Lynn Walter Gelhar (born 1936) is an American civil engineer focusing in hydrology and is currently Professor Emeritus at Massachusetts Institute of Technology. [1] [2] He is recognized for pioneering research in stochastic subsurface hydrology, has leading research in the area of field-scale contaminant transport experiments, and has extensive experience on the hydrologic aspects of nuclear waste disposal.
Gelhar was born in 1936 in the central Wisconsin sand country ( A Sand County Almanac ) [3] [4] . He grew up in the small agricultural village of Oakfield, Wisconsin located at the foot of the Niagara Escarpment, graduating from Oakfield High School in 1954. He studied Civil Engineering at the University of Wisconsin, specializing at the graduate level in hydrology and fluid mechanics, with minors in mathematics and meteorology; his doctorate was completed in 1964. During his graduate study he also worked with the Soil Conservation Service(USDA) on design of water control structures and at Fairbanks-Morse & Co. on large pumping systems for flood control and water supply projects.
In 1964 he joined the faculty of the Department of Civil Engineering at the Massachusetts Institute of Technology (MIT) as an Assistant Professor, and was promoted to Associate Professor in 1969. In 1973 he joined the faculty of the Geoscience Department at the New Mexico Institute of Mining and Technology (NMT); as Professor of Hydrology he coordinated of the graduate program in hydrology. In 1983 he returned to MIT as full Professor, and retired in 1996, becoming Professor Emeritus while continuing to direct graduate student research. Sabbatical leaves included visits at Stanford University (1971), Karlsruhe Institute of Technology (1978), Ecole des Mines de Paris (1978), Royal Institute of Technology (KTH, Stockholm) (1986), Swiss Federal Institute of Technology in Zurich (1986), University of Western Australia and the Commonwealth Scientific and Industrial Research Organization (Perth) (1987), Lawrence Berkeley Laboratory (1993) and King Abdulaziz University (KAU), Jeddah, (2012).
Gelhar is recognized as a leading authority on stochastic subsurface hydrology. In 1982 he received the American Geophysical Union's Horton Award [5] in recognition of his pioneering work in stochastic subsurface hydrology, in 1983 was elected a Fellow [6] in the American Geophysical Union, cited particularly for work in stochastic methods, and in 1987 he was the recipient of the O. E. Meinzer Award [7] by the Geological Society of America for three papers dealing with stochastic methods. He is the author of the textbook Stochastic Subsurface Hydrology [8] (1993), and has authored 160 technical publications. He has broad experience in fundamental and applied water-related research, but is best known for his theoretical work describing contaminant transport in naturally heterogenous aquifers using stochastic methods. [9] He has also been instrumental in developing large-scale long-term field experiments designed to evaluate the new theoretical results, including field sites on Cape Cod, [10] near Columbus, Mississippi, [11] and a vadose zone site in the New Mexico desert near Las Cruces. [12] His review of worldwide data on field-scale dispersion in aquifers [13] is frequently cited in applied investigations aquifer contamination. His publications are widely cited, as reflected by his inclusion in the 2001 ISI Highly Cited list of scientists in Engineering and in Ecology/Environment. [14] In Google Scholar he is credited with more than 16,000 citations, being the most highly cited individual in the field of Groundwater Hydrology. [15]
Gelhar has experience in public service and consulting with government and industry on aspects of groundwater hydrology, dealing particularly with hazardous and nuclear waste issues. He has served on several multidisciplinary review teams, including groups reviewing environmental aspects of the Hanford Site in Washington, and the WIPP nuclear waste disposal site in New Mexico. At the WIPP site regional groundwater conditions may make the site susceptible to localized salt dissolution [16] [17] [18] [19] [20] and associated features like breccia pipes and sinkholes, [21] which could compromise the long-term stability of the site. Such uncertainties are intertwined with the complex politics of WIPP. [22] For the nuclear weapons test site in Nevada, he chaired a panel reviewing groundwater modeling for that region of southwestern Nevada as part of an assessment of groundwater contamination effects from underground weapons testing. [23] [24] At the Hanford site in Washington he was involved in hydrologic aspects of the high-level nuclear waste facility that was proposed in the basalt [25] [26] and was a member of a panel reviewing science and technology of Hanford environmental cleanup. [27] At Hanford there is a unique threat to the long-term stability of waste disposal facilities associated with the potential for mega floods with water hundreds of meters deep sweeping over the site, as has happened repeatedly as recently as 13,000 years ago (Missoula Floods). He was a member of a review group that assessed the groundwater conditions at the proposed Yucca Mountain nuclear waste disposal site [28] and has contributed a chapter to a book exploring uncertainties associated with Yucca Mountain. [29] While on sabbatical leaves in France, Switzerland and Sweden he worked with scientists involved in the radioactive waste disposal programs in those countries, in Sweden preparing a report on flow and transport in fractured rocks for their agency dealing with radioactive waste disposal. [30]
Radioactive waste is a type of hazardous waste that contains radioactive material. Radioactive waste is a result of many activities, including nuclear medicine, nuclear research, nuclear power generation, rare-earth mining, and nuclear weapons reprocessing. The storage and disposal of radioactive waste is regulated by government agencies in order to protect human health and the environment.
The Hanford Site is a decommissioned nuclear production complex operated by the United States federal government on the Columbia River in Benton County in the U.S. state of Washington. The site has been known by many names, including Site W and the Hanford Nuclear Reservation. Established in 1943 as part of the Manhattan Project, the site was home to the Hanford Engineer Works and B Reactor, the first full-scale plutonium production reactor in the world. Plutonium manufactured at the site was used in the first atomic bomb, which was tested in the Trinity nuclear test, and in the Fat Man bomb that was used in the bombing of Nagasaki.
The Yucca Mountain Nuclear Waste Repository, as designated by the Nuclear Waste Policy Act amendments of 1987, is a proposed deep geological repository storage facility within Yucca Mountain for spent nuclear fuel and other high-level radioactive waste in the United States. The site is on federal land adjacent to the Nevada Test Site in Nye County, Nevada, about 80 mi (130 km) northwest of the Las Vegas Valley.
Hydrogeology is the area of geology that deals with the distribution and movement of groundwater in the soil and rocks of the Earth's crust. The terms groundwater hydrology, geohydrology, and hydrogeology are often used interchangeably.
The Waste Isolation Pilot Plant, or WIPP, is the world's third deep geological repository licensed to store transuranic radioactive waste for 10,000 years. The waste is from the research and production of United States nuclear weapons only. The plant started operation in 1999, and the project is estimated to cost $19 billion in total.
The Savannah River Site (SRS) is a U.S. Department of Energy (DOE) reservation in the United States in the state of South Carolina, located on land in Aiken, Allendale, and Barnwell counties adjacent to the Savannah River, 25 miles (40 km) southeast of Augusta, Georgia. The site was built during the 1950s to refine nuclear materials for deployment in nuclear weapons. It covers 310 square miles (800 km2) and employs more than 10,000 people.
The vadose zone, also termed the unsaturated zone, is the part of Earth between the land surface and the top of the phreatic zone, the position at which the groundwater is at atmospheric pressure. Hence, the vadose zone extends from the top of the ground surface to the water table.
The Nuclear Waste Policy Act of 1982 is a United States federal law which established a comprehensive national program for the safe, permanent disposal of highly radioactive wastes.
A deep geological repository is a way of storing hazardous or radioactive waste within a stable geologic environment. It entails a combination of waste form, waste package, engineered seals and geology that is suited to provide a high level of long-term isolation and containment without future maintenance. This will prevent any radioactive dangers. A number of mercury, cyanide and arsenic waste repositories are operating worldwide including Canada and Germany and a number of radioactive waste storages are under construction with the Onkalo in Finland being the most advanced.
Groundwater recharge or deep drainage or deep percolation is a hydrologic process, where water moves downward from surface water to groundwater. Recharge is the primary method through which water enters an aquifer. This process usually occurs in the vadose zone below plant roots and is often expressed as a flux to the water table surface. Groundwater recharge also encompasses water moving away from the water table farther into the saturated zone. Recharge occurs both naturally and through anthropogenic processes, where rainwater and or reclaimed water is routed to the subsurface.
La Crosse Boiling Water Reactor (LACBWR) is a retired Boiling Water Reactor (BWR) nuclear power plant located near La Crosse, Wisconsin in the small village of Genoa, in Vernon County, Wisconsin, approximately 17 miles south of La Crosse along the Mississippi River. It was located directly adjacent to the coal-fired Genoa Generating Station. The site is owned and was operated by the Dairyland Power Cooperative (DPC).
Deep borehole disposal (DBD) is the concept of disposing high-level radioactive waste from nuclear reactors in extremely deep boreholes instead of in more traditional deep geological repositories that are excavated like mines. Deep borehole disposal seeks to place the waste as much as five kilometres (3 mi) beneath the surface of the Earth and relies primarily on the thickness of the natural geological barrier to safely isolate the waste from the biosphere for a very long period of time so that it should not pose a threat to humans and the environment. The concept was originally developed in the 1970s, but in 2014 a proposal for a first experimental borehole was proposed by a consortium headed by Sandia National Laboratories.
A hydrologic model is a simplification of a real-world system that aids in understanding, predicting, and managing water resources. Both the flow and quality of water are commonly studied using hydrologic models.
FEHM is a groundwater model that has been developed in the Earth and Environmental Sciences Division at Los Alamos National Laboratory over the past 30 years. The executable is available free at the FEHM Website. The capabilities of the code have expanded over the years to include multiphase flow of heat and mass with air, water, and CO2, methane hydrate, plus multi-component reactive chemistry and both thermal and mechanical stress. Applications of this code include simulations of: flow and transport in basin scale groundwater systems , migration of environmental isotopes in the vadose zone, geologic carbon sequestration, oil shale extraction, geothermal energy, migration of both nuclear and chemical contaminants, methane hydrate formation, seafloor hydrothermal circulation, and formation of karst. The simulator has been used to generate results for more than 100 peer reviewed publications which can be found at FEHM Publications.
GoldSim is dynamic, probabilistic simulation software developed by GoldSim Technology Group. This general-purpose simulator is a hybrid of several simulation approaches, combining an extension of system dynamics with some aspects of discrete event simulation, and embedding the dynamic simulation engine within a Monte Carlo simulation framework.
Groundwater pollution occurs when pollutants are released to the ground and make their way into groundwater. This type of water pollution can also occur naturally due to the presence of a minor and unwanted constituent, contaminant, or impurity in the groundwater, in which case it is more likely referred to as contamination rather than pollution. Groundwater pollution can occur from on-site sanitation systems, landfill leachate, effluent from wastewater treatment plants, leaking sewers, petrol filling stations, hydraulic fracturing (fracking) or from over application of fertilizers in agriculture. Pollution can also occur from naturally occurring contaminants, such as arsenic or fluoride. Using polluted groundwater causes hazards to public health through poisoning or the spread of disease.
Noam Weisbrod is a Hydrology Professor at the Department of Environmental Hydrology and Microbiology of the Zuckerberg Institute for Water Research (ZIWR), which is part of the Jacob Blaustein Institutes for Desert Research (BIDR) at Ben-Gurion University of the Negev (BGU). Weisbrod served as director of ZIWR from 2015 to 2018. In 2018 he became director of BIDR and was reelected for a second term in summer 2022.
Jean Marie Bahr is a hydrogeologist who examines how the physical and chemical composition of groundwater and how that controls the mass transportation of groundwater. She currently is an Emeritus Professor at the University of Wisconsin Madison in the department of geosciences.
The Chernobyl disaster remains the major and most detrimental nuclear catastrophe which completely altered the radioactive background of the Northern Hemisphere. It happened in April 1986 on the territory of the former Soviet Union. The catastrophe led to the increase of radiation in nearly one million times in some parts of Europe and North America compared to the pre-disaster state Air, water, soils, vegetation and animals were contaminated to a varying degree. Apart from Ukraine and Belarus as the worst hit areas, adversely affected countries included Russia, Austria, Finland and Sweden. The full impact on the aquatic systems, including primarily adjacent valleys of Pripyat river and Dnieper river, are still unexplored.
J. Jaime Gómez-Hernández is a Spanish Civil Engineer specialized in Geostatistics and Hydrogeology. He is a full professor of Hydraulic Engineering at the School of Civil Engineering of the Technical University of Valencia. He was conferred the William Christian Krumbein Medal in 2020 from the International Association for Mathematical Geosciences. He also received the 2020 Prince Sultan bin Abdulaziz International Prize for Water, in the field of Groundwater.
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