Automatic Arctic sea ice density measuring device
A density measurement and density detection technology, which is applied in measurement devices, specific gravity measurement, special data processing applications, etc., can solve problems such as non-real-time performance, and achieve the effects of simple steps, low cost, and true and reliable measurement results.
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Embodiment approach 1
[0014] 1. Installation of polar sea ice density measurement device
[0015] The polar sea ice density measuring device of the present invention is suitable for fixed-point monitoring of sea ice, so at first to select a suitable observation point before installation, it is advisable to level the ice in that year, and the sea ice has frozen to a certain thickness (20-30cm above), select the observation point. Drill a 50cm long and 10cm wide ice crevice on the ice surface, then install the sea ice density sensor upright in the ice crevice, and use a cross bar to hold the sensor so as not to fall from the ice crevasse. The single-chip microcomputer controller is installed in an instrument box, and the single-chip microcomputer controller and the sea ice density sensor are connected by wires. The power supply for the whole device is a large-capacity wound lead-acid battery.
[0016] 2. Measurement steps of polar sea ice density
[0017] The device for measuring sea ice density o...
Embodiment approach 2
[0027] In the traditional sampling method to measure sea ice density, generally, a uniform cut of an ice core of 20 cm is used as a sample for density measurement to meet the research needs. Therefore, the support 1 in the present invention is provided with a pair of acoustic wave emitting elements and acoustic wave receiving elements every 15cm from top to bottom, and the diameter of the acoustic wave emitting and receiving elements is 5cm, which ensures that the sea ice is monitored every 20cm. Polar sea ice generally has a thickness of about 2 meters in winter, so setting up 10 pairs of transmitting and receiving elements can meet the needs of the thickness change within 2 meters during the growth of sea ice. Others are the same as Embodiment 1.
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