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Page Title: TRIGONOMETRIC LEVELING
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CHAPTER 7 INDIRECT LEVELING/LEVEL AND TRAVERSE COMPUTATIONS
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Engineering Aid 1 - Advanced Structural engineering guide book
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Figure 7-3.—Lines of indirect levels.

Figure 7-1.—Diagram of a two-base altimeter survey. communication,  a  timepiece  is  needed  for  each altimeter.  These  timepieces  are  synchronized,  and  the altimeter readings are taken at prearranged intervals. Figure 7-1 shows a diagram of the two-base method when three altimeters are used. This figure shows the known elevations of the lower (Sta. A) and upper (Sta. B)  base  stations.  Altimeter  readings  at  each  of  the  base stations and at field station C are also shown. The difference in elevation is computed by direct proportion, using  either  the  lower  base  or  the  upper  base  as reference.  For  example,  to  find  the  differences  in elevation between Sta. A and Sta. C, we proceed as follows: Then this result is added to the elevation of Sta. A, as shown in solution No. 1, figure 7-1. If we use the upper base  as  a  reference,  you  compute  the  difference  in elevation by using the same method; but to compute from Sta. B, subtract the result, as shown in solution No. 2, figure 7-1. For a more accurate result, altimeter surveys should be made on days when there is not much variation in barometric  pressure.  Windy  days  when  detached  clouds are  traveling  rapidly  should  be  avoided  because alternating sunlight and shade over the survey area can cause fluctuations in the altimeter reading. Steady barometric  pressures  generally  occur  on  days  with gentle winds and an overcast sky. The recommended time for observations is 2 to 4 hours after sunrise and 2 to 4 hours before sunset. Midday observation must be avoided if possible. Remember, you must shade the instrument at all times, and you must avoid jarring the instrument suddenly during its transfer from one station to  another. TRIGONOMETRIC LEVELING When  you  know  the  vertical  angle  and  either  the horizontal or slope distance between two points, you can apply the fundamentals of trigonometry to calculate the difference in elevation between the points. That is the basic  principle  of  trigonometric  leveling.  This  method of  indirect  leveling  is  particularly  adaptable  to  rough, uneven  terrain  where  direct  leveling  methods  are impracticable or too time consuming. As in any survey, the equipment that you will use in trigonometric leveling depends  on  the  precision  required.  For  most trigonometric-leveling surveys of ordinary precision, angles are measured with a transit, or alidade, and distances are measured either with a tape or by stadia, which you will study in chapter 8. On reconnaissance surveys the vertical angles may be measured with a clinometer, and distances maybe obtained by pacing. The  method  used  in  trigonometric  leveling  is described in the following paragraphs: 7-2

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