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Naturally Adsorbed Gas Survey (NAGS)


NAGS - Naturally Adsorbed Gas Survey - Basics


NAGS – Naturally Adsorbed Gas Survey – unique gas geochemical technology based on the analysis of hydrocarbon and non-hydrocarbon gases naturally adsorbed by subsoil rocks. NAGS is designed for prospecting of hydrocarbon accumulations and mineral deposits.  NAGS is much more informative compared with traditional geochemical prospecting methods dealing with free form of gases. NAGS deals with gases tightly adsorbed by subsoil rocks, so that sampling conditions’ temperature, humidity, mass and preservation of material during transportation are not critical.  Componential composition of gases naturally adsorbed by subsoil rocks is characteristic of fundamental geological processes taking place in the subsurface.   NAGS is applied to detect HC’s and mineral deposits and produce maps of gas-geochemical anomalies closely related to outlines of mineral deposits and HC accumulations.   In oil & gas applications the technology produces accurate results of oil to water contact.  Superposition of independently acquired datasets of STeP and NAGS provides a more accurate prediction of mineral potential compared to traditional exploration technologies.

During the NAGS process, 50-70 gram subsoil rock samples, collected at the target area, are crushed and ground.  The NAGS technology requires that 50-70 gram subsoil rock samples are collected in the analyzed area. They are crushed, screened, and heated to approximately 225 ºС in order to thermally desorb gas and analyze it.  Composition of thermo-desorbed gas is analyzed for С1 – С5 HC-components, О2, N2, H2 and CO2 using a gas chromatograph unit.  Adsorbed HC gases contain all the homologs of CH4 thus allowing for application of gas characterization criteria.  A typical survey, depending on the license block size, may require sampling of 100 to a few  thousand points per target anomaly.

NAGS sample collection is performed in 2 to 3 stages. The first stage may require that samples are collected with the distance of 2 to 4 km between the points.  The second and potentially third stages, with due regard to the first sampling, are carried out at finer spacing of approximately 100 meters over the potential mineral or HC anomaly.

Resulting maps depict the areal distribution of about 20 gas attributes (HC gases, О2, N2, H2 and CO2) and Eh and pH indices. The maps of quantitative characteristics of adsorbed HC- gases, О2, N2, H2 and CO2, Eh and pH, as well as various correlations of these attributes, result in a conclusion about the presence and type of potential mineral anomaly.

The results of each stage dictate the survey strategy, identifying locations of possible anomalies and sampling at even finer distance between points of 50 meters, if necessary.

 





NAGS At Work


NAGS prospecting attributes and gas-geochemical criteria vary depending on the type of a mineral deposit under study.  The variation of such parameters is caused by certain material effects of hydrocarbon and mineral deposits as well as related fields (radioactive, electrical, magnetic, etc.) on the composition of hydrocarbon fluids (gases) ascending from the Earth entrails to the surface.

As shown (below) on the example of a uranium deposit, the effect of radioactivity on the adsorption of gases (particularly, of hydrocarbon gases – HCads) by rocks suggests that radiation causes increased adsorption of hydrocarbon gases by more than 5 times with a trend of prevailing adsorption of heavier homologs of methane.  The nature of this effect is explained by a more intense ionization of heavy homologs of methane.  Radioactive mineralization is manifested in a sharp growth of adsorption of HC gases with the prevailing adsorption of heavy homologs of methane.  Low values of Eh in the zones of anomalous HC adsorption comply with the concept of uranium deposition in zones characterized by reduction conditions.  These zones are also characterized by the highest values of pH.  It is likely that deep fluids of the reduction type (Eh) under alkalinity conditions (pH) facilitated the precipitation of uranium in these zones, where uranium was transported to from adjacent indigenous deposits.

Approximately 10 gas-geochemical attributes and additional prospecting criteria (including ΣHC-gases, Total content of heavy HC’s, Σ nonHC-gases, Н2/HC, N2/O2, CO2/N2, рН, Eh) are applied in prospecting by NAGS technology (some of these attributes are presented here).


Area of Interest Satellite Image

Satellite Image of the area


Area Sampling Points

Sampling Points 1 st Stage

HC adsorbed - click for larger image

CH4 - click for larger image

HC heavy total - click for larger image

CO2 - click for larger image

Eh - click for larger image

pH