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:<math>\mbox{PI} = \frac{q}{\bar{p} - p_{\rm wf}} \mbox{ (for oil)} = \frac{q\mu B}{\bar{p}^{2} - p_{\rm wf}^{2}} \mbox{ (for gas)}</math> :<math>r_{\rm d} = \left(\frac{kt}{376\phi \mu c_{\rm t}}\right)^{1/2}</math>

! Port category || Port size range (r₃₅), &mu;

:<math>\mbox{K}_{\rm a} = \frac{2000 \mbox{ P}_{\rm atm}\mbox{QL}\mu}{\mbox{A}(\mbox{P}_{1} - \mbox{P}_{2})}</math>

:<math>H_{\rm o} : \mu = \mu_{0}\quad H_{\rm a} : \mu \neq \mu_{0}</math> :<math>\bar{x} - \frac{t^{*}s}{\sqrt{n}} \leq \mu \leq \bar{x} + \frac{t^{*}s}{\sqrt{n}}</math>

...lab}}{\mbox{P}_{\rm c\ lab}}\right) = 0.29 \times \frac{367}{204} = 0.52 \mu</math>

:<math>k = \frac{162.6qB\mu}{mh}</math> ...s = 1.151 \left[\frac{\Delta p_{1{\rm hr}}}{m} - \log \left(\frac{k}{\phi \mu c_{\rm t}r_{\rm w}^{2}}\right) + 3.23\right]</math>

...d, including tectonic elements. SR = San Rafael swell; KU = Kaibab uplift; MU = Monument uplift; WF = Waterpocket fold; A = Absaroka thrust fault. (c) Co

:<math>\frac{kh}{\mu} = \frac{162.6qB_{\rm o}}{m}</math> ...\left[\frac{\big(P^{*} - P_{\rm ave}\big)}{m} - \log \left(\frac{kt}{\phi\mu c_{\rm t}r_{\rm w}^{2}}\right) + 3.23\right]</math>

..._1 \pi r_{c1}^4}{8} + \frac{n_2 \pi r_{c2}^4}{8} \right ] \frac{\Delta P}{\mu L}</math> :<math>q = \frac{nh_f w_f^3}{12} \frac{\Delta P}{\mu L}</math>

:<math>q = (A/L)(k/\mu)\Delta p</math> :<math>p = p_{\rm wf} + \frac{q\mu B}{2\pi kh} \ln (r/r_{\rm w})</math>

<math>Nc = \frac{(v * \mu)}{\sigma} \text{ (1)}</math> ...dial composite reservoir.<ref name=Liuetal_2018>Liu, Q., Lu, H., Li, L., & Mu, A. (2018). Study on characteristics of well-test type curves for composite

:<math>k = \frac{2000 P_{in } \mu Q_{a } L}{A [P_{in}(P_{in} - P_{out}) P_{out}]}</math>

:<math>\text{Q} = \text{K } \Delta \text{A} \mu \text{L}</math>

: <math>\mu_{P, T} = \mu_1 \left ( \frac{\mu}{\mu_1} \right )</math>

# ''MR'' (mu-rho)= this property is sensitive towards the change in lithology. Sandstone

...Mbadinga, Y. F. Liu, S. Z. Yang, J. F. Liu, R. Q. Ye, J. D. Gu, and B. Z. Mu, 2015, [https://www.nature.com/articles/srep09801 Insights into the anaerob

:<math>k_{a} = \frac{2000p_{a}\mu q_{a}L}{(p_{1}^{2} - p_{2}^{2})A}</math>