Mud Logging Service

Mud logging

A mud logging unit is installed on the rig when geologic information must be retrieved on a timely basis. If the formations drilled are not well known or if a specific geologic horizon is targeted, mineralogical data from cuttings brought to the surface with the mud might be essential. For example, secondary hydrothermal mineralization is a key indicator to locate a viable horizon as a geothermal reservoir. Changes in the mineralogical composition of the formations can require adjustments in the mud program. The main task of a mud logging unit is to monitor and collect all necessary information to ensure an uninterrupted drilling process. This includes the measurement of gases, mudflow rates (in and out), temperatures, drill rates, depth, and pressures. Gases monitored include hydrogen sulfide (H2S) and carbon dioxide (CO2). H2S is poisonous, very corrosive when dissolved in water, and flammable as a gas. When dissolved in water (of the mud) it lowers the mud pH increasing corrosion tendencies. As a gas, it is transported to the surface when air is applied as the drilling fluid. Carbon dioxide is soluble in water and can form carbonic acid in the drilling fluid which reduces the mud pH and makes it more corrosive. It is important to detect the gases promptly using a mud-gas trap during mud drilling or an air-gas trap during air drilling, so appropriate abatement measures can be taken. The depth and the drilling rate of the drill rig are also monitored by the mudlogger. A sudden increase in the drilling rate might help indicate fracture zones, which are of great interest in the geothermal drilling process.

• Qualitative techniques are used as the basis for formation pressure evaluation analysis.

   Parameters monitored include:

1. Dxc (the primary measurement)
2. Gas relationships (background gas,
3. Connection and trip gases, ECD, MW)
4. Drilling Fluid Temperature.
5. Drilling Fluid Conductivity.
6. Rotary Torque, Fill, Overpull.
7. Cuttings character;
8. Cavings? Shape, volume.

• Analysis of formation pressures in shaly sequences qualifying under-compaction disequilibrium.