How can Seismo Electric Technology help you or your clients find well water?

YOU’RE THE REALTOR, THE LAND BROKER AND/OR THE LOAN OFFICER…

Your client just paid for a  dry well! They need help finding the water before they drill another hole in the ground but who can help them? Of all the technology out there which ones are bogus and which are legit? We can help!

How can Seismo Electric Technology help you or your clients find well water?

 The purpose of our technology is to save people from drilling dry and/or low yielding water wells or shall we say holes in the ground. Since 2001 we’ve used seismo electric technology developed by Dr. J. Millar & Dr. R. Clarke of the U.K. to locate groundwater (aquifers) for clients seeking to find an aquifers depth & yield before attempting to drill water wells.

Why do people consider me an expert in Seismo electric technology?

Through AquaLocate USA & affiliated companies I have been involved in successfully providing more than 35,000 individual seismo electric soundings throughout the U.S., Canada, MX, NZ, AU, India, Oman & Saudi Arabia.

 How Seismo electric technology works: The seismo electric method somewhat resembles the seismic method which is often used in oil field exploration. The main difference between seismo electric systems and seismic systems is that the seismo electric method is much simpler to use and a seismic system only records rock structure information and cannot provide any unequivocal information about the aquifer such as the actual groundwater depth and yield.

More specifically: The GF3500 and a seismic source are used together to generate and collect the seismo electric signal. The seismic source is used to create a sound wave (pulse).  These sound waves move through the aquifer and the water in the aquifer moves relative to the rock formation. Ions in the water are dragged away from their partners bound to the rock and the electrical disturbance created travels to the surface at the speed of light and is detected by the antenna array. Each signal is separated in time from its neighbors by the propagation time of the down going seismic pulse. This gives unambiguous depth and thickness data, as with reflection seismic. The form of each signal gives information about the depth, thickness and quality of the aquifer and this is used to estimate the likely yield from a water well drilled at the survey site. The data is saved and a final written report is compiled once the information is reviewed and approved by a state licensed Geophysicist, Geologist and/or or Hydro Geologist (regulations vary by state).

Unfortunately we are often the second call a client makes. They pay for a dry well that’s been drilled, have lost a significant amount of money then turn to us to fix it (find the water). When professionals like you are in the know and can refer businesses like us, you have the advantage of helping your client avoid paying for a dry well!  

 How can we help you? Give me a call at 888.808.8598  http://www.aqualocate.com