{"title":"螯合剂作为一种具有负反应顺序的刺激液:稀释程度越高的溶液与碳酸盐反应越快","authors":"Igor B. Ivanishin, H. Samouei","doi":"10.2118/206376-ms","DOIUrl":null,"url":null,"abstract":"\n Chelating agents are used to stimulate high-temperature carbonate reservoirs and remove mineral scales. For field applications, commercial chelates—EDTA, DTPA, GLDA, etc.—are commonly supplied as 35–50 wt% (1.2–1.7 M) solutions and diluted two times in water. However, the dependence of the reaction rate on the concentration of chelate in solution has never been quantified. This paper focuses on determining the kinetics of calcite dissolution as a function of the dilution factor of commonly used chelates at acidic pH. Using a rotating disk apparatus, the kinetics of calcite marble dissolution in 0.1–0.25 M EDTA (pH=4.9–5.0), 0.1–0.25 M DTPA (pH=3.5–5.0), and 0.28–0.85 M GLDA (pH=3.7–5.0) solutions has been investigated. The dissolution of calcite in all chelates has a negative fractional-order that increases with temperature in the range -0.6 < n < -1.9. Thus, less concentrated chelate solutions react faster with calcite, and the effect of chelate dilution becomes less pronounced with a temperature increase. For example, three times dilution of pH≈3.7 commercial GLDA solution—from commonly used 50 vol% (0.85 M) to 16.7 vol% (0.28 M)—increases calcite dissolution rate 8.4, 4.9, 2.7, and 2.0 times at 98.6, 116.6, 134.6, and 188.6°F, respectively. Dilution of pH=5.0 EDTA and pH=3.5 DTPA from 0.25 M to 0.1 M increases the dissolution rate of calcite 1.4–3.1 times at 98.6–188.6°F. Probable reasons for such an unusual reaction behavior are discussed in the paper. Presented results are integral for designing the stimulation operations in carbonate reservoir rocks and the removal of carbonate scales.","PeriodicalId":10928,"journal":{"name":"Day 2 Wed, September 22, 2021","volume":"174 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2021-09-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Chelating Agents as a Stimulation Fluid with a Negative Reaction Order: More Diluted Solutions React Faster with Carbonates\",\"authors\":\"Igor B. Ivanishin, H. Samouei\",\"doi\":\"10.2118/206376-ms\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\\n Chelating agents are used to stimulate high-temperature carbonate reservoirs and remove mineral scales. For field applications, commercial chelates—EDTA, DTPA, GLDA, etc.—are commonly supplied as 35–50 wt% (1.2–1.7 M) solutions and diluted two times in water. However, the dependence of the reaction rate on the concentration of chelate in solution has never been quantified. This paper focuses on determining the kinetics of calcite dissolution as a function of the dilution factor of commonly used chelates at acidic pH. Using a rotating disk apparatus, the kinetics of calcite marble dissolution in 0.1–0.25 M EDTA (pH=4.9–5.0), 0.1–0.25 M DTPA (pH=3.5–5.0), and 0.28–0.85 M GLDA (pH=3.7–5.0) solutions has been investigated. The dissolution of calcite in all chelates has a negative fractional-order that increases with temperature in the range -0.6 < n < -1.9. Thus, less concentrated chelate solutions react faster with calcite, and the effect of chelate dilution becomes less pronounced with a temperature increase. For example, three times dilution of pH≈3.7 commercial GLDA solution—from commonly used 50 vol% (0.85 M) to 16.7 vol% (0.28 M)—increases calcite dissolution rate 8.4, 4.9, 2.7, and 2.0 times at 98.6, 116.6, 134.6, and 188.6°F, respectively. Dilution of pH=5.0 EDTA and pH=3.5 DTPA from 0.25 M to 0.1 M increases the dissolution rate of calcite 1.4–3.1 times at 98.6–188.6°F. Probable reasons for such an unusual reaction behavior are discussed in the paper. Presented results are integral for designing the stimulation operations in carbonate reservoir rocks and the removal of carbonate scales.\",\"PeriodicalId\":10928,\"journal\":{\"name\":\"Day 2 Wed, September 22, 2021\",\"volume\":\"174 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-09-15\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Day 2 Wed, September 22, 2021\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.2118/206376-ms\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Day 2 Wed, September 22, 2021","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2118/206376-ms","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
螯合剂用于刺激高温碳酸盐储层,去除矿物结垢。对于现场应用,商业螯合物- edta, DTPA, GLDA等-通常以35-50 wt% (1.2-1.7 M)的溶液提供,并在水中稀释两倍。然而,反应速率对溶液中螯合物浓度的依赖性从未被量化。本文重点研究了在酸性pH下方解石溶解动力学与常用螯合物稀释系数的关系。利用旋转圆盘装置,研究了方解石大理岩在0.1-0.25 M EDTA (pH= 4.9-5.0)、0.1-0.25 M DTPA (pH= 3.5-5.0)和0.28-0.85 M GLDA (pH= 3.7-5.0)溶液中的溶解动力学。在-0.6 < n < -1.9范围内,方解石在所有螯合物中的溶解均呈负分数阶,随温度的升高而增加。因此,浓度较低的螯合剂溶液与方解石反应更快,并且随着温度的升高,螯合剂稀释的效果变得不那么明显。例如,将pH≈3.7的商业GLDA溶液稀释三倍,从常用的50 vol% (0.85 M)稀释到16.7 vol% (0.28 M),在98.6、116.6、134.6和188.6°F下,方解石溶解率分别增加8.4、4.9、2.7和2.0倍。当pH=5.0 EDTA和pH=3.5 DTPA从0.25 M稀释到0.1 M时,方解石的溶解率提高了1.4-3.1倍,温度为98.6-188.6°F。本文讨论了这种不寻常反应行为的可能原因。所得结果对设计碳酸盐岩储层增产作业和去除碳酸盐岩结垢具有重要意义。
Chelating Agents as a Stimulation Fluid with a Negative Reaction Order: More Diluted Solutions React Faster with Carbonates
Chelating agents are used to stimulate high-temperature carbonate reservoirs and remove mineral scales. For field applications, commercial chelates—EDTA, DTPA, GLDA, etc.—are commonly supplied as 35–50 wt% (1.2–1.7 M) solutions and diluted two times in water. However, the dependence of the reaction rate on the concentration of chelate in solution has never been quantified. This paper focuses on determining the kinetics of calcite dissolution as a function of the dilution factor of commonly used chelates at acidic pH. Using a rotating disk apparatus, the kinetics of calcite marble dissolution in 0.1–0.25 M EDTA (pH=4.9–5.0), 0.1–0.25 M DTPA (pH=3.5–5.0), and 0.28–0.85 M GLDA (pH=3.7–5.0) solutions has been investigated. The dissolution of calcite in all chelates has a negative fractional-order that increases with temperature in the range -0.6 < n < -1.9. Thus, less concentrated chelate solutions react faster with calcite, and the effect of chelate dilution becomes less pronounced with a temperature increase. For example, three times dilution of pH≈3.7 commercial GLDA solution—from commonly used 50 vol% (0.85 M) to 16.7 vol% (0.28 M)—increases calcite dissolution rate 8.4, 4.9, 2.7, and 2.0 times at 98.6, 116.6, 134.6, and 188.6°F, respectively. Dilution of pH=5.0 EDTA and pH=3.5 DTPA from 0.25 M to 0.1 M increases the dissolution rate of calcite 1.4–3.1 times at 98.6–188.6°F. Probable reasons for such an unusual reaction behavior are discussed in the paper. Presented results are integral for designing the stimulation operations in carbonate reservoir rocks and the removal of carbonate scales.