Seismic ionospheric disturbance research shows that ionospheric change caused by seismic activity exists in seismic ionospheric precursory phenomena of space plasma change before an earthquake. For example

the electronic total content (TEC)

electron density (Ne)

ion density (Ni)

electron temperature (Te)

and ion temperature (Ti) are abnormal. Therefore

monitoring earthquakes and providing an early warning is feasible by measuring pre-earthquake plasma changes. The Langmuir probe effectively detects space plasma and can be used to measure parameters such as electron density and electron temperature. The feasibility of the Langmuir probe in seismic remote sensing observation is studied based on the mission of the China seismo-electromagnetic satellite.The Langmuir probe payload consists of three parts: a sensor

an extension rod

and an electronics box. The sensor has a spherical configuration; its upper hemisphere is a collecting electrode

and its lower hemisphere is a protective electrode. The same sweep voltage is applied to the upper and lower hemispheres to eliminate the terminal effect of the connecting point between the traditional spherical structure and the boom. The sensor surface is coated with TiN material to ensure uniform surface work function and to prevent space atomic oxygen erosion. The Langmuir probe is designed with two sensors

each of which is redundant.The plasma environment calibration test of the Langmuir probe flight model was conducted in INAF-IAPS. The test method measures the electron density and temperature at six different distances from the plasma source and compares the results with the measured results of the INAF-IAPS reference Langmuir probe. The calibration test result shows that the Langmuir probe test data are consistent with the test data of the INAF-IAPS reference Langmuir probe. Thus

the design of the Langmuir probe can achieve the missions of the satellite.The scientific data of the Langmuir probe include level 0

level 1

and level 2 data. The interference is removed from the raw data

the error is corrected

and repetition is eliminated to generate level 0 data. The level 0 data are revised by calibration parameters to produce level 1 data

which are preliminary physical data. The level 2 data are the final physical data

which contain geographic and geomagnetic coordinates

satellite time

space position

and satellite attitude information.With the launch of the China seismo-electromagnetic satellite

the Langmuir probe is applied for the first time in the field of earthquake remote sensing observation in China. The electron density and temperature are obtained by the Langmuir probe

and the ion density and temperature are obtained by a plasma analyzer. Other space electromagnetic information is obtained by an electric field instrument and a magnetometer. These data are studied synthetically to provide a new method for seismic stereoscopic observation and exploration for early earthquake prediction.