浙江地方猪种线粒体DNA多态及遗传多样性研究

用ApaⅠ、AvaⅠ、BamHⅠ、BclⅠ、BglⅠ、BglⅡ、ClaⅠ、DraⅠ、Eco RI、Eco RV、HaeⅡ、HincⅡ、HindⅢ、HpaⅠ、KpnⅠ、PstⅠ、PvuⅠ、PvuⅡ、SacⅠ、SalⅠ、ScaⅠ、SmaⅠ、StuⅠ、XbaⅠ和XhoⅠ等25种识别6个碱基对的限制性内切酶分析了浙江地方品种猪、浙江野猪等30个个体的线粒体DNA,共检出30种限制性态型(morph),可归结成3种单倍型,其中BamHⅠ-B、BclⅠ-B、DraⅠ-B和XbaⅠ-C为首次发现;各单倍型间平均遗传距离(p)为0.005,群体的平均多态度(#pi#)为0.0008,均处于遗传多样性贫乏范围。

中国牦牛线粒体DNA多态性及遗传分化

用20种限制性内切酶分析了我国5个牦牛群体90个个体的限制性片段长度多态性，其中AvaI，AvaⅡ、Bg1Ⅱ、EcoRＩ．HindⅢ、HpaＩ6个酶切类型具有多态性, 共发现５种mtDNA单倍型，每种单倍型中检出50-55个位点，并利用双酶切制定出其物理图谱。

青海湖裸鲤 mtDNA 遗传多样性的初步研究

该文用 BclⅠ、AvaⅠ、BamHⅠ、PstⅠ、KpnⅠ、PvuⅡ 共6种限制性内切核酸酶, 分析了15尾青海湖裸鲤 mtDNA 的限制性片段长度多态性, 共检测出20个酶切位点, 发现 BclⅠ、BamHⅠ和 PvuⅡ 三种酶切类型具有多态性. 根据不同个体 mtDNA 的酶切类型, 青海湖裸鲤存在4种 mtDNA 单倍型, 计算 mtDNA 多态度 π 值为 0.0043, 初步认为青海湖裸鲤在线粒体 DNA 上存在较丰富的群体内变异。

云南保种山羊线粒体DNA限制性酶切研究

　采用碱变性法,提取来自云南省不同地区4个保种山羊的13个个体的线粒体DNA(mtDNA),并用ApaⅠ,AvaⅠ,BamHⅠ,BclⅠ,BcIⅠ，BglⅡ,ClaⅠ,DraⅠ, EcoRⅠ,EcoRⅤ,HaeⅠ,HindⅢ,KpnⅠ,PstⅠ,PvuⅡ,SacⅠ,SalⅠ,SmaⅠ,StuⅠ和XhoⅠ等20种限制性内切酶进行酶切分析。结果发现它们的线粒体DNA的分子量大 小约为15.8Kb；不同限制性内切酶的酶切位点分别为：DraⅠ有7个酶切位点，AvaⅢ有6个酶切位点，EcoRⅤ和StuⅠ共有5个酶切位点，HindⅡ和HaeⅡ有4个酶 切位点，BamHⅠ,BglⅡ,PstⅠ和PvuⅡ有3个酶切位点，ApaⅠ，ClaⅠ有两个酶切位点，其余有1个酶切位点。各保种山羊间未发现变异，说明云南的4个保种山 羊极可能来自于共同的母性祖先。

云南龙陵黄山羊线粒体DNA限制性酶切分析

采用碱性变性法提取来自于龙陵县不同地区的18只黄山羊个体的线粒体DNA(mtDNA),并用Apa I、Ava I、BamH I、Bcl I、Bgl I、Bgl II、Cla I、Dra I、EcoR I、EcoR V、Hae I、Hind III、Kpn I、Pst I、Pvu II、Sac I、Sal I、Sma I、Stu I和Xba I等20种限制性内切酶进行酶切分析。 结果发现龙陵黄山羊线粒体DNA的分子量大小约为15.8Kb;不同酶的酶切位点分别为:Dra I有7个酶切位点,Ava II有6个酶切位点,EcoR V和Stu I共有5个酶切位点,Hind III和Hea II有4个酶切位点,BamH I、Bgl II、Pst I和Pvu II有3个酶切位点,Apa I、Cla I有2个酶切位点,其余有1个酶切位点。

雌核发育银鲫两个不同品系线粒体DNA比较

于 1 996年 4月在中国科学院水生生物研究所关桥实验场取得银鲫E系 ( 8♀ ,2♂ )和D系 ( 9♀ ,1♂ )的卵巢 (♀ )或肝脏 (♂ )组织 ,分离纯化其线粒体DNA ,以此为材料 ,用 2 5种限制性内切酶分析了银鲫这两个雌核发育系的线粒体DNA ,构建了两系鱼mtDNA的 1 9种酶 41个位点的酶切图谱。统计比较酶切片段的大小 ,发现 5种内切酶 (AvaⅡ ,BamHⅠ ,BglⅠ ,SphⅠ ,XbaⅠ )酶切位点在两个雌核发育系间存在差异。这些多态性 ,既可以作为区分两个雌核发

地震资料叠前储层预测综合研究--以辽中凹陷东二下段浊积扇气藏为例

Reservoir prediction techniques from prestack seismic are among the most important ones for exploration of lithologic hydrocarbon reservoir. In this paper, we set the turbidite fan sandstone reservoir in Liao-Zhong depress as our researching target, and aims to solve the apllication difficulties on pre-stack inversion in the area, where the drilling data is scarce and the reservoir is lateral varied. Meanwhile, AVO analysis and pre-stack inversion for gas-bearing detection is systematically researched. The seismic reflection characters of gas-bearing sandstone in turbidite fan with different fluid content are defined, after analyzing results from AVO seismic simulation and porous fluid replacement of real log data, and under the guides of the seismic characters from classical gas-bearing sandstone reservoir and numerical simulation for complicate gas-bearing sandstone. It is confirmed that detecting gas-bearing sandstone in turbidite fan via AVO technologies is feasible. In terms of AVO analysis, two AVO characters, fluid detection factor and product of intercept and gradient, can effectively identify top and bottom boundaries and lateral range of tuibidite gas sand by comparing real drilling data. Cross-plotting of near and far angle stack data could avoid the correlation existing in P-G analysis. After comparing the acoustic impedance inversions with routine stacked data and AVO intercept, impedance derived from AVO intercept attribute could reduce the acoustic impedance estimating error which is caused by AVO. On the aspect of elastic impedance inversion, the AVO information in the pre-stack gathers is properly reserved by creating partial angle stack data. By the far angle elastic impedance alone, the gas sand, with abnormally low range of values, can be identified from the background rocks. The boundary of gas sand can also be clearly determined by cross-plotting of near and far angle elastic impedances. The accuracy of far angle elastic impedance is very sensitive to the parameter K, and by taking the statistical average of Vp/Vs on the targeted section in key wells, the accuracy of low frequency trends is gurranteed; the intensive absorsion within the area of the gas sand, which tends to push the spectral of seismic data to the lower end, will cause errors on the inversion result of elastic impedance. The solution is to confine the inversion on the interested area by improving the wavelet. On the aspect of prestack AVA simultaneous inversion, the constraint of local rock-physical trends between velocities of P-wave、S-wave and density successfully removes the instability of inversion, thus improves the precision of the resulting elastic parameters. Plenty of data on rock properties are derived via AVO analysis and prestack seismic data inversion. Based on them, the fluid anomaly is analysized and lithological interpretation are conducted. The distribution of gas sand can be consistently determined via various of ways, such as cross-plotting of P and G attributes, near and far partial angle stack data, near and far angle elastic impedances, λρ and Vp/Vs, etc. The shear modulo and density are also reliable enough to be used for lithological interpretation. We successfully applied the AVO analysis and pre-stack inversion techniques to gas detecting for turbidite fan sand reservoir in Liao-Zhong depression.

裂缝型储层检测方法——P波方位各向异性技术

Nowadays, the exploration of fractured reservoir plays a vital role in the further development of petroleum industry through out the world. Fractured hydrocarbon reservoirs are widely distributed in China. Usually, S-wave technique prevails, but it also has its disadvantage, prohibitive expense in S-wave data acquisition and processing. So directly utilizing P-wave data to detect fractures, comes to our mind. We briefly introduce theoretical model (HTI) for fractured reservoir. Then study Ruger’s reflectivity method to recognize reflection P-wave reflection coefficient of the top and bottom interface of HTI layer respectively, and its azimuth anisotropy character. Base on that study, we gives a review and comparison of two seismic exploration technologies for fractures available in the industry-- P-wave AVO and AVA. They has shown great potential for application to the oil and gas prediction of fractured reservoir and the reservoir fine description．Every technique has its disadvantage, AVO limited to small reflection angle; and AVA just offering relatively results. So that, We can draw a conclusion that a better way to any particular field is using synthesis of multiple data sources including core、outcrop、well-test、image logs、3D VSPs, generally to improve the accuracy.

泥岩裂缝储层地震识别的理论和方法

During the exploration of fractured reservoirs, worldwide difficult problems will be encountered: how to locate the fractured zones, how to quantitatively determine the azimuth, density, and distribution of the fractures, and how to compute the permeability and porosity of the fractures. In an endeavor to solve these problems, the fractured shale reservoir in SiKou area of ShengLi oil field was chosen as a study area. A study of seismic predictive theory and methods for solving problems encountered in fractured reservoir exploration are examined herein. Building on widely used current fractured reservoir exploration techniques, new seismic theories and methods focusing on wave propagation principles in anisotropic medium are proposed. Additionally, integrated new seismic data acquisition and processing methods are proposed. Based on research and application of RVA and WA methods from earlier research, a new method of acoustic impedance varying with azimuth (IPVA) creatively is put forth. Lastly combining drilling data, well log data, and geologic data, an integrated seismic predictive method for cracked reservoir bed was formed. A summary of the six parts of research work of this paper is outlined below. In part one, conventional geologic and geophysical prediction methods etc. for cracked reservoir exploration are examined, and the weaknesses of these approaches discussed. In part two, seismic wave propagation principles in cracked reservoirs are studied. The wave equation of seismic velocity and attenuation factor in three kinds of fracture mediums is induced, and the azimuth anisotropy of velocity and attenuation in fracture mediums is determined. In part three, building on the research and application of AVA and WA methods by a former researcher, a new method of acoustic impedance creatively varying with azimuth (IPVA) is introduced. A practical software package utilizing this technique is also introduced. In part four, Base on previously discussed theory, first a large full azimuth 3d seismic data (70km~2) was designed and acquired. Next, the volume was processed with conventional processing sequence. Then AVA, WA, and IPVA processing was applied, and finally the azimuth and density of the fractures were quantitatively determined by an integrated method. Predictions were supported by well data that indicate the approach is highly reliable. in part five, geological conditions contributing to cracked reservoir bed formation are analyzed in the LuoJia area resulting in the discovery that the main fractured zones are related to fault distribution in the basin, that also control the accumulation of the oil and gas, the generation mechanisms and types of fractured shale reservoirs are studied. Lastly, by using full 3D seismic attributes, azimuth and density of cracked reservoir zones are successfully quantitative predicted. Using an integrated approach that incorporates seismic, geologic and well log data, the best two fractured oil prospects in LouJia area are proposed. These results herein represent a break through in seismic technology, integrated seismic predictive theory, and production technology for fractured reservoirs. The approach fills a void that can be applied both inside China, and internationally. Importantly, this technique opens a new exploration play in the ShengLi oil field that while difficult has substantial potential. Properly applied, this approach could play an important role toward stabilizing the oil field' production. In addition, this technique could be extended fracture exploration in other oil fields producing substantial economic reward.

双聚焦偏移速度估计与可分表示叠前弹性反演

In exploration seismology, the geologic target of oil and gas reservoir in complex medium request the high accuracy image of the structure and lithology of the medium. So the study of the prestack image and the elastic inversion of seismic wave in the complex medium come to the leading edge. The seismic response measured at the surface carries two fundamental pieces of information: the propagation effects of the medium and the reflections from the different layer boundaries in the medium. The propagation represent the low-wavenumber component of the medium, it is so-called the trend or macro layering, whereas the reflections represent the high-wavenumber component of the medium, it is called the detailed or fine layering. The result of migration velocity analysis is the resolution of the low-wavenumber component of the medium, but the prestack elastic inversion provided the resolution of the high-wavvenumber component the medium. In the dissertation, the two aspects about the migration velocity estimation and the elastic inversion have been studied.Firstly, any migration velocity analysis methods must include two basic elements: the criterion that tell us how to know whether the model parameters are correct and the updating that tell us how to update the model parameters when they are incorrect, which are effected on the properties and efficiency of the velocity estimation method. In the dissertation, a migration velocity analysis method based on the CFP technology has been presented in which the strategy of the top-down layer stripping approach are adapted to avoid the difficult of the selecting reduce .The proposed method has a advantage that the travel time errors obtained from the DTS panel are defined directly in time which is the difference with the method based on common image gather in which the residual curvature measured in depth should be converted to travel time errors.In the proposed migration velocity analysis method, the four aspects have been improved as follow:? The new parameterization of velocity model is provided in which the boundaries of layers are interpolated with the cubic spline of the control location and the velocity with a layer may change along with lateral position but the value is calculated as a segmented linear function of the velocity of the lateral control points. The proposed parameterization is suitable to updating procedure.? The analytical formulas to represent the travel time errors and the model parameters updates in the t-p domain are derived under local lateral homogeneous. The velocity estimations are iteratively computed as parametric inversion. The zero differential time shift in the DTS panel for each layer show the convergence of the velocity estimation.? The method of building initial model using the priori information is provided to improve the efficiency of velocity analysis. In the proposed method, Picking interesting events in the stacked section to define the boundaries of the layers and the results of conventional velocity analysis are used to define the velocity value of the layers? An interactive integrate software environment with the migration velocity analysis and prestack migration is built.The proposed method is firstly used to the synthetic data. The results of velocity estimation show both properties and efficiency of the velocity estimation are very good.The proposed method is also used to the field data which is the marine data set. In this example, the prestack and poststack depth migration of the data are completed using the different velocity models built with different method. The comparison between them shows that the model from the proposed method is better and improves obviously the quality of migration.In terms of the theoretical method of expressing a multi-variable function by products of single-variable functions which is suggested by Song Jian (2001), the separable expression of one-way wave operator has been studied. A optimization approximation with separable expression of the one-way wave operator is presented which easily deal with the lateral change of velocity in space and wave number domain respectively and has good approach accuracy. A new prestack depth migration algorithm based on the optimization approximation separable expression is developed and used to testing the results of velocity estimation.Secondly, according to the theory of the seismic wave reflection and transmission, the change of the amplitude via the incident angle is related to the elasticity of medium in the subsurface two-side. In the conventional inversion with poststack datum, only the information of the reflection operator at the zero incident angles can be used. If the more robust resolutions are requested, the amplitudes of all incident angles should be used.A natural separable expression of the reflection/transmission operator is represented, which is the sum of the products of two group functions. One group function vary with phase space whereas other group function is related to elastic parameters of the medium and geological structure.By employing the natural separable expression of the reflection/transmission operator, the method of seismic wave modeling with the one-way wave equation is developed to model the primary reflected waves, it is adapt to a certain extent heterogeneous media and confirms the accuracy of AVA of the reflections when the incident angle is less than 45'. The computational efficiency of the scheme is greatly high.The natural separable expression of the reflection/transmission operator is also used to construct prestack elastic inversion algorithm. Being different from the AVO analysis and inversion in which the angle gathers formed during the prstack migration are used, the proposed algorithm construct a linear equations during the prestack migration by the separable expression of the reflection/transmission operator. The unknowns of the linear equations are related to the elasticity of the medium, so the resolutions of them provided the elastic information of the medium.The proposed method of inversion is the same as AVO inversion in , the difference between them is only the method processing the amplitude via the incident angle and computational domain.