| Assigned: | 13 February, 1998 |
| Due: | Try to do at at least up to Step 4 by 23 February. Do more if you can - it will be worth it. E-mail me your reduced gravity file (or tell me the filename). If you manage to get all the way through this exercise, e-mail me an example of a section you produced, and/or a Postscript file of the plots you made. |
After a busy day in the field collecting gravity data, the investigator must next correct all the raw gravity readings to remove all of the expected effects of changes in latitude, elevation, tides, etc. before the fun part of interpretation starts.
This is a straightforward procedure but can be tedious and unnecessarily time consuming if done by hand (especially if you have to compute tidal corrections!). To make this process a bit less onerous, the program Xreduce was written to allow the investigator to enter raw gravity observations directly into a spread sheet type format and ask the computer to compute Simple Bouguer Anomalies.
In this exercise you will learn a few of the basic functions of Xreduce. You should also consult the manual for this program at http://gretchen.geo.rpi.edu/roecker/manuals/Xreduce/Xreduce.html for information on how this program works.
Starting the program.
Xreduce follows a lot of the same procedures as Xgrav, so starting up the program and getting it going are pretty similar. Once you've set up the DISPLAY properly, start the program by typing
Xreduce
A window should appear that looks similar the the Xgrav window (with panels and a canvas).
Creating a Gravity Data File.
The following are actual Raw Gravity readings from a survey by the 1997 Applied Geophysics class in Canajoharie:
Canajoharie Field Site Raw Gravity Data
North East Elev Raw Grav Station Date Time
44 -74.5 0 880.232 BASE1 97 4 12 10 15
0 0 0 880.340 BASE2 97 4 12 16 15
50 35 -0.3 879.97 ST1 97 4 12 11 10
100 40 -0.4 879.909 ST2 97 4 12 11 25
150 45 -0.1 879.177 ST3 97 4 12 11 38
200 50 -0.23 879.752 ST4 97 4 12 11 50
250 55 -0.35 877.93 ST5 97 4 12 12 43
300 60 -0.15 879.387 ST6 97 4 12 12 55
350 70 -0.15 878.7 ST7 97 4 12 13 4
400 80 -0.5 878.565 ST8 97 4 12 13 11
500 90 1 878.072 ST10 97 4 12 13 17
600 100 0.65 878.033 ST12 97 4 12 13 24
700 110 0.95 880.097 ST14 97 4 12 13 26
800 120 0.75 880.285 ST16 97 4 12 13 32
900 130 -0.9 881.795 ST18 97 4 12 13 36
1000 140 -2.4 882.482 ST20 97 4 12 13 43
1100 150 -2.6 883.56 ST22 97 4 12 14 37
1200 160 -3 882.95 ST24 97 4 12 14 44
1300 170 -2.63 882.87 ST26 97 4 12 14 49
1400 180 -1.97 882.673 ST28 97 4 12 14 55
1500 190 -1.95 883.548 ST30 97 4 12 15 3
1600 200 -1.6 884.1 ST32 97 4 12 15 10
1700 210 -2.6 884.868 ST34 97 4 12 15 13
1800 220 -1.7 885.177 ST36 97 4 12 15 17
1900 230 -2.6 885.883 ST38 97 4 12 15 23
2000 240 -4.6 889.868 ST40 97 4 12 15 28
2100 250 -5.25 892.072 ST42 97 4 12 15 33
2200 260 -7.55 895.703 ST44 97 4 12 15 41
The positional coordinates of the stations (in the North, East, and Elev) columns are the relative location distances, in FEET, from the base station (location =(0,0,0)). For example, station ST42 is 2100 feet North, 250 feet East, and 5.25 feet BELOW the base station (BASE1 and BASE2).
The Raw Grav column are the readings taken right from the meter (the RPI D Meter).
The "Station" is an arbitrary identifier for the point taken.
The final columns are the date (All data from April 12, 1997) and local time (ranging from 10:15 to 16:15).
Your first task is to input this information into the program. Here is how you do it:
NOTE ON POSITION: This program expects that the first two entries will be the starting and ending Base station readings. The first base station entry should show position in longitude and latitude and the second in postion relative to the local coordinate system (typically the base station is the origin, so this is just (0,0). Also note that the order of input is East, then North, while the those in the data table above are (North, East).
For purposes of this exercise, quit the program and restart it before doing the next step so that you will try the "READ" function.
Reducing a Gravity Data File.
In this step you reduce the data, which means you convert the raw gravity readings into Free Air or Bouguer Anomalies.
NOTE:The status of Gravity Data Files is controlled by the buttons on the second row that say "DEL GRAV", "SEL GRAV", "GRAV++" and "GRAV--". These buttons do the same operations as the "SEL DAT", "DEL DAT" buttons of Xgrav.
After you select "OK" the program will type a bunch of lines on the screen from which you started Xreduce. When it is finished, the "REDUCE GRAV" button will return to its normal color and shade.
Plotting/Viewing a Gravity Data File.
You can make a map showing the locations of your gravity data stations using the "DRAW" button. If you have any data or map files in memory this function will draw a map of them in the canvas part of the window. You can make a hard copy of this picture by useing the PS-PREF and PS-DUMP buttons (in that order) to generate a PostScript file.
Selecting a Gravity Profile
Very often we want to make a 2D profile of our readings for further modeling. Xreduce makes this easy to do by allowing you to project points onto a vertical plane (hence reducing the 3D problem to a 2D problem). What you want to do first is decide that the orientation of your profile should be (many times it is perpendicular to some geologic trend), and which data point you want to include in the profile. The way you impliment your decision is to draw a box (or "Section") on the screen. All of the stations within the box will be selected for the profile, and their coordinates will be projected onto a plane that bisects the box. Here is a step by step of how you do this:
You now should have a line on the screen with a cross ("+") at each end. Now you are ready to draw in the box.