% Generated by roxygen2: do not edit by hand
% Please edit documentation in R/calc_CosmicDoseRate.R
\name{calc_CosmicDoseRate}
\alias{calc_CosmicDoseRate}
\title{Calculate the cosmic dose rate}
\usage{
calc_CosmicDoseRate(
  depth,
  density,
  latitude,
  longitude,
  altitude,
  corr.fieldChanges = FALSE,
  est.age = NA,
  half.depth = FALSE,
  error = 10,
  ...
)
}
\arguments{
\item{depth}{\link{numeric} (\strong{required}):
depth of overburden (m). For more than one absorber use \cr
\code{c(depth_1, depth_2, ..., depth_n)}}

\item{density}{\link{numeric} (\strong{required}):
average overburden density (g/cm³). For more than one absorber use \cr
\code{c(density_1, density_2, ..., density_n)}}

\item{latitude}{\link{numeric} (\strong{required}):
latitude (decimal degree), N positive}

\item{longitude}{\link{numeric} (\strong{required}):
longitude (decimal degree), E positive}

\item{altitude}{\link{numeric} (\strong{required}):
altitude (m above sea-level)}

\item{corr.fieldChanges}{\link{logical} (\emph{with default}):
correct for geomagnetic field changes after Prescott & Hutton (1994).
Apply only when justified by the data.}

\item{est.age}{\link{numeric} (\emph{with default}):
estimated age range (ka) for geomagnetic field change correction (0-80 ka allowed)}

\item{half.depth}{\link{logical} (\emph{with default}):
How to overcome with varying overburden thickness. If \code{TRUE} only half the
depth is used for calculation. Apply only when justified, i.e. when a constant
sedimentation rate can safely be assumed.}

\item{error}{\link{numeric} (\emph{with default}):
general error (percentage) to be implemented on corrected cosmic dose rate estimate}

\item{...}{further arguments (\code{verbose} to disable/enable console output).}
}
\value{
Returns a terminal output. In addition an
\linkS4class{RLum.Results} object is returned containing the
following element:

\item{summary}{\link{data.frame} summary of all relevant calculation results.}
\item{args}{\link{list} used arguments}
\item{call}{\link{call} the function call}

The output should be accessed using the function \link{get_RLum}.
}
\description{
This function calculates the cosmic dose rate taking into account the soft-
and hard-component of the cosmic ray flux and allows corrections for
geomagnetic latitude, altitude above sea-level and geomagnetic field
changes.

This function calculates the total cosmic dose rate considering both the
soft- and hard-component of the cosmic ray flux.

\strong{Internal calculation steps}

(1)
Calculate total depth of all absorber in hg/cm² (1 hg/cm² = 100 g/cm²)

\deqn{absorber = depth_1*density_1 + depth_2*density_2 + ... + depth_n*density_n}

(2)
If \code{half.depth = TRUE}

\deqn{absorber = absorber/2}

(3)
Calculate cosmic dose rate at sea-level and 55 deg. latitude

a) If absorber is > 167 g/cm² (only hard-component; Allkofer et al.  1975):
apply equation given by Prescott & Hutton (1994) (c.f. Barbouti & Rastin
1983)

\deqn{D0 = C/(((absorber+d)^\alpha+a)*(absober+H))*exp(-B*absorber)}

b) If absorber is < 167 g/cm² (soft- and hard-component): derive D0 from
Fig. 1 in Prescott & Hutton (1988).

(4)
Calculate geomagnetic latitude (Prescott & Stephan 1982, Prescott &
Hutton 1994)

\deqn{\lambda = arcsin(0.203*cos(latitude)*cos(longitude-291)+0.979*
sin(latitude))}

(5)
Apply correction for geomagnetic latitude and altitude above sea-level.
Values for F, J and H were read from Fig. 3 shown in Prescott & Stephan
(1982) and fitted with 3-degree polynomials for lambda < 35 degree and a
linear fit for lambda > 35 degree.

\deqn{Dc = D0*(F+J*exp((altitude/1000)/H))}

(6)
Optional: Apply correction for geomagnetic field changes in the last
0-80 ka (Prescott & Hutton 1994). Correction and altitude factors are given
in Table 1 and Fig. 1 in Prescott & Hutton (1994). Values for altitude
factor were fitted with a 2-degree polynomial. The altitude factor is
operated on the decimal part of the correction factor.

\deqn{Dc' = Dc*correctionFactor}

\strong{Usage of \code{depth} and \code{density}}

(1) If only one value for depth and density is provided, the cosmic dose
rate is calculated for exactly one sample and one absorber as overburden
(i.e. \code{depth*density}).

(2) In some cases it might be useful to calculate the cosmic dose rate for a
sample that is overlain by more than one absorber, e.g. in a profile with
soil layers of different thickness and a distinct difference in density.
This can be calculated by providing a matching number of values for
\code{depth} and \code{density} (e.g. \verb{depth = c(1, 2), density = c(1.7, 2.4)})

(3) Another possibility is to calculate the cosmic dose rate for more than
one sample of the same profile. This is done by providing more than one
values for \code{depth} and only one for \code{density}. For example,
\code{depth = c(1, 2, 3)} and \code{density = 1.7} will calculate the cosmic dose rate
for three samples in 1, 2 and 3 m depth in a sediment of density 1.7 g/cm³.
}
\note{
Despite its universal use, the equation to calculate the cosmic dose
rate provided by Prescott & Hutton (1994) is falsely stated to be valid from
the surface to 10^4 hg/cm² of standard rock. The original expression by
Barbouti & Rastin (1983) only considers the muon flux (i.e. hard-component)
and is, by their own definition, only valid for depths between 10-10^4
hg/cm².

Thus, for near-surface samples (i.e. for depths < 167 g/cm²) the equation
of Prescott & Hutton (1994) underestimates the total cosmic dose rate, as it
neglects the influence of the soft-component of the cosmic ray flux. For
samples at zero depth and at sea-level the underestimation can be as large
as ~0.1 Gy/ka. In a previous article, Prescott & Hutton (1988) give another
approximation of Barbouti & Rastin's equation in the form of

\deqn{D = 0.21*exp(-0.070*absorber+0.0005*absorber^2)}

which is valid for depths between 150-5000 g/cm². For shallower depths (<
150 g/cm²) they provided a graph (Fig. 1) from which the dose rate can be
read.

As a result, this function employs the equation of Prescott & Hutton (1994)
only for depths > 167 g/cm², i.e. only for the hard-component of the cosmic
ray flux. Cosmic dose rate values for depths < 167 g/cm² were obtained from
the "AGE" program (Gruen 2009) and fitted with a 6-degree polynomial curve
(and hence reproduces the graph shown in Prescott & Hutton 1988). However,
these values assume an average overburden density of 2 g/cm³.

It is currently not possible to obtain more precise cosmic dose rate values
for near-surface samples as there is no equation known to the author of this
function at the time of writing.
}
\section{Function version}{
 0.5.3
}

\examples{

##(1) calculate cosmic dose rate (one absorber)
calc_CosmicDoseRate(depth = 2.78, density = 1.7,
                    latitude = 38.06451, longitude = 1.49646,
                    altitude = 364, error = 10)

##(2a) calculate cosmic dose rate (two absorber)
calc_CosmicDoseRate(depth = c(5.0, 2.78), density = c(2.65, 1.7),
                    latitude = 38.06451, longitude = 1.49646,
                    altitude = 364, error = 10)

##(2b) calculate cosmic dose rate (two absorber) and
##correct for geomagnetic field changes
calc_CosmicDoseRate(depth = c(5.0, 2.78), density = c(2.65, 1.7),
                    latitude = 12.04332, longitude = 4.43243,
                    altitude = 364, corr.fieldChanges = TRUE,
                    est.age = 67, error = 15)


##(3) calculate cosmic dose rate and export results to .csv file
#calculate cosmic dose rate and save to variable
results<- calc_CosmicDoseRate(depth = 2.78, density = 1.7,
                              latitude = 38.06451, longitude = 1.49646,
                              altitude = 364, error = 10)

# the results can be accessed by
get_RLum(results, "summary")

#export results to .csv file - uncomment for usage
#write.csv(results, file = "c:/users/public/results.csv")

##(4) calculate cosmic dose rate for 6 samples from the same profile
##    and save to .csv file
#calculate cosmic dose rate and save to variable
results<- calc_CosmicDoseRate(depth = c(0.1, 0.5 , 2.1, 2.7, 4.2, 6.3),
                              density = 1.7, latitude = 38.06451,
                              longitude = 1.49646, altitude = 364,
                              error = 10)

#export results to .csv file - uncomment for usage
#write.csv(results, file = "c:/users/public/results_profile.csv")

} 

\section{How to cite}{
Burow, C., 2025. calc_CosmicDoseRate(): Calculate the cosmic dose rate. Function version 0.5.3. In: Kreutzer, S., Burow, C., Dietze, M., Fuchs, M.C., Schmidt, C., Fischer, M., Friedrich, J., Mercier, N., Philippe, A., Riedesel, S., Autzen, M., Mittelstrass, D., Gray, H.J., Galharret, J., Colombo, M., Steinbuch, L., Boer, A.d., 2025. Luminescence: Comprehensive Luminescence Dating Data Analysis. R package version 1.1.2. https://r-lum.github.io/Luminescence/
}

\references{
Allkofer, O.C., Carstensen, K., Dau, W.D., Jokisch, H., 1975.
Letter to the editor. The absolute cosmic ray flux at sea level. Journal of
Physics G: Nuclear and Particle Physics 1, L51-L52.

Barbouti, A.I., Rastin, B.C., 1983. A study of the absolute intensity of muons at sea level
and under various thicknesses of absorber. Journal of Physics G: Nuclear and
Particle Physics 9, 1577-1595.

Crookes, J.N., Rastin, B.C., 1972. An
investigation of the absolute intensity of muons at sea-level. Nuclear
Physics B 39, 493-508.

Gruen, R., 2009. The "AGE" program for the
calculation of luminescence age estimates. Ancient TL 27, 45-46.

Prescott, J.R., Hutton, J.T., 1988. Cosmic ray and gamma ray dosimetry for
TL and ESR. Nuclear Tracks and Radiation Measurements 14, 223-227.

Prescott, J.R., Hutton, J.T., 1994. Cosmic ray contributions to dose rates
for luminescence and ESR dating: large depths and long-term time variations.
Radiation Measurements 23, 497-500.

Prescott, J.R., Stephan, L.G., 1982. The contribution of cosmic radiation to the environmental dose for
thermoluminescence dating. Latitude, altitude and depth dependences. PACT 6, 17-25.
}
\seealso{
\link{BaseDataSet.CosmicDoseRate}
}
\author{
Christoph Burow, University of Cologne (Germany)
, RLum Developer Team}
