1a) There is no formula to convert from a
time pulse to a
DLF. An integration technique is used. This technique is explained in a newsletter article. If you don't have a hard copy of the
November 1994 issue, you can find it in the
Newsletters section of this web site. Here is
the direct link to that issue. The article begins on page 9.
1b) The maximum table frequency is the frequency where the DLF curve (you are about to generate) stops. This should coincide with your analysis cut-off frequency.
1c) The DLF curve is a generated set of points. This setting determines how many points make up the curve. You want enough so that the interpolation (between points) is accurate. You don't have to go crazy here, 25 to 40 points is usually enough.
2a) MU + KU = -Mu<sub>g</sub> from Gupta eq 1.13.
2b) For a seismic analysis, the loading on the system is taken from "u<sub>g</sub>", at each natural frequency of the system. For all other spectrum types, the DLF value at the natural frequency is used instead, because there is no Mu<sub>g</sub>.
3) The mass participation factor simply gives an indication of the importance of the modes (natural frequencies) relative to one another, in the overall system response.
4) Check the reference section of this website. There are a number of texts listed in the "General Engineering Reference" section.