# US 10,310,071 B1 · Standoff geophysical anomaly detection system and method > Agents: this data is available as JSON from the patentgrep API and MCP server — see https://patentgrep.com/llms.txt - Number: US 10,310,071 B1 - Document ID: US10310071B1 - Status: Granted - Kind: B1 - Application number: 11/999,033 - Filed: 2008-09-16 - Granted: 2019-06-04 - Earliest claimed: 2007-09-17 - Assignees: The United States of America as represented by the Secretary of the Army - Applicants: David Mark Hull; Gregory Alton Holifield - Inventors: David Mark Hull; Gregory Alton Holifield - Web page: https://patentgrep.com/patent/US10310071B1 ## CPC - G01S 13/885: {for ground probing (prospecting or detecting using electromagnetic waves G01V3/12)} - G01V 3/08: operating with magnetic or electric fields produced or modified by objects or geological structures or by detecting devices (with electromagnetic waves G01V3/12) - G01V 3/12: operating with electromagnetic waves {(operating with millimetre waves G01V8/005)} - H01Q 1/27: Adaptation for use in or on movable bodies (H01Q1/08, H01Q1/12, H01Q1/18 take precedence) - G01S: RADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES - G01V: GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS (means for indicating the location of accidentally buried, e.g. snow-buried, persons A63B29/02) - H01Q: ANTENNAS, i.e. RADIO AERIALS (radiators or antennas for microwave heating H05B6/72) ## Abstract A system and method for measuring the complex resistivity of a ground section. One embodiment utilizes stand-off capacity-coupled resistivity (CCR) sensing to inject current into the ground at a frequency within the range of 1 Khz to 1 MHz. A sensor detects the voltage which is used to determine the complex resistively of the ground and, thus, ground content. The system and method permits surveys to be conducted at speeds of 10-20 mph or more. Alternatively, current is injected into the ground along a plasma channel that is enabled with a high energy laser. Alternatively, an alpha particle generator may be used to inject the current. Multiple frequencies may be used within the range of 1 KHz to 1 MHz to produce an impedivity spectroscopy to thereby determine and/or display a map of ground content. ## Claims ### Claim 1 A method of measuring the complex resistivity of underground materials using capacitively-coupled resistivity (CCR) sensing over the frequency range from about 1 kHz to about 1 MHz comprising: positioning at least one source element in proximity to the ground to capacitively induce current into the ground at a predetermined frequency in the range of about 1 kHz to about 1 MHz; positioning at least one sensor in proximity to the ground to capacitively receive current from the ground; receiving the current transmitted through at least a portion of the ground at the at least one sensor; making measurements of complex resistivity at the predetermined frequency; and processing the complex resistivity based upon the measurements taken to determine the ground content. ### Claim 2 (depends on 1) The method of claim 1 further comprising displaying the results of the complex resistivity results. ### Claim 3 (depends on 1) The method of claim 1 further comprising providing current into the ground at more than one frequency within the frequency range of about 1 kHz to 1 MHz. ### Claim 4 (depends on 1) The method of claim 1 wherein at least one of the source element or sensor is mounted on a movable platform. ### Claim 5 (depends on 4) The method of claim 4, wherein the movable platform is mounted on a trailer pulled by a vehicle and is adjustable for ground clearance, and further comprises a guard positioned between the source and the ground, wherein guard is driven at the same potential as the at least one source and the at least one sensor such that there is substantially no electric field between them so that the effects of the vertical movement of the platform due to undesirable ground surface conditions are negated when measuring the complex resistivity. ### Claim 6 (depends on 1) The method of claim 1 wherein an impedivity spectroscopy of the ground is taken only in frequency range of 1 kHz to 1 MHz. ### Claim 7 (depends on 1) The method of claim 1 wherein the source element and sensor comprise a dipole-dipole configuration. ### Claim 8 (depends on 7) The method of claim 7 wherein the induced current penetrates into the ground to a depth of substantially one fifth the distance of the dipole-dipole configuration. ### Claim 9 (depends on 1) The method of claim 1 wherein the source element and sensor comprise a pole-potential gradient configuration. ### Claim 10 (depends on 1) The method of claim 1 wherein the current is injected into the ground along a plasma channel that is enabled with a high energy laser. ### Claim 11 (depends on 1) The method of claim 1 wherein the induced current is generated by the at least one source with an operating voltage that is in the range of one to five kV. ### Claim 12 A system for measuring the complex resistivity and providing a representational image of a portion of the ground comprising: a current generator for generating alternating current at a frequency within the frequency range of about 1 kHz to about 1 MHz; at least one source member operatively connected to the current generator for inducing the generated electric current into the ground; at least one sensor for sensing the electrical potential of the electric field in the ground created by the electric current; a receiver for receiving the measurements of the electrical potential of the ground; a processor for calculating the complex resistivity and creating a representative display of ground content based upon the complex resistivity; and a display operatively connected to the processor for mapping the portion of the ground in which current was induced. ### Claim 13 (depends on 12) The system of claim 12 wherein the at least one source member and at least one sensor are configured in an array, and the depth of the ground being displayed is one fifth of the distance across the array. ### Claim 14 (depends on 12) The system of claim 12, wherein the at least one source member and the at least one sensor are arranged in a Wenner alpha array, a Wenner beta array, a Wenner gamma array, a pole-pole array, a dipole-dipole array, a pole-dipole array, a Wenner array, a Schlumberger array, an equatorial dipole-dipole array, or any combination thereof. ### Claim 15 (depends on 14) The system of claim 14, further comprising software configured to render a map of the ground from the electrical potential recorded by the processor for calculating the complex resistivity. ### Claim 16 A method of determining the location of underground materials and/or objects comprising: delivering an alternating current to the ground through a source element configured to induce current into the ground in a non-contacting manner; measuring an electrical potential associated with the current with at least one sensor in a non-contacting manner; recording the electrical potential with a resistivity meter coupled to the at least one sensor electrode to thereby determine the complex resistivity; and rendering a map of the ground from the electrical potential recorded by the resistivity meter. ### Claim 17 (depends on 16) The method of claim 16 wherein a charged-particle beam is used to inject current into the ground. ### Claim 18 (depends on 16) The method of claim 16 wherein current is injected into the ground along a plasma channel that is enabled with a high energy laser. ### Claim 19 (depends on 16) The method of claim 16 further comprising a current generator for generating an electrical current at a predetermined frequency equal to or greater 1 kHz and a processor for processing the received measurements of the electromagnetic field induced into at least a portion of the ground through at the at least one sensor and processing the complex resistivity based upon the measurements taken to determine the ground content.