25.1
Leveling is a technique to determine the difference in elevation between various points on the Earth.
Elevation is the vertical distance above or below the region’s mean sea level.
Specific points of known elevation, called benchmarks, are established within a region to carry out leveling in that region.
The general methods of leveling are trigonometric, barometric, and spirit leveling.
The elevation of an inaccessible point P can be determined using trigonometric leveling by measuring the horizontal distance and angle to point P. Then, using trigonometric principles, point P’s elevation is determined.
Barometric leveling can be used to determine the elevation of point C using three altimeters. One is positioned at point C, and the other two are at locations A and B of known elevation.
Air pressure readings from these altimeters are used to calculate point C’s elevation.
Spirit or direct leveling determines the elevation of point D using leveling instruments by taking vertical measurements to point D with reference to a horizontal line of predetermined elevation.
Subtracting the vertical measurement from the horizontal line’s elevation gives point D’s elevation.
수준측량은 먼 지점 사이의 고도 차이를 결정하는 데 사용되는 측량 절차입니다. 고도는 기준점 위 또는 아래의 수직 거리, 일반적으로 평균 해수면(MSL)을 말합니다. 미국에서는 종종 세인트 로렌스 해로를 따라 있는 뿌왕뜨-오-뻬흐의 평균 해수면 관측소를 기준으로 고도를…