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Jumat, 19 April 2019

BASICS OF PETROLEUM RESERVOIR ENGINEERING


BASICS OF PETROLEUM RESERVOIR ENGINEERING

UNDERSTANDING OF RESERVOIR ENGINEERING PIRSON:
"RESERVOIR ENGINEERING MAY BE DEFINED AS THE ART OF FORECASTING THE FUTURE PERFORMANCE OF A GEOLOGIC OIL AND / OR GAS RESERVOIR FROM WITH PRODUCTION IS OBTAIN ACCORDING TO PROBABLE AND PREASSUMED CONDITIONS."

EXPLANATION
"Reservoir Engineering" is a branch of "Petroleum Engineering" with its main task is forecasting the behavior of the reservoir, the rate of production and the amount of oil or gas that can be produced from a well, a group of wells, or from all reservoirs, in the future based on possible assumptions , or from existing past history.

The Modified McKelvey box shows resource status categories.

Reservation Estimation and Uncertainty
LIMITATION
  • Estimates of oil and gas reserves under conditions of uncertainty.
  • Definition of reserves and uncertainty.
  • Technical, economic and political uncertainty.
  • How to reduce uncertainty.
Definition of Uncertainty: not necessarily happening, it has not been clearly defined, without / lacking clarity.

Type of Uncertainty
  • Technical, Economical, Political.
  • Technical Uncertainty: geophysical, geological, petrophysical, or engineering risk.
  • Economic Uncertainty: risk of price, capital and operating costs, profit sharing and taxes.
  • Political uncertainty: country risk - governance stability, ownership status of oil production and (concessions, PSC, TAC, JOB, KKKS, etc ...)

Reservoir Engineering
In general, a "Reservoir Engineer" will relate to:
  • Basic data, data on physical / chemical-chemical-physics, rock and reservoir fluid properties,
  • Determination of the amount of reserves, both initial and remaining,
  • Fluid flow in porous media,
  • Well test, including: pressure test, productivity, communication between reservoir and / or layer,
  • The behavior of the reservoir, future maintenance of reservoir behavior based on past behavior,
  • Increased recovery,
  • Economic analysis.

STAGE IN LEARNING "RESERVOIR ENGINEERING"
Phase I
Better known as the basic introduction stage of reservoir technique, which addresses reservoir techniques in general, the static and dynamic properties of rocks and reservoir fluids, reservoir properties, permeability, fluid flow such as pressure production rate and fluid pushing efficiency, saturation, capillary pressure reflecting distribution fluid saturation in the reservoir, compressibility which reflects the effect of changes in pressure on both fluid and rock.

Phase II
Known as the basic application phase of reservoir engineering, it discusses the definition of reserves and their calculations, the behavior of reservoirs and the application of fluid flow equations in porous media, phasing out reservoir production.

Stage III
Known as a further application of reservoir techniques, it discusses the analysis and interpretation of fluid flow equations in porous media such as well tests.

Stage III
Known as the "RESERVOIR SIMULATION" stage

Reservoir Engineering
1. Reservoir Limits
Reservoir boundary is the dividing boundary between hydrocarbon areas and non-hydrocarbon areas, which can be:
  • Geological boundary
  • Limits of differences in hydrocarbon fluids, such as water oil limits, gas-water boundaries, or gas-oil boundaries.

2. Reservoir Clarification based on geological traps
  • Trap Structure
  • Stratigraphic Traps
  • Combination Traps

3. Level / degree of reservoir heterogeneity
  • Uniform and non-uniform
  • Homogeneous and heterogeneous
  • Isotropic and un-isotropic

4. Reservoir classification based on fluids
  • Oil Reservoir: black oil, volatile oil
  • Reservoir Gas: dry gas and wet gas

5. Reservoir classification based on initial pressure
  • Undersaturated Reservoir
  • Saturated Reservoir

6. Reservoir classification based on the driving mechanism
  • Soluton gas drive
  • Gas cap drive
  • Water drive
  • Combination drive

7. Plans and types of tests to be carried out according to the type of reservoir.
8. Plan for reservoir development, drainage patterns related to the location of the production and injection time, number of wells, etc.
9. Plan for drainage of reservoirs and stages of production
  • Primary production (natural depletion)
  • Secondary recovery (water or gas injection)
  • Tertiary recovery (enhanced oil recovery)

Reserves
IOIP/ IGIP (initial oil in place / initial gas in place)
Is the amount of oil or gas in a reservoir that is calculated volumetically based on geological data as well as drilling, or material balance based on physical properties of fluid and production reservoir rock and reservoir behavior, or it can also be done by calculation of reservoir simulation.

Reserves
1. Proven Reserves:
The amount of hydrocarbon fluid that can be produced which amount can
proven by a high degree of certainty.
  • The results of log reliable qualitative analysis
  • Successful content research and testing
  • Can produce at a commercial production level
2. Potential Reserves (Probable and Possible):
This reserve is based on a geological map and still requires research with further drilling.

HOW TO APPLY OIL RESERVES



RESERVE CLASSIFICATION



Type of Estimated Reserves
  • Deterministic Based Reserves Estimates - each parameter uses the best assumption.
  • Probabilistic Based Reserves Estimates - quantification of uncertainty.

Reliability of Reserves Estimates
  • Data quantity and quality
  • Competence and Integrity Reservation Estimator

Proved Reserves Guidelines
  • Known Reservoir
  • Existing Economic and Operating Conditions
  • Actual Production or Conclusive Formation Test
  • Improved Recovery under Certain Conditions
  • How to Incorporate New Technology
KNOWN RESERVOIRS
  • Penetrated by a Wellbore and Confirmed as Hydrocarbon - Bearing.
  • Downdip Limits - Contacts or Low Known Hydrocarbons - example.
  • Known Areas
  • Fault limitations and distance between wells.

Effect of Economic Calculations on Estimated Reserves
  • Prices and Cost as of the Date of Reserves Estimate. Price Change Only as a Allowed Contractual Agreement - no escalations based on future conditions.
  • Existing Operating Conditions and Equipment in place, and limited to economically feasible projects and "state-of-the-art" technology.

Production or Testing Requirements for Proved Reserves
  • Formation Test
    • Drill-Stem Test (DST)
    • Conclusive Formation Test
  • FavorableWell Log Response or Core Analysis

Determination of Production Phase
a. Early Stage Production (primary)
  • Naturally, that is production which occurs because the reservoir energy is able to lift fluid to the surface.
  • Artificial lift, still using the reservoir energy coupled with external force (for example a bobbin pump, the pump subsides) or by reducing the weight of the liquid in the well column (for example with a gaslift).

b. Second Stage Production (Secondary)
  • Maintain stability and / or add energy to the reservoir directly by injecting water or gas in a well, then producing it from another well.

c. Advanced Stage Production (Enhanced Oil Recovery)
  • Heat injection: huff puff, steam (steam), in situ combustion
  • Injection of materials: chemicals, surfactants, polymers
  • Miscible injection: C02 or N2 gas




Reservoir Simulation
Reservoir simulation is one method used to:
1. Estimating the contents of the initial gas oil in the reservoir.
2. Large identification and influence of aquifers.
3. Identify the effect of faults in the reservoir.
4. Estimating fluid distribution.
5. Identify vertical relationships between layers.
6. Production forecasting for the future.
7. Production forecasting by including alternative development:
  • Amount of addition of production wells
  • Types / ways to increase production
  • Amount of addition of injection wells
  • System / shape / pattern area
8. Make several cases to optimize oil production

Simulation is a reservoir form / model that is mathematically elaborated. Where the model is made and considered as the actual situation, in accordance with existing reservoir parameters, or reliable assumptions.

Simulation Equipment
  • Hardware (computers and their peripherals)
  • Software (simulator)
  • Reservoir as a model

Simulation Implementation Steps
  • Data preparation
  • Initialization
  • Alignment
  • Forecasting
  • Economy

Simulator type
  • 1 Phase (gas reservoir)
  • Black Oil Model
  • Compositional Model
  • Miscible Model


Some examples of Reservoir Simulator

Reference:
  • Wahyono Kuswo, 2008, Dasar-Dasar Teknik Reservoir Migas, Ikatan Ahli Teknik Perminyakan Indonesia (Iatmi)
  • S. Naji, Hassan Dr., 2004, Petroleum Reserves Estimation Methods, A Report Submitted to the Energy Studies Department OPEC Secretariat
  • www.petrobjects.com

Selasa, 16 April 2019

SOURCE ROCK GEOCHEMISTRY PRA-TERSIER AKIMEUGAH BASIN, PAPUA


SOURCE ROCK GEOCHEMISTRY PRA-TERSIER AKIMEUGAH BASIN, PAPUA


The Akimeugah Basin is located north of the southern Papuan basement high (Merauke Ridge) which separates it from the Arafura Basin to the south. This basin Judging from its association with surrounding basins, the akimeugah basin is associated with basins that have produced hydro-coal in the West Papua Basin and Australian basins. From tracing various journals and articles, the geochemical literature will provide an overview of the active host rocks in the area.

The index map of the Akimeugah and Sahul Basins is based on the Indonesian Sediment Basin Map (Badan Geologi, 2009).

The Akimeugah Basin begins as a passive margin, which is a basin formed by rifting on the northern edge of the Australian continent at the edge of this bank, experiencing cracking due to a part of the mass in its northern part which is about to move and move from Australia. In this crack, horst and graben are formed which in the graben are deposited sediments of Paleozoic and Mesozoic synrifting. Then, when this part is separated and away from Australia (drifting) sediment drifting is deposited which is generally in the form of shale or limestone, this event occurs until Paleogene.
 
Tectonic maps and cross sections of the foreland basin

At the age of Neogen, Akimeugah collided with the Central Range of Papua (Back of Papua). Since that's the type foreland basin Akimeugah. Passive Paleozoic-Neogen margins are bent into the lower Banda line and Central Range. Then at the front of the buckling (foredeep) deposited molassic sediments which are erosional products from nearby heights. However, and burial by the sedimentary part of the passive margin molasses, Akimeugah has ripened Paleozoic, Mesozoic, or Paleogene host rock in the graben. move flips from foredeep to the forebulge (the direction in the direction of the passive margin which is not bent like foredeep) laterally, or moves vertically towards the immobilization deformation zone in the impact area. The main control of the Akimeugah basin is rifting and drifting in the Mesozoic-Paleogene Paleozoicum, and collisions on Neogene (Awang Satyana, in Sabarnas Agus 2011)

Stratigraphy of the Akimeugah Basin

The Akimeugah Basin consists of pre-cambrian-tertiary deposits. The basic rock consists of Gabro rocks aged pre-cambrian and Metamorphic rocks. Followed by the deposition of the Permian Dolomite Modio formation and the Aiduna Formation which are deposited incongruously. Then it was harmoniously deposited on top of Mesozoic clastic formations (Tipuma, Kopai, Woniwogi, Piniya and Ekmai Formations), as well as some carbonate coatings locally. Above the Ekmai Formation, overlaid by clastic and limestone Paleocene-Miocene age (Waripi, Lower Yawee, Adi Members, and Upper Yawee) are out of tune. The last deposition was the final claystone of the late Miocene to Plio-Pleistocene and the uncoated local carbonate, the Buru Formation.

GEOCHEMICAL METHOD
The geochemical approach is the process of identifying active host rocks beginning with evaluating the quantity of organic material using the parameters Petter and Cassa, 1994. Determination of the quality of organic material uses a modified Van Krevelen diagram in Hunt, 1996. And Determination of maturity level using the parameters Petter and Cassa, 1994. used consisted of analysis of TOC content, Rock-Eval Pyrolysis, and Vitrinite (RO) reflection.

Identification of Parent Rock
The process of identifying host rock intervals in the aqueduct basin is carried out in several wells. Where the host rock evaluation focuses on the Woni - Wogi Formation and Aiduna Formation

Organic Material Quantity
The source rock identification begins by analyzing the host rock quantity and the ability to generate hydrocarbon. The quantity of host rock is assessed by looking at the value of total organic content (TOC) expressed in units of the percentage by weight of dry rock. Analysis of the source rock quantity is done by making a TOC curve to the depth at the intervals of each formation, as follows:

a) Woni - Wogi Formation
The Woni-wogi Formation at the Early Cretaceous age with the lithology of sandstone, shale and siltstone consisting of having a value of organic material content is 0.34 wt - 2.9 wt% based on the classification of organic material content into the Poor - V. Good category (Peters and Cassa, 1994). Judging from the ability to generate hydrocarbons with parameters S1 + S2 (Potential Yield) the value is 0.2 mgHC / g - 6.21 mgHC / g which is included in the Poor-Good category (Peters and Cassa, 1994). This data shows that this formation has the potential to become host rock.

TOC content of Woni-Wogi Formation and Ability to generate
Hydrocarbons

b) Aiduna Formation
Aiduna Formation at Permian age with shale lithology has a value of organic material content which is 0.39 wt% - 3.45 wt% based on the classification of organic material content into the Poor - V. Good category (Peters and Cassa, 1994). Judging from the ability to generate hydrocarbons using the parameter value S1 + S2 (Potential Yield) with a value of 0.33 mgHC / g - 10.47 mgHC / g into the Poor-V.good category (Peters and Cassa, 1994). This data shows that this formation has the potential to become host rock

Quality of Organic Materials
The quality of organic material influences whether or not the potential of sedimentary rocks to become host rock, which is represented by the kerogen type of host rock. Kerogen type is influenced by the constituent material and its depositional environment. Kerogen type also determines the final active rock product in the form of oil, oil / gas or gas. Determination of kerogen type in this study using a modified van Krevelen diagram plot. The modification is to replace the plot of the H / C to O / C ratio to the ratio of the hydrogen index (HI) to Tmaks. This is done because there is little analysis that gets H / C, O / C and oxygen index (OI) data. Analysis of the quality of organic material using Tmax Vs HI values, as follows:

a) Woni - wogi Formation
The results of plotting HI vs Tmax data from 49 samples in this formation indicate that the kerogen type in the Woni-wogi formation has kerogen Type II - III (Modified Van Kravelen Diagram in Hunt 1996) which is dominated by kerogen type III (Prone Gas). Tmax data shows that this formation has a mature maturity level

Quality of the Woni - Wogi Formation

b) Aiduna Formation
Kerogen type analysis based on HI Vs Tmaks data conducted on 22 samples in the Aiduna formation shows that this formation has a kerogen type II - III which tends to produce a mixture of oil and gas dominated by type III (gas). Also based on Tmax data, this formation has entered the maturity window. With maturity level not yet mature.

Quality of Aiduna Formation

Maturity
Analysis of the maturity of organic material will determine the depth interval (window of maturity) of active host rock that produces hydrocarbons. Maturity analysis is done by looking at the value of vitrinite (Ro) reflectance. Maturity analysis based on vitrinite reflectance (Ro) is based on reflection values ​​(Ro) derived from kerogen, especially from vitrinite. Maturity analysis using Ro is done by combining the whole well so that the trend of maturity values ​​is obtained in a regional (Figure 6). The results of the Ro value analysis indicate that the maturity window in this basin is 7000 feet below sea level. This proves that the Woni-Wogi Formation and also the Aiduna Formation have entered the maturity window. Ro is done by combining all the wells so that the trend of maturity values ​​can be obtained regionally (Figure 6). The results of the Ro value analysis indicate that the maturity window in this basin is 7000 feet below sea level. This proves that the Woni-Wogi Formation and also the Aiduna Formation have entered the maturity window.

Regional Maturity

Immersion History
The results of modeling the history of 1D immersion in a well show that the maturity of the host rock occurs at the age of miocene at a depth of 1980 m or 6500 ft. It is this sediment yield that has the role of ripening pre-tertiary host rock. Where the speed of sedimentation takes place very quickly due to the large supply of erosion from the high sediment produced by the collusion of neogeneous ferns.

History of Immersion of a Well in the Akimeugah Basin

CONCLUSION
The results of the identification of pre-tertiary host rocks in the Akimeugah Basin indicate that the intervals of the host rock of the Woni-Wogi formation and Aiduna formation have poor organic matter content - good. In addition, the two formations have a kerogen type dominated by type III kerogen which will tend to produce gas and have entered the maturity window. This shows that the woni-wogi and Aiduna formations are active host rocks in the Akimeugah basin.
The maturation of this formation occurs during the middle myoses, where a lot of this fast and sedimentary sediment originates from collusion which occurs at that time which successfully ripens the pratersier host rock of this basin.


Reference:

  • Harahap, B.H. 2012. Tectonostratigraphy of the Southern Part of Papua and Arafura Sea, Eastern Indonesia, Indonesian Journal of Geology, Vol. 7
  • Huang, W.Y. dan Meinschein, W.G. 1979. Sterol as Ecological Indicators: Petroleum Geochemistry. Bandung. PreConvention short course IAGI : Awang H. Satyana 2004.
  • Peck, J.M. and Soulhol, B., 1986. Pre- Tertiary Tensional Periods and Their Effects on the Petroleum Potential of Eastern Indonesia. Proceedings Indonesian Petroleum Association, 15th Annual Convention, 341-369.
  • Peters, K.E. dan Cassa, M.R. 1994. Applied Source Rock Geochemistry, dalam Magoon, L.B. and Dow, W.G., eds., The Petroleum System - From Source to Trap: AAPG Memoir, 60
  • Satyana, A. 2015. Petroleum Geochemistry for Exploration and Production of Conventional and Unconventional Hydrocarbons. Short Course: IPA 2015
  • Subarnas, Agus. 2011. Penyelidikan Pendahuluan Kandungan Gas Dalam Batuan Serpih DiDaerah Subroto, E. (2004): Pengenalan Geokimia Petroleum. Bandung :Penerbit ITB
  • Waghete Dan Sekitarnya, Kabupaten Deiyai Provinsi Papua. Prosiding Hasil Kegiatan Pusat Sumber Daya Geologi Tahun 2011
  • Yudha Situmorang, et al, 2017, STUDI GEOKIMIA BATUAN INDUK AKTIF PRA-TERSIER CEKUNGAN AKIMEUGAH, LEPAS PANTAI PAPUA SELATAN, Padjajaran Geoscince Journal
  • Waples, D. 1985. Geochemistry in Petroleum Exploration, International Human Resources Development Corporation, Boston.
  • http://geomagz.geologi.esdm.go.id/cekungan-akimeugah-dan-sahul-harapan-baru-penemuan-migas/
  • https://dzulfadlib.wordpress.com/tag/lapangan-minyak/