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PTRL3030/5021/6021: Reservoir Characterisation Assignment 1 This individual assignment should be handed in before 5pm on Wednesday, 5th July electronically as PDF or word document as single file. Note...

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PTRL3030/5021/6021: Reservoir Characterisation Assignment 1

This individual assignment should be handed in before 5pm on Wednesday, 5th July electronically as PDF or word document as single file. Note that tables 1 and 2 are available as text file on Moodle – please load the table corresponding to your student ID.

Q1. Consider the data publicly available from fourteen wildcat wells in the National Petroleum Reserve in Alaska (https://certmapper.cr.usgs.gov/data/PubArchives/of00-200/wells/WELLIDX.HTM). The wells are distributed as given in Fig. 1 with corresponding formation tops (in ft) and exact well locations given in Tab. 1.

Figure 1: Well locations of 14 wildcat wells given by public USGS report 00-200.

Table 1: Formation tops and well locations for 14 wildcat wells given by public USGS report 00-200.

Well # Name Torok Pebble SH Kingak SH Sag River SS Shublik BasementLatitude Longitude 1 Awuna XXXXXXXXXX023 2 East Simpson XXXXXXXXXX XXXXXXXXXX XXXXXXXXXXKugrua XXXXXXXXXX XXXXXXXXXX XXXXXXXXXXLisburne XXXXXXXXXX 5 Seabee XXXXXXXXXX XXXXXXXXXXSouth Barrow XXXXXXXXXX XXXXXXXXXXSouth Barrow XXXXXXXXXX XXXXXXXXXX XXXXXXXXXXSouth Barrow XXXXXXXXXX XXXXXXXXXXSouth Barrow XXXXXXXXXX XXXXXXXXXX XXXXXXXXXXSouth Barrow XXXXXXXXXX XXXXXXXXXX XXXXXXXXXXTulageak XXXXXXXXXX XXXXXXXXXX XXXXXXXXXXTunalik XXXXXXXXXX XXXXXXXXXX XXXXXXXXXXWalakpa XXXXXXXXXX XXXXXXXXXX XXXXXXXXXXWalakpa XXXXXXXXXX XXXXXXXXXX156.953

a. (10 marks) Initialise the random number generator in Matlab with your student number. Starting in pristine state after this initialisation, draw an integer in the interval [1;3]. Here ‘1’ stands for the Torok formation, ‘2’ for Pebble Shale and ‘3’ for Sag River Sandstone. Then choose five wells with valid tops (Tab. 1) randomly using a similar approach in Matlab. b. (10 marks) Discretise the chosen well locations on a 50x50 grid and visualize the grid (e.g. use 0 for a cell containing no well and 1 for a well-containing cell). c. (20 marks) For the chosen wells and formation enter the respective formation tops at their locations in the grid. Populate the 50x50 grid with interpolated formation tops from the known points using i) nearest neighbour and ii) inverse distance weighting techniques (p=2). Discuss the resulting maps.

Q2. Consider a log quality task for the same field as in Q1. a. (15 marks) For the first well as chosen above (with valid log data in the respective interval), carry out a quality control for RHOB, NPHI and DT in the Sag River Sandstone unit. b. (15 marks) Calculate the correlation coefficients between RHOB, NPHI and DT (in pairs).

Q3. Consider a layered sequence discovered in a fluvial delta with some evidence of cross-bedding. The bottom layer is a horizontally continuous shale layer with varying height and has been eroded at places by a river system. The middle layer (sandstone) is heterogeneous and only partially continuous as the river changed direction over time and filled in the channels of the layer below. The top layer is a sandstone of low permeability. It exhibits a continuous top and bottom surface, covers the channel system, and varies in thickness. a. (15 marks) Choose an appropriate grid to discretise this layered system and give a reason for your approach. Illustrate your argument graphically. b. (15 marks) Choose three physical measurements to capture essential properties to characterise flow. Pay attention to both horizontal/vertical resolution and field of view. How do these measures help you to characterise the reservoir?

Answered 47 days After May 18, 2022

Solution

Aditi answered on Jul 05 2022
98 Votes
3. The storage and querying of geographical data are both components of the method that grids provide. Grids have the capacity to store a variety of data, including porosity, permeability, and fluid saturation. We are informed in this part of the query that our structure was found in an environment that was transitional between a river and a delta. Our layered sequence consists of the following:
a. • The uppermost layer is composed of sandstone with low permeability
• The middle layer is composed of discontinuous sandstone that has been eroded over time.
• Shale that is continuous along the base but varies in height is in the bottom layer.
This may be seen in the diagram that is shown below:
Figure 1
The permeability of shale is quite poor. In this scenario, we would have to suppose that the bottom layer is unable to support the horizontal mobility of hydroca
ons or fluids because of its location. Because of this, measuring the permeability of this layer is not something that is necessary. In addition to this, we might make the assumption that the shale functions as a ba
ier. Either we need to utilize separate grid cells that change in thickness for each x, y place or we need to alter the amount of grid cells that are present for each x, y position so...
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