HELP: Quantitative Analysis Equations - Gas DST

NOTE: Much of this web page is taken from the lecture notes "Modern Concepts in Drillstem Testing Part 2 Quantitative Analysis"2 by Hugh W. Read, Author & Instructor.

Conventional Horner Type Pressure Buildup Analysis Conditions Assumed for Analysis Procedure

For a disccussion of the theory of pressure buildup interpretaton and the derivation of the pertinent equations the reader is referred to the original now classical paper by Horner(1).

90% of all quantitative Drill Stem Test analysis is based on Horner's method of analysis which assumes the following ideal conditions:

i) Radial flow
Radial flow is flow into the well bore equally from all directions in the formation. By and large condition is met by most DST's through linear systems such as fractures, narrow channel sands etc. are obvious exceptsion which may be handled separately.

ii) a homogeneous reservoir
Homogeneity in a reservoir denotes constant characteristics throughout the length and thickness. Any values calculated from test data then becomes averages over the length and/or thickness.

iii) "steady-state" conditions of flow
"Steady-state" flow condiitions imply a rate and pressure drawdown (which is responsible for the flow) which is constant.

iv) infinite reservoir
An infinite reservoir is one in which there are no finite limits or depletion. All DST's in wildcat wells can be considered to test infinite reservoirs, except those testing very small local porosity or fracture developments which in any event deplete rapidly and are not commercial.

v) single phase flow
Single phase flow assumes that only one phase is entering the well bore. Thus for example any gas produced with oil is considered as solution gas and any liquids in a gas test are considered as condensation of gases in the pipe or immediate well bore vicinity.

Method of Construction of Horner plot - Gas Drill Stem Test

This example is from the Xit 1; DST 1 in the Upper Kearny Member from 5690.0 ft to 5745.0 ft dst-gas.las. The Gas Rates and Pressure Summary Data will be needed in performing the plot and quantitative analysis and is listed as follows,

Gas Rates Table
FlowElapsedPressureGas RateChoke
PeriodTime(psig)(Mcf/day)(in)
110.014.0577000.01.0
120.024.0817000.01.0
130.028.0907000.01.0
210.026.0865000.01.0
220.033.01012000.01.0
230.035.01057000.01.0
240.036.01076000.01.0
250.036.01076000.01.0
260.037.01098000.01.0
Pressure Summary Table
TimePressureTemperatureAnnotation
(min)(psig)(deg F)
0.02748.7854122.407204Initial Hydrostatic
5.5155.137894123.1147Open to Flow 1
36.0496.501312121.527901Shut-in 1
96.0853.742798126.989899End Shut-in 1
97.0233.796402126.3834Open to Flow 2
156.5435.617401115.143501Shut-in 2
280.0850.436829125.351997End Shut-in 2
285.52727.0625126.5923Final Hydrostatic

See the paper "Recent Developments in the Interpretation and Application of DST Data" by L.F.Maier(3). There were a number of DST papers that seem to use the Pressure squared method. Reid suggests that the linear Horner plot was sufficient. A future version of the DST Tool may allow the user to select between Pressure or Pressure squared in a Horner plot analysis.

(1) The data necessary for this plot is a set of detailed readings of pressures and times during each shut in period plus the total amount of time spent flowing the well.

(2) Arrange the data in tablular form where,

T = Cumulative flowing time (minutes)
ΔT = Times during shut in that each pressure is read (minutes)
P = Pressure read during shut in time (psig)
P2 = Pressure squared (psig2)

Shut In 1 (Initial)
Total Flow Time (T) = 30 minutesa
Time (ΔT)(T+ΔT)/ΔTPressure (P)TemperaturePressure squared (P2)
(min)(psig)(deg F)(psig2)
0.0---496.501312121.527901246,512.25
4.08.50841.170715125.614502707,566.97
8.04.75844.496826126.780701713,180.25
12.03.50846.328003126.656998716,274.47
16.02.88847.812927126.512199718,781.80
20.02.50848.991882126.430603720,784.02
24.02.25849.629028126.429497721,871.14
28.01.07850.446777126.441704723,265.20
32.01.94850.998596126.487801724,201.00
36.01.83851.615723126.541397725,256.62
40.01.75851.901672126.6035725,733.61
44.01.68852.340271126.679298726483.48
48.01.63852.739502126.757896727,165.51
52.01.57853.130676126.837502727,830.80
56.01.54853.542114126.921898728,530.53
60.01.50853.742798126.989899728,871.99
Shut In 2 (Final)
Total Flow Time (T) = 59.25 + 30 = 89.25 minutesb
Time (ΔT)(T+ΔT)/ΔTPressure (P)TemperaturePressure squared (P2)
(min)(psig)(deg F)(psig2)
0.0---435.617401115.143501189,764.78
4.023.31825.081787119.8134680,757.01
8.012.16830.118713121.163101689,099.21
12.08.44833.033508121.227501693,938.98
16.06.68835.235901121.179703697,625.86
20.05.46837.006775121.144402700,585.74
24.04.72838.476685121.177597703,048.71
28.04.19839.725891121.214996705,146.47
32.03.79840.914917121.298103707,129.63
36.03.48841.682373121.412399708,425.22
40.03.23842.520203121.562202709,839.95
44.03.03843.182373121.730797710,952.51
48.02.86844.06543121.915604712,454.16
52.02.72844.552002122.107803713,264.70
56.02.59844.938416122.306713,923.60
60.02.49845.54541122.5158714,954.80
64.02.39846.011902122.712097715,732.92
68.02.31846.609009122.936401716,748.49
72.02.24846.955078123.124702717,341.24
76.02.17847.331421123.330902717,968.13
80.02.12847.858093123.534203718,866.58
84.02.06848.078918123.712997719,239.69
88.02.01848.460205123.904503719,884.37
92.01.97848.756104124.090897720,393.54
96.01.93848.997009124.264297720,801.00
100.01.89849.177612124.4431721,106.67
104.01.86849.583923124.618301721,786.18
108.01.83849.724426124.773598722,024.08
112.01.80850.115723124.930603722,704.01
116.01.77850.256226125.089798722,942.07
120.01.74850.521973125.233299723,384.27
124.01.72850.436829125.351997723,231.18
From the Pressure Summary Table
(a) Shut-in 1 Time - Open to Flow 1 Time { 38.5 - 8.5 = 30.0 minutes }
(b) Shut-in 2 Time - Open to Flow 2 Time + Total Flow Time from (a) { 159.0 - 99.75 + 30.0 = 89.25 minutes }

In the table note that the Shut In 1 & 2 periods were broken down into 4 minute intervals.

The Pressure Summary Table gives a summary of the DST Pressure-Temperature-Time Readings at specific points. This DST had a 30.0 minute preflow and a 59.25 minute main flow. Thus 'T' for the Shut In 1 (Initial) period = 30.0 minutes since there was a total of 30 minutes flow time prior to Shut In 1 (Initial). T for the Shut In 2 (Final) period becomes 89.25 minutes ( 30 minutes preflow + 59.25 minutes mainflow since T is the cumulative flow time prior to shut in.

The quantity (T + ΔT)/ΔT is mathematically the same as 1 + (T/&DeltaT) thus for the Shut In 2 (Final) period example the (T + ΔT)/ΔT for the first increment = (89.25+4)/4 = 23.31, which is the same as 1 + (89.25/4) = 1 + 22.31 = 23.31.

(3) The Horner plot is then constructed by plotting log10[(T+ΔT)/ΔT] vs P2 for each point.


Figure 2. Horner Plot for Gas DST

(4) In Figure 2 both Shut In Pressure-Time curves have been plotted. In order to determine the static reservoir pressure the linear portion is extrapolated to the left hand margin where the value of the time function (T + ΔT)/ΔT = 1. Since the logarithm of 1 is zero the log10[(T + ΔT)/ΔT ] = 0 (or infinity) at this point. Thus we are extrapolating the Horner straight line to a 'infinite' shut in time where completely static pressure prevails. In the example here the static pressure squared ~ 738,000.0 psig2 or 859.0 psig. Both Shut In intervals extrapolations yield this value. In cases where the Shut In 2 (Final) extrapolation is substantially less than the Shut In 1 (Initial) depletion is indicated. ( If the depletion factor 100.0 * Shut In [(Initial)-(Final))/(Initial) ] is greater than 4%, then the idications of depletion can be considered serious or sustantial.

(5) The final piece of information which is obtained form the Horner plot is the "slope" (m) of the striaght line segment. Numerically this is the difference between the pressure at log10[(T + ΔT)/ΔT ]=0 and at log10[(T + ΔT)/ΔT ]=1. where the slope is simply the change in pressure over one complete log cycle. The slope in this example using the Shut In (Final) slope m=0.061 psi2/cycle. The slope is used in the calculations to derive permeability and other reservoir parameters.

Transmissibility (K*h/μ), Permeability Thickness (K*h), Permeability (K)

The pressure build-up equation applicable to gas wells is expressed by

Po2 = Pf2 - mg * log10[(T+ΔT)/ΔT].

The build-up plot of Po2 vs. log10[(T+ΔT)/ΔT] is constructed and extrapolated to log10[ (T+ΔT)/ΔT ] to zero to obtain Pf2 and mg, the slope of the line.

mg = 1632 * qg * μ * Z * Tf / (K * h) [psi2] / [log cycle]
qg = flow rate [Mcf] / [day]
μ = viscosity [cp]
Z = Gas Deviation Factor ( Compressibility factor)
Tf = Formation Temperature [oR]; oR = oF + 459.67
h = vertical thickness of continuous porosity [ft]
K = average effective permeability [md]

This states that the slope of the buildup is representative of a given fluid having physical properties μ, Z, Tf flowing at a rate qg through a formation having physical properties K * h.

Note: the flow rate (q) is computed by using an average of the final gas rates in the gas rates table.

Transmissibility can be found my rearranging the slope as follows,

Transmissibility: K * h / μ = 162.6 * q * B / m [md]-[ft]/[cp]
Permeability Thickness: K * h = ( Transmissibility ) * μ [md]-[ft]
Permeability: K = ( Permeability Thickness ) / h [md]

Damage Ratio (DR), Skin factor (S), and related quantities

Damage Ratio (DR) - A numerical value used to predict the flow rate if the damage were removed. In essence the DR becomes a number which when multiplied by the flow rate which existed at the time of the test will yield the flow rate if the damage (or improvement) over the natural condition is removed. This flow rate will be the rate at the same flowing pressure drawdown which existed during the test. From the definition of DR if a zone is neither damaged nor improved then q theoretical is identical to q actual and DR = 1.

Pi2 - Pwf2
DR = ------------------------------------------------ - 2.85
mg * log { [ k * To / ( φ * μ * c * rw2 ) ] }

where,

Pi = Initial static reservoir pressure [psig]
Pwf = Bottom Hole Flowing Pressure (FFP) [psig]
mg = slope from the Horner plot [psi] / [log cycle]
K = Permeability ( K ) [md]
To = Flow Time [min]
φ = Porosity
μ = viscosity [cp]
c = compressibility [vol]/[vol]/[psi]
rw = well bore radius [ft]

If K, φ, μ, c and rw are not known then the Damage Ratio can be estimated by,
Pi2 - Pwf2
EDR = ----------------- + 2.65
mg * log { To }

Skin factor (S) - A numerical quantity which attempts to describe the amount of damage or improvement. The numerical value of skin is so defined that a positive value for the skin factor indicates a damaged condition and a negative skin factor indicates improvement over the natural condition. The skin factor is zero when neither skin damage nor improvement are present i.e. no alterations to natural condition.
- -
|Pi2 - Pwf2 K * To |
S = 1.1515 * |-------------- - log------------------ + 5.01|
| mg φ * μ * c * rw2|
- -
Pi = Initial static reservoir pressure [psig]
Pwf = Bottom Hole Flowing Pressure (FFP) [psig]
mg = slope from the Horner plot [psi] / [log cycle]
K = Permeability ( K ) [md]
To = Flow Time [min]
φ = Porosity
μ = viscosity [cp]
c = compressibility [vol]/[vol]/[psi]
rw = well bore radius [ft]

If φ, μ, c and rw are not known then the Skin factor (S) can be estimated by,
- -
|Pi2 - Pwf2 |
S = 1.1515 * |----------- - log(K * To * Pi) + 1.40|
| mg |
- -

Pressure Drop Across a Damage Zone ΔPskin The additional pressure drop during flow caused by the presence of skin (ΔPskin) may be calculated as follows,

ΔPskin = - Pwf + √( Pwf2 + 0.87 * S * m )

where,

S = Skin factor
Pwf = Bottom Hole Flowing Pressure (FFP) [psig]
m = slope from the Horner plot [psi] / [log cycle]

Radius of Investigation (RI) The radius of investigation is the radial distance from the well bore which the pressure disturbance from the DST has investigated ( in other words "how far out into the zone the DST has looked").

RI = 2.6408 * √( K*To / ( φ * μ * c ) )

where,

Pi = Initial static reservoir pressure [psig]
K = Permeability ( K ) [md]
To = Flow Time [min]
φ = Porosity
μ = viscosity [cp]
c = compressibility [vol]/[vol]/[psi]

If φ, μ, and c are not known then the Radius of Investigation (RI) is as follows,

For Gas: RI = 0.125 * √( K * Tf * Pi )

Effects of Turbulence(2) The skin factor and damage ratio values computed from the preceding equations do not take account of the additional pressure drop which is caused by turbulence in gas flow. The turbulence factor is not easy to determine precisely in DST's, however, an approximate empirical relationship between turbulence and permeability has been determined.

Step 1 The flowing pressure corrected for turbulence (Pwfc) is computed as follows,

- - --
| 0.129 * G * Tf * Z * q2 |1 1 ||
Pwfc = √|(Pwf + 14.65)2+----------------------------*|-----||
| K4/3 * h 2 |rw RI||
- - --
Pwf = Bottom Hole Flowing Pressure (FFP) [psig]
G = Gas Specific Gravity (air = 1)
Tf = Formation Temperature [oR]; oR = oF + 459.67
Z = Gas Deviation Factor ( Compressibility factor)
q = Flow Rate - [ Mcf ] / [ Day ]
K = Permeability [md]
h = thickness [ft]
rw = well bore radius [ft]
RI = Radius of Investigation [ft]

Step 2 The value of (Pwfc) is then substituted for (Pwf) in the skin factor (S) and damage ratio (DR) equations to determine the true skin factor (S) and damage ratio (DR) to exclude the effects of turbulence.

Step 3 The pressure drop due to turbulence (ΔPt) may also be of interest and may be calculated simply as,

ΔPt = - Pwf + √( Pwf2 + 0.87 * mg * S )

Absolute Open Flow Capacity (qAOF) A theorectical quantity which describes the maximum flow rate of a gas zone at zero sandface pressure. It is an unattainable rate in practice but from it may be derived the flow rates at any practical flowing pressure.

Houpert equation: Pi*Pi - Pwf*Pwf = a*q + b*q*q, where

1424 * Tf * Z
a (Laminar Flow) = ------------------* ( ln(re/rw) - 0.75 + S )
(K * h / μ)
0.129 * G * Tf * Z
b (turbulence factor) = ------------------------* ln ( (1/rw) - (1/re) )
K4/3 * h2

Pwf = 0 by definition
-a + √( a * a + 4 * b * Pi * Pi )
qAOF=----------------------------------------
2 * b
Pi = Initial static reservoir pressure [psig]
Pwf = Bottom Hole Flowing Pressure (FFP) [psig]
K = Permeability ( K ) [md]
h = vertical thickness of continuous porosity [ft]
μ = viscosity [cp]
Z = Gas Deviation Factor ( Compressibility factor)
Tf = Formation Temperature [oR]; oR = oF + 459.67
G = Gas Specific Gravity (air = 1)
re = drainage radius [ft]
rw = well bore radius [ft]

If b = 0 then qAOF = Pi * Pi / a

References:
(1) Pressure Build-Up in Wells, by D.R. Horner, 3rd World Petroleum Congress, May 28 - June 6, 1951 , The Hague, the Netherlands http://www.onepetro.org/mslib/servlet/onepetropreview?id=WPC-4135&soc=WPC
(2) Drillstem Test Interpretation Seminar, Author & Instructor: H.W.Reid
(3) Recent Developments in the Interpretation and Application of DST Data, by L.F.Maier Journal of Petroleum Technology Volume 14, Number 11, November 1962, pgs 1213-1222 http://www.onepetro.org/mslib/servlet/onepetropreview?id=00000290