Soil Electrical Conductivity
Electrical conductivity of soil paste extracts from the Lower Arkansas River Valley, at sites upstream and downstream of the John Martin Reservoir.
data(ArkansasRiver)
The format is: List of 2 $ upstream : num [1:823] 2.37 3.53 3.06 3.35 3.07 ... $ downstream: num [1:435] 8.75 6.59 5.09 6.03 5.64 ...
Electrical conductivity is a measure of soil water salinity.
This data set was supplied by Eric Morway (emorway@usgs.gov).
Eric D. Morway and Timothy K. Gates (2011) Regional assessment of soil water salinity across an extensively irrigated river valley. Journal of Irrigation and Drainage Engineering, doi:10.1061/(ASCE)IR.1943-4774.0000411
data(ArkansasRiver) lapply(ArkansasRiver, summary) upstream <- ArkansasRiver[[1]] downstream <- ArkansasRiver[[2]] ## Fit normal inverse Gaussian ## Hyperbolic can also be fitted but fit is not as good fitUpstream <- nigFit(upstream) summary(fitUpstream) par(mfrow = c(2,2)) plot(fitUpstream) fitDownstream <- nigFit(downstream) summary(fitDownstream) plot(fitDownstream) par(mfrow = c(1,1)) ## Combined plot to compare ## Reproduces Figure 3 from Morway and Gates (2011) hist(upstream, col = "grey", xlab = "", ylab = "", cex.axis = 1.25, main = "", breaks = seq(0,20, by = 1), xlim = c(0,15), las = 1, ylim = c(0,0.5), freq = FALSE) param <- coef(fitUpstream) nigDens <- function(x) dnig(x, param = param) curve(nigDens, 0, 15, n = 201, add = TRUE, ylab = NULL, col = "red", lty = 1, lwd = 1.7) hist(downstream, add = TRUE, col = "black", angle = 45, density = 15, breaks = seq(0,20, by = 1), freq = FALSE) param <- coef(fitDownstream) nigDens <- function(x) dnig(x, param = param) curve(nigDens, 0, 15, n = 201, add = TRUE, ylab = NULL, col = "red", lty = 1, lwd = 1.7) mtext(expression(EC[e]), side = 1, line = 3, cex = 1.25) mtext("Frequency", side = 2, line = 3, cex = 1.25) legend(x = 7.5, y = 0.250, c("Upstream Region","Downstream Region"), col = c("black","black"), density = c(NA,25), fill = c("grey","black"), angle = c(NA,45), cex = 1.25, bty = "n", xpd = TRUE)
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