Groundwater flow meter
AssigneeK-V Associates, Inc.
InventorsWilliam B. Kerfoot, Stuart M. Skinner, Jr.
Life of this patent
Estimating the term…
Abstract
Flow characteristics of a fluid through a permeable solid medium are determined by introducing a predetermined quantity of thermal energy at a highly localized point within the medium and subsequently mapping temperatures around such point to determine the direction and rate of fluid flow through the medium.
Claims20
The method of measuring a flow characteristic of a fluid, which comprises the steps of:
- (a) providing a heat conductive porous medium;
- (b) heating a localized region of said heat conductive porous medium through which fluid is flowing, the heat conductivity of the porous medium being substantially greater than the heat conductivity of the fluid;
- and
- (c) measuring the temperature of the medium at at least two regions spaced from said localized region and determining a flow characteristic of the fluid therefrom.
The method of measuring a flow characteristic of a fluid, which comprises the steps of:
- (a) heating a localized region of a heat conductive medium through which fluid is flowing, the heat conductivity of the medium being substantially greater than the heat conductivity of the fluid;
- (b) measuring the temperature of the medium at at least two regions spaced from said localized region and determining a flow characteristic of the fluid therefrom, and
- the heating of step (a) is effected by heating the medium for a short period of time at said localized region and effecting step (b) subsequent to such heating.
The method of measuring flow characteristics of a fluid, which comprises the steps of:
- (a) establishing a thermal field in a porous medium disposed within the fluid under test, the heat conductivity of the medium being at least 10 times greater than the heat conductivity of the fluid;
- (b) measuring temperature peaks within different regions of the thermal field;
- and
- (c) determining a flow characteristic of the fluid from the measurements of step (b).
The method of measuring the direction of flow of a fluid, which comprises the steps of:
- (a) positioning a porous medium in the flowing fluid, said medium having an array of temperature sensors therein and having heat conductivity much greater than that of the fluid;
- (b) heating the medium for a short period of time at a localized position spaced from said sensors;
- (c) measuring the temperature peaks at said sensors due to the heat applied in step (a) subsequent to cessation of the heating of step (b);
- and
- (d) determining the direction of fluid flow from the measurements of step (c).
The method of measuring the direction and rate of flow of a fluid, which comprises the steps of:
- (a) positioning a porous medium in the flowing fluid, said medium having an array of temperature sensors therein and having heat conductivity much greater than that of the fluid;
- (b) heating the medium for a short period of time at a localized position spaced from said sensors;
- (c) measuring the temperature peaks at said sensors due to the heat applied in step (b) subsequent to cessation of the heating of step (b);
- and
- (d) determining the direction and rate of flow of the fluid from the measurements of step (c).
The method of measuring the rate of flow if a fluid, which comprises the steps of:
- (a) positioning a porous medium in the flowing fluid, said medium having a pair of temperature sensors therein which are spaced apart in the direction of flow of the fluid whose flow rate is to be measured and having heat conductivity much greater than that of the fluid;
- (b) heating the medium for a short period of time at a localized position spaced between said temperature sensors;
- (c) measuring the peak temperature differential between said sensors due to the heat applied in step (b) subsequent to cessation of the heating of step (b);
- and
- (d) determining the rate of fluid flow from the measurement of step (c).
The method of obtaining a linear measurement of capillary groundwater flow which comprises the steps of:
- (a) providing a porous mass composed of uniform spherical particles having a diameter within the range of 0.1-1.0 mm and a heat conductivity of at least 10 times that of water and having an array of heat sensors embedded therein and a heating source centrally disposed among said sensors;
- (b) embedding the porous mass within the ground so as to be exposed to groundwater flow;
- (c) energizing said source for a predetermined time;
- (d) measuring the peak differentials in temperature exhibited between diametrically opposed sensors of said arrays;
- and
- (e) determining groundwater flow as a linear function of the maximum peak differential measured in step (d).
Dependencies are inferred from the claim text.