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.
水准测量是一种用于确定相远距离点之间高程差异的测量程序。高程是指高于或低于参考基准面(通常是平均海平面 (MSL))的垂直距离。在美国,高程通常参考圣劳伦斯海道沿线的里穆斯基神父点(Father Point Rimouski)的平均海平面站。为了使基准面易于获取,整个地区建立了永久性标记。这些标记称…