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It shows that the reservoir rock consists of silty and fine-grained arkose, and has low compositional maturity and medium textural maturity. The clastic rocks experienced a series of complex diagenesis as compaction, cementation, pressure solution and dissolution.

结果表明,该储集岩为粉细-细粒岩屑质长石砂岩,成分成熟度普遍较低,结构成熟度中等-较好;储层岩石经历了压实、胶结、压溶和溶解等一系列成岩作用,具有低孔低渗的特点。

It shows that the reservoir rock consists of fine arkose and litharenite lithic feldspar, whose elastic granule appears subangular, compositional maturity is low and textural maturity is medium; the clastic rocks had experienced a series of complex diagenesis as compaction, cementation, pressure solution and dissolution; and the sandstones are of low porosity and low permeability.

结果表明,该储集岩为细粒的长石砂岩和岩屑长石砂岩,颗粒呈次棱角状,成分成熟度普遍较低,结构成熟度中等-较好;经历了压实、胶结、压溶和溶解等一系列成岩作用;储集岩具有低孔、低渗的特点。

The main diagenesis includes compaction, cementation, corrosion and dissolution, etc.

典型的成岩作用类型包括压实作用,胶结作用和溶蚀、溶解作用等。

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公司自96年成立以来,以强大的工程技术实力和优良的品质管理,成为东莞市知名企业,在全国各地区享有极高的声誉,公司引进国外先进技术大量生产批发精雕油泥,云艺牌精雕油泥,彩色油泥,橡皮泥,胶泥,软陶泥,防水泥,模具泥,雕塑工作,烤箱,压泥机,软陶设计与制作,AB水,PU树脂,不饱合树脂,各种硅油,日本信越KF-96、二甲基硅油,乳化硅油,硅胶,矽利康,食品消泡剂、学生用橡皮泥、手板泥、彩色油泥、精雕泥、环氧AB胶,青红胶,水晶胶,目结土、软陶泥、按键胶原料、水溶性硅油、乳化硅油、日本信越钾基耐高温硅油及各种硅油、波丽水、促进剂、轻粉、硬化剂、片碱、烧碱、钛白粉、扎模带、脱脂纱布、蚊帐布、修边针、修胚枪油、修胚枪、玻璃纤维,纤维布、热溶胶、油漆消光粉、油污干洗剂、凡士林、陶瓷脱模剂、青红胶、钾肥皂、矽油、矽胶、模具胶、矽利康、回收废硅胶。。。

The coarse clastic rock of the braided channel of the fan-delta plain is formed when sedimentary water body is in the salinity stage of active tectonic period, the cotemporaneous cementation is intense and the cementation of the carbonate and sulphate has intense packing action in eogenetic stage of shallow buried.

构造相对活跃期为沉积水体咸化期,主要发育扇三角洲平原亚相的辫状河道粗碎屑岩,同生期胶结作用强,而浅埋藏早成岩阶段碳酸盐和硫酸盐胶结物充填强烈,致使物性进一步变差,并且不利于晚成岩A阶段的溶蚀作用进行。

Through the methods of polarizing microscope and cathodoluminescence, the diagenesis of Late Carboniferous phylloid algal reefs in southern Guizhou is studied, which indicates diagenesis are mainly of bio-binding and baffling actions, micritization, cementation, compaction-pressure solution, fracture, recrystallization and dissolution in type.

东北大学资源与土木工程学院,沈阳110004通过偏光显微镜研究和阴极发光技术,对黔南晚石炭世叶状藻礁灰岩的成岩作用做了详细研究,认为礁灰岩主要成岩作用类型有:生物黏结障积作用、泥晶化作用、胶结作用、压实压溶作用、破裂作用、重结晶作用和溶解作用等。

By studying reservoir rock characteristics, diagenesis and physical property, investigation showed that there were distributary channel, branch channel, mouth bar, distal bar, sand sheet, lakeshore, shallow lake and limestone flat . we concluded that the reservoir of N1~N21 is low porosity and permeability reservoir with the types of primary porosity and secondary intergranular porosity, which is in the early diagenetic stage B into the late diagenetic stage A subperiod. The role of effecting reservoir physical property is deposition, cementation, dissolution and tectonic rupture. After researching of reservoir, we divided it into three categories and division the favorable facies belt and relatively favorable. We think that the favorable facies belt is braided river delta front and partly shallow lake in east of the Fault Ⅶ. favorable reservoir is in the first and the second class.

进一步研究了本区碎屑岩储层的岩石学特征、成岩作用特征、物性特征,研究认为该区储集体类型有分流河道砂体、分支河道砂体、河口坝、远砂坝、席状砂砂体、滨湖砂滩、浅湖砂坝砂体及灰坪;N1层属于低孔、特低渗储层,孔隙类型以原生、次生粒间溶孔为主;分析了影响储层物性的因素主要为沉积作用、胶结作用、溶蚀作用和构造破裂作用;进行了储层评价与有利相带预测,将储层分为三类并划分了有利区带、较有利区带,认为Ⅶ号断层以东的辫状河三角洲前缘亚相和部分浅湖亚相是N1的有利储集相带,储层以Ⅰ、Ⅱ类为主。

Further, a hemagglutination elution test revealed that the 6593S virus was unable to release from hemagglutinated RBC. Through the protein structure modeling, it was suggested that the change in amino acid residue 443 of neuraminidase might alter the neuraminidase catalytic sites.

而进一步透过蛋白质结构模拟分析,可以知道6593S小溶斑病毒神经胺酸酶第443个胺基酸残基的改变,使得小溶斑病毒神经胺酸酶酵素催化位置和唾液酸及神经胺酸酶抑制药物之间结合的键结有所改变,此结果可和实验结果相互印证。

Porosity evolution influenced by those diageneses is also analyzed. The dissolution and alteration of feldspars and unstable rock fragments are the main constructive diageneses, but the compaction, pressure solution and cementation are the main destructive diageneses which are unavoidable.

溶蚀作用与蚀变作用是形成砂岩储层的两大建设性成岩作用,云母类矿物的水解作用对孔隙的形成也起到一定的积极作用;但机械压实、压溶作用和胶结作用则是储层形成过程中不可避免的破坏性成岩作用。

For same felted and coated fertilizer, the shape of nutrient dissolved curves were similar in different sand column but dissolved ratios were not.

同一种胶结包膜型缓/控释肥料在不同粒径砂柱里氮磷钾溶出率曲线形状近似,但溶出率不同。

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