Paper No. 0
Presentation Time: 10:30 AM
AN INCREMENTAL-ISOTHERMAL MODEL FOR RADIOGENIC ISOTOPE ACCUMULATION WITH CHANGING TEMPERATURE
Accumulation of radiogenic daughter isotope reflects decay and
loss processes that are functions of time (t) and temperature (T).
The theory of cooling ages described by the classic work of Dodson provides
a framework to consider apparent age, kinetic parameters for loss, and
closure temperature. Its application, however, is restricted by several
assumptions, including a monotonic cooling process and an initial zero
daughter concentration that preclude many situations, for example, where
heating and partially resetting are involved. A forward-modeling,
incremental-isothermal approach is proposed to overcome these restrictions
and reveal the accumulation of radiogenic isotope (and apparent age) with
time in any given T-t path. It assumes that daughter isotope
loss in nature can be described by an Arrhenius relationship for a first-order
reaction or diffusion. Using the incremental-isothermal model, a
known or prescribed T-t path is discretized into many small intervals
in which the temperature (Ti) is constant as is the reaction
coefficient, ki. The solution to the rate equation
applied to an individual interval i is, in simplified and general
form: xi=(lCp/ki)(1-e-kiDt)+xi-1e-kiDt
, where: xi is the concentration of daughter at the end
of time interval i; l is the decay constant;
Cp
is the concentration of the parent (here neglecting change with time);
and Dt is the time step. Among
the advanges of such modeling are: 1) it allows simulation of any complex
T-t path, including multiple stages of cooling and heating; 2) it
does not require an assumption of zero initial daughter concentration and,
thus, is suitable for middle-low temperature processes; and, 3) it can
explicitly yield concentration or apparent age evolution for different
minerals along a complex T-t path. The application of the
method is illustrated using the K-Ar system in various minerals and a variety
of T-t paths. The results of the modeling provide a new perspective
for understanding the meaning of apparent isotopic ages.