Sondeos

,

Pozos

,

Buscar aguas subterranea

,

Videos de pozos

,

Telecomunicaciones wimax

,

Automatizaci髇 y Telecontrol

,
image image image image
TDEM Time-domain electromagnetic technology (TDEM) is effective in determining the electrical conductivity in soils from a few meters to 1000 meters and more. From the moment that the conductivity is strongly correlated to soil properties, the TDEM represents an important tool for soil mapping as well as for determining lateral and vertical changes of the properties in them. This method, which can be used in the design of drilling test or profiling, is an important tool in hydrological research in sedimentary/alluvial environments and in the characterization of sequences with the presence of lenses of brackish water into the coastal environment.
Georadar Ground Penetrating Radar or GPR (GPR) is a geophysical method that uses radar pulses to image the subsurface. This non-destructive method uses electromagnetic radiation in the microwave band width (frequency UHF / VHF) of the radio spectrum, and detects the reflected signals from subsurface structures.
Tomography The "electric" quadrupole method consists of introducing a continuous electrical current on the surface of the ground through two electrodes of "current". Voltage is measured by another pair of electrodes. From the value of the injected current and the measured voltage, is obtained the "apparent resistivity" of subsoil.
URP Water Technologies has a team of geophysic testification for in-situ drilling tests and technical experts to diagnose them. With immediate geographic availability nationally and diagnostic capability for drilling to 1,000 m, Water Technologies accurately analyzes the hydrogeological state and electromechanical facilities to optimize the exploitation of them and provides turnkey solutions for their setup.

Geophysics

Water Technologies has a team of experts specialized in well logging and geophysical prospection as well as surface, which have the most advanced resources currently available.

Water Technologies uses the latest equipments of Geophysics, which operate both the development of specific tasks, such as design, programming and campaigns that respond to very different objectives. Related to the surface geophysics, electrical geophysical recognitions are conducted, as well as electromagnetic, seismic and GPR, with interpretation resolutions up to 2000 m depth according to the method used.

Water Technologies uses geophysical methods applied interchangeably to surface and drilling programs that affect to hydrogeological studies search and characterization of aquifers, control and monitoring of salinity, flow measurements, water quality and determination of hydrogeological parameters in drill tests (porosity, permeability, etc. ..).

Search in WTECH

Curvatura en los estratos.

En este video, se observa como el sondeo atraviesa del pliegue tipo anticlinal por la zona de charnela. Se aprecia claramente la curvatura de los estratos en ambos flancos del pliegue. En general, un pliegue anticlinal tiene su origen en esfuerzos tect贸nicos de diverso tipo, tales como: presiones tangenciales, deslizamiento o corrimiento, intrusi贸n o eyecci贸n de materiales desde 谩reas m谩s profundas, o deformaciones verticales del sustrato. En este caso concreto, se debe a la resultante compresiva de esfuerzos tangenciales.
 

Falla vertical perforada

En este video, se aprecia la presencia de un cambio litol贸gico asociado a una falla subvertical, atravesada por el sondeo durante la perforaci贸n. Una falla vertical est谩 producida por un reajuste de los materiales cuando las fuerzas tect贸nicas superan la resistencia de las rocas. La zona de ruptura puede tener una superficie bien definida, denominada plano de falla y su formaci贸n va acompa帽ada de un deslizamiento de las rocas tangencial a este plano, que es lo que se observa en el video como un cambio de coloraci贸n en la roca.
 

Cambio de coloraci贸n en la roca.

Se puede observar un cambio en la coloraci贸n de la roca, asociado a un cambio litol贸gico. En car谩cter seudohorizontal de los estratos en esa zona, provoca ese cambio con la profundidad de perforaci贸n. Una variaci贸n en las condiciones de sedimentaci贸n de los materiales y/o durante los procesos de litificaci贸n y diag茅nesis, tiene como resultante el car谩cter heterog茅neo de los materiales del subsuelo.
 
 
Water Technologies
Contact +34 968 901 004
+34 968 901 067
contacto@wtech.es
wtech.es
Location C/ Central 13, 3C
Torre Godoy 30100
MURCIA | Spain
VIEW MAP