首页> 外文会议>Annual convention of the indonesian petroleum association >LABORATORY STUDY OF DRILLING MUDRHEOLOGY AND ANALYSIS OF CHEMICAL COMPOSITION FROM LOCAL CLAY-ILITE MINERALS IN CENTRAL SUMATRA RIAU
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LABORATORY STUDY OF DRILLING MUDRHEOLOGY AND ANALYSIS OF CHEMICAL COMPOSITION FROM LOCAL CLAY-ILITE MINERALS IN CENTRAL SUMATRA RIAU

机译:苏门答腊中中部​​苏立特 - 伊岩矿物质钻探沟槽沟槽学及其分析的实验室研究

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Bentonite is an absorbent agent of clay of aluminum phyllosilicate which contains a majority of Montmorillonite substances. There are two common types of Bentonite, Na-Bentonite and Ca-Bentonite. The mineral clay Illite from Riau, Central Sumatra is more likely to lead to Ca-Bentonite.Laboratory studies are needed to compare Illite to the Na-Bentonite from the Cretaceous Benton Shale near Rock River, Wyoming, United States. To establish the rheology of clay-based mudtestingis performed in the laboratory of the Petroleum Engineering Department, Islamic University of Riau. Laboratory tests obtained values for rheological properties such as density, viscosity, yield point, plastic viscosity and gel strength. On testing, NaCO3 was added as ion exchangers and to add elements of Na in the sludge. Established values were density of 8.6 ppg, viscosity 1.5 cp, yield point 0.5 lb / ft2, gel strength 1°. Meanwhile, to find out the composition and structure of mineral clay SEM and EDX analysis were conducted giving values of C 14.52%, MgO 0.66%, Al2O328.08%, SiO2 49.30%, K2O 3.02%, TiO2 1.13%, FeO 1.87%, CuO 1.43%. Resultswere obtained from rheological analysis of drilling mud and chemical composition analysis of mineral clay Illite fe-rich from Riau, Central Sumatra with the addition of NaCo3 additive. Then rheological properties will be obtained from Illite sludge based muds which would be compared with Bentonite which is generally used as the base material for making drilling mud with API Spec13 A standard..
机译:膨润土是铝的层状硅酸盐含有多数的蒙脱石物质的粘土的吸收剂。有两种常见类型的膨润土,钠基膨润土和钙基膨润土。从廖内矿物粘土,伊利石,中央苏门答腊更可能导致钙Bentonite.Laboratory研究来伊利从白垩纪顿页岩靠近岩石河,怀俄明州,美国比较钠基膨润土。建立在石油工程系,廖内的伊斯兰大学的实验室进行基于粘土mudtestingis的流变。实验室试验的流变性质,例如密度,粘度,屈服点,塑性粘度和凝胶强度而得到的值。上测试,碳酸钠对芦笋加入作为离子交换剂,并在污泥中添加的Na元素。既定值分别为8.6分,粘度1.5厘泊,屈服点0.5磅/平方英尺,凝胶强度为1°的密度。同时,找出矿物粘土的组成和结构的SEM和EDX分析进行了给人Ç14.52%的值,氧化镁0.66%,Al2O328.08%的SiO 2 49.30%,K2O 3.02%,二氧化钛1.13%,FeO的1.87%, CuO的1.43%。 Resultswere从钻井泥浆和矿物粘土,伊利石富铁从廖内,苏门答腊中部的化学成分分析与加碳酸钠对芦笋添加剂的流变分析得到。然后流变性质将从基于伊利石污泥泥浆,其将与膨润土进行比较,其通常用作用于制备钻井泥浆与API Spec13的标准基底材料来获得..

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