sm4sd-Package: sm4sd: A package for computing the conductivity of the pore...

Description Details

Description

The sm4sd provides several methods to extract the pore water electrical conductivity based on data including Hilhorst model (deterministic model) and time-varying dynamic linear model approach.

Details

Salt concentration of bulk is a strong indicator for world's agricultural productivity. One way to mesure it is through determining the pore water conductivity of soil, σp. According to Hilhorst, σp can be determined from the equation:

σp=εpσb/bσb=0)
where

The values εb and σb can be mesured in the bulk soil using a dielectric sensor; εp is a function of temperature; and εσb=0 appear as a offset of the linear relationship between εb and σb depending on soil type. In his work, he recommended using 4.1 as a generic offset.

Once the offset is fixed, this model is deterministic. The producer of capacitance soil moisture sensors 5TE recommends the use the an offset εσb=0 of 6 while another study found that this value is appropriate and does not present a good linear relationship between εb and σb Giving the randomness, Basem, Jose and Gerd described a statistical approach using the time-varying dynamic linear model (dlm). In this work, they considered the offset εσb=0 as an unknow parameter which is also estimaded by the model. The model can be formulated as follow:

yt = Atxt + vt
xt = xt-1 + wt
where

The sm4sd contrains several classes:

For more details, check the class definitions.


4301350/sm4sd documentation built on June 14, 2020, 4:22 p.m.