Shusheng Guo, Shiyue Wang, S. Daungkaew, Bei Gao, S. Chouya, O. Mullins, Jesus A. Cañas, S. Betancourt, A. Gisolf, T. Khunaworawet, D. Ling
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These new techniques can help many clients in the EAG and as well as other basins to accurately quantify N2 without the need to wait for PVT laboratory analysis which generally takes several months to complete.\n Detection of non-hydrocarbon gases in oil and gas fluids, such as nitrogen gas, is very important for reservoir assessment and management. N2 content affects reserve estimation, especially in the area where reservoir fluids have high N2 contents. In our experience, there are several basins in Asia where N2 and CO2 coexist in the same reservoirs. N2 was charged into reservoirs from the source rock in the same geological time as Hydrocarbon (HC). The CO2 then later charged into the same reservoirs. Xu et al (2008) and Mullins (2019) suggested that the ratio of HC. and N2 are in proportional for each basin. However, the CO2 which was later charged are variable in each reservoir depending on CO2 source and charging area. The relationship between HC. and N2 can be used to predict amount of N2 using three proposed methods (1) Basin Base Method (2) Iteration Methods using DFA spectrometer and InSitu Density measurements., and (3) Equation of State (EOS) Method. This nitrogen prediction techniques were developed to better characterize reservoir fluids and overcome the limitation of the existing technology that's unable to detect and measure nitrogen at downhole conditions. This method can offer extra information, especially for our new Ora Intelligent Wireline Formation Tester technology where answer products will be expanded to tailor client objectives.\n The N2 and HC. relationship from each basin are examined in detail from our DFA and PVT data base. The ratio of N2 and HC. were then recorded as initial value for Basin Base Method. Then the second N2 prediction technique that uses individual hydrocarbon compositions and downhole density measurements were conducted to calculate missing N2 mass from spectrometer measurements. A ternary diagram was prepared to visualize and determine correlation of the gas composition components. It was found that straight line can be obtained on the Ternary diagram between N2, HC., and CO2 for each reservoir. A detailed calculation based on fluid components and partial densities together with iteration process allows to estimate the mass percentage of nitrogen. The results were then compared with actual value from PVT lab. These nitrogen prediction techniques already have been tested and validated using various datasets from South East Asia and other. This technique can be extended to be part of Reservoir Fluid Geodynamic (RFG) to evaluate lateral reservoir connectivity and to better understand CO2 and N2 charge to reservoirs.","PeriodicalId":11011,"journal":{"name":"Day 3 Thu, March 24, 2022","volume":"124 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2022-03-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"New Innovative Methods to Predict N2 in Real Time: Expand New Wireline Formation Testing Platform Products to Fit Basins\",\"authors\":\"Shusheng Guo, Shiyue Wang, S. Daungkaew, Bei Gao, S. Chouya, O. Mullins, Jesus A. Cañas, S. Betancourt, A. Gisolf, T. Khunaworawet, D. Ling\",\"doi\":\"10.4043/31487-ms\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\\n Since early 1990's, Downhole Fluid Analysis (DFA) has been developed to monitor mud filtrate contamination for Wireline Formation Tester downhole sampling. 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N2 was charged into reservoirs from the source rock in the same geological time as Hydrocarbon (HC). The CO2 then later charged into the same reservoirs. Xu et al (2008) and Mullins (2019) suggested that the ratio of HC. and N2 are in proportional for each basin. However, the CO2 which was later charged are variable in each reservoir depending on CO2 source and charging area. The relationship between HC. and N2 can be used to predict amount of N2 using three proposed methods (1) Basin Base Method (2) Iteration Methods using DFA spectrometer and InSitu Density measurements., and (3) Equation of State (EOS) Method. This nitrogen prediction techniques were developed to better characterize reservoir fluids and overcome the limitation of the existing technology that's unable to detect and measure nitrogen at downhole conditions. 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引用次数: 0
摘要
自20世纪90年代初以来,井下流体分析(DFA)就被开发出来,用于监测电缆地层测试器井下取样的泥浆滤液污染。DFA还可以实时提供准确的储层流体信息,如碳氢化合物成分(包括CO2)。然而,DFA技术无法测量氮气,因为氮气在近红外区域(NIR)没有吸收。因此,井下任何光谱仪都无法直接检测到。本文将介绍可用于预测每个储层中N2含量的创新方法。这些新技术可以帮助EAG和其他盆地的许多客户准确量化N2,而无需等待PVT实验室分析,通常需要几个月的时间才能完成。油气流体中非烃气体(如氮气)的检测对储层评价和管理具有重要意义。N2含量影响储量估算,特别是在储层流体N2含量高的地区。根据我们的经验,亚洲有几个盆地在同一储层中同时存在N2和CO2。N2与烃(HC)在同一地质时代从烃源岩充入储层。随后,二氧化碳被充入相同的储存库。Xu et al .(2008)和Mullins(2019)认为HC的比值。和N2在各盆地呈正比关系。然而,根据不同的CO2源和不同的充注区域,每个储层的充注CO2量是不同的。HC的关系。可采用3种方法(1)盆地基础法(2)DFA谱仪迭代法和原位密度测量法。(3)状态方程(EOS)法。开发这种氮预测技术是为了更好地表征储层流体,克服了现有技术无法在井下条件下检测和测量氮的局限性。这种方法可以提供额外的信息,特别是对于我们新的Ora智能电缆地层测试技术,答案产品将扩展以适应客户的目标。N2和HC。从我们的DFA和PVT数据库中详细检查了每个盆地的关系。N2和HC的比值。然后记录为盆地基础法的初始值。然后,采用第二种氮气预测技术,利用单个碳氢化合物组成和井下密度测量数据,计算光谱仪测量数据中缺失的氮气质量。制作了三元图,以直观地显示和确定气体组成成分的相关性。结果表明,在N2、HC的三元图上可以得到一条直线。和每个储层的二氧化碳。基于流体组分和局部密度的详细计算以及迭代过程可以估计氮的质量百分比。然后将结果与PVT实验室的实际值进行比较。这些氮预测技术已经使用来自东南亚和其他地区的各种数据集进行了测试和验证。该技术可以扩展为储层流体地球动力学(RFG)的一部分,以评估储层的横向连通性,并更好地了解储层的CO2和N2电荷。
New Innovative Methods to Predict N2 in Real Time: Expand New Wireline Formation Testing Platform Products to Fit Basins
Since early 1990's, Downhole Fluid Analysis (DFA) has been developed to monitor mud filtrate contamination for Wireline Formation Tester downhole sampling. DFA can also provide accurate reservoir fluid information in real time such as hydrocarbon composition including CO2. However, DFA technology cannot measure Nitrogen because N2 has no absorption in the Near Infrared Region (NIR). Therefore, it cannot be directly detected with any spectrometer measurement downhole. This paper will present innovative methods that can be used to predict the amount of N2 in each reservoir. These new techniques can help many clients in the EAG and as well as other basins to accurately quantify N2 without the need to wait for PVT laboratory analysis which generally takes several months to complete.
Detection of non-hydrocarbon gases in oil and gas fluids, such as nitrogen gas, is very important for reservoir assessment and management. N2 content affects reserve estimation, especially in the area where reservoir fluids have high N2 contents. In our experience, there are several basins in Asia where N2 and CO2 coexist in the same reservoirs. N2 was charged into reservoirs from the source rock in the same geological time as Hydrocarbon (HC). The CO2 then later charged into the same reservoirs. Xu et al (2008) and Mullins (2019) suggested that the ratio of HC. and N2 are in proportional for each basin. However, the CO2 which was later charged are variable in each reservoir depending on CO2 source and charging area. The relationship between HC. and N2 can be used to predict amount of N2 using three proposed methods (1) Basin Base Method (2) Iteration Methods using DFA spectrometer and InSitu Density measurements., and (3) Equation of State (EOS) Method. This nitrogen prediction techniques were developed to better characterize reservoir fluids and overcome the limitation of the existing technology that's unable to detect and measure nitrogen at downhole conditions. This method can offer extra information, especially for our new Ora Intelligent Wireline Formation Tester technology where answer products will be expanded to tailor client objectives.
The N2 and HC. relationship from each basin are examined in detail from our DFA and PVT data base. The ratio of N2 and HC. were then recorded as initial value for Basin Base Method. Then the second N2 prediction technique that uses individual hydrocarbon compositions and downhole density measurements were conducted to calculate missing N2 mass from spectrometer measurements. A ternary diagram was prepared to visualize and determine correlation of the gas composition components. It was found that straight line can be obtained on the Ternary diagram between N2, HC., and CO2 for each reservoir. A detailed calculation based on fluid components and partial densities together with iteration process allows to estimate the mass percentage of nitrogen. The results were then compared with actual value from PVT lab. These nitrogen prediction techniques already have been tested and validated using various datasets from South East Asia and other. This technique can be extended to be part of Reservoir Fluid Geodynamic (RFG) to evaluate lateral reservoir connectivity and to better understand CO2 and N2 charge to reservoirs.