Sour-Gas-Reservoir Exploitation in Croatia

2011 ◽  
Vol 6 (02) ◽  
pp. 91-95
Author(s):  
Lidia Hrncevic ◽  
Katarina Simon ◽  
Zdenko Kristafor ◽  
Matija Malnar
Keyword(s):  
Gas Reservoir ◽  
Sour Gas

Effect of sulphur deposition on well performance in a sour gas reservoir

2017 ◽  
Vol 96 (4) ◽  
pp. 886-894 ◽  
Author(s):  
Jinghong Hu ◽  
Zhengdong Lei ◽  
Zhangxin Chen ◽  
Zhanguo Ma
Keyword(s):  
Well Performance ◽  
Gas Reservoir ◽  
Sulphur Deposition ◽  
Sour Gas

Modeling of sulfur plugging in a sour gas reservoir

2013 ◽  
Vol 11 ◽  
pp. 18-22 ◽  
Author(s):  
Jinghong Hu ◽  
Shunli He ◽  
Jinzhou Zhao ◽  
Yongming Li
Keyword(s):  
Gas Reservoir ◽  
Sour Gas

scholarly journals Experimental Study on the Elemental Sulfur Solubility in Sour Gas Mixtures

2021 ◽  
Vol 9 ◽  
Author(s):  
Rui Zhang ◽  
Shaohua Gu ◽  
Liang Huang ◽  
Daqian Zeng ◽  
Tong Li ◽  
...  
Keyword(s):  
Experimental Data ◽  
Elemental Sulfur ◽  
Large Error ◽  
Gas Mixtures ◽  
Type Model ◽  
Gas Reservoir ◽  
Sulfur Solubility ◽  
Experimental Conditions ◽  
Increasing Temperature ◽  
Sour Gas

The investigation of elemental sulfur solubility plays critical roles on sour gas reservoir development. In this paper, the solubility of elemental sulfur was directly measured by static method with gas samples from well M1 of a sour gas reservoir in Sichuan Basin. The results show that the solubility of elemental sulfur ranges from 0.001 g/cm3 to 0.968 g/cm3 at 40–98.9 MPa and 15–49.8 MPa. The elemental sulfur solubility increases with increasing temperature and pressure, especially when the pressure is greater than 30 MPa. Moreover, the H2S content in sour gas mixtures is also an important factor affecting elemental sulfur solubility. The elemental sulfur solubility increases with increasing H2S content of the sour gas mixtures. The experimental data in this paper display a consistent trend with the reported experimental data. Based on the experimental results, the chrastil-type model, Robert’s model and Hu’s model were investigated and compared. The results show that the chrastil-type model by fitting experimental data in this paper has less error and higher accuracy in calculating elemental sulfur solubility in M gas reservoir. The chrastil-type models proposed in the literature, meanwhile, are only based on the regression of specific gas components and experimental conditions, which lead to a large error in the calculation of elemental sulfur solubility of sour gas samples in this research. The research results provide important basic data and technical support for the development of M gas reservoir.

scholarly journals A Model for Predicting Elemental Sulphur Induced Permeability Damage in a Fractured Sour Gas Reservoir

2020 ◽  
Author(s):  
Gbadegesin Adeyemi ◽  
Adesina Fadairo ◽  
Temitope Ogunkunle ◽  
Adebowale Oladepo ◽  
Amachree Alozie ◽  
...  
Keyword(s):  
Elemental Sulphur ◽  
Gas Reservoir ◽  
Permeability Damage ◽  
Sour Gas

Successful Proppant Fracturing of Ultradeep Sour Gas Reservoir

1989 ◽  
Author(s):  
J.W. Ely ◽  
W.J. Cobb ◽  
B. Elkin ◽  
D.D. Bell
Keyword(s):  
Gas Reservoir ◽  
Sour Gas

Stimulation of a Deep Sour Gas Reservoir Using Gelled Acid

2002 ◽  
Author(s):  
H.A. Nasr-El-Din ◽  
S.H. Al-Mutairi ◽  
M. Al-Jari ◽  
A.S. Metcalf ◽  
W. Walters
Keyword(s):  
Gas Reservoir ◽  
Sour Gas ◽  
Stimulation Of

Earthquakes near Rocky Mountain House, Alberta, and their relationship to gas production facilities

1986 ◽  
Vol 23 (2) ◽  
pp. 172-181 ◽  
Author(s):  
Robert J. Wetmiller
Keyword(s):  
Field Survey ◽  
Rocky Mountain ◽  
Gas Production ◽  
Earthquake Activity ◽  
Gas Reservoir ◽  
Regional Seismicity ◽  
Thrust Faulting ◽  
Northern United States ◽  
East West ◽  
Sour Gas

A 1980 field survey of earthquake activity near Rocky Mountain House, Alberta, using one digital and six conventional seismographs, recorded 146 microearthquakes (M ≤ 3.4) in 23 days and located 67 of them. The located events, and probably the unlocated events as well, all occurred in a small zone approximately 4 km north–south by 4 km east–west by 1 km thick, centred near 52°12.5′N, 115°15′W at a depth of 4.0 km, with an uncertainty of ±2 km on each of the location coordinates. The activity occurred below and (or) in the Strachan D-3A sour gas reservoir, which is a Devonian-aged limestone reef complex in a section of nearly flat-lying, unfaulted sediments. The earthquakes had a composite thrust-faulting mechanism with generally north-trending, intermediate-dipping planes in the presence of a regional deviatoric stress field that was horizontally compressive and oriented approximately east–west. The earthquake activity may be related to the extraction of the natural gas and related fluids from the reservoir, but the exact relationship cannot be documented at this time.The earthquake activity in the region increased dramatically after the production of gas from the reservoir began in the early 1970's. The tight cluster of activity found by the field survey suggests that all the activity in the region occurred in the same small zone but that earlier events may have been mislocated. Earthquake activity in western Alberta generally is not induced and occurs within a regional seismicity belt spatially continuous with the Intermountain Seismic Belt of the northern United States, but the earthquake activity in Canada seems to be tectonically distinct from that in the U.S.A., being characterized by thrust faulting and horizontally compressive stress.

Sign in / Sign up

Export Citation Format

Share Document