Method of geohydrodiagnostics.

As the prototype is undertaken the method of seismological reconnaissance on A.S.YEYASHCH8YAE OF THE USSR MDI with 01/01/00, which includes the excitation of seismic oscillations/vibrations, the registration of the signals reflected by seismic receivers and subsequent obratoku of the obtained results.

To deficiencies in this method can be attributed complexity and insignificant authenticity.

The target/purpose of the proposed invention is an increase in the reliability of the authenticity of the detection of the underground sources of water with the determination of the depth of their bedding and power of the horizon/level.

The stated goal is reached by the fact that from the antenna, connected to the source of SHF power into the earth/ground to the fixed/recorded angle they direct the signal of microwave s-band the subsequent quantitative fixation by the instrument- receiver of reflected from the source of water signal and the mathematical calculation of the parameters of source on the angle of the installation of antenna and the distance from the antenna to the point of emergence of the signal reflected.

The proposed method is based on effekteusileniya and otrazhegniya of elektromagnishchnychykh of the waves of microwave range from the fixed mass of the moving flow of water.Upon falling of the electromagnetic ray/beam of microwave diapazorna into water on top occurs the excitation of its molecules and the conversion of the summary field, whose vector is directed upward perpendicular to the earth's surface.

In the figure of predstvlena of the output of the realization of method.

Antenna 1, connected to the source of SHF power 2, is established/installed to the fixed/recorded angle to the earth's surface in the assumed location of water.The reflected from the water signal is recovered by instrument by receiver (gauge of energy flow poise -19 or imeritelem of the strength of field NFM).

Method is achieved as follows.The 1 ray/beam of the SHF power of microwave range directed from the antenna interesects the flow (or fixed surface) of water, in this case appears the perpendicular to the earth's surface otazhennyy signal, which is recovered by instrument- receiver.

On the distance from the site of installation of antenna to the point of emergence of the ray/beam of (l) and on the known angle of setting the antenna of (d) by trigonometric calculations is found the depth of the bedding of the water-bearing horizon/level.

yu = of l*tg(d)

Arranging/locating antenna at different removals/distances across the flow are defined the power of the water-bearing horizon/level Pyu and the width of flow B. Debit flow will be defined as polshchad' of cross section multiplied by a maximally possible rate of flow of water (0.05 km/h).

For diagnostics of the fixed masses of water they direct antenna at an angle view 45 to the horizon, since the reflection of SHF power occurs at angle of 90 to the entering ray/beam.The depth of bedding in this case will be determined from the formula of yu=l/2.

The practically proposed method can be realized as follows.Antenna is established/installed vertically together with the source of SHF power in transportation means, instrument- receiver is arranged/located a number.For detecting the flows of water with a width of from 50 meters and more the speed of transportation means tyuey ogranichevayut to 40 km/h.Being stopped on by readings/indications of instrument- receiver is produced quantitative geo-hydrodiagnostics using method described above.

The zyavlyaemym method already found 40 underground sources with a depth of bedding of from 6 to 120 meters.

The authenticity of method composes the value, close to 100%, error in the determination of depth is within the limits +/- 5%.

The application of the proposed method makes it possible completely to forego reconnaissance boring, which gives the significant economic effect