology Theory as guide, the theoretical and practice break through as the goal, and the existing problems in the past as the break through direction, to explore and establish a valid reservoir formation and distribution models for igneous strata in the profile of the eastern faulted basins. After investigating the distribution of the igneous rocks and review the history of the igneous rocks reservoirs in basins, the author focused on the following issues and correspondingly the following progresses have been made: 1.Come to a new basin evolution and structure model named "Combined-Basin-bodies Model" for Jiyang even Eastern faulted basins based on the study on the origin and evolution of Jiyang & Changwei basins, depending on this model, every faulted basin in the Bo-hai Bay Basin is consisted of three Basin-Bodies including the Lower (Mesozoic), Middle (Early Tertiary) and the Upper (Late Tertiary) Bodies, each evolved in different geo-stress setting and with different basin trend, shape and igneous-sedimentary buildings system, and from this one to next one, the basin experienced a kind of process named "shape changing" and "Style changing". 2. Supposed a serious of new realizations as follows (1) There were "multi-level magma sources" including Upper mantel and the Lower, Middle and even the Upper Shell magma Chambers in the historical Magma Processes in the basins; (2) There were "multi-magma accessing or pass" from the first level (Mantel faults) to the second, third and fourth levels (that is the different levels of fault in the basin sediment strata) worked in the geo-historical and magma processes; (3) Three tectonic magma cycles and more periods have been recognized those are matched with the "Basin -body-Model" and (4)The geo-historical magma processes were non-homogeneous in time and space scale and so the magma rocks distributed in "zones" or "belts". 3. The study of magma process's effect on basin petroleum conditions have been made and the following new conclusions were reached: (1) the eruptive rocks were tend to be matched with the "caped source rock", and the magma process were favorable to the maturing of the source rocks. (2) The magma process were fruitful to the accumulation of the non-hydrocarbon reservoirs however a over magma process may damage the grade of resource rock; (3) Eruptive activity provided a fruitful environment for the formation of such new reservoir rocks as "co-eruptive turbidity sandstones" and "thermal water carbonate rocks" and the intrusive process can lead to the origin of "metamorphism rock reservoir"; (4) even if the intrusive process may cause the cap rock broken, the late Tertiary intrusive rocks may indeed provide the lateral seal and act as the cap rock locally even regionally. All above progresses are valuable for reconstructing the magma-sedimentary process history and enriching the theory system of modem petroleum geology. 4. A systematic classification system has been provided and the dominating factors for the origin and distribution of igneous rock reservoirs have been worked out based on the systematic case studies, which are as follows: (1) The classification is given based on multi-factors as the origin type, litho-phase, type of reservoir pore, reservoir ability etc., (2) Each type of reservoir was characterized in a detailed way; (3) There are 7 factors dominated the intrusive reservoir's characteristics including depth of intrusion, litho-facies of surrounding rocks, thickness of intrusive rock, intrusive facies, frequency and size of the working faults, shape and tectonic deformation of rock, erosion strength of the rock and the time of the intrusion ect., in the contrast, 4 factors are for eruptive rocks as volcanic facies, frequency and size of the working faults, strength of erosion and the thermal water processing. 5. Several new concept including "reservoir litho-facies", "composite-volcanic facies" and "reservoir system" ect. Were suggested, based on which the following models were established: (1) A seven reservoir belts model for a intrusive unit profile and further more, (2) a three layers cubic model consisted of three layer as "metamorphic roe layer", "marginal layer" and "the core"; (3) A five zones vertical reservoir sequence model consisted of five litho-facies named A, B, C, D and E for a original lava unit and furthermore three models respectively for a erosion, subsidence and faulted lava unit; (4) A composite volcanic face model for a lava cone or a composite cone that is consisted of three facies as "crater and nearby face", "middle slope" and "far slope", among which, the middle slope face is the most potential reservoir area and producible for oil & gas. 6. The concept of "igneous reservoir" was redefined as the igneous, and then a new concept of "igneous reservoir system" was supposed which means the reservoir system consisted of igneous and associated non-igneous reservoirs, with non-hydrocarbon reservoir included. 7. The origin and distribution of igneous reservoir system were probed and generalized for the exploration applications, and origin models of the main reservoir sub-systems have been established including those of igneous, related non-igneous and non-hydrocarbon. For intrusive rocks, two reservoir formation models have been suggested, one is called "Original or Primary Model", and the another one is "Secondary Model"; Similarly, the eruptive rock reservoirs were divided in three types including "Highly Produced", "Moderately Produced" and "Lowly Produced" and accordingly their formation models were given off; the related non-igneous reservoir system was considered combination of eight reservoirs, among which some ones like the Above Anticline Trap are highly produced; Also, the non-hydrocarbon. Trap system including five kinds of traps was discussed. 8. The concept models for four reservoir systems were suggested, which include the intrusive system consisted of 7 kinds of traps, the land eruptive system with 6 traps, the under water eruptive system including 6 kinds of traps and the non-hydrocarbon system combined by 5 kinds of traps. In this part, the techniques for exploration of igneous reservoir system were also generalized and probed, and based on which and the geological progresses of this paper, the potential resources and distributions of every reservoir system was evaluated and about 186 millions of reserves and eight most potential non-hydrocarbon areas were predicted and outlined. The author believe that the igneous reservoir system is a very important exploration area and its study is only in its early stage, the framework of this paper should be filled with more detailed studies, and only along way, the exploration of igneous reservoir system can go into it's really effective stage.