Water balance is known as the balance of water entering the system and the water that leaves within a specified time, but to understand it better we need to understand: what is a watershed? Unterstood as a whole, a unity, as a system, as the space bounded by the union of all the headers that form the main river through the territory drained by a single natural drainage system.
Read MoreA watershed can be defined as “the topographic area within which apparent surface water runoff drains to a specific point on a stream or to a waterbody such as a lake” (Shimon, 2010), this way a watershed works as a large water collector converting water inputs into runoff and water storage (Chavarri, 2012). Knowing watershed´s hydrological characteristics (precipitation, runoff, evapotranspiration, and groundwater infiltration) allows to evaluate spatial and temporal water resources availability, it is useful for water resources allocation and flow control. Water balance is a tool that allows knowing basin characteristics by application of the mass conservation principle or continuity equation (Rose, 2004; Essam, 2007), according to rhis principle, any difference between inputs and outputs must be reflected in a change in the storage of water within the budget area (UNESCO, 1988; Shimon, 2010).
Read MoreThis question has been popular for the last three or four years. I have been using Quantum GIS (QGIS) from version 0.8, and now QGIS is on version 2.4.
Read MoreTutorial about how to apply styles in QGIS.
Read MoreSimple tutorial about cross seccions with the Profile Tool plugin on QGIS.
Read MoreHi Saul, I am Giuseppe and I watched your lessons on ModelMuse on YouTube. I’m trying to learn how to use that software, maybe you can help me if you have time.
Read MoreInstallation Guide for OpenFoam 2.3.0 on Ubuntu 14.04
Read MoreThis project is part of NASA/EOS project to estimate global terrestrial evapotranspiration from earth land surface by using satellite remote sensing data. MOD16 global evapotranspiration product can be used to calculate regional water and energy balance, soil water status; hence, it provides key information for water resource management.
Read MoreOnce again I had a crush with the question whether Feflow or Modflow. I think this question is related to how bad are we selling environmental services and environmental software.
It is a matter of faith
Read MoreExercise developed and modified by Karen Martinez, Sandra Teruya and Saul Montoya
This example is a simulation of a mining dump which is a continuous source of concentrated leachate.
Read MoreThis tutorial is intended to be a basic reference in Python programming for water resources professionals. The script covers many steps on the data management, representation and analysis with the most common Python commands and libraries. It is encouraged to review first all the described steps with the provided input data and then apply to the user own hydrological data. The same analysis will be ported to Julia on future tutorials to have a overview of the similarities / differences between programming in Python or Julia for hydrological data.
Read MoreNumerical modeling has become an important part on most hydrogeological investigations. We can even say that the use of numerical models is on “fashion” in decision making processes about groundwater resources.
Numerical models are mathematical interpretations of nature and groundwater flow. They can have limitations, but still they are the best tools available for the understanding of current groundwater flow conditions and the simulation of predictive scenarios on groundwater resources.
This post shows the 10 most important reasons why a common hydrogeologist should know MODFLOW. Reasons are classified among scientific, professional and others.
Calibration of groundwater flow models in mining
Read MoreSurface water and groundwater surrounding a mining operation can be significantly affected by contaminated seepage from the Acid Rock Drainage (ARD) in waste-dumps and tailing deposits. An evaluation for prevention and mitigation of environmental impacts generated by the DAR is necessary to minimize impact to the environment.
Read MoreThe MODFLOW SUB-WT code has been developed to simulate vertical compaction in regional groundwater flow models due to pumping.
MODFLOW SUB-WT can simulate changes in groundwater storages and compaction in discontinuous layers or extensive confining units. The MODFLOW SUB-WT modeling code considers the compaction of a particular layer of the numerical model as a function of effective effort changes in the layer.
Read MoreAfter my last job as a staff groundwater modeler, I have received 6 unsolicited job offers. Of course many modelers with more years and more conections than I, have received much more offers, however, I feel happy with my humble record. The point of this comparison is that senior groundwater modelers with experience in mining hydrogeology are really scarce. Mining and consultant companies are looking for talented groundwater modelers, and somehow there are not much modelers coming out from the universities.
Read MoreWhen I was in second semester of my master degree, the course director gave me this advice: “Learn MODFLOW and you will have a job”. That was a small and sincere advice that helped me on the last eight years as hydrogeologist – numerical modeler. Nowadays, I want to give the guidelines for people interested in how to be a senior hydrogeologist in 6 years.
Read MoreMODFLOW is the groundwater modelling software developed by the U.S. Geological Survey (USGS). It appeared in 1984 and has had a constant developement till now. MODFLOW’s capacities allow the representation of regional or local groundwater flow and its interaction with superficial water bodies.
Read MoreBefore talking about the different researches that have had as main focus water resources, I think it is necessary to explain first what geostatistics is.
Geostatistics is a type of statistics that is used to analyze and interpret geographically referenced data. It is not restricted to work only with point data, it also works with GIS layers to explore spatial variation, improve generation of digital elevation models (DEM) and their respective simulations, optimize spatial sampling, etc. [1]
Read MoreSince an homogenous aquifer was modelled, there is an interest in comparing the results with an analytical solution. Some formulas give the drawdown value into the well for a steady flow in confined and unconfined aquifers that are homogeneous, isotropic and infinite in the horizontal extent with a single full penetrating well.
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