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Equations: Sand production

The equations of the “Sand production” lessons in “Oil and gas production”, with their conditions and units, and what each symbol means in them.

Mohr–Coulomb strength criterion in principal effective stresses
σ1′=C0+q σ3′,q=tan⁡2 ⁣(45∘+φ2)=1+sin⁡φ1−sin⁡φ,C0=2S0q\sigma'_1 = C_0 + q\,\sigma'_3,\qquad q = \tan^2\!\left(45^\circ + \frac{\varphi}{2}\right) = \frac{1 + \sin\varphi}{1 - \sin\varphi},\qquad C_0 = 2S_0\sqrt{q}

any identical units of stress. The stresses are effective, that is, less the pore pressure

Holds when: The intermediate principal stress σ2′\sigma'_2 does not affect the strength (in reality it affects it a little, usually strengthening the rock). The straight line is an approximation. At large confinements the strength curve flattens, and in loose sands the cohesion is close to zero. The strength is the peak one, the greatest stress of the test. After the peak a weak rock goes on carrying part of the load.

Sand production: types, prediction and cost of the problem →
Hoop stress at the wall of the hole of a thick-wall cylinder
σθ=2 P ρ2ρ2−1,ρ=Dd\sigma_\theta = \frac{2\,P\,\rho^2}{\rho^2 - 1},\qquad \rho = \frac{D}{d}

any identical units of pressure; the diameters in the same units

Holds when: The rock is elastic up to failure. The pressure in the hole is atmospheric (the pore pressure is not maintained in the test). This is the Lamé solution for a thick-wall pipe under external pressure. The axial stress does not enter the formula.

Sand production: types, prediction and cost of the problem →
Effective hoop stress at the wall of an open wellbore during production
σθ′=2σh′+(2−A) (pˉ−pwf),A=α(1−2ν)1−ν\sigma'_\theta = 2\sigma'_h + (2 - A)\,(\bar p - p_{wf}),\qquad A = \frac{\alpha(1 - 2\nu)}{1 - \nu}

any identical units of pressure

Holds when: A vertical open hole, with both horizontal stresses equal. The rock is elastic, and the Biot coefficient in the strength criterion is 1. Steady radial inflow, and the pore pressure at the wall equals the bottomhole pressure. The stress along the axis of the well at the moment of failure is intermediate and does not affect the failure. After noticeable depletion this may stop being true: the effective axial stress at the wall becomes the greatest (example below), and the formula is optimistic. With unequal horizontal stresses, in place of 2σh′2\sigma'_h we have 3σH′−σh′3\sigma'_H - \sigma'_h, and for a perforation tunnel 3σ1′−σ3′3\sigma'_1 - \sigma'_3, where σ1′\sigma'_1 and σ3′\sigma'_3 are the two effective stresses in the plane of its cross-section.

Sand production: types, prediction and cost of the problem →
Critical drawdown and critical depletion (open hole)
Δpcr=Cw−2σh,i′−2(1−A)(pi−pˉ)2−A,(pi−pˉ)cr=Cw−2σh,i′2(1−A)\Delta p_{\text{cr}} = \frac{C_w - 2\sigma'_{h,i} - 2(1 - A)(p_i - \bar p)}{2 - A},\qquad (p_i - \bar p)_{\text{cr}} = \frac{C_w - 2\sigma'_{h,i}}{2(1 - A)}

any identical units of pressure

Holds when: The same as for the formula for the wall. The depletion is uniform over the reservoir, and the reservoir deforms only vertically. CwC_w does not change with time. In reality water cut and load cycles lower it. A negative Δpcr\Delta p_{\text{cr}} means that the wall has already failed without drawdown.

Sand production: types, prediction and cost of the problem →
Settling velocity of a grain in a fluid at rest (Stokes' law)
vs=g d2 (ρs−ρl)18 μv_s = \frac{g\,d^2\,(\rho_s - \rho_l)}{18\,\mu}

SI

Holds when: A single spherical grain. The Reynolds number of the grain, ρlvsd/μ\rho_l v_s d/\mu, is less than one. Otherwise the resistance is greater, and the formula overstates the velocity. The fluid is at rest and the wellbore is vertical. At a high concentration the grains hinder each other and settle more slowly, and in a deviated wellbore they quickly slide to the lower wall.

Sand production: types, prediction and cost of the problem →
The largest grain that passes through a pore of a packing of equal spheres
dmax⁡=(23−1)D≈0.155 D(dense packing),dmax⁡=(2−1)D≈0.414 D(cubic)d_{\max} = \left(\frac{2}{\sqrt3} - 1\right)D \approx 0.155\,D\quad\text{(dense packing)},\qquad d_{\max} = \left(\sqrt2 - 1\right)D \approx 0.414\,D\quad\text{(cubic)}

any units of length

Holds when: The spheres are equal. In a dense packing three touching grains form a triangular constriction, and in a cubic packing a square one of four. Real gravel is a mixture of grains between two sieves, and it is not perfectly round. The estimate shows the order of magnitude and not an exact limit.

Sand control methods →
Uniformity coefficient of a sand
C=D40D90C = \frac{D_{40}}{D_{90}}

dimensionless

Holds when: The sizes are found from the cumulative curve by interpolation between the sieves in the logarithms of the size. The sample represents the productive interval. If there are several samples, we choose the protection by the finest of the productive layers.

Sand control methods →
Choosing the gravel by the median sizes
D50,g=(5–6) D50,sD_{50,g} = (5\text{–}6)\,D_{50,\text{s}}

any units of length, the same for both sizes

Holds when: The sand is well or moderately sorted. The gravel is of a narrow size: almost all the mass is between two neighbouring sieves. For poorly sorted sands the criterion by the median is not reliable. We then use the Schwartz criterion: the size of the gravel DpD_p is taken as six times the same size DpD_p of the sand, and the point of the curve is chosen by the sorting: D10D_{10} for CC up to 5, D40D_{40} for CC from 5 to 10, and D70D_{70} for CC above 10 (the worse the sorting, the finer the point of choice). And we run sand retention tests.

Sand control methods →
Calculated mass of gravel for a pack in casing
M=ρg(1−ϕg)[π4(Dc2−ds2)(Ls+Lr)+n π4dp2 lp]M = \rho_g(1 - \phi_g)\left[\frac{\pi}{4}\left(D_c^2 - d_s^2\right)(L_s + L_r) + n\,\frac{\pi}{4}d_p^2\,l_p\right]

SI

Holds when: The reserve above the screen makes up for settling and compaction of the pack as the well works. Tunnels and voids behind the casing usually take more gravel than their dimensions give, especially if the reservoir has already produced sand. So a placed mass larger than calculated is a good sign, and a smaller one is a reason to check.

Sand control methods →

Symbols

SymbolMeaning and context
pˉ\bar p
(pi−pˉ)cr(p_i - \bar p)_{\text{cr}}
AA
CC
C0C_0
CwC_w
Δpcr\Delta p_{\text{cr}}
dd
DD
D40, D90D_{40},\ D_{90}
D50,sD_{50,\text{s}}
D50,gD_{50,g}
Dc, dsD_c,\ d_s
dmax⁡d_{\max}
  • diameter of the largest sphere that passes through a pore between neighbouring grains, mmSand control methods
D, dD,\ d
gg
Ls, LrL_s,\ L_r
MM
n, dp, lpn,\ d_p,\ l_p
  • number of perforation tunnels, their diameter and their length behind the casing, —, m, mSand control methods
PP
pi, pˉp_i,\ \bar p
pwfp_{wf}
qq
S0S_0
vsv_s
μ\mu
ρg, ϕg\rho_g,\ \phi_g
ρs, ρl\rho_s,\ \rho_l
σ1′, σ3′\sigma'_1,\ \sigma'_3
σh′\sigma'_h
σh,i′\sigma'_{h,i}
σθ′\sigma'_\theta
σθ\sigma_\theta
φ\varphi