Showing 96 of total 96 results (show query)

arsilva87

soilphysics:Soil Physical Analysis

Basic and model-based soil physical analyses.

Maintained by Anderson Rodrigo da Silva. Last updated 3 years ago.

18.1 match 11 stars 4.83 score 12 scripts

framverse

framrsquared:FRAM Database Interface

A convenient tool for interfacing with FRAM access databases in R environments.

Maintained by Ty Garber. Last updated 2 months ago.

6.9 match 6 stars 5.06 score 9 scripts

bioxgeo

geodiv:Methods for Calculating Gradient Surface Metrics

Methods for calculating gradient surface metrics for continuous analysis of landscape features.

Maintained by Annie C. Smith. Last updated 1 years ago.

cpp

3.8 match 11 stars 5.88 score 23 scripts 1 dependents

cran

OrgMassSpecR:Organic Mass Spectrometry

Organic/biological mass spectrometry data analysis.

Maintained by Nathan Dodder. Last updated 8 years ago.

1.8 match 3.68 score 2 dependents

tkdweber

spsh:Estimation and Prediction of Parameters of Various Soil Hydraulic Property Models

Estimates model parameters of soil hydraulic property functions by inverting measured data. A wide range of hydraulic models, weighting schemes, global optimization algorithms, Markov chain Monte Carlo samplers, and extended statistical analyses of results are provided. Prediction of soil hydraulic property model parameters and common soil properties using pedotransfer functions is facilitated. Parameter estimation is based on identically and independentally distributed (weighted) model residuals, and simple model selection criteria (Hoege, M., Woehling, T., and Nowak, W. (2018) <doi:10.1002/2017WR021902>) can be calculated. The included models are the van Genuchten-Mualem in its unimodal, bimodal and trimodal form, the the Kosugi 2 parametric-Mualem model, and the Fredlund-Xing model. All models can be extended to account for non-capillary water storage and conductivity (Weber, T.K.D., Durner, W., Streck, T. and Diamantopoulos, E. (2019) <doi:10.1029/2018WR024584>. The isothermal vapour conductivity (Saito, H., Simunek, J. and Mohanty, B.P. (2006) <doi:10.2136/vzj2006.0007>) is calculated based on volumetric air space and a selection of different tortuosity models: (Grable, A.R., Siemer, E.G. (1968) <doi:10.2136/sssaj1968.03615995003200020011x>, Lai, S.H., Tiedje J.M., Erickson, E. (1976) <doi:10.2136/sssaj1976.03615995004000010006x>, Moldrup, P., Olesen, T., Rolston, D.E., and Yamaguchi, T. (1997) <doi:10.1097/00010694-199709000-00004>, Moldrup, P., Olesen, T., Yoshikawa, S., Komatsu, T., and Rolston, D.E. (2004) <doi:10.2136/sssaj2004.7500>, Moldrup, P., Olesen, T., Yoshikawa, S., Komatsu, T., and Rolston, D.E. (2005) <doi:10.1097/01.ss.0000196768.44165.1f>, Millington, R.J., Quirk, J.P. (1961) <doi:10.1039/TF9615701200>, Penman, H.L. (1940) <doi:10.1017/S0021859600048164>, and Xu, X, Nieber, J.L. Gupta, S.C. (1992) <doi:10.2136/sssaj1992.03615995005600060014x>).

Maintained by Tobias KD Weber. Last updated 5 years ago.

1.7 match 1.00 score 3 scripts