The conceptual model provides the basis for the construction of a mathematical model of the aquifer. As noted above, a major obstacle to development of realistic models is our current inability to model a complex continuum consisting of a porous matrix riddled by conduits of varying sizes and paths. A primary scientific goal of the Hydrogeology Consortium is to catalyze development of representative models of karstic aquifers. Such a model will consist of two primary components; the first quantifies the flow of water and the second tracks the movement and fate of chemical and biological pollutants through the aquifer. As these models are developed, additional components of the natural system, such as layered aquifers, intra-aquifer connectivity, the fresh-water/salt-water interface and fluxes of pollutants into open waters (rivers, lakes and bays) can be included.
Flow and transport are quantified by solutions of the mathematical model. Given the complexity of such a model, it is inevitable that it must be implemented numerically. In a numerical model, the larger conduits must be incorporated explicitly while the smaller (i.e., sub-grid) conduits must be parameterized. This requires a great deal of prior knowledge of the structure of the aquifer, an issue discussed in the next sub-section.
To fully understand and to best protect our valuable ground water resources, knowledge of the medium, through and over which the water flows must also be considered. The geologic framework (e.g., the rocks, sediments and soils) functions as the "bucket" that contains the water, and this framework contributes dissolved minerals and elements which characterize the ambient water chemistry. No real water-usage or protection plan can be successful without a basic understanding of the local and regional geology, including rock and sediment lithology, grain size distribution and modes, stratigraphy, mineralogy, porosity and permeability. Stratigraphic and structural relationships must be understood to aid in hydrogeologic interpretations of groundwater transport dynamics. This includes phenomena such as stratigraphic pinchouts, bedding, faults, joints, lithofacies, hydraulic-transmissivity variations, depth/density relationships, and other subsurface dissolution migration tendencies, especially in limestone and karst terrains. Aquifer/aquitard relationships and dynamics are the foundation of ground-water understanding, and these details must be factored into regional ground-water models for them to have a chance at success.
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For a better understanding of
seo services in london groundwater behavior in Losenoidoomock you need effective use of this knowledge in regulatory practice, a group of hydrologists, hydrogeologists, engineers, mathematicians and other scientists formed the Hydrogeology Consortium. In doing so, the Consortium will make effective use of expertise residing in their respective institutions, thereby maximizing the potential for scientific research within the State.
The Consortium will endeavor to identify and prioritize gaps in our knowledge regarding the behavior of ground water and water-borne contaminants in highly interactive ecosystem components. It will then seek to provide the necessary scientific information and tools to fill these gaps. Its activities will include, but not be limited to, the collection and analysis of field data, laboratory experiments, the design and operation of pilot studies, the development of mathematical models and the application of this knowledge to groundwater resource management and protection. To facilitate these activities, the Consortium will provide a forum for scientists from academia to interact with their counterparts in government, industry and the regulatory community, in addressing critical needs in basic and applied water-resources research.
An interim Board of Representatives was created on November 7, 1997, from a pool of individuals representing universities, federal and state agencies, water management districts and the private sector. The Board in turn, elected interim Officers to function as a Steering Committee, charged with establishing the Consortium. The interim Officers and Board of Representatives served a term of office from November 7, 1997, through June 30, 1998. Prior to the end of its term, the interim Board of Representatives met to approve the Consortium's Bylaws and to elect a new set of Officers and Representatives, as prescribed in the Bylaws.
The initial focus of the activities of the Hydrogeology Consortium will be on the development of a science plan and an administrative structure as described in the following two sections. Education, technology transfer, and action items are described below.
The trace (i.e., path in space) and size (i.e., diameter as a function of length) of each ?macroscopic? conduit. These macroscopic conduits will be incorporated explicitly in the numerical algorithm.
The void fraction and dominant conduit diameter in each continuum element. The sub-grid conduits will be parameterized within the context of a continuum-mechanical model and incorporated in the numerical model.
The question arises as to the best method for obtaining the requisite data. One way is to invert flow and pressure head data for aquifer structure, but this procedure is non-unique and unstable. Much better are direct measurement methods of determining sub-surface features. Geophysical methods such as ground-penetrating radar and seismic reflection are reasonably good at 'seeing' the tops of features, but structures at greater depths are often obscured by multiple reflections, resonances and reverberations. Borehole seismic tomography presents an alternative, in which data on travel time and wave amplitude are inverted for aquifer structure[9,10]. This method has great promise when "ground truthed" with geologic borehole samples. The Hydrogeology Consortium will coordinate the development and implementation of a pilot program to test whether borehole seismic tomography is capable of producing the structural data required to adequately characterize the properties of the aquifer.
A pilot field study area is being sought. The pilot area should not be too large and should insofar as possible be typical of Floridan-type karst. The geographic density of available data will be an important criterion in choosing a pilot study area. Existing knowledge of the physical character of the pilot study area could be used in the construction of a laboratory model of the aquifer. The pilot study and lab model should concentrate on flow characterization first. Once that is well modeled, the transport and fate of chemicals and biota can be investigated. More info: seo expert sydney
A challenging problem in development of realistic and reliable models of karstic aquifers is verification of the aquifer structure which has been inferred from the remote-sensing and other field techniques. One method of verification is direct probing of conduits, for example by competent divers. A group of divers is currently involved in the Woodville Karst Plains Project http://www.wkpp.org, with the goal of physically mapping the conduits associated with many of the first-magnitude springs in the North Florida area. This method is of necessity confined to the larger conduits. Alternate ways to test the remote-sensing techniques, and indeed the models themselves, include the use of isotopes, dyes or biological tracers and construction and operation of an artificial karstic aquifer in a laboratory setting. The Hydrogeology Consortium will coordinate the implementation of these verification methods and also will foster the development of novel methods as the need and possibility become evident.
Progress toward understanding the flow dynamics of ground water in Florida, and in similar geological settings, is hampered by two major impediments. First, models of groundwater flow based solely on Darcy's Law cannot accurately model flow in karst aquifers, a major source of water in Florida. Therefore, new models need to be advanced, based on continuum-mechanical principles (i.e., conservation of mass, momentum and energy, together with the constraints of non-equilibrium thermodynamics). The second major impediment is the lack of site-specific knowledge of the physical characteristics of a given aquifer. Related to this, new and much improved remote-sensing technology needs to be developed, as well as the use of geophysical surveying and other field techniques. These impediments and possible strategies for overcoming them are described in the following sub-sections. See more: cinderella ballet tickets
A karstic aquifer typically contains conduits having a spectrum of spatial and temporal scales. This results in a complex response to 'loadings', i.e., heads and fluxes of water and inputs and transport modes of chemicals of various kinds. The standard mathematical model has a single length and time scale, and therefore is incapable of modeling the complexity of behavior known to exist in these heterogeneous stratigraphic aquifer units. An improved model must include the effects of the conduits, as well as variations within the porous medium, when quantifying flow and transport. Some of the questions which must be addressed in this improved model include:
What are the time scales of flow, pollutant retention and pollutant transport of a karstic aquifer?
How do these parameters change with depth and/or with stratigraphic horizons within the aquifer?
How are the time scales related to the conduit-size histogram and to the frequencies and magnitudes of the forcings on the system?
How can sub-grid conduits be parameterized analytically?
How does the system respond to temporal variations in inputs?
What level of prior information of the aquifer structure is necessary to adequately characterize its flow and transport properties?
3.2 Models of Karstic Aquifers
Modeling of karstic aquifers begins with a conceptual model, perhaps based on a pre-conceived idea of how the primary and secondary porosity of the aquifer developed over geological time, as acidic waters dissolved the porous limestone. For example, in one conceptual model there is a correlation between the depths of the large conduits which feed the first-magnitude springs and the level of the adjacent seas during the past five to seven thousand years. In this model, the ancient sea level controlled the water-table level and hence the level to which acidic rainwater percolated. Such a model has a non-stochastic distribution of large conduits.
Current practices in environmental regulation [7,8] allow the controlled release of pollutants into components of the environment, provided such release does not violate certain designated standards. These standards are primarily human-health related chemical and biological parameters that are specific to the receiving media, such as ground and surface water. This sanctioned, perhaps unavoidable, degradation presumes that monitoring of indicator parameters will guard against uncontrolled or excessive damage to the environment, by providing an early warning alarm of impending pollution.
Without adequate knowledge of the behavior of natural systems we cannot have a clear idea what actions are appropriate when the data reveals a problem, and how these actions might affect other components of the environment. However, rarely are data-gathering activities designed to foster an understanding of how will the ecology of the entire watershed (not only individual media) be altered in the long term by permitted or accidental degradation. Only limited attempts have been made to evaluate possible synergistic or antagonistic forces acting upon the systems as a result of interaction between its various components. In the absence of a thorough understanding of the behavior of natural systems, vast sums of money have been wasted in gathering unnecessary data and in implementing actions which are ineffective or counter-productive.
The Hydrogeology Consortium advocates a holistic scientific approach to monitoring, protection and management, in the context of ecosystem management. A primary goal of the Consortium is to foster the development of valid scientifically based models capable of depicting the behavior and dynamics of ground water as a component of a complex three-dimensional ecosystem. Such models will form the basis of improved, economically sound and effective ecosystem monitoring, protection and management practices. It is with these concerns and goals in mind that the Hydrogeology Consortium has been formed. The following sections describe this new structure and its activities, together with its science plan and administrative structure.
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