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Equations: Inflow and lift: nodal analysis

The equations of the “Inflow and lift: nodal analysis” lessons in “Oil and gas production”, with their conditions and units, and what each symbol means in them.

Pressure budget of the production system
pˉR−psep=Δpres+Δpcomp+Δptbg+Δpchoke+Δpline\bar p_R - p_{sep} = \Delta p_{\text{res}} + \Delta p_{\text{comp}} + \Delta p_{\text{tbg}} + \Delta p_{\text{choke}} + \Delta p_{\text{line}}

any pressure unit, the same for all terms

Holds when: Steady state (nothing changes with time): the same flow passes through every element, with the volumes given at the same conditions. Each term depends on the rate and on the fluid properties. So the equality holds at only one rate: the operating rate. The weight of the fluid column counts as part of the tubing loss. In a vertical well it is usually the largest term.

Nodal analysis of the production system →
Inflow curve to the node
pnode=pˉR−Δpup(q)p_{node} = \bar p_R - \Delta p_{\text{up}}(q)

any consistent units of pressure and rate

Holds when: Steady state: the reservoir pressure does not change during the calculation. All rates are given at the same conditions.

Nodal analysis of the production system →
Outflow curve from the node
pnode=psep+Δpdown(q)p_{node} = p_{sep} + \Delta p_{\text{down}}(q)

any consistent units of pressure and rate

Holds when: The separator pressure is held constant. The losses in each element are worked out for the real composition of the flow: gas, oil and water.

Nodal analysis of the production system →
Outflow curve for liquid without gas in vertical tubing
pwf=pwh+ρgH+λ Hd ρv22,v=4qπd2p_{wf} = p_{wh} + \rho g H + \lambda\,\frac{H}{d}\,\frac{\rho v^2}{2},\qquad v = \frac{4q}{\pi d^2}

SI

Holds when: Single-phase incompressible liquid (its volume does not change with pressure): the pressure along the whole length of the tubing is above the bubble point pressure, and there is no free gas. Vertical tubing of constant diameter. In a deviated (slanted) well, the weight of the column uses the true vertical depth, and friction uses the length along the hole. The density and the friction factor are constant. Speeding up of the flow is ignored. The flow is turbulent (swirling, not smooth): the Reynolds number Re=ρvd/μRe = \rho v d/\mu is above a few thousand. λ\lambda depends on ReRe and on how rough the pipe wall is. English-language literature also uses the Fanning friction factor, which is four times smaller: fF=λ/4f_F = \lambda/4.

Nodal analysis of the production system →
Condition for a stable operating point (quasi-static)
 dpout dq> dpin dq\frac{\dd p_{\text{out}}}{\dd q} > \frac{\dd p_{\text{in}}}{\dd q}

any consistent units

Holds when: A simplified quasi-static treatment (each state is taken as if the flow had time to settle): the inertia of the flow and the compressibility of the gas in the wellbore are ignored. Real swings of the operating mode (for example, repeated surges of gas and liquid) are studied with dynamic models.

Nodal analysis of the production system →
Productivity index
J=qpˉR−pwfJ = \frac{q}{\bar p_R - p_{wf}}

metric oilfield units (m³/d, MPa)

Holds when: Stabilised flow. Single-phase inflow: pwf≥pbp_{wf} \ge p_b. The pressures are converted to the same depth. For a difference, absolute pressure (measured from zero) and gauge pressure (measured above atmospheric pressure) work equally well, as long as both are of the same kind.

Inflow performance relationship (IPR) →
Inflow to a well in pseudo-steady state
q=2πkh (pˉR−pwf)μB[ln⁡rerw−34+S]q = \frac{2\pi k h\,(\bar p_R - p_{wf})}{\mu B\left[\ln\dfrac{r_e}{r_w} - \dfrac{3}{4} + S\right]}

SI

Holds when: Pseudo-steady state in a circular drainage area with a closed (impermeable) outer boundary and the well at the centre. For an area of another shape, the term ln⁡(re/rw)−3/4\ln(r_e/r_w) - 3/4 is replaced by an expression with a shape factor. Single-phase inflow of a slightly compressible liquid, by Darcy's law. A uniform reservoir (the same properties everywhere). Imperfect penetration (the well does not open the whole pay thickness) and damage to the near-wellbore zone are included in SS.

Inflow performance relationship (IPR) →
Vogel's equation
qqmax=1−0.2 pwfpˉR−0.8(pwfpˉR)2\frac{q}{q_{max}} = 1 - 0.2\,\frac{p_{wf}}{\bar p_R} - 0.8\left(\frac{p_{wf}}{\bar p_R}\right)^2

dimensionless form: the rates in any one unit, and the pressures likewise

Holds when: The reservoir pressure is not above the bubble point pressure (pˉR≤pb\bar p_R \le p_b); solution gas drive. Stabilised inflow. The equation is an empirical generalisation (a rule drawn from many calculated cases) of results for wells with an undamaged near-wellbore zone (S=0S = 0). Low water cut (little water in the produced liquid). With a gas cap (a layer of free gas above the oil), a high water cut or high-viscosity oil, the accuracy is lower. It is better to take absolute pressures. At reservoir pressures of tens of megapascals, the difference from gauge pressures is small.

Inflow performance relationship (IPR) →
Composite IPR
q={J (pˉR−pwf),pwf≥pb,qb+Jpb1.8[1−0.2 pwfpb−0.8(pwfpb)2],pwf<pb,qb=J (pˉR−pb)q = \begin{cases} J\,(\bar p_R - p_{wf}), & p_{wf} \ge p_b,\\[6pt] q_b + \dfrac{J p_b}{1.8}\left[1 - 0.2\,\dfrac{p_{wf}}{p_b} - 0.8\left(\dfrac{p_{wf}}{p_b}\right)^2\right], & p_{wf} < p_b, \end{cases}\qquad q_b = J\,(\bar p_R - p_b)

any consistent units (for example, m³/d and MPa)

Holds when: pˉR>pb\bar p_R > p_b: above the bubble point pressure the inflow is single-phase. Below the bubble point pressure the curve is of the Vogel type, but it is built from pbp_b, not from the reservoir pressure. Stabilised flow. The effect of the near-wellbore zone is included in JJ.

Inflow performance relationship (IPR) →
Productivity index from a test below the bubble point pressure
J=q1(pˉR−pb)+pb1.8[1−0.2 pwf,1pb−0.8(pwf,1pb)2]J = \frac{q_1}{(\bar p_R - p_b) + \dfrac{p_b}{1.8}\left[1 - 0.2\,\dfrac{p_{wf,1}}{p_b} - 0.8\left(\dfrac{p_{wf,1}}{p_b}\right)^2\right]}

as for the composite curve

Holds when: The same as for the composite curve. The bubble point pressure is known from a PVT study of an oil sample.

Inflow performance relationship (IPR) →
Fetkovich's inflow equation
q=C (pˉR2−pwf2)nq = C\,(\bar p_R^2 - p_{wf}^2)^n

qq in m³/d, pressures in MPa (absolute)

Holds when: Stabilised rates (a flow-after-flow test: one stable rate after another) or isochronal rates (every rate held for the same time). The pressures are absolute. The formula contains their squares, and a difference of squares of gauge pressures is not equal to a difference of squares of absolute ones. The reservoir pressure is not above the bubble point pressure. If it is above, the formula describes only the part of the curve below pbp_b.

Inflow performance relationship (IPR) →
Gas inflow equation with an exponent
qg=C (pˉR2−pwf2)nq_g = C\,(\bar p_R^2 - p_{wf}^2)^n

qgq_g in thousand m³/d, pressures in MPa (absolute)

Holds when: Stabilised or isochronal rates. Absolute pressures. An empirical relationship: extrapolation far beyond the tested drawdowns is unreliable.

Inflow performance relationship (IPR) →
Two-term gas inflow equation
pˉR2−pwf2=a qg+b qg2\bar p_R^2 - p_{wf}^2 = a\,q_g + b\,q_g^2

pressures in MPa (absolute), qgq_g in thousand m³/d

Holds when: Stabilised rates. aa and bb are found from a test at several rates: the dependence of (pˉR2−pwf2)/qg(\bar p_R^2 - p_{wf}^2)/q_g on qgq_g is a straight line with slope bb and intercept aa on the ordinate axis.

Inflow performance relationship (IPR) →
Flow efficiency
FE=pˉR−pwf−ΔpSpˉR−pwf=JactualJidealFE = \frac{\bar p_R - p_{wf} - \Delta p_S}{\bar p_R - p_{wf}} = \frac{J_{\text{actual}}}{J_{\text{ideal}}}

dimensionless; the pressures in the same units

Holds when: Single-phase inflow, stabilised flow. The additional pressure loss is proportional to the rate (the skin factor does not depend on the rate).

Inflow performance relationship (IPR) →
Productivity index at zero drawdown
J∗=1.8 qmaxpˉR=1.8 J1+0.8 pwf/pˉRJ^* = \frac{1.8\,q_{max}}{\bar p_R} = \frac{1.8\,J}{1 + 0.8\,p_{wf}/\bar p_R}

any consistent units

Holds when: The shape of the curve is of the Vogel type (pˉR≤pb\bar p_R \le p_b).

Inflow performance relationship (IPR) →
Conversion to a future reservoir pressure
Jf∗=Jp∗ (kro/μoBo)f(kro/μoBo)p,qmax,f=Jf∗ pˉR,f1.8J^*_f = J^*_p\,\frac{\left(k_{ro}/\mu_o B_o\right)_f}{\left(k_{ro}/\mu_o B_o\right)_p},\qquad q_{max,f} = \frac{J^*_f\,\bar p_{R,f}}{1.8}

the ratio is dimensionless; J∗J^* and qmaxq_{max} are in the units of the current curve

Holds when: The shape of the curve will also be of the Vogel type in the future. krok_{ro} comes from the saturation forecast (material balance, an accounting of the fluids in the reservoir) and the relative permeability curves. μo\mu_o and BoB_o come from PVT data at the future pressure. The properties of the near-wellbore zone do not change.

Inflow performance relationship (IPR) →
Vogel's equation with the flow efficiency of the well
qqmaxFE=1=1.8 FE(1−pwfpˉR)−0.8 FE2(1−pwfpˉR)2\frac{q}{q_{max}^{FE=1}} = 1.8\,FE\left(1 - \frac{p_{wf}}{\bar p_R}\right) - 0.8\,FE^2\left(1 - \frac{p_{wf}}{\bar p_R}\right)^2

dimensionless form

Holds when: A Vogel-type inflow for an undamaged well. The additional pressure loss in the near-wellbore zone is proportional to the rate. At FE>1FE > 1 the formula applies as long as pwf′≥0p'_{wf} \ge 0, that is, at pwf≥pˉR (1−1/FE)p_{wf} \ge \bar p_R\,(1 - 1/FE). Below that it gives a physically meaningless result.

Inflow performance relationship (IPR) →
Pressure gradient in upward multiphase flow
 dp dz=ρs gcos⁡θ+λ ρns vm22d+( dp dz)acc\frac{\dd p}{\dd z} = \rho_s\,g\cos\theta + \lambda\,\frac{\rho_{ns}\,v_m^{2}}{2d} + \left(\frac{\dd p}{\dd z}\right)_{\text{acc}}

SI: the gradient in Pa/m; 1 kPa/m = 0.0442 psi/ft

Holds when: Steady upward flow in a pipe of constant cross-section. The properties of the phases and the velocities are taken at the average pressure and temperature of a section. That is why the pipe is calculated in short sections. Friction is written in the simplest, homogeneous form (the mixture is treated as uniform): from the no-slip density and the velocity of the mixture. Different methods define the density and the friction factor in different ways. The acceleration component usually does not exceed a few per cent. It matters only at high gas velocities near the wellhead.

Multiphase flow in tubing →
Mixture density with and without slip
ρs=ρLHL+ρG (1−HL),ρns=ρLλL+ρG (1−λL)\rho_s = \rho_L H_L + \rho_G\,(1 - H_L), \qquad \rho_{ns} = \rho_L \lambda_L + \rho_G\,(1 - \lambda_L)

kg/m³; the fractions are dimensionless

Holds when: The liquid density is the average of the oil and water densities, weighted by their volumes at tubing conditions. Within a section the phases are mixed well enough that the density can be averaged by volume.

Multiphase flow in tubing →
Drift-flux model for upward flow
vG=C0 vm+vd  ⇒  1−HL=vSGC0 vm+vd,vd≈0.35g d (ρL−ρG)ρLv_G = C_0\,v_m + v_d \;\Rightarrow\; 1 - H_L = \frac{v_{SG}}{C_0\,v_m + v_d}, \qquad v_d \approx 0.35\sqrt{\frac{g\,d\,(\rho_L - \rho_G)}{\rho_L}}

SI

Holds when: Upward bubble or slug flow in a vertical pipe. The model does not suit annular flow, and it overestimates the liquid holdup there. C0C_0 and the coefficient 0.35 are empirical constants (found from experiments). The formula for vdv_d describes the rise of large bubbles that fill almost the whole cross-section. Small bubbles rise more slowly: in water at about 0.2–0.25 m/s. In inclined pipes the drift velocity depends on the angle.

Multiphase flow in tubing →
Gradient including acceleration
 dp dz=ρsgcos⁡θ+λ ρnsvm2/(2d)1−Ek,Ek=ρns vm vSGp\frac{\dd p}{\dd z} = \frac{\rho_s g\cos\theta + \lambda\,\rho_{ns} v_m^{2}/(2d)}{1 - E_k}, \qquad E_k = \frac{\rho_{ns}\,v_m\,v_{SG}}{p}

SI

Holds when: The gas expands isothermally, and its volume is inversely proportional to the pressure. The liquid is incompressible (its volume does not change with pressure), and the mass flow rate of the mixture is constant along the length. The momentum flux is calculated for the homogeneous mixture — without slip of the phases.

Multiphase flow in tubing →
Darcy friction factor in turbulent flow (the Haaland formula)
1λ=−1.8 log⁡10 ⁣[(ε/d3.7)1.11+6.9Re]\frac{1}{\sqrt{\lambda}} = -1.8\,\log_{10}\!\left[\left(\frac{\varepsilon/d}{3.7}\right)^{1.11} + \frac{6.9}{Re}\right]

dimensionless quantities; ε\varepsilon and dd in the same units

Holds when: Turbulent flow, ReRe greater than about 4000. The formula approximates the implicit Colebrook–White equation (one that must be solved by trial) with an error of the order of 1–2%.

Multiphase flow in tubing →
Critical pressure ratio for a gas
rc=(p2p1)c=(2k+1)kk−1r_c = \left(\frac{p_2}{p_1}\right)_c = \left(\frac{2}{k+1}\right)^{\frac{k}{k-1}}

dimensionless

Holds when: An ideal gas, expansion without heat exchange or friction (isentropic); kk is constant. The velocity of the gas upstream of the choke is small compared with the velocity in the narrowest part. At p2/p1≤rcp_2/p_1 \le r_c the flow is critical and the flow rate does not depend on p2p_2. At p2/p1>rcp_2/p_1 > r_c it is subcritical.

Chokes, surface pressure losses and well temperature →
Gas flow rate through a choke
m˙=CdA2kk−1 p1ρ1[r2/k−r(k+1)/k],r=max⁡ ⁣(p2p1, rc)\dot m = C_d A \sqrt{\frac{2k}{k-1}\,p_1 \rho_1 \left[r^{2/k} - r^{(k+1)/k}\right]},\qquad r = \max\!\left(\frac{p_2}{p_1},\ r_c\right)

SI

Holds when: Isentropic expansion of an ideal gas, corrected for the gas deviation factor at the conditions upstream of the choke; kk is constant. The velocity of the gas upstream of the choke is small (the orifice is much smaller than the pipe); there is no liquid in the flow. Below the critical ratio, put rcr_c into the formula. The flow rate then does not depend on the pressure downstream of the choke.

Chokes, surface pressure losses and well temperature →
Liquid flow rate through a choke
q=CdA2 (p1−p2)ρq = C_d A \sqrt{\frac{2\,(p_1 - p_2)}{\rho}}

SI

Holds when: An incompressible single-phase liquid. The pressure in the contracted section is above the pressure at which it boils or releases gas. The velocity upstream of the orifice is small compared with the velocity in it. If the orifice is close in size to the pipe, divide the flow rate by 1−(d/D)4\sqrt{1 - (d/D)^4}. CdC_d is empirical (found from experiments). In classical hydraulics it is about 0.6 for an orifice in a thin wall and about 0.8 for a short cylindrical nozzle. For a particular choke the manufacturer gives it.

Chokes, surface pressure losses and well temperature →
Gilbert-type correlations (critical flow)
pwh=b q GLR cSap_{wh} = \frac{b\,q\,\text{GLR}^{\,c}}{S^{a}}

oilfield units: psig, STB/d, scf/STB, 1/64″

Holds when: Critical flow only. The pressure downstream of the choke is no more than about 0.5–0.6 of the pressure upstream (for Gilbert, less than 1/1.7 ≈ 0.59). The constants come from measurements in particular fields and with particular beans. Outside these conditions the accuracy falls, so check the correlation against rate measurements. In Gilbert's original the constant is 435, with the GLR in thousands of cubic feet per barrel (Mscf/bbl). This is the same formula: 10.0⋅10000.546≈43510.0\cdot 1000^{0.546} \approx 435. Different publications give the pressure as gauge or as absolute. At pressures of a few megapascals the difference is one to three per cent.

Chokes, surface pressure losses and well temperature →
Equivalent diameter of two parallel lines
deq=(d12.5+d22.5)0.4d_{\text{eq}} = \left(d_1^{2.5} + d_2^{2.5}\right)^{0.4}

any identical units of length

Holds when: Single-phase turbulent flow with the same friction factor in both lines. The lines have equal length between common points. For a gas–liquid mixture this is only an estimate. The phases need not divide between the lines in the same proportion, and the real gain is sometimes smaller than the calculated one.

Chokes, surface pressure losses and well temperature →
Relaxation distance (Ramey's method)
A=w cp (ke+rUf)2π rU keA = \frac{w\,c_p\,(k_e + r U f)}{2\pi\,r U\,k_e}

SI

Holds when: Steady flow in the wellbore. Heat capacity and thermal conductivities are constant. The heat resistances of the well design do not change with depth. The rocks are uniform. Far from the well the temperature equals the geothermal one. Not included: cooling of the gas as it expands, the work of the gas against gravity, and heating by friction. For an oil well the corrections are usually small, but because of the gas the flow is in fact slightly colder than calculated. For a gas well they are significant (see the advanced section).

Chokes, surface pressure losses and well temperature →
Flow temperature in a producing well
Tf(z)=T0+GTz+GTA[1−e−(H−z)/A]T_f(z) = T_0 + G_T z + G_T A\left[1 - e^{-(H - z)/A}\right]

any consistent units (°C and m)

Holds when: A vertical well and a linear geothermal gradient. The fluid enters the well at the reservoir temperature. The same assumptions as for the relaxation distance.

Chokes, surface pressure losses and well temperature →
Time function at large times
f(t)≈12ln⁡(4tD)−γE2,tD=α trwb2f(t) \approx \tfrac{1}{2}\ln\left(4 t_D\right) - \tfrac{\gamma_E}{2},\qquad t_D = \frac{\alpha\,t}{r_{wb}^{2}}

dimensionless

Holds when: Large dimensionless times, which in practice means after the first days or weeks of operation. This is the same line-source asymptotic formula (the long-time approximation) as in reservoir flow (Line-source solution and the pressure function). At small times the long-time formula underestimates ff and so overestimates the heat loss. The calculated flow temperature is then lower than the true one. For small times use the full time function, for example the approximation of Hasan and Kabir, which is valid for all times.

Chokes, surface pressure losses and well temperature →
Temperature downstream of the choke
T2≈T1−μˉJT (p1−p2),μJT=(∂T∂p)hT_2 \approx T_1 - \bar\mu_{JT}\,(p_1 - p_2),\qquad \mu_{JT} = \left(\frac{\partial T}{\partial p}\right)_{h}

°C and MPa

Holds when: Throttling without heat exchange with the surroundings. The kinetic energy before and after the choke is small, so the enthalpy is constant. The coefficient varies with pressure and temperature. At large pressure drops it is more accurate to calculate with an equation of state, keeping the enthalpy constant. For a gas with liquid, also allow for the heat capacity of the liquid.

Chokes, surface pressure losses and well temperature →
Hydrate formation temperature of a sweet natural gas (Towler and Mokhatab)
Th=13.47ln⁡p+34.27ln⁡γg−1.675ln⁡p ln⁡γg−20.35T_h = 13.47\ln p + 34.27\ln\gamma_{\text{g}} - 1.675\ln p\,\ln\gamma_{\text{g}} - 20.35

oilfield: ThT_h in °F, pp in psia; degrees Celsius are (Th−32)/1.8(T_h - 32)/1.8, pressure in psia is the pressure in MPa multiplied by 145.04

Holds when: A sweet natural gas (without appreciable hydrogen sulfide or carbon dioxide) with a specific gravity of about 0.55–1.0, in the presence of fresh water. The formula reproduces the chart by gas specific gravity. But gases of the same density and different composition may form hydrates under clearly different conditions (for a gas close to pure methane the estimate is too high by several degrees). Salts in the water and inhibitors lower the hydrate formation temperature. For design decisions, calculate from the composition.

Chokes, surface pressure losses and well temperature →
Speed of sound in a uniform gas–liquid mixture (Wood's formula)
1ρmcm2=αρGcG2+1−αρLcL2,ρm=αρG+(1−α)ρL\frac{1}{\rho_m c_m^{2}} = \frac{\alpha}{\rho_G c_G^{2}} + \frac{1-\alpha}{\rho_L c_L^{2}},\qquad \rho_m = \alpha\rho_G + (1-\alpha)\rho_L

SI

Holds when: The phases are finely mixed and move together. The length of the sound wave is much greater than the size of the bubbles. The gas in the bubbles is compressed isothermally (at constant temperature, because it has time to exchange heat with the liquid), so that ρGcG2≈p\rho_G c_G^2 \approx p. There is no mass exchange between the phases.

Chokes, surface pressure losses and well temperature →
Thermal resistance of the well design
12π rU=12πrtihf+∑iln⁡(ri+1/ri)2πki\frac{1}{2\pi\,rU} = \frac{1}{2\pi r_{ti} h_f} + \sum_i \frac{\ln(r_{i+1}/r_i)}{2\pi k_i}

SI; resistance per metre of length, K·m/W

Holds when: Steady radial heat flow through coaxial layers (layers one inside another, around the same axis). The annulus is treated as a layer that conducts heat. Natural convection of the liquid in it (and radiation, if it holds gas) increases heat transfer. Without them rUrU is too low and the calculated flow temperature is too high.

Chokes, surface pressure losses and well temperature →
Completion efficiency
Ec=JJOH=XX+Sc,X=ln⁡rerw−34E_c = \frac{J}{J_{\text{OH}}} = \frac{X}{X + S_c},\qquad X = \ln\frac{r_e}{r_w} - \frac34

dimensionless; natural logarithm

Holds when: pseudo-steady-state flow (the pressure falls at the same steady rate everywhere in the drainage area) in a circular area. For another shape, replace XX with 12ln⁡(4A/(γCArw2))\tfrac12\ln\big(4A/(\gamma C_A r_w^2)\big), γ=1.781\gamma = 1.781 (Pseudo-steady-state flow and the shape factor) unlike the flow efficiency (FE), it includes only the completion skins, not damage and not the incomplete opening of the interval

Effect of completion on inflow →
Perforation skin by the component method
sp=sH+sV+swbs_p = s_H + s_V + s_{wb}

dimensionless

Holds when: a uniform reservoir, perforated over the whole thickness; the tunnels are clean, with no crushed zone and no damage (these are added separately) the flow follows Darcy's law (the pressure drop is proportional to the rate); at high velocities in the tunnels an inertial skin is added (Inflow at high rates: non-Darcy flow)

Effect of completion on inflow →
Plane part
sH=ln⁡rwrw′(θ),rw′(θ)={lp/4,θ=0∘αθ (rw+lp),θ≠0∘s_H = \ln\frac{r_w}{r_w'(\theta)},\qquad r_w'(\theta) = \begin{cases} l_p/4, & \theta = 0^\circ\\ \alpha_\theta\,(r_w + l_p), & \theta \ne 0^\circ \end{cases}

any units of length

Holds when: a plane problem: tunnels of infinite conductivity, seen in a horizontal cross-section

Effect of completion on inflow →
Vertical part
sV=10a hD b−1 rD b,a=a1lg⁡rD+a2,b=b1rD+b2hD=hlpkHkV,rD=rp2h(1+kVkH),h=1ns\begin{gathered} s_V = 10^{a}\,h_D^{\,b-1}\,r_D^{\,b},\qquad a = a_1\lg r_D + a_2,\qquad b = b_1 r_D + b_2\\ h_D = \frac{h}{l_p}\sqrt{\frac{k_H}{k_V}},\qquad r_D = \frac{r_p}{2h}\left(1 + \sqrt{\frac{k_V}{k_H}}\right),\qquad h = \frac{1}{n_s}\end{gathered}

dimensionless; lg⁡\lg is the base-10 logarithm; lengths in the same units

Holds when: an approximation of numerical solutions for hD≤10h_D \le 10 and rD≥0.01r_D \ge 0.01; outside these limits a numerical calculation is needed

Effect of completion on inflow →
Wellbore part
swb=c1 ec2rwD,rwD=rwlp+rws_{wb} = c_1\,e^{c_2 r_{wD}},\qquad r_{wD} = \frac{r_w}{l_p + r_w}

dimensionless

Holds when: the same model as for sHs_H; the casing and the cement are impermeable

Effect of completion on inflow →
Skin of the crushed zone
sc=hlp(kkc−kks)ln⁡rcrps_c = \frac{h}{l_p}\left(\frac{k}{k_c} - \frac{k}{k_s}\right)\ln\frac{r_c}{r_p}

dimensionless; natural logarithm

Holds when: the inflow into the tunnel is uniform along its length and radial through the thin ring. In reality it is concentrated nearer the end of the tunnel, so the formula gives a lower limit for the skin the thickness and permeability of the zone are taken from charge tests under reservoir conditions, or estimated; in this lesson's examples they are assumed

Effect of completion on inflow →
Tunnels end inside the damaged zone
sdp=(kks−1)ln⁡rsrw+kks sp,rs=rw+lss_{dp} = \left(\frac{k}{k_s} - 1\right)\ln\frac{r_s}{r_w} + \frac{k}{k_s}\,s_p,\qquad r_s = r_w + l_s

dimensionless; natural logarithm

Holds when: lp<lsl_p < l_s: the whole zone where the flow converges on the tunnels lies in damaged rock this is an upper limit: when the ends of the tunnels are close to the edge of the zone, part of the flow reaches them from undamaged rock, and the skin is smaller

Effect of completion on inflow →
Tunnels pass right through the damaged zone
sdp≈sH+sV(l~p)+swb ⁣(r~wrw+lp)l~p=lp−(1−ksk)ls,r~w=rw+(1−ksk)ls\begin{gathered} s_{dp} \approx s_H + s_V(\tilde l_p) + s_{wb}\!\left(\frac{\tilde r_w}{r_w + l_p}\right)\\ \tilde l_p = l_p - \left(1 - \frac{k_s}{k}\right)l_s,\qquad \tilde r_w = r_w + \left(1 - \frac{k_s}{k}\right)l_s\end{gathered}

dimensionless

Holds when: lp>lsl_p > l_s. The tunnel ends are in undamaged rock, so the plane part does not change at phasings of 45–180°. At 0° its equivalent radius lp/4l_p/4 depends on the tunnel length beyond the wall, and there l~p\tilde l_p is used an approximation. When ks→0k_s \to 0, it is the component method for a casing of radius rw+lsr_w + l_s, with the skin counted from the true radius rwr_w (an impermeable ring is the same as a thicker casing). When ks=kk_s = k, it gives the usual sps_p. A check against a numerical solution of the plane problem shows a difference of no more than 0.15 hDh_D calculated with the length l~p\tilde l_p must stay at 10 or less

Effect of completion on inflow →
Skin of the tunnels filled with gravel
Sg=8 k h Lkg n d2S_g = \frac{8\,k\,h\,L}{k_g\,n\,d^2}

any consistent units: kk and kgk_g in the same units, and hh, LL, dd in the same units too

Holds when: linear flow along tunnels of equal length and diameter; the whole inflow is divided equally among the nn tunnels the gravel is uniform; clogging by fine particles, mixing with the reservoir sand and leftovers of the completion fluid are allowed for by a reduced kgk_g

Effect of completion on inflow →
Inertial losses in the tunnels with gravel
Dg=32 kh β ρ B Lπ μ n2d4D_g = \frac{32\,k h\,\beta\,\rho\,B\,L}{\pi\,\mu\,n^2 d^4}

SI

Holds when: the Forchheimer equation in each tunnel (Darcy's law plus a term that grows with the square of the velocity; see Inflow at high rates: non-Darcy flow). For gas, ρB\rho B is replaced by the gas density at standard conditions, and the viscosity is taken at bottomhole conditions the β\beta of the gravel grows as it gets clogged. We estimate it from tests or from correlations with the permeability of the gravel

Effect of completion on inflow →
Measured skin of a perforated well
S=Spp+hhw(sp+sc+Sd,eff)+Sg+DqS = S_{pp} + \frac{h}{h_w}\left(s_p + s_c + S_{d,\text{eff}}\right) + S_g + Dq

dimensionless

Holds when: simple addition is an approximation: the parts interact (damage and perforation, as in the section on the damaged zone) DqDq is separated out by well tests at several rates (Inflow at high rates: non-Darcy flow); the other terms do not depend on the rate

Effect of completion on inflow →
Exact equivalent radius of tunnels in a cased well
rw′(180∘)=R2−rw22R,rw′(0∘)=lp24R,R=rw+lpr_w'(180^\circ) = \frac{R^2 - r_w^2}{2R},\qquad r_w'(0^\circ) = \frac{l_p^2}{4R},\qquad R = r_w + l_p

any units of length

Holds when: a plane problem; the casing and the cement are impermeable, and the tunnels have infinite conductivity

Effect of completion on inflow →
Elasticity of the rate with respect to a parameter
Ex=Δq/qΔx/x≈q(x+Δx)−q(x−Δx)2 q⋅xΔxE_x = \frac{\Delta q/q}{\Delta x/x} \approx \frac{q(x + \Delta x) - q(x - \Delta x)}{2\,q}\cdot\frac{x}{\Delta x}

dimensionless

Holds when: small changes: the elasticity describes the response near the base case and does not replace a calculation of big changes for fractions and for quantities near zero (water cut, skin factor) a relative step is inconvenient; their effect is shown in absolute steps or in ranges

Well performance sensitivity analysis →
Linear estimate of the change of the operating rate
Δq≈δin+δout1/J+sout\Delta q \approx \frac{\delta_{\text{in}} + \delta_{\text{out}}}{1/J + s_{\text{out}}}

metric oilfield units (MPa, m³/d)

Holds when: small changes, for which the curves near the operating point can be replaced by straight lines a change of JJ also changes the slope of the inflow; for big changes (a reservoir treatment, a change of tubing) the whole new point is calculated

Well performance sensitivity analysis →

Symbols

SymbolMeaning and context
m˙\dot m
Δq\Delta q
( dp/ dz)acc(\dd p/\dd z)_{\text{acc}}
aa
AA
a1, a2, b1, b2a_1,\ a_2,\ b_1,\ b_2
bb
BB
BoB_o
b, c, ab,\ c,\ a
B, μB,\ \mu
CC
C0C_0
  • distribution coefficient: allows for the gas being concentrated near the axis of the pipe, where the velocity is higher; about 1.2 for slug flow in a vertical pipe, —Multiphase flow in tubing
c1, c2c_1,\ c_2
CdC_d
cm, cG, cLc_m,\ c_G,\ c_L
Δpchoke\Delta p_{\text{choke}}
Δpcomp\Delta p_{\text{comp}}
  • loss in the near-wellbore zone and the completion (the perforations and gravel pack that connect the well to the rock): pwfs−pwfp_{wfs} - p_{wf}, where pwfp_{wf} is the bottomhole flowing pressure, MPaNodal analysis of the production system
dd
d1, d2d_1,\ d_2
deqd_{\text{eq}}
DgD_g
  • non-Darcy coefficient of the tunnels with gravel; the inertial skin is DgqD_g q, s/m³ (for a rate at standard conditions)Effect of completion on inflow
Δpdown(q)\Delta p_{\text{down}}(q)
EcE_c
EkE_k
  • dimensionless acceleration number — the share of the pressure drop that goes to accelerating the mixture, —Multiphase flow in tubing
ExE_x
ff
FEFE
gg
GLR\text{GLR}
hh
HH
hD, rDh_D,\ r_D
HL, λLH_L,\ \lambda_L
h, lph,\ l_p
JJ
J∗J^*
JactualJ_{\text{actual}}
JidealJ_{\text{ideal}}
J, JOHJ,\ J_{\text{OH}}
  • productivity of the well, and of an undamaged open hole of the same radius in the same drainage area (the part of the reservoir that feeds the well), m³/(d·MPa)Effect of completion on inflow
kk
kck_c
kek_e
kgk_g
kH, kVk_H,\ k_V
krok_{ro}
ksk_s
  • permeability of the rock around the crushed zone: kk if the tunnel is in the undamaged reservoir, and the permeability of the damaged zone if the tunnel is in it, mDEffect of completion on inflow
k, hk,\ h
k, h, L, n, dk,\ h,\ L,\ n,\ d
k, ksk,\ k_s
LL
lpl_p
Δpline\Delta p_{\text{line}}
ln⁡\ln
log⁡10\log_{10}
M, Z1, T1M,\ Z_1,\ T_1
nn
nsn_s
pp
l~p\tilde l_p
p1−p2p_1 - p_2
p1, p2p_1,\ p_2
p1, ρ1p_1,\ \rho_1
pbp_b
pin(q)p_{\text{in}}(q)
pnodep_{node}
pout(q)p_{\text{out}}(q)
psepp_{sep}
pwfp_{wf}
pwf,1p_{wf,1}
pwhp_{wh}
p, fp,\ f
qq
q1q_1
qbq_b
qgq_g
qmaxq_{max}
qmax, pˉR, pwfq_{max},\ \bar p_R,\ p_{wf}
qmaxFE=1q_{max}^{FE=1}
q, pˉR, pwfq,\ \bar p_R,\ p_{wf}
rr
pˉR\bar p_R
R\mathcal{R}
RR
rc, rpr_c,\ r_p
rer_e
ri, ri+1, kir_i,\ r_{i+1},\ k_i
rpr_p
rs, lsr_s,\ l_s
rti, hfr_{ti},\ h_f
rwr_w
rw, lpr_w,\ l_p
rw′r_w'
rw′(θ)r_w'(\theta)
rwbr_{wb}
rwDr_{wD}
pˉR, pwf\bar p_R,\ p_{wf}
pˉR,f\bar p_{R,f}
ReRe
Δpres\Delta p_{\text{res}}
  • pressure loss in the reservoir: pˉR−pwfs\bar p_R - p_{wfs}, where pwfsp_{wfs} is the flowing pressure at the sandface (the wall of the well), MPaNodal analysis of the production system
rUr U
SS
ΔpS\Delta p_S
scs_c
ScS_c
Sd,effS_{d,\text{eff}}
sdps_{dp}
SgS_g
Sg, DqS_g,\ Dq
sHs_H
sH, sV, swbs_H,\ s_V,\ s_{wb}
  • parts of the method: sHs_H is the same as without damage (at 0° phasing, with l~p\tilde l_p instead of lpl_p), sVs_V is calculated with l~p\tilde l_p, and swbs_{wb} with rwD=r~w/(rw+lp)r_{wD} = \tilde r_w/(r_w + l_p), —Effect of completion on inflow
souts_{\text{out}}
sps_p
sp, scs_p,\ s_c
SppS_{pp}
sVs_V
swbs_{wb}
tt
T0+GTzT_0 + G_T z
T1, T2T_1,\ T_2
tDt_D
Tf(z)T_f(z)
ThT_h
Δptbg\Delta p_{\text{tbg}}
  • loss in lifting through the tubing, including the weight of the fluid column and the pressure lost in the downhole equipment: pwf−pwhp_{wf} - p_{wh}, where pwhp_{wh} is the wellhead pressure, MPaNodal analysis of the production system
Δpup(q)\Delta p_{\text{up}}(q)
vv
vdv_d
vGv_G
vmv_m
vSGv_{SG}
r~w\tilde r_w
  • equivalent wall radius: the casing is as if “extended” into the damaged zone (do not confuse it with the equivalent radius rw′r_w'), mEffect of completion on inflow
w cpw\,c_p
XX
x, Δxx,\ \Delta x
zz
α\alpha
αθ\alpha_\theta
β\beta
γE\gamma_E
γg\gamma_{\text{g}}
δin\delta_{\text{in}}
δout\delta_{\text{out}}
ε\varepsilon
θ\theta
  • inclination of the hole — the deviation from the vertical; cos⁡θ  dz\cos\theta\,\dd z is the increment of true vertical depth, —Multiphase flow in tubing
λ\lambda
μ\mu
μJT\mu_{JT}
μˉJT\bar\mu_{JT}
μo\mu_o
ρ\rho
ρL, ρG\rho_L,\ \rho_G
ρm, ρG, ρL\rho_m,\ \rho_G,\ \rho_L
ρns\rho_{ns}
ρs\rho_s