My Henssge online tool (small layout; large layout) solves the bi-exponential formula as laid out in Henssge and Madea (2004) Estimation of the time since death in the early post-mortem period. Forensic Science International 144 (2004) 167-175.
Henssge at the time still regarded the solution to be obtained, by calculators, to necessarily employ some iteration procedure and I do remember some Casio and Hewlett Packard programs that were programmed with iterations. They took a while to get there.
It is now 2015.
I implemented this pHp online tool roughly ten years ago, basically without thinking a lot, in 2005, because the approach is obvious.
I only sat down to write this because it was stated that this could not be done using pHp, when our IT guys proposed that, so the bet was over 1 cup of coffee, which I won #holdmybeer.
I love pHp because it stays where you put it, and it is superbly accessible. Obviously this works, and it works very fast.
The pHp code was hand written using a simple text editor.
It later was modified to contain value delimiting comments and tables helping with the correction factor and so on. It was also validated, in addition to or own tests it was later validated by South African forensic pathologists.
There is a small layout geared towards mobile device usage and a large layout with larger displays in mind; that also contains ancillary information such as corrective factor tables.
So, how is that done?
In essence, following exactly Henssge, we establish the estimate for the time of death
as a function of body core temperature
, environmental temperature
, initial body core temperature at time of death
(which is usually but not necessarily
), and as function of the body mass
to be estimated here and the corrective factor
(basically modelling environmental aspects of cooling such as humidity and body covers, see the large layout for detailed numerical suggestions).
So all one wants to do is find the solution for something like this equation:
(1)
(2)
with
(3)
Up to an ambient temperature TU≤23.2∘C: Eq. 1; for any ambient temperature TU≥23.3∘C: Eq. 2.
With pHp, the approach is obviously brute force to be fast, and it seems that I used the thinking behind the Newton Raphson method to pragmatically get the job done.
This equation is not hard to understand: given realistic values for all given variables, you will have estimated or guessed the correct time of death estimate
once the terms on both sides of the equal signs are actually equal, and you are close to guessing the correct time of death estimate according to this model once you approximate equality. So when
(as in Eq. 1 or 2), it follows that
.
Just performing a forward calculation of both terms of that equations 1 and 2, using a large vector of all
possible time of death estimates
with
will yield
different equations.
The difference between both terms (on the right and left side of the equation) tells you how close you guessed, and you have guessed well once the difference approximates zero, and if we calculate a few hundred options for
and
across a set of some possible time of death estimates, the whole set of
and
will contain a best guess i where
is minimal, if not zero.
So, I just shove a vector
of all possible sensibly relevant times of death
(tip: some
discrete values are totally enough or so to cover the extent of the method somewhere between time of death estimates ranging from around an hour to two or so days) through the following equation in order to determine, at once, all
values for the difference vector
with
and as a solution, identify the one value
for which
.
So in essence, within two steps of actually “calculating” something, basically, you are done.
For better method application, the coefficients differ, depending on specifics, maybe see the paper with regard to this [link].