Product Description

The Handheld Gamma Spectrometer is designed to accurately measure the concentrations of natural uranium (U), thorium (Th), and potassium (K) in the ground, rocks, and other environmental samples. Whether you're exploring uranium deposits or monitoring environmental radiation, this device delivers precise, reliable, and efficient results.
Key Features:
High Accuracy: Advanced detection technology ensures precise measurement of natural radioactive nuclides.
Portable & Lightweight: Easy to carry and operate in the field, perfect for on-site analysis.
Wide Applications: Ideal for uranium exploration, geological surveys, environmental radiation monitoring, and mineral resource assessment.
User-Friendly Interface: Intuitive design for quick data collection and analysis.
Durable & Reliable: Built to withstand harsh field conditions.
Applications:
Uranium Exploration: Quickly identify and assess uranium deposits.
Environmental Monitoring: Detect and monitor natural radiation levels in soil, water, and air.
Geological Research: Analyze rock samples for natural radioactive elements.
Radiation Safety: Ensure compliance with environmental and safety regulations.
Detector |
φ2"x2 4" BGO |
Energy resolution |
≤12% ( 137Cs ) |
Measuring range |
eU: 1~1000x10-6 (Ur) eTh: 1~ 1000x10-6 (Ur) |
Relative error |
eK: 0.2%~ 1 00% |
Power supply |
eU,eTh: ES7%; eK: E≤12% |
Temperature |
Recharge lithium battery 0°C~+50°C |
Humidity |
≤90% (40°C ) |
Weight |
2 9kg |

Magnetotelluric sounding is a kind of branch method of electrical method by changing the frequency of electromagnetic field. It uses the skin effect of electromagnetic induction, that is, the penetration of high-frequency electromagnetic field is shallow, the penetration of low-frequency electromagnetic field is deep, and the frequency of electromagnetic field is changed to achieve the purpose of sounding under the condition that the distance between the field source and the receiving point is unchanged.
It is a geophysical exploration method using natural alternating electromagnetic fields to study the electrical structure of the earth. Because it does not need artificial power supply, low cost, easy to work, not shielded by high resistance layer, high resolution of low resistance layer, and exploration depth varies with the frequency of electromagnetic field, shallow can be tens of meters, deep up to hundreds of kilometers
