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JQY-1 Fluid Sampler Probe
PRODUCT PARAMETERS
- High torque motor drives the ball screw
- Sample capacity 1L, larger chambers can be customized
Description
Abstract
JQY-1 Fluid Sampler Probe is a probe tube with an electric valve installed on the cavity. Before the probe tube is placed in the borehole, the valve remains normally closed. The winch lowers the probe tube to the specified depth. The computer activates the electric valve on the probe tube through the software. After the cavity is filled with fluid, the electric valve on the probe tube is activated again through the software to keep it normally closed. Then the probe tube is taken out and the manual valve at the bottom of the probe tube is used to pour the sample.

Applicable Conditions
● Cased
● Bare hole fill with water
● Bare Dry hole
Applications
● Groundwater and well water quality surveys
● Environmental investigation
● Investigate water quality conditions at different depths
● Field sampling laboratory analysis
Features
● High torque motor drives the ball screw
● Sample capacity 1L, larger chambers can be customized
Specifications
| Volume | 1L |
| Valve drive | Motor drive |
| Signal output | Bipolar encoding |
FAQ
① In SI, it is m·s-2, and one percent of it is the international unit abbreviation g.u.;
② Conversion between SI and CGS: 1g.u.=10-1 mGal
Gravitational field: The space around the earth with gravity is called the gravitational field.
Gravitational potential: The gravitational potential W in the gravitational field is equal to the work done by a particle of unit mass moving from infinity to that point.
① The normal gravity field of the earth: Assuming that the earth is a rotating ellipsoid (reference plane), the surface is glossy, the internal density is uniform, or it is distributed in concentric layers, the density of each layer is uniform, and the deviation of the shape of the ellipsoid from the geoid is very small, then the gravity field generated by the earth is the normal gravity field.
② The normal gravity value is only related to the latitude, the smallest at the equator and the largest at the poles, with a difference of about 50,000 g.u.; the rate of change of the normal gravity value with latitude is the largest at 45° latitude, and zero at the equator and the poles; the normal gravity value decreases with increasing altitude, and its rate of change is -3.086 g.u.. The main feature of the long-term change is the "westward drift" of the geomagnetic elements, both the dipole field and the non-dipole field drift westward, and have a global nature.
The gravitational field strength is equal to the gravitational acceleration in both numerical and dimensional terms, and the two are in the same direction. In gravity exploration, all references to gravity refer to gravitational acceleration. The gravitational field strength at a point in space is equal to the gravitational acceleration at that point.
Gravity exploration is an exploration method that is based on the density difference of rocks and ores. Since density difference will cause local changes in the normal gravity field of the earth (i.e. gravity anomaly), it is used to solve geological problems by observing and studying gravity anomalies.
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