Shale Gas Flashcards

1
Q

The gas accumulated on the surface of a solid material, such as a grain of areservoirrock, or more particularly the organic particles in ashalereservoir. Measurement of adsorbed gas andinterstitial gas, which is the gas contained inporespaces, allows calculation of gas in place in a reservoir.

A

adsorbed gas

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2
Q

Predictable variation of a property of a material with the direction in which it is measured, which can occur at all scales. For a crystal of amineral, variation in physical properties observed in different directions is aeolotropy (also known as anisotropy). In rocks, variation in seismic velocity measured parallel or perpendicular to bedding surfaces is a form of aeolotropy. Often found where platy minerals such as micas and clays align parallel to depositional bedding as sediments are compacted, aeolotropy is common in shales.

A

aelotropy

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3
Q

An example used for comparison. In oil and gasexploration, geoscientists and engineers compare new prospects and fields with fields and surface exposures thought to be similar indepositional environmentandreservoircharacterto guide predictions. Wide variations inshalereservoirs create doubt about the utility of analog comparisons.

A

analog

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4
Q

Having directionally dependent properties. For a crystal of amineral, variation in physical properties observed in different directions is anisotropy. In rocks, variation inseismicvelocity measured parallel or perpendicular to bedding surfaces is a form of anisotropy. Often found where platy minerals such as micas and clays align parallel to depositional bedding as sediments are compacted, anisotropy is common in shales.

A

anisotropic

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5
Q

Predictable variation of a property of a material with the direction in which it is measured, which can occur at all scales. For a crystal of amineral, variation in physical properties observed in different directions is anisotropy. In rocks, variation in seismic velocity measured parallel or perpendicular to bedding surfaces is a form of anisotropy. Often found where platy minerals such as micas and clays align parallel to depositional bedding as sediments are compacted, anisotropy is common in shales.

A

anisotropy

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6
Q

The direction in which a deviated or horizontal well is drilled relative to magnetic north. Most horizontal wells inshalereservoirs are drilled in the direction of the minimum horizontalstress. This allows for the creation of multiple hydraulic fractures that arenormalto the wellbore.

A

azimuth

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7
Q

A depression in thecrustof the Earth, caused by plate tectonic activity and subsidence, in which sediments accumulate.Sedimentarybasins vary from bowl-shaped to elongated troughs. Basins can be bounded by faults.Riftbasins are commonly symmetrical; basins along continental margins tend to be asymmetrical. If richhydrocarbonsource rocks occur in combination with appropriate depth and duration of burial, then apetroleum systemcan develop within the basin. Most basins contain some amount ofshale, thus providing opportunities forshale gasexplorationandproduction.

A

basin

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8
Q

The fraction of naturally occurring, inflammable organic matter that is extractable from rock using organic solvents. Manypetroleumprecursors are composed of bitumen, but most are formed fromkerogenin the process of petroleumgeneration. Bitumen includes hydrocarbons such asasphaltandmineralwax. Typically solid or nearly so, brown or black, bitumen has a distinctive petroliferous odor. Laboratory dissolution with organic solvents allows determination of the amount of bitumen in samples, an assessment ofsource rockrichness. Burial and heating of kerogenyieldbitumen, thenliquid hydrocarbons, and thenhydrocarbongas. Understanding organic content is especially important inshalereservoirs because the shale is both the source rock and thereservoirrock in thepetroleum system.

A

bitumen

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9
Q

Aflow crossinstalled on top of afrac treewheretreating ironis connected andtreatment fluidenters the frac tree.

A

buffalo head/ frac head/goat head

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10
Q

The physical and chemical alteration of sediments andporefluids at temperatures and pressures higher than those ofdiagenesis. Catagenesis involves heating in the range of 50° to 150°C [122° to 302°F]. At these temperatures, chemical bondsbreakdown inkerogenand clays withinshale, generatingliquid hydrocarbons. At the high end of this temperature range, secondarycrackingof oil molecules can generate gas molecules.

A

catagenesis

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11
Q

A trailer in which fracturing engineers can monitorformation pressuresand other critical information pertaining to thefracturingprocess.

A

command trailer

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12
Q

A generic term used to describe the events and equipment necessary to bring a wellbore intoproductiononce drilling operations have been concluded, including but not limited to the assembly of downholetubularsand equipment required to enable safe and efficient production from an oil orgas well. Completion quality can significantly affect production fromshalereservoirs.

A

completion

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13
Q

A prediction of how effectively rock may be stimulated usinghydraulic fracturing. Completion quality (CQ) is an engineering assessment of factors that determine the effectiveness of hydraulic fracture treatments and includes the ability to initiate and create an inducedfracture network, the degree ofreservoircontact of the newly createdfractures, the level of connection to thenatural fracturesystem of those created fractures and ability of the stimulated reservoir to deliver gas or oil into the well.

A

completion quality (CQ)

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14
Q

Afrac treein which multiplefrac valvesare contained in a single large body such that the overall height of the frac tree is reduced.

A

composite frac tree

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15
Q

A type of areally extensivereservoirthat containshydrocarbonthroughout, rather than containing a watercontactor being significantly affected by a water column or a definedstructuralclosure. The areal extent of a continuous reservoir, such as ashalereservoir, can be as large as the extent of thesedimentary basinin which the shale was deposited.

A

continuous reservoir

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16
Q

Areservoirin which buoyant forces keep hydrocarbons in place below a sealing caprock. Reservoir and fluid characteristics of conventional reservoirs typically permit oil ornatural gasto flow readily into wellbores. The term is used to make a distinction fromshaleand other unconventional reservoirs, in which gas might be distributed throughout the reservoir at thebasinscale, and in which buoyant forces or the influence of a water column on the location of hydrocarbons within the reservoir are not significant.

A

conventional reservoir

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17
Q

Laboratory study of a sample of ageologicformation, usuallyreservoirrock, taken during or after drilling a well. Economic and efficient oil and gasproductionis highly dependent on understanding key properties of reservoir rock, such asporosity,permeability, andwettability. Geoscientists have developed a variety of approaches, including log andcoreanalysis techniques, to measure these properties. Core analysis is especially important inshalereservoirs because of the vertical andlateralheterogeneityof the rocks. Core analysis can include evaluation ofrock propertiesandanisotropy; organic matter content,maturity, and type; fluid content; fluidsensitivity; and geomechanical properties. This information can be used to calibrate log andseismicmeasurements and to help in well andcompletiondesign, well placement, and other aspects of reservoir production.

A

core analysis

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18
Q

The total amount of oil and gas recovered from areservoiras of a particular time in the life of thefield. Cumulativeproductioncan be referenced to a well, a field, or abasin.

A

cumulative production

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19
Q

The intentionaldeviationof a wellbore from the path it would naturally take. This is accomplished through the use of whipstocks,bottomhole assembly(BHA) configurations, instruments to measure the path of the wellbore in three-dimensional space, data links to communicate measurements taken downhole to the surface,mudmotors and special BHA components and drill bits, including rotary steerable systems, and drill bits. The directionaldrilleralso exploits drilling parameters such as weight onbitand rotary speed to deflect the bit away from the axis of the existing wellbore. In some cases, such as drilling steeply dipping formations or unpredictable deviation in conventional drilling operations, directional-drilling techniques may be employed to ensure that the hole is drilled vertically. While many techniques can accomplish this, the general concept is simple: point the bit in the direction that one wants to drill. The most common way is through the use of a bend near the bit in a downhole steerable mud motor. The bend points the bit in a direction different from the axis of the wellbore when the entiredrillstringis not rotating. By pumping mud through the mud motor, the bit turns while the drillstring does not rotate, allowing the bit to drill in the direction it points. When a particular wellbore direction is achieved, that direction may be maintained by rotating the entire drillstring (including the bent section) so that the bit does not drill in a single direction off the wellbore axis, but instead sweeps around and its net direction coincides with the existing wellbore. Rotary steerable tools allow steering while rotating, usually with higher rates of penetration and ultimately smoother boreholes. Directional drilling is common inshalereservoirs because it allows drillers to place theboreholeincontactwith the most productivereservoirrock.

A

deviated drilling

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20
Q

The physical, chemical or biological alteration of sediments intosedimentaryrockat relatively low temperatures and pressures that can result in changes to the rock’s original mineralogy and texture. After deposition, sediments are compacted as they are buried beneath successive layers ofsedimentand cemented by minerals thatprecipitatefrom solution. Grains of sediment, rock fragments and fossils can be replaced by other minerals during diagenesis.Porosityusually decreases during diagenesis, except in rare cases such as dissolution of minerals anddolomitization. Diagenesis does not includeweatheringprocesses.Hydrocarbongenerationbegins during diagenesis. There is not a clear, accepted distinction between diagenesis andmetamorphism, although metamorphism occurs at pressures and temperatures higher than those of the outercrust, where diagenesis occurs.

A

diagenesis

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21
Q

The intentionaldeviationof a wellbore from the path it would naturally take. This is accomplished through the use of whipstocks, bottomhole assembly (BHA) configurations, instruments to measure the path of the wellbore in three-dimensional space, data links to communicate measurements taken downhole to the surface,mudmotors and special BHA components and drill bits, including rotary steerable systems, and drill bits. The directional driller also exploits drilling parameters such as weight onbitand rotary speed to deflect the bit away from the axis of the existing wellbore. In some cases, such as drilling steeply dipping formations or unpredictable deviation in conventional drilling operations, directional-drilling techniques may be employed to ensure that the hole is drilled vertically. While many techniques can accomplish this, the general concept is simple: point the bit in the direction that one wants to drill. The most common way is through the use of a bend near the bit in a downhole steerable mud motor. The bend points the bit in a direction different from the axis of the wellbore when the entiredrillstringis not rotating. By pumping mud through the mud motor, the bit turns while the drillstring does not rotate, allowing the bit to drill in the direction it points. When a particular wellbore direction is achieved, that direction may be maintained by rotating the entire drillstring (including the bent section) so that the bit does not drill in a single direction off the wellbore axis, but instead sweeps around and its net direction coincides with the existing wellbore. Rotary steerable tools allow steering while rotating, usually with higher rates of penetration and ultimately smoother boreholes. Directional drilling is common inshalereservoirs because it allows drillers to place theboreholeincontactwith the most productivereservoirrock.

A

directional drilling

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22
Q

The amount of oil and gas expected to be economically recovered from areservoirorfieldby the end of its producing life. Estimated ultimaterecoverycan be referenced to a well, a field, or abasin.

A

estimated ultimate recovery

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23
Q

An area in which hydrocarbon accumulations or prospects of a given type occur. For example theshalegas plays in North America include the Barnett, Eagle Ford, Fayetteville, Haynesville, Marcellus, and Woodford, among many others. Outside North America,shale gaspotential is being pursued in many parts of Europe, Africa, Asia, and South America.

A

exploration play/ play

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24
Q

The measurement and analysis offormationand fluid properties through examination of formationcuttingsor through the use of tools integrated into thebottomhole assemblywhile drilling, or conveyed onwirelineordrillpipeafter aboreholehas been drilled. Formation evaluation is performed to assess the quantity and producibility of fluids from areservoir. Formation evaluation guides wellsite decisions, such as placement of perforations and hydraulicfracturestages, and reservoirdevelopmentandproductionplanning.

A

formation evaluation

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25
Q

Also known aslogging while drillingorLWD, the measurement offormationproperties during the excavation of the hole, or shortly thereafter, through the use of tools integrated into the bottomhole assembly. LWD, while sometimes risky and expensive, has the advantage of measuring properties of a formation before drilling fluids invade deeply. Further, many wellbores prove to be difficult or even impossible to measure with conventionalwirelinetools, especially highly deviated wells. In these situations, the LWD measurement ensures that some measurement of the subsurface is captured in theeventthat wireline operations are not possible. Timely LWD data can also be used to guide well placement so that the wellbore remains within the zone of interest or in the most productive portion of areservoir, such as in highly variableshalereservoirs.

A

formation evaluation while drilling/ logging while drilling

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26
Q

Pressureabove which injection of fluids will cause therockformationtofracturehydraulically.

A

formation fracture pressure/ fracturing pressure

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27
Q

An abbreviation forfracturing fluid, a fluid injected into a well as part of astimulationoperation. Fracturing fluids forshalereservoirs usually contain water,proppant, and a small amount of nonaqueous fluids designed to reduce frictionpressurewhile pumping the fluid into the wellbore. These fluids typically includegels, friction reducers, crosslinkers, breakers and surfactants similar to household cosmetics and cleaning products; these additives are selected for their capability to improve the results of the stimulation operation and the productivity of the well.

A

frac fluid

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28
Q

Another term forhydraulic fracturing, astimulationtreatment routinely performed on oil and gas wells in low-permeabilityreservoirs. Specially engineered fluids are pumped at highpressureand rate into thereservoirinterval to be treated, causing a verticalfractureto open. The wings of the fracture extend away from the wellbore in opposing directions according to the natural stresses within theformation.Proppant, such as grains ofsandof a particular size, is mixed with the treatment fluid to keep the fracture open when the treatment is complete. Hydraulic fracturing creates high-conductivitycommunication with a large area of formation and bypasses anydamagethat may exist in the near-wellbore area.

A

frac job

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29
Q

AChristmas treeinstalled specifically for the fracturing process. A frac stack typically consists of upper and lowermaster valves,flow cross,wing valves,goat head, andswab valve. Frac stacks generally have larger bores and higher pressure ratings thanproduction treesto accommodate the high flow rates and pressures necessary forhydraulic fracturing.

A

frac stack/ frac tree

30
Q

A crack or surface of breakage withinrocknot related to foliation or cleavage inmetamorphicrock along which there has been no movement. A fracture along which there has beendisplacementis afault. When walls of a fracture have moved only normal to each other, the fracture is called ajoint. Fractures can enhance permeability of rocks greatly by connecting pores together, and for that reason, fractures are induced mechanically in some reservoirs in order to boosthydrocarbonflow. Fractures may also be referred to as natural fractures to distinguish them from fractures induced as part of areservoirstimulationor drilling operation. In someshalereservoirs, natural fractures improveproductionby enhancingeffective permeability. In other cases, natural fractures can complicate reservoir stimulation.

A

fracture/ natural fracture

31
Q

That portion of a dual-porosityreservoirspermeabilitythat is associated with thesecondary porositycreated by open, natural fractures. In many of these reservoirs,fracturepermeability can be the major controlling factor of the flow of fluids.

A

fracture permeability

32
Q

A fluid injected into a well as part of astimulationoperation. Fracturing fluids forshalereservoirs usually contain water,proppant, and a small amount of nonaqueous fluids designed to reduce frictionpressurewhile pumping the fluid into the wellbore. These fluids typically includegels, friction reducers, crosslinkers, breakers and surfactants similar to household cosmetics and cleaning products; these additives are selected for their capability to improve the results of the stimulation operation and the productivity of the well.

A

fracturing fluid

33
Q

The gaseous phase present in areservoiror other contained area. Gas may be found either dissolved in reservoir fluids or as free gas that tends to form a gas cap beneath the topsealon the reservoirtrap. Both free gas and dissolved gas play important roles in the reservoir-drive mechanism.

A

free gas

34
Q

Shale that produces natural gas. A shale that is thermally mature enough and has sufficient gas content to produce economic quantities of natural gas.

A

gas shale

35
Q

Thegeologicspecialty that deals with understanding how rocks, stresses, pressures, and temperatures interact. This understanding is used to solveoilfieldproblems, such as optimizinghydraulic fracturingtreatments ofshalereservoirs. Geomechanics specialists typically work with experts ingeophysics,geology, petrophysics,reservoirengineering, drilling engineering, androckphysics to solve geomechanical problems and addressproductionchallenges in shale reservoirs.

A

geomechanics

36
Q

Abbreviation for gas initially in place, the volume of gas in a reservoir before production.

A

GIIP

37
Q

The quality of variation inrock propertieswith location in areservoirorformation.Shalegas reservoirs are heterogeneous formations whose mineralogy, organic content, natural fractures, and other properties vary from place to place. This heterogeneity makespetroleumsystemmodeling,formation evaluation, andreservoir simulationcritical to maximizingproductionfrom shale reservoirs.

A

heterogeneity

38
Q

Possessing the quality of variation inrock propertieswith location in areservoirorformation.Shalegas reservoirs are heterogeneous formations whose mineralogy, organic content, natural fractures, and other properties vary from place to place. This heterogeneity makespetroleumsystemmodeling,formation evaluation, andreservoir simulationcritical to maximizingproductionfrom shale reservoirs.

A

heterogeneous

39
Q

Flow control unit used in the pressurization of fluid employed inhydraulic fracturing.Fracturing fluidenters the missile at low pressure and is directed to the pump trucks for pressurization. High-pressure fluid returns to the missile and is directed to the well or, in the case of amultiwell pad, to afrac manifold.

A

high-pressure manifold/ missile

40
Q

The intentionaldeviationof a wellbore from the path it would naturally take to a horizontal trajectory. Horizontallateralsections can be designed to intersect natural fractures or simply tocontactmore of the productiveformation. Horizontal drilling is accomplished through the use of whipstocks,bottomhole assembly(BHA) configurations, instruments to measure the path of the wellbore in three-dimensional space, data links to communicate measurements taken downhole to the surface,mudmotors and special BHA components, including rotary steerable systems and drill bits. While many techniques can accomplish this, the general concept is simple: Direct thebitin the direction that one wants to drill. By placing a bend near the bit in a downhole steerablemud motor, the bend points the bit in a direction different from the axis of the wellbore when the entiredrillstringis not rotating. By pumping mud through the mud motor, the bit turns while the drillstring does not rotate, allowing the bit to drill in the direction it points. When a particular wellbore direction is achieved, that direction may be maintained by rotating the entire drillstring (including the bent section) such that the bit does not drill in a single direction off the wellbore axis. Instead, the bit sweeps around and its net direction coincides with the existing wellbore. Rotary steerable tools allow steering while rotating, usually with higher rates of penetration and ultimately smoother boreholes. Horizontal drilling is common inshalereservoirs because it allows drillers to place theboreholein contact with the most productivereservoirrock.

A

horizontal drilling

41
Q

A technique totrackthe propagation of a hydraulicfractureas it advances through aformation. Microseisms are detected, located, and displayed in time for scientists and engineers to approximate the location and propagation of the hydraulic fracture. Software providesmodeling,surveydesign, microseismic detection and location,uncertaintyanalysis, data integration, and visualization forinterpretation. Computer imagery is used to monitor the activity in 3D space relative to the location of the fracturing treatment. The monitored activities are animated toshowprogressive fracture growth and the subsurface response to pumping variations. When displayed in real time, the microseismic activity allows one to make changes to thestimulationdesign to ensure optimalreservoircontact. Also known as microseismic monitoring, this technique delivers information about the effectiveness of the stimulation of a reservoir that can be used to enhance reservoirdevelopmentinshalegas completions.

A

hydraulic fracturing monitoring/ microseismic monitoring

42
Q

Astimulationtreatment routinely performed on oil and gas wells in low-permeabilityreservoirs. Specially engineered fluids are pumped at highpressureand rate into thereservoirinterval to be treated, causing a verticalfractureto open. The wings of the fracture extend away from the wellbore in opposing directions according to the natural stresses within theformation.Proppant, such as grains ofsandof a particular size, is mixed with the treatment fluid to keep the fracture open when the treatment is complete. Hydraulic fracturing creates high-conductivitycommunication with a large area of formation and bypasses anydamagethat may exist in the near-wellbore area.

A

hydraulic fracturing

43
Q

The gas stored in theporespace of areservoirrock. Measurement of interstitial gas andadsorbed gas, which is the gas accumulated on the surface of another solid material, such as a grain of reservoir rock, allows calculation of gas in place in a reservoir.

A

interstitial gas/ pore gas

44
Q

The naturally occurring, solid, insoluble organic matter that occurs in source rocks and can yield oil upon heating. Kerogen is the portion of naturally occurring organic matter that is nonextractable using organic solvents. Typical organic constituents of kerogen are algae and woody plant material. Kerogens have a high molecular weight relative tobitumen, or soluble organic matter. Bitumen forms from kerogen duringpetroleumgeneration. Kerogens are described as Type I, consisting of mainly algal and amorphous (but presumably algal) kerogen and highly likely to generate oil; Type II, mixedterrestrialandmarinesource material that can generate waxy oil; and Type III, woody terrestrial source material that typically generates gas.

A

kerogen

45
Q

The process of asourcerockbecoming capable of generating oil or gas when exposed to appropriate pressures and temperatures. As asource rockbegins to mature, it generates hydrocarbons. As anoil-pronesource rock matures, thegenerationof heavy oils is succeeded bymediumand light oils and condensates. Above a temperature of approximately 100°C [212°F], onlydry gasis generated, and incipientmetamorphismis imminent. Thematurityof a source rock reflects the ambientpressureand temperature as well as the duration of conditions favorable forhydrocarbongeneration. Understanding maturation is especially important inshalereservoirs because of the shales dual role as source rock andreservoirrock.

A

maturation

46
Q

The last stage ofmaturationand conversion of organic matter to hydrocarbons. Metagenesis occurs at temperatures of 150° to 200°C [302° to 392°F]. At the end of metagenesis,methane, ordry gas, is evolved along with nonhydrocarbon gases such as CO2, N2, and H2S, as oil molecules are cracked into smaller gas molecules.

A

metagenesis

47
Q

Afine-graineddetritalsedimentaryrockformed byconsolidationofclay- andsilt-sized particles. Mudrocks are highly variable in their clay content and are often rich incarbonatematerial. As a consequence, they are less fissile, or susceptible to splitting along planes, than shales. Mudrocks may include relatively large amounts of organic material compared with otherrock typesand thus have potential to become richhydrocarbonsourcerocks. The typical fine grain size and lowpermeability, a consequence of the alignment of their platy or flaky grains, allow mudrocks to form goodcaprocks for hydrocarbon traps. However, mudrocks are also capable of beingreservoirrocks, as evidenced by the many wells drilled into them to produce gas.

A

mudrock

48
Q

Natural gas produced fromshalereservoirs is known asshale gas. The composition of the gas stream is a function of thethermal maturityof therock. Thermallyimmaturerocks will contain heavierhydrocarboncomponents, possibly even liquid components.Overmaturereservoirs typically contain appreciable quantities ofcarbon dioxide[CO2].

A

natural gas

49
Q

The creation of holes in thecasingorlinerto achieve efficient communication between thereservoirand the wellbore. This process is integral to the optimal creation of hydraulic fractures. Geomechanical analysis is commonly conducted before perforatingshalereservoirs to account for the relationship betweenformationstresses and productivity.

A

perforate

50
Q

A technique used to represent the history of asedimentary basin, including the processes and components necessary to formpetroleum: a petroleumsourcerock, areservoir, a trapping mechanism, aseal, and the appropriate relative timing offormationof these. Usinggeologic, geophysical, and engineering data, scientists create a 3Dmodelof the subsurface that can be used to understand whether petroleum is present and how much might exist in potential traps. Petroleum systems models can be used to help predictporepressureand plan well construction andfielddevelopment. A useful petroleum systems model can be used to identify and explain inconsistencies in the data. The resulting models are valuable duringexplorationfor identifying resource richness, such assweetspots in unconventional plays such asshalegas, and during field development andproductionfor improvingcompletionefficiency. Petroleum systemsmodelingis distinct fromreservoir simulationin that it covers a largerscalethat might include multiple oil and gas fields and considers a geologic time frame of millions of years rather than a production time frame of years or decades.

A

petroleum system modeling

51
Q

A term used to describe water produced from a wellbore that is not atreatment fluid. The characteristics of produced water vary and use of the term often implies an inexact or unknown composition. It is generally accepted that water within the pores ofshalereservoirs is not produced due to its lowrelative permeabilityand itsmobilitybeing lower than that of gas.

A

produced water

52
Q

Sized particles mixed withfracturing fluidto hold fractures open after ahydraulic fracturingtreatment. In addition to naturally occurringsandgrains, man-made or specially engineered proppants, such asresin-coated sand or high-strength ceramic materials likesinteredbauxite, may also be used. Proppant materials are carefully sorted for size and sphericity to provide an efficient conduit forproductionof fluid from thereservoirto the wellbore.

A

proppant

53
Q

A type of geochemical analysis in which arocksample is subject to controlled heating in an inert gas to or past the point of generating hydrocarbons in order to assess its quality as a source rock, the abundance of organic material in it, itsthermal maturity, and the quality of hydrocarbons it might generate or have generated. Pyrolysis breaks largehydrocarbonmolecules into smaller molecules. This process is used to determine the quality ofshaleas a source rock and is instrumental in evaluatingshale gasplays.

A

pyrolysis

54
Q

An operation to restimulate a well after an initial period ofproduction. Refracturing operations attempt tobypassnear-wellbore damage, reestablish good connectivity with thereservoir, and tap portions of the reservoir with higherporepressure. Refracturing operations are also performed after a period of production that can alter the stresses in a reservoir due todepletion; the restimulation can allow the newfractureto reorient along a differentazimuth. A successful refracturing operation restores well productivity to near original or even higher rates of production and extends the productive life of a well.

A

refracturing

55
Q

Amodelof a specific volume of the subsurface that incorporates all thegeologiccharacteristics of thereservoir. Such models are used to quantify characteristics within the subsurface volume that are relatively stable over long periods of time and can, therefore, be considered static. These attributes include thestructuralshape and thicknesses of the formations within the subsurface volume being modeled, their lithologies, and theporosityandpermeabilitydistributions. These last two characteristics often vary significantly from location to location within the volume, resulting inheterogeneity. However, porosity and permeability are stable in the near-geologic timeframe and do not change due to the movement of fluids or gases through any of the formationsporespaces. The result ofreservoir characterizationis a reservoir characterization model (also known as a static model and sometimes referred to as a geologic model).Shalegas reservoir rocks require the analysis of high-qualityseismicdata,core, and log measurements and engineering data to produce an accurate reservoir characterization model. This model is then used as input intoreservoir simulation, during which reservoir engineers add other reservoir characteristics, such as pressures, temperatures, and fluid and gas compositions. These features can change due to the movement of fluids or gases through any of the formations pore spaces. Since these are dynamic in their nature over short timeframes, onceproductionis initiated these models are referred to as dynamic models. Thorough reservoir simulations (dynamic models) that are based on accurately developed reservoir characterizations (static models) can be of significant value in optimizing well placement andfield-developmentplanning.

A

reservoir characterization model

56
Q

A prediction of the likelihood of a rock to yield commercial quantities of hydrocarbons. Reservoir quality (RQ) is a geologic, engineering and economic assessment of a resource, its reserves and their producibility. The term RQ includes the following factors: volume of oil or gas in place, organic content (TOC),thermal maturity,effective porosity, fluidsaturations—oil, gas and water, reservoir thickness and intrinsicpermeability.

A

reservoir quality (RQ)

57
Q

A tool designed to drill directionally with continuous rotation from the surface, eliminating the need toslideasteerable motor. Rotary steerable systems typically are deployed when drilling directional, horizontal, or extended-reach wells. State-of-the-art rotary steerable systems have minimal interaction with theborehole, thereby preserving borehole quality. The most advanced systems exert consistent side force similar to traditional stabilizers that rotate with thedrillstringor orient thebitin the desired direction while continuously rotating at the same number of rotations per minute as the drillstring.

A

rotary steerable system

58
Q

Afine-grained, fissile, detrital sedimentaryrockformed byconsolidationof clay- andsilt-sized particles into thin, relatively impermeable layers. It is the most abundant sedimentary rock. Shale can include relatively large amounts of organic material compared with otherrock typesand thus has potential to become a richhydrocarbonsource rock, even though a typical shale contains just 1% organic matter. Its typical fine grain size and lack ofpermeability, a consequence of the alignment of its platy or flaky grains, allow shale to form a good cap rock for hydrocarbon traps. Gas shows from shales during drilling have led some shales to be targeted as potential gas reservoirs. Various clay types and volumes influence the quality of thereservoirfrom a petrophysical and geomechanical perspective. The quality of shale reservoirs depends on their thickness and extent, organic content,thermal maturity, depth andpressure, fluid saturations, and permeability, among other factors.

A

shale

59
Q

Natural gasproduced fromgas shaleformations.

A

shale gas

60
Q

Containingshale, afine-grained, fissile, detrital sedimentaryrockformed byconsolidationof clay- andsilt-sized particles into thin, relatively impermeable layers. It is the most abundant sedimentary rock. Shale can include relatively large amounts of organic material compared with otherrock typesand thus has potential to become a richhydrocarbonsource rock, even though a typical shale contains just 1% organic matter. Its typical fine grain size and lack ofpermeability, a consequence of the alignment of its platy or flaky grains, allow shale to form a good cap rock for hydrocarbon traps. Gas shows from shales during drilling have led some shales to be targeted as potential gas reservoirs. Various clay types and volumes influence the quality of thereservoirfrom a petrophysical and geomechanical perspective. The quality of shale reservoirs depends on their thickness and extent, organic content,thermal maturity, depth andpressure, fluid saturations, and permeability, among other factors.

A

shaly

61
Q

Arockrich in organic matter which, if heated sufficiently, will generate oil or gas. Typical source rocks, usually shales or limestones, contain about 1% organic matter and at least 0.5%total organic carbon(TOC), although a rich source rock might have as much as 10% organic matter. Rocks of marine origin tend to beoil-prone, whereasterrestrialsource rocks (such as coal) tend to begas-prone. Preservation of organic matter without degradation is critical to creating a good source rock, and necessary for a completepetroleumsystem. Under the right conditions, source rocks may also bereservoirrocks, as in the case ofshale gasreservoirs.

A

source rock

62
Q

An operation in which numerousreservoirintervals are hydraulically stimulated in succession. Stagedhydraulic fracturingoperations are commonly performed from horizontal wellbores placed inshalegas reservoirs. Using geomechanical data, engineers are able to optimize the placement of perforations and fracturing stages to maximize gasproduction.

A

staged fracturing

63
Q

A treatment performed to restore or enhance the productivity of a well. Stimulation treatments fall into two main groups,hydraulic fracturingtreatments andmatrixtreatments. Fracturing treatments are performed above thefracturepressureof thereservoirformationand create a highly conductive flow path between the reservoir and the wellbore. Matrix treatments are performed below the reservoir fracture pressure and generally are designed to restore the naturalpermeabilityof the reservoir followingdamageto the near-wellbore area. Stimulation inshalegas reservoirs typically takes the form of hydraulic fracturing treatments.

A

stimulation/ well stimulation

64
Q

Colloquial expression for a target location or area within aplayor areservoirthat represents the bestproductionor potential production. Geoscientists and engineers attempt tomapsweetspots enable wellbores to be placed in the most productive areas of the reservoir. Sweet spots inshalereservoirs may be defined bysource-rockrichness or thickness, by natural fractures, or by other factors, usinggeologicaldata such ascore analysis,well logdata, orseismicdata.

A

sweet spot

65
Q

The degree of heating of a source rock in the process of transformingkerogenintohydrocarbon. Thermalmaturityis commonly evaluated by measuringvitrinitereflectance or bypyrolysis.

A

thermal maturity

66
Q

Describing a relatively impermeable reservoirrockfrom whichhydrocarbonproductionis difficult. Reservoirs can be tight because of smaller grains ormatrixbetween larger grains, or they might be tight because they consist predominantly ofsilt- orclay-sized grains, as is the case forshalereservoirs.Stimulationof tight formations can result in increased production from formations that previously would have been abandoned or produced uneconomically.

A

tight

67
Q

Gas produced from a relativelyimpermeablereservoirrock.Hydrocarbonproductionfromtightreservoirs can be difficult withoutstimulationoperations. Stimulation of tight formations can result in increased production from formations that previously might have been abandoned or been produced uneconomically. The term is generally used for reservoirs other than shales.

A

tight gas

68
Q

The concentration of organic material insourcerocks as represented by the weight percent of organic carbon. A value of approximately 0.5% total organic carbon by weight percent is considered the minimum for an effectivesource rock, although values of 2% are considered the minimum forshalegas reservoirs; values exceeding 10% exist, although some geoscientists assert that high total organic carbon values indicate the possibility ofkerogenfillingporespace rather than other forms of hydrocarbons. Total organic carbon is measured from 1-g samples of pulverizedrockthat are combusted and converted to CO or CO2. If a sample appears to contain sufficient total organic carbon to generate hydrocarbons, it may be subjected topyrolysis.

A

total organic carbon (TOC)

69
Q

An umbrella term for oil andnatural gasthat is produced by means that do not meet the criteria for conventionalproduction. What has qualified as unconventional at any particular time is a complex function of resource characteristics, the availableexplorationand production technologies, the economic environment, and thescale,frequencyand duration of production from the resource. Perceptions of these factors inevitably change over time and often differ among users of the term. At present, the term is used in reference to oil and gas resources whoseporosity,permeability, fluid trapping mechanism, or other characteristics differ from conventionalsandstoneandcarbonatereservoirs. Coalbedmethane, gas hydrates,shalegas, fractured reservoirs, andtightgas sands are considered unconventional resources.

A

unconventional resource

70
Q

A measure of thethermal maturityof organic matter. This analytical method was developed to rank thematurityof coals and is now used in other rocks to determine whether they have generated hydrocarbons or could be effective source rocks. Thereflectivityof at least 30 individual grains ofvitrinitefrom arocksample is measured under a microscope. The measurement is given in units of reflectance, % Ro, with typical values ranging from 0% Roto 3% Ro, with values for gas-generating source rocks typically exceeding 1.5%. Strictly speaking, the plant material that forms vitrinite did not occur prior to Ordovician time, although geochemists have established a scale of equivalent vitrinite reflectance for rocks older than Ordovician.

A

vitrinite reflectancce

71
Q

Activities associated with drilling a wellbore to intercept one of more specified locations. The term usually is used in reference to directional or horizontal wells that are oriented to maximizecontactwith the most productive parts of reservoirs viahydraulic fracturingor to optimize intersection with natural fractures. Geomechanical analysis of natural fractures and stresses andgeologicalanalysis of thereservoirare critical to successful well planning. Advancedformation evaluationand drilling technology support the drilling operation in real time.

A

well placement

72
Q

The description of a proposed wellbore, including the shape, orientation, depth,completion, and evaluation. Well plans might be relatively simple for vertical wellbores. Directional or horizontal wellbores require more detailed planning about where to land the well and begindirectional drilling, how long the directional or horizontal section should be, and how to evaluate and complete the well.Shalegas wells, many of which are horizontal wells, require highly detailed well plans to optimizeproductionfrom reservoirs that are vertically and laterally heterogeneous.

A

well plan