Estudo de geotermia rasa na cidade de Humaitá-AM

From October 2007 to September 2008 a geothermal monitoring experiment was conducted at depths of 0.02 m, 0.5 m and 1.0 m to quantify the variations of temperature, thermal conductivity and the shallow geothermal heat flow at places with and without vegetation cover in the Humaita city, Amazonas. The influence of the vegetation cover on the shallow geothermal system was observed in the sites studied. There were variations of monthly average values of temperature between the places with and without vegetation cover. During the "dry" period, this variation was up to 6.01oC at the depth of 0.02 m, and 2.84oC at the depth of 1.0 m. During the "rainy" period, however, the variation was up to 2.94oC, at the depth of 0.02 m, and 2.51oC at the depth of 1.0 m. The difference of the daily extreme values of temperature between sites with and without vegetation cover were 3.97oC during the "rainy" period and 9.63oC during the "dry" period, at the depth of 0.02 m. It was noticed that at 06:00 PM the magnitude of the temperature remained high compared to other times on the day studied. The values of the thermal conductivity were 0.54 W/moC during the "dry" period, and 1.23 W/moC during the "rainy" period. The values of the shallow geothermal flows at depths of 0.5 m and 1.0 m, were 2.51 W/m2 and 0.64 W/m2, respectively. These values are 103 larger than the terrestrial heat flow in the region. The thermal variations at0.5 m to 1.0 m depth are influenced by external sources that reach the surface and cannot be neglected. The thermal variations recorded in this work are important and fundamental to better understanding the shallow geothermal structure in the southern, part of Amazonas state, and they also contribute as input to models that allow the mitigation or elimination of the effects caused by anthropogenic actions.