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gas hydrate - CCOP

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RESULTS<br />

By Government:<br />

The outcomes of the first two projects, Mae Tha and Mae Lamao, carried out by academic<br />

institutions (see above), were inconclusive. This may be due to several factors such as<br />

insufficient prior knowledge on drilling, well completion (PVC connecting), core sample<br />

collection, field data collection procedures for <strong>gas</strong> and lab testing of core samples. Moreover,<br />

there was lack of knowledge on the <strong>gas</strong> reserve calculation.<br />

In 2006, the DMF made another attempt at CBM evaluation. The project site is at Mae Lamao<br />

(Mae Sod Basin), in Northern Thailand. This time a private company was awarded the<br />

contract and the exploration methodology was changed from the previous two projects. The<br />

core samples (coal) were collected in a canister filled with water and then sent for laboratory<br />

testing for <strong>gas</strong> volume and quality. As of now, the results are pending.<br />

Mae Tha<br />

Production and observation wells<br />

The location of one production well and two observation wells were arranged in a triangular<br />

pattern. Major factors that were considered include thickness of and continuity of coal beds,<br />

depth of coal beds, and structural geology.<br />

Construction of production and observation wells were commenced after drilling was<br />

completed. This is the stage in which pipes are installed. The depth below the coal beds was<br />

plugged with clay and plugged by cement above the coal up to the surface while at the depth<br />

interval where coal beds were found, a screen was installed to allow coalbed <strong>gas</strong> to flow into<br />

the well. Gravel pack is placed to coal bed up to 4 meters.<br />

The depth interval where coal beds were found in both production and observation wells is<br />

show in Table 1. The enclosing strata are made up of mudstone, claystone, shale, sandstone,<br />

and unconsolidated clay. The coal-bearing strata are divided into the upper coal bed and the<br />

lower coal bed. The upper coal bed is found at the depth of 12-16 meters with the thickness of<br />

4 meters. The lower coal bed is found at the depth of 204-207.5 meters with the thickness of<br />

3.5 meters. Between the upper and lower coal beds, mudstone and claystone, with an<br />

aggregate thickness of 188 meters, are present in the depth interval of 16-204 meters.<br />

Hole Name<br />

Table 1. Coal Depth Interval<br />

Total Depth (m.)<br />

Depth to Coal<br />

Seam (Top/bottom)<br />

Coal<br />

Thickness (m.)<br />

MTO 1/46 213.00 200.80-202.20 1.40<br />

MTO 2/46 220.00 195.50-198.20 2.70<br />

MTP 1/46 209.00 204.00-207.50 3.50<br />

134 New Energy Resources in the <strong>CCOP</strong> Region - Gas Hydrates and Coalbed Methane

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