Determination of free volume of a rock sample using high pressure adsorption data
10156507 ยท 2018-12-18
Assignee
Inventors
- Benjamin Howard Davidson (West Jordan, UT, US)
- Keith Howarth Greaves (Salt Lake City, UT, US)
- David Clark Atwood (North Salt Lake, UT, US)
- Robert Michael Griffin (Salt Lake City, UT, US)
Cpc classification
G01N15/0893
PHYSICS
International classification
G01N31/00
PHYSICS
G01N15/08
PHYSICS
Abstract
A method of characterizing free volume of a rock sample includes test operations that measure pressure decay data from stepwise pressurization of the rock sample with a test gas. An initial free volume of the rock sample is calculated as a function of the pressure decay data. An initial maximum storage capacity of the rock sample is derived as a function of the initial free volume of the rock sample. A volume of test gas adsorbed as a liquid is calculated based on the maximum storage capacity of the rock sample. An updated free volume of the rock sample is calculated based on the initial free volume and the volume of the test gas adsorbed as a liquid. An updated maximum storage capacity of the rock sample is derived as a function of the updated free volume. Calculations of the volume of test gas adsorbed as a liquid, the updated free volume and the updated maximum capacity of the rock sample can be repeated until the updated maximum storage capacity and the updated free volume converge respectively to give the maximum storage capacity and free volume of the rock sample.
Claims
1. A method of characterizing free volume of a rock sample to estimate productivity of a reservoir including: iteratively measuring pressure decay data during each of a plurality of pressurization stages of the rock sample pressurized with a test gas from a pressurizing source, wherein the pressure decay data comprises a beginning pressure and a final pressure subjected to by the rock sample and a beginning source pressure of the pressurizing source, and wherein the beginning source pressure is varied across the plurality of pressurizing stages such that the test gas is successively adsorbed in a pore space of the rock sample through the plurality of pressurization stages, wherein the rock sample is obtained from the reservoir and comprises a shale; calculating a beginning free volume available to the test gas in the rock sample based at least on the pressure decay data of a pressurization stage of the plurality of pressurization stages, wherein the beginning free volume corresponds to a pore space volume available to the test gas at a beginning of the pressurization stage; calculating a liquid volume of the test gas adsorbed as a liquid by the rock sample, during the pressurization stage, based at least on the pressure decay data; calculating an updated free volume available to the test gas in the rock sample based at least on the beginning free volume reduced by the liquid volume of the test gas adsorbed as the liquid during the pressurization stage; deriving an updated maximum storage capacity of storing the test gas in the rock sample based at least on the updated free volume; comparing the beginning free volume and the updated free volume to generate a difference; continuing the plurality of pressurization stages until the difference does not exceed a pre-determined threshold; and estimating, subsequent to reaching the difference not exceeding the pre-determined percentage, the productivity based on the updated maximum storage capacity of storing the test gas.
2. The method according to claim 1, wherein the test gas does not include helium.
3. The method according to claim 2, wherein the test gas is methane.
4. The method according to claim 1, wherein the rock sample is pressurized above a pressure corresponding to a percentage of a Langmuir volume based on a Langmuir isotherm curve.
5. The method according to claim 1, wherein the rock sample is a shale.
6. The method according to claim 5, wherein the shale has a total organic carbon content of less than 2.5%.
7. A method of characterizing free volume of a rock sample to estimate productivity of a reservoir including: iteratively measuring pressure decay data during each of a plurality of pressurization stages of the rock sample pressurized with a test gas from a pressurizing source, wherein the pressure decay data comprises a beginning pressure and a final pressure subjected to by the rock sample, and a beginning source pressure of the pressurizing source, wherein the rock sample comprises shale of the reservoir, wherein the test gas is successively adsorbed in a pore space of the rock sample through the plurality of pressurization stages, wherein the rock sample is obtained from the reservoir; calculating a beginning free volume available to the test gas in the rock sample based at least on the pressure decay data of a pressurization stage of the plurality of pressurization stages, wherein the beginning free volume corresponds to a pore space volume available to the test gas at a beginning of the pressurization stage; calculating a liquid volume of the test gas adsorbed as a liquid by the rock sample, during the pressurization stage, based at least on the pressure decay data; calculating an updated free volume available to the test gas in the rock sample based at least on the beginning free volume reduced by the liquid volume of the test gas adsorbed as the liquid during the pressurization stage; comparing the beginning free volume and the updated free volume to generate a difference; continuing the plurality of pressurization stages until the difference does not exceed a pre-determined threshold; and estimating, subsequent to reaching the difference not exceeding the pre-determined percentage, the productivity based on the updated free volume available to the test gas in the rock sample.
8. The method according to claim 7, wherein the test gas does not include helium.
9. The method according to claim 8, wherein the test gas is methane.
10. The method according to claim 7, wherein the rock sample is pressurized above a pressure corresponding to a percentage of a Langmuir volume based on a Langmuir isotherm curve.
11. The method according to claim 7, wherein the shale has a total organic carbon content of less than 2.5%.
Description
BRIEF DESCRIPTION OF THE DRAWINGS
(1)
(2)
(3)
(4)
(5)
(6)
(7)
(8)
DETAILED DESCRIPTION
(9) It has been proposed that using helium to determine the sample free volume may produce an error if the effects of pore size-dependent void volume (porosity) are not considered. See, Daniel J. K. Ross and R. Marc Bustin, Impact of Mass Balance Calculations on Adsorption Capacities in Microporous Shale Gas Reservoirs, Fuel, Volume 86, Issues 17-18, December 2007, pp. 2696-2706, http://dx.doi.org/10.1016/j.fuel.2007.02.036 (http://www.sciencedirect.com/science/article/pii/S0016236107001202).
(10) More particularly, Ross et al. propose that the error in adsorption calculations due to helium void volume calibrations for high pressure methane isotherms is most significant with low organic carbon content, moisture equilibrated shales, and mudrocks in which the overall adsorptive capacity is low. In such samples negative adsorption can be calculated due to the void volume of helium used in the mass balance calculations exceeding the void volume of methanea reflection of greater pore space accessibility of the smaller helium molecule than the larger methane molecule. In order to address the issue of the pore space being available to helium, a workflow is described for determining the free volume in a shale sample by using a test gas other than helium, such as methane.
(11) As will be appreciated by those of skill in the art, the term free volume refers to the total pore space in a sample that can hold the un-adsorbed gas. When gas is adsorbed, it is stored on the surface of the sample in liquid form, which occupies a volume in the pore space that subtracts from the free volume. Typical isotherm tests show that the storage capacity of a sample (which represents the amount of test gas adsorbed by the sample) approaches a maximum value (i.e., the Langmuir volume,
(12)
(13) The reference cell 302 is fluidly coupled to a helium supply and to a test gas supply by a three-way valve 315, which may be electrically controlled. A vent valve 317, which may be electrically controlled, is positioned in the helium/test gas supply line. The reference cell 302 and the sample cell 304 are fluidly coupled by a valve 316, which likewise may be electrically controlled.
(14) The porosimeter 300 also includes a controller and/or computer processing system 320 that includes control logic that interfaces to the electrically controlled valves 315, 316 via wired or wireless signal paths therebetween for control of the operation of the valves 315, 316, that interfaces to the pressure sensors 308, 310 via wired or wireless signal paths therebetween for pressure measurements and recordation of such pressure measurements during operation of the porosimeter 300, and that interfaces to the temperature sensors 307, 312 via wired or wireless signal paths therebetween for temperature measurements and recordation of such temperature measurements during operation of the porosimeter 300. The control logic of the controller and/or computer processing system 320 (which can be embodied in software that is loaded from persistent memory and executed in the computing platform of the computer processing system 320) is configured to control the different parts of the porosimeter 300 to carry out a sequence of operations (workflow) that characterizes the free volume of the sample placed in the sample cell 304. The control logic can be configured by user input or a testing script or other suitable data structure, which is used to configure the controller or the computer processing system 320 in order to carry out control operations that are part of the workflow as described herein. For example, the user input or the testing script or other suitable data structure can specify parameters (such as pressures, flow rates, temperatures, etc.) for such control operations of the workflow.
(15) An embodiment of a workflow is illustrated in the flow chart of
(16) At block 402 the sample is pressurized in stages to a pressure above the pressure at which adsorption of the test gas does not predominate. This pressure can be defined as the pressure corresponding to a certain percentage of the Langmuir volume. For example, a pressure above the pressure corresponding to 85% of the Langmuir volume could be used as a pressure threshold. Also, the pressure can be a pressure above the pressure which the sample is subject to in the rock formation. For example, the valve 316 is initially closed to isolate the sample cell 304 from the reference cell 302. The valve 315 is positioned to introduce test gas into the reference cell 302 to pressurize the reference cell 302 to an initial pressure of about 100 psig (7.03 kg/square cm gauge) for the first stage. With the reference cell 302 charged to a known pressure, the initial pressures P.sub.1 and P.sub.2 of the reference and sample cells 302, 304 are recorded and the valve 315 is then closed. With the valve 315 closed and the reference cell 302 charged, the valve 316 is opened to allow the test gas from the reference cell 302 to move into the sample cell 304 where some of the test gas can adsorb into the sample. After a time period elapses, the pressures P.sub.1 and P.sub.2 in the sample cell 304 and reference cell 302 will equilibrate. During this time period the pressures P.sub.1 and P.sub.2 are recorded. Once the pressures are equilibrated, the final pressures P.sub.1 and P.sub.2 are recorded and valve 316 is closed. Then, these operations are repeated for further stages of pressurization. The process of charging and equalizing pressure may be repeated multiple times, such as nine times, each time increasing the final pressures of P.sub.1 and P.sub.2 until the final pressure of P.sub.2 corresponds to the pressure threshold mentioned above.
(17) Pressure test data for nine pressurization stages or data runs is shown below as a matrix. As indicated, at the end of the pressurization the test sample is pressurized to 3857 psig (271.1 kg/square cm gauge). Also, for each test run, compressibility factors (z) are determined (as will be appreciated by those of skill in the art), as shown in the matrix
(18)
below.
(19) At block 403 an initial free volume of the sample is calculated based on the pressure and compressibility factor matrices as follows. The gauge pressures in the pressure matrix may be converted to absolute pressures for purposes of the calculations. Then, each matrix is divided into vectors for performing calculations for each pressure step run as follows:
Pref.sub.i:=Press.sup.0
.sup. Pref.sub.f:Press=
.sup.1
.sup. Psam.sub.i:=Press
.sup.2
.sup. Psam.sub.f:=Press
.sup.0
(1)
zref.sub.i:=z.sup.0
.sup. zref.sub.f:=z
.sup.1
zsam.sub.i:=z
.sup.2
zsam.sub.f:=z
.sup.3
(2)
(20) where Pref.sub.i refers to the initial pressure of the reference cell 302,
(21) Pref.sub.f refers to the final pressure of the reference cell 302,
(22) Psam.sub.i refers to the initial pressure of the sample cell 304,
(23) Psam.sub.f refers to the final pressure of the sample cell 304,
(24) zref.sub.i refers to the initial compressibility factor of the fluid in the reference cell 302,
(25) zref.sub.f refers to the final compressibility factor of the fluid in the reference cell 302,
(26) zsam.sub.i refers to the initial compressibility factor of the fluid in the sample cell 304, and
(27) zsam.sub.f refers to the final compressibility factor of the fluid in the sample cell 304.
(28) The free volume (V.sub.free) of the sample can be calculated in block 403 from the following equation:
(29)
(30) The free volume (V.sub.free) calculated using Equation (3) for each of the nine test runs is shown in the following matrix:
(31)
(32) The free volume of the sample decreases as the volume of the adsorbed test gas increases. When the sample stops adsorbing, the free volume stops changing. For example, as shown in the V.sub.free matrix above, the free volume converges to about 96 cm.sup.3 when the sample stops adsorbing. A graphical representation of the free volume as a function of pressure is shown in
(33) At block 404 the adsorption and storage capacity of the sample can be calculated based on the initial free volume (V.sub.free) calculated in block 403. The following example describes the calculations for determining the adsorption of test gas of the sample and storage capacity of the sample based on the initially determined free volume calculated in block 403. Table 1 lists values that are used in the equations that follow for determining the adsorption of test gas of the sample.
(34) TABLE-US-00001 TABLE 1 Symbol Definition Value T Temperature ( C.) 130.37 Vref Reference Volume (cc) 91.26 W Sample Weight (grams) 214.49 Tsc Temperature at standard 273.15 conditions ( C.) Zsc Compressibility at standard 0.9999 conditions Psc Pressure at standard 14.696 conditions (psia) TC Temperature at current T + 273.15 conditions ( K) Pbar Barometric Pressure 762 (mm/Hg)
(35) Initially, a gas formation volume factor (B.sub.sc) can be calculated as follows:
(36)
(37) Then, a ratio of absolute pressure to compressibility factor (PZ.sub.ratio) can be calculated for each pressure in the pressure matrix as follows:
(38)
(39) Then, the volume adsorbed (V.sub.ads0) for the first pressure point can be calculated in units of cubic centimeters per gram as follows:
(40)
(41) Initially, during the testing, the sample does not contain any adsorbed gas. Thus, the gas content for the first pressure point (GC.sub.0) can be expressed as:
GC.sub.0:=V.sub.ads.sub.
(42) Then, for the additional pressure stages, the volume adsorbed for each pressure point can be added to the gas content previously calculated as follows:
(43)
(44) The gas content (GC) calculated from Equation (8) can then be converted from units of cm.sup.3/gm to units of scf/ton as follows:
GC(scf/ton)=GC(cm.sup.3/gm)32.037.(9)
(45) The matrix of values for the gas content (GC) derived from Equations (4) - (9) for the nine test runs follows:
(46)
(47) The equilibrium pressure in absolute terms (P.sub.eq) can be calculated as follows:
P.sub.eq:=Psam.sub.f+P.sub.bar(10)
The matrix of the values of equilibrium pressure (P.sub.eq) for the nine test runs is:
(48)
(49) A ratio of respective equilibrium pressure to gas content can be calculated as follows:
(50)
(51) The slope (a) and the intercept (b) of a best fit line (least squares) that relates the equilibrium pressure to gas content ratio as a function of pressure can be obtained by the following equation:
(52)
(53) Then the Langmuir coefficients can be determined from the slope and the intercept of the line derived from Equation (12) as follows:
(54)
(55) The Langmuir equation can then be plotted as a function of pressure according to the following equation:
(56)
where the pressure P can be taken from the final pressure values for the sample cell 304 listed in the above pressure matrix.
(57) The Langmuir curve corresponding to the example data is shown in
(58) As noted above, when a sample is pressurized at pressures at or above the pressure at which the storage capacity is maximized, it is assumed that the maximum amount of adsorbed gas is already present on the surface of the sample as a liquid, such that the free volume determined at or above such pressures will actually be inaccurate (i.e., will be too low).
(59) In block 405, this inaccuracy can be corrected by calculating the maximum volume of adsorbed liquid from the maximum storage capacity derived in block 404.
(60) Table 2 lists various values and parameters that are used to determine the maximum volume of adsorbed liquid.
(61) TABLE-US-00002 TABLE 2 Parameter Definition Value for Example sc Total Cumulative Storage 33.8 Capacity (scf/ton) wt Sample Weight (grams) 214.49 .sub.liq Density of liquid phase at 422.37 atmospheric pressure and just below boiling point (kg/m.sup.3) R Universal Gas Constant (J/K) 8.314 P Atmospheric Pressure at standard 1 conditions (atm) T Temperature at standard 293.15 conditions ( K) .sub.molar Molar Density (gm/mol) 16.043 z Compressibility at standard 0.99814 conditions
(62) The gas volume adsorbed at standard conditions (V.sub.st) can be expressed as a function of the maximum storage capacity derived in block 404 (sc) as follows:
V.sub.st=scwt(14)
(63) The number of moles adsorbed (n) can be expressed as follows:
n=PV.sub.st/RTz(15)
(64) The mass adsorbed (m.sub.ads) can be calculated as follows:
m.sub.ads=n.sub.molar(16)
(65) The maximum volume of adsorbed liquid (V) can then be calculated as follows:
V=m.sub.ads/.sub.liq(17)
(66) Thus, from
(67) In block 406, the maximum volume of adsorbed liquid calculated in block 405 (in this example, 0.5 cm.sup.3) is added back to the free volume of the sample calculated in block 403 (in this example, 96 cm.sup.3) to yield an updated free volume (in this example, 96.5 cm.sup.3).
(68) Then, at block 407 the Langmuir curve of Equation (14) can be recalculated based on the updated value of the free volume calculated in block 406 and the pressure data from the test runs. An example of such a recalculated Langmuir curve is shown in
(69) At block 408 the maximum storage capacity derived in block 407 can be compared to the initially determined maximum storage capacity derived in block 404. If the maximum storage capacity derived in block 407 deviates from the initially determined maximum storage capacity derived in block 404 by more than a certain amount, it may be determined that the storage capacity has not been finally determined. In this case, the operation can continue to block 410 where the liquid volume of adsorbed methane can be calculated from the maximum storage capacity derived in block 407 (e.g., using Equations (14)-(17) as described above) and then the operation continues to repeat blocks 406 to 408 to compare the maximum storage capacity derived in block 407 to the maximum storage capacity derived in the previous iteration of block 407. These iterations continue until the value of the storage capacity converges (e.g., the value does not change more than a predetermined percentage between iterations). As the value of the storage capacity converges, the value of the free volume also converges. In this case, the free volume for this fully converged storage capacity can be equated to the free volume of the sample. At this point, the process can end as shown.
(70) As shown in
(71) There have been described and illustrated herein several embodiments of a method of determining storage capacity and free volume. While particular embodiments have been described, it is not intended that the invention be limited thereto, as it is intended that the invention be as broad in scope as the art will allow and that the specification be read likewise. Thus, while a particular ordering of operations has been disclosed, it will be appreciated that other orderings may be performed as well. Moreover, while particular test apparatus configurations have been disclosed in reference to a workflow, it will be appreciated that other configurations could be used as well. It will therefore be appreciated by those skilled in the art that yet other modifications could be made to the disclosed embodiments without deviating from its scope as claimed.