conc_soil_mixing | R Documentation |
Compute nuclide concentration in a vertically-mixed steady-state soil, using the approach of Foster et al. (2015)
conc_soil_mixing(h, E, rhos, rhob, p, L, S, fqz = 1)
h |
soil thickness (cm) |
E |
erosion rate (m/Ma) |
rhos |
soil density (g/cm3) |
rhob |
bedrock density (g/cm3) |
p |
production and decay parameters for the nuclide (4 elements vector)
|
L |
Attenuation length (3 elements vector in g/cm2)
|
S |
scaling factors (2 elements vector)
|
fqz |
quartz enrichment factor (default 1) |
Nuclide concentration in soil (at/g)
#' data("prm") # production and decay data p = prm data("Lambda") # attenuation length data L = Lambda altitude = 1000 # site elevation in m latitude = 20 # site latitude in degrees P = atm_pressure(alt=altitude,model="stone2000") # atmospheric pressure at site S = scaling_st(P,latitude) # Stone 2000 scaling parameters rhob = 2.65 # bedrock density (g/cm3) rhos = rhob/2 # soil density (g/cm3) E = 10^seq(log10(0.1),log10(100),length.out = 100) # denudaton rate (m/Ma) plot(NA,xlim=range(E),ylim=c(0.02,6),log="xy", xlab="Denudation rate (m/Ma)",ylab="Concentration (10^6 at/g)") h = 100 # soil depth (cm) C = conc_soil_mixing(h,E,rhos,rhob,p[,1],L,S) lines(E,C/1e6) h = 200 # soil depth (cm) C = conc_soil_mixing(h,E,rhos,rhob,p[,1],L,S) lines(E,C/1e6,col="red") h = 1000 # soil depth (cm) C = conc_soil_mixing(h,E,rhos,rhob,p[,1],L,S) lines(E,C/1e6,col="green") legend("topright",c("1 m","2 m","10 m"),lty=1,col=c("black","red","green"),title="Mixing depth")
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