Instructions
UM-0085-B09  DT80 Range User Manual  Page 80 
RG 
c..dIV  IV Contents 
Example: 
21..40IV 
c+0 
Contains the count of cycles for the first cycle size class 
21IV 
c+1 
Contains the count of cycles for the second cycle size class 
22IV 
c+2 
Contains the count of cycles for the third cycle size class 
23IV 
  ⇓ 
⇓ 
⇓ 
d–7 
Contains the count of cycles for the last cycle size class 
33IV 
Summary data 
d–6 
Contains the count of cycles that over-ranged the maximum cycle size 
34IV 
d–5 
Contains the count of all cycles 
35IV 
d–4 
Contains the maximum buffered cycles 0..100 (or 99999 if the buffer has overflowed and 
buffered half-cycles have been lost) 
36IV 
d–3 
Contains the minimum valley encountered 
37IV 
d–2 
Contains the maximum peak encountered 
38IV 
d–1 
Contains the total number of good points 
39IV 
d–
0 
Contains the total number of "in error" points (out of range, for example) 
40IV 
In practice, some cycles do not close immediately and are buffered until a closure is detected. Variable d–4 contains a 
count of these unclosed or "half cycles". 
Note: The rainflow channel option can be used on a maximum of 16 channels. 
Rainflow cycle data is collected at a rate dependent on the frequency of influences deforming the structure under test. 
These might be quite slow events (such as waves crashing against a sea wall), or quite fast (such as a high speed boat 
hull travelling through waves). 
Place the channel being sampled for rainflow in a schedule that’s triggered fast enough to take sufficient readings during 
a cycle to adequately characterise the loop closures. For example, the schedule 
RA50T 3BGI(RAINFLOW:a:b:c..dIV,W) 
measures the input every 50ms (20 times/sec), and counts loop closures. The W channel option declares this as a 
working channel (does not return or log the individual samples of strain-stress. 
Reporting Rainflow Data 
Rainflow data is collected over long periods of time using the RAINFLOW channel option. Then, periodically, the rainflow 
cycle histogram can be retrieved by a computer, using the 
RAINFLOW command. 
To report the rainflow cycle histogram, send the original rainflow channel option exactly as originally defined for the 
channel, but as a command. That is, send the command: 
RAINFLOW:a:b:c..dIV 
 The DT80 returns a tabular report as illustrated below: 
RAINFLOW:72:5:1..27IV 
Rainflow ( 5% rejection) 01/01/2000 00:03:43 
 n IV/CV  Range Mean Cycles 
============================================== 
 1 1 0.0 0.0 0 
 2 2 3.6  11.4 27 
 3 3 7.2 11.3 6 
 4 4 10.8 12.4 6 
 5 5 14.4 11.9 6 
 6 6 18.0 12.8 9 
 7 7 21.6 12.3  2 
 8 8 25.2 0.0 0 
 9 9 28.8 0.0 0 
 10 10 32.4 0.0 0 
 11 11 36.0 18.0 1 
 12 12 39.6 0.0 0 
 13 13 43.2 0.0 0 
 14 14 46.8 0.0 0 
 15 15 50.4 0.0 0 
 16 16 54.0 0.0 0 
 17 17 57.6 0.0 0 
 18 18 61.2 0.0 0 
 19 19 64.8 0.0 0 
 20 20 68.4 0.0 0 
 21 21 >= 72.0 0.0 0 
============================================== 
Total cycles  58 
Peak/Valley mean 12.6 
Max Peak 71 
Min Valley -1 
Max buffered cycles 11 
Valid input points % 100.00 










