Control Factors of Solutional Voids in Feldspars and Favorable Zone Forecast of Chang 2 Oil Reservoir Group in the Midwest Ordos Basin

The development of pores in a clastic reservoir is one of the most important research subjects in oil-gas exploration and development, whereas the many reasons for the formation of secondary porosity have increased the degree of difficulty in such research. Thus the research aims are to discover the controlling factors of solutional voids in feldspars and to predict favorable regions for these voids. Macroscopic and systematic researches into the relationship between the kaolinite content in the feldspar solutional void developed area of the Chang 2 reservoir group of the Triassic Yanchang Formation in the Midwest Ordos Basin and the solutional void in feldspar have been made, and from this it can be determined that the kaolinite content has an indicative function to the distribution of the solutional void in feldspar. Solutional void in feldspar is relatively well developed at the area where kaolinite content is high. Although the factors affecting kaolinite content are complicated, yet that of the research area is mainly affected by the impact of the leaching atmospheric water acting on the palaeogeomorphology. Three favorable zone belts for the development of solutional voids in feldspars are forecasted on the basis of restoration of palaeogeomorphology.

Diageneses and Their Influences on Reservoir Properties of Chang 2 Oil Member in Renshan Region, Zhidan Oilfield, Ordos Basin

1 Introduction Yanchang Formation in Upper Triassic,Ordos basin contains the most abundant hydrocarbon resources in North China(Wang et al.,2014).The sandstones are the most important oil-bearing reservoirs in Yanchang

长2油藏注水井清防垢技术研究与应用

长庆油田分公司第四采油厂长2油藏注水井结垢严重,影响正常的注水开发。在对长2油藏水井垢样化学组成分析结果的基础上,研制了一种碱性清垢剂,该清垢剂对长2油藏水井垢样中酸不溶部分的清垢率可达49.7%;筛选出一种对长2油藏各区块具有普适性的阻垢剂A;针对长2油藏垢样组成特点,制定了盐酸+碱性清垢剂+阻垢剂A三段式清防垢方案,经现场试验验证效果优于普通酸化。

鄂尔多斯盆地志丹地区长2储层成岩作用及其对孔隙度演化的影响

通过岩心观察、铸体薄片鉴定、粒度分析、扫描电镜、电子探针、X射线衍射分析、核磁共振实验、流体包裹体、真实砂岩微观模型驱替等分析资料,对志丹地区长2储层砂岩成岩作用、成岩演化阶段及孔隙度演化与驱替效率之间的关系进行了研究。结果表明,砂岩经历了压实作用、压溶作用、胶结作用和溶蚀作用的改造,研究区长2油层组现今处于中成岩A期;应用Beard砂岩原始孔隙度恢复公式,计算出长2储层未固结砂岩的原始孔隙度平均39.09%;压实、压溶作用对储层物性影响最大,可以使原始孔隙度减少15.41%,减孔率为39.42%;胶结作用会进一步减少原始孔隙度,使孔隙度损失12.72%,减孔率为32.46%,而绿泥石薄膜的普遍发育则对于原生孔隙具有一定的保护作用;此外,长石和岩屑的溶蚀作用也对储层物性起到明显的改善作用,并且溶蚀作用产生的高岭石充填在孔隙中形成的晶间孔也可以成为储集空间,使孔隙度增加4.2%,增孔率为10.76%;各种成岩作用造成孔隙度变化对于储层的驱替效率影响不同,其中压实作用的增强对降低驱替效率影响最大,而强烈的溶蚀作用会使储层的驱替效率增加,以方解石胶结为主的胶结作用会降低储层驱替效率,而以绿泥石膜胶结为主的胶结作用对储层驱替效率影响相对较小。