connate water

Connate water is trapped in rock strata at the time of formation.

Connate water contains gas dissolved in aqueous solution.

Their colors and cementation appear to be the result of ground or connate water alteration after their deposition.

Average connate water saturation.

During the "boiling" process, boron present in the connate waters, or derived from the thermal break down of clay minerals, partitions into the steam.

Non-meteoric forms of groundwater are connate water and magmatic water, also termed juvenile water.

Stress levels rise and fall episodically, and earthquakes can cause large volumes of connate water to be expelled from fluid-filled fractures.

In order to use this model for the relative permeability exponents the data must be corrected for connate water saturation and residual oil saturation.

In the case of SP logging, the two aqueous solutions are the well bore fluid (drilling mud) and the formation water (connate water).

Asphaltite: Blanket and vein type deposits due to the process of de asphaltite in natural crude oil due to thermal action and connate water.

Whether the mud contains more or less salt than the connate water will determine the which way the SP curve will deflect opposite a permeable formation.

Electrical heating increases the temperature of the soil and groundwater by conducting current through the resistive connate water that fills the porosity of the soil.

Because rock containing connate water is typically formed from ocean sediments, connate water is normally saline.

Just as production-induced reservoir pressure decline causes gas to evolve from solution in petroleum, gas evolves from solution in connate water as the result of production from a pool.

In any matrix which has some porosity, the pore spaces will be filled with a fluid of oil, gas (either hydrocarbon or otherwise) or formation water (sometimes referred to as connate water).

Such studies should embrace a variety of deposits including unperturbed sediments and tailing.,, with contrasting mineralogies, and should include assessment of alteration effects and connate water and/or groundwater chemistry in contrast to tailings disposed on-land.

This study will examine how O2 is consumed in the reservoir and will concentrate on the impact of oxidation reactions with regard to the composition and emulsification characteristics of the oil and the pH levels of the connate water.

Accumulations of hydrocarbons are invariably associated with aqueous fluids (formation waters), which may occur as extensive aquifers underlying or interdigitated with hydrocarbon bearing layers, but always occur within the hydrocarbon bearing layers as connate water.