Rowan Cockett rowanc1

There are two different forms of Richards equation that differ on how they deal with the non-linearity in the time-stepping term. Here we reproduce results from a seminal paper, and show the ease with which you can do this in SimPEG and Richards python packages.

In this tutorial we will create a simple linear problem from scratch using the SimPEG framework.

Playing with anisotropy in SimPEG.

In this tutorial we will go over creating a mesh, and the basics of numbering, counting, and naming conventions. With these skills you can move faster, and move between different meshes (hopefully) with ease!

Working to incorporate DC resistivity inversions in the new SimPEG framework.

	%% Print Table
	%
	% This function will print an ASCII table, for example:
	%
	% Decrease in Error, t_fo = 100
	% ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
	% mu=0.1 mu=0.5 mu=1.0
	% .--------------------------------------------
	% h=0.01 \| 8.692922e-01 8.530311e-01 4.018080e-01
	% h=0.02 \| 5.797046e-01 6.220551e-01 7.596669e-02

	import numpy as np
	import matplotlib.pyplot as plt



	def syntheticSeismogram(v, rho, d):
	"""
	function syntheticSeismogram()

	syntheicSeismogram generates a synthetic seismogram for a simple 1-D

	clear;
	clear CLASSES;
	clc;
	close all;
	try
	dbquit('all');
	clear;
	end;

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	<div class="highlight"><pre><span class="kn">import</span> <span class="nn">visiblegeology</span> <span class="kn">as</span> <span class="nn">VG</span>
	<span class="n">GH</span> <span class="o">=</span> <span class="p">(</span>
	<span class="n">VG</span><span class="o">.</span><span class="n">Erosion</span><span class="p">()</span> <span class="o">+</span>