9:59:59.000,9:59:59.000 Speaker: Nay wells are affected by a well[br]skin, a low permeability layer that 9:59:59.000,9:59:59.000 surrounds the well and causes the drawdown[br]in the skin to be less than- er to be 9:59:59.000,9:59:59.000 greater than the drawdown that[br]would be expected otherwise. 9:59:59.000,9:59:59.000 So, we can see this in the, in the sketch. 9:59:59.000,9:59:59.000 This line here is the expected drawdown[br]using, uh, the Jacob analysis, or 9:59:59.000,9:59:59.000 perhaps some other analysis, but as we[br]get right in the vicinity of the well, we 9:59:59.000,9:59:59.000 see that there's a low permeability zone[br]here, and the head goes like so, follows 9:59:59.000,9:59:59.000 this dashed line. 9:59:59.000,9:59:59.000 And as a result, this is the expected[br]drawdown based on our theoretical analysis. 9:59:59.000,9:59:59.000 It is using the properties of the aquifer,[br]uh, out here away from the well 9:59:59.000,9:59:59.000 [stammering] in this region, but in fact[br]we observe that the drawdown at the well 9:59:59.000,9:59:59.000 is here, so the drawdown is greater, um,[br]and that results from the extra headloss 9:59:59.000,9:59:59.000 due to the well skin. 9:59:59.000,9:59:59.000 So we want to characterize this, and one[br]way to characterize it is to use the well 9:59:59.000,9:59:59.000 efficiency, which is the ratio of the[br]expected drawdown from our theoretical 9:59:59.000,9:59:59.000 analysis to the observed drawdown,[br]what actually occurs in the field. 9:59:59.000,9:59:59.000 So we need a way to calculate what the[br]expected drawdown is, and we can do 9:59:59.000,9:59:59.000 this with the Jacob analysis. 9:59:59.000,9:59:59.000 What I'm showing here is a version of the[br]Jacob analysis that's set up to calculate 9:59:59.000,9:59:59.000 the head- er I guess this is the drawdown[br]here, um, as a- at a particular time. 9:59:59.000,9:59:59.000 So, the important thing to recognize is[br]right here. 9:59:59.000,9:59:59.000 The radial distance that we're using here[br]is the radius of the well. 9:59:59.000,9:59:59.000 What we used in the previous analysis[br]was the radial distance of the monitering 9:59:59.000,9:59:59.000 well, where our data were made. 9:59:59.000,9:59:59.000 In this case, we need to use the radial-[br]the radius of the well itself. 9:59:59.000,9:59:59.000 This time here, that's the time, the[br]elapsed time, for a data point that we're 9:59:59.000,9:59:59.000 gonna use to determine the observed[br]drawdown. 9:59:59.000,9:59:59.000 The calculation goes like so: we put in[br]the observed time and the radius 9:59:59.000,9:59:59.000 of the well, and everything else is pretty[br]much the same, the s and the t we've 9:59:59.000,9:59:59.000 calculated using a monitoring well out[br]here in the formation. 9:59:59.000,9:59:59.000 The performance here of the monitoring[br]well, the head in the monitoring well, is 9:59:59.000,9:59:59.000 not effected by the skin, so when we[br]calculate TNS from the monitoring well 9:59:59.000,9:59:59.000 data, we're getting something that's[br]really just affected by the, um, 9:59:59.000,9:59:59.000 formation properties.