Thermal and hydraulic aspects of the KTB drill site

The extensive data sets obtained by the KTB drilling project (lithological and structural information, BHT values, temperature logs, rock thermal properties) provide a unique opportunity to construct realistic thermal models and thus to shed light on thermal conditions in the upper crust. Our numerical simulation study, a Swiss contribution to the German KTB drilling project, aims to understand the steady-state thermal and hydraulic field in the surroundings of the KTB. The simulations consider state-of-the-art petrophysical aspects relevant to deep, pressurized, high-temperature structures and were performed on discretized 2-D/3-D finite-element meshes that contain topography, geological structures and hydrogeological features. Our analysis of the KTB temperature field suggests three zones of particular geothermal settings: a low-heat-flow zone in the uppermost layers with a transition to high heat flow at 500 m depth; the underlying region accessed by the borehole with its characteristic uniform gradient; and the mid-lower crust that must be responsible for the high-heat-flow regime at the KTB site. The two first zones are treated in the present paper. A 3-D thermo-hydraulic model was set up in order to evaluate the first 2000 m, including the uppermost 500 m low-heat-flow zone. This model incorporates the complex geological information from the KTB pilot hole and topography-driven fluid flow. The lateral boundaries of the model were carefully chosen by analysing the flow pattern within a large, regional 3-D domain. The drilled section is analysed by a 2-D model using the available structural information. Due to dominating refraction effects, a careful temperature gradient analysis has to be carried out for such steeply dipping, anisotropic structures. Both models indicate a thermal regime dominated by diffusive heat transfer. Hydraulic flow seems to be important only for the uppermost (≈400 m) part of the drilled depth section; our simulations do not support significant fluid circulation at greater depths. In the drilled section the rather uniform gradient and the pronounced vertical heat-flow variations can now be explained. Finally, the potential and the limitation of the analysis of heat flows and temperature gradients are demonstrated. Heat-flow interpretations are conclusive only for nearly horizontally layered, isotropic geological units. In steeply dipping and anisotropic formations the heat-flow field is perturbed over a large distance (>1 km) around the point of interest. In such geological units only the temperature gradient interpretation can provide reliable information on the surrounding materia

Investigation of Natural Effective Gamma Dose Rates case study: Ardabil Province in Iran

Gamma rays pose enough energy to form charged particles and adversely affect human health. Since, the external exposure of human beings to natural environmental gamma radiation normally exceeds that from all man-made sources combined, natural background gamma dose rates and corresponding annual effective doses were determined for selected cities of Ardabil province from 2009 to 2010. Outdoor gamma dose rates were measured using an Ion Chamber Survey Meter in 105 locations in selected districts. Average absorbed dose for Ardabil, Sar-Ein, Germy, Neer, Shourabil Recreational Lake, and Kosar were determined as 265, 219, 344, 233, 352, and 358 nSvh-1, respectively. Although dose rates recorded for Germi and Kosar are comparable with some areas with high natural radiation background, however, the dose rates in other districts are well below the levels reported for such locations. Average annual effective dose due to indoor and outdoor gamma radiation for Ardabil province was estimated to be 1.73 (1.35-2.39) mSv, which is on average 2 times higher than the world population weighted average

A new heat flux model for the Antarctic Peninsula incorporating spatially variable upper crustal radiogenic heat production

A new method for modelling heat flux shows the upper crust contributes up to 70% of the Antarctic Peninsula's subglacial heat flux, and that heat flux values are more variable at smaller spatial resolutions than geophysical methods can resolve. Results indicate a higher heat flux on the east and south of the Peninsula (mean 81 mWm-2) where silicic rocks predominate, than on the west and north (mean 67 mWm-2) where volcanic arc and quartzose sediments are dominant. Whilst the data supports the contribution of HPE-enriched granitic rocks to high heat flux values, sedimentary rocks can be of comparative importance dependent on their provenance and petrography. Models of subglacial heat flux must utilize a heterogeneous upper crust with variable radioactive heat production if they are to accurately predict basal conditions of the ice sheet. Our new methodology and dataset facilitate improved numerical model simulations of ice sheet dynamics

The Paleogeothermal Conditions of the Swiss Molasse Basin: Implications for Hydrocarbon Potential La paléogéothermie du bassin molassique suisse : implications pour le potentiel hydrocarbures

The paleogeothermal conditions in the Swiss Molasse basin (Tertiary foredeep sediments north of the Alps) have been investigated by means of coalification studies. These data suggest a generally low-temperature geothermal regime in the Molasse basin which apparently prevailed since the deposition of the sediments. In the light of these findings some general trends for the hydrocarbon potential can be specified; corresponding exploration targets are delineated. On a tenté de reconstruire la paléogéothermométrie du bassin molassique suisse (sédiments tertiaires d'avant-fosse des Alpes du Nord) à partir de l'étude des phénomènes de houillification. Les résultats suggèrent qu'un régime géothermique de basse température a prédominé la plupart du temps depuis le dépôt des sédiments. On en déduit quelques tendances générales pour le potentiel en hydrocarbures ainsi qu'une délimitation des objectifs pour l'exploration pétrolière

Thermal and hydraulic aspects of the KTB drill site

ISSN:1365-246XISSN:0956-540