DENTON, Texas – Homeowners, renters and business owners in Lafayette Parish are encouraged to look over newly-revised preliminary flood maps in order to determine their flood risks and make informed decisions.
Following is a summary of key federal disaster aid programs that can be made available as needed and warranted under President Obama’s major disaster declaration issued for the Soboba Band of Luiseño Indians.
Assistance for Tribal Governments Can Include as Required:Language English
WASHINGTON – The U.S. Department of Homeland Security’s Federal Emergency Management Agency (FEMA) announced that federal disaster aid has been made available to the Soboba Band of Luiseño Indians and ordered federal aid to supplement the Tribe’s efforts in the area affected by severe storms, flooding, and mudslides during the period of December 4-6, 2014.Language English
Heidi Koontz ( Phone: 303-202-4763 );
Two new U.S. Geological Survey publications that highlight historical hydraulic fracturing trends and data from 1947 to 2010 are now available.
Hydraulic fracturing is presently the primary stimulation technique for oil and gas production in unconventional resource reservoirs. Comprehensive, published, and publicly available information regarding the extent, location, and character of hydraulic fracturing in the United States is scarce.
“These national-scale data and analyses will provide a basis for making comparisons of current-day hydraulic fracturing to historical applications,” said USGS scientist and lead author Tanya Gallegos.
“We now have an improved understanding of where the practice is occurring and how hydraulic fracturing characteristics have changed over time.”
This national analysis of data on nearly 1 million hydraulically fractured wells and 1.8 million fracturing treatment records from 1947 through 2010 is used to identify hydraulic fracturing trends in drilling methods and use of proppants (sand or similar material suspended in water or other fluid to keep fissures open), treatment fluids, additives, and water in the United States. These trends are compared to peer-reviewed literature in an effort to establish a common understanding of the differences in hydraulic fracturing and provide a context for understanding the costs and benefits of increased oil and gas production. The publications also examine how newer technology has affected the amount of water needed for the process and where hydraulic fracturing has occurred at different points in time. Although hydraulic fracturing is in widespread use across the United States in most major oil and gas basins for the development of unconventional oil and gas resources, historically, Texas had the highest number of records of hydraulic fracturing treatments and associated wells documented in the datasets.
These datasets also illustrate the rapid expansion of water-intensive horizontal/directional drilling that has increased from 6 percent of new hydraulically fractured wells drilled in the United States in 2000 to 42 percent of new wells drilled in 2010. Increased horizontal drilling also coincided with the emergence of water-based “slick water” fracturing fluids. This is one example of how the most current hydraulic fracturing materials and methods are notably different from those used in previous decades and have contributed to the development of previously inaccessible unconventional oil and gas production target areas, namely in shale and tight-sand reservoirs.
In a long-term field study, U.S. Geological Survey (USGS) and Virginia Tech scientists have found that changes in geochemistry from the natural breakdown of petroleum hydrocarbons underground can promote the chemical release (mobilization) of naturally occurring arsenic into groundwater. This geochemical change can result in potentially significant arsenic groundwater contamination.
While arsenic is naturally present in most soils and sediments at various concentrations, it is not commonly a health concern until it is mobilized by a chemical reaction and dissolves into groundwater. Elevated arsenic levels in groundwater used for drinking water is a significant public health concern since arsenic, a toxin and carcinogen, is linked to numerous forms of skin, bladder, and lung cancer.
For the past 32 years, a collaborative group of government, academic, and industry-supported scientists have studied the natural attenuation (biodegradation over time) of a 1979 petroleum spill in the shallow, glacial aquifer at the National Crude Oil Spill Fate and Natural Attenuation Research Site, near Bemidji, Minnesota.
Working at this intensively surveyed site, the researchers in this USGS-led investigation focused on a specific question: whether naturally occurring arsenic found in the glacial aquifers in this area might be mobilized in the presence of hydrocarbons because of chemical interactions involving iron hydroxides which also occur naturally. To address this question, arsenic concentrations were measured for several years in groundwater and in sediment up-gradient, within, and down-gradient from the hydrocarbon plume at Bemidji.
Carefully measured samples from the field reveal that arsenic concentrations in the hydrocarbon plume can reach 230 micrograms per liter — 23 times the current drinking water standard of 10 micrograms per liter. Arsenic concentrations fall below 10 micrograms per liter both up-gradient and down-gradient from the plume.
The scientists attributed the elevated arsenic in the hydrocarbon plume to a series of interrelated geochemical and biochemical processes that involve arsenic and iron oxides (both are commonly found in sediments across the country) and the metabolization of carbon–rich petroleum by microbes in anoxic (low oxygen) conditions. The complex chemical process is explained further at this USGS website and in the published research article.
The results from this work also suggest that the arsenic released in the plume may reattach to aquifer sediments down-gradient from the plume. This reattachment could be considered good news for limiting the extent of the arsenic contamination in the groundwater. However, the chemical reattachment process may also be reversible, highlighting the need for long–term monitoring of arsenic and other chemicals that pose a water quality concern in areas associated with petroleum hydrocarbon leaks and spills.
The presence and amount of naturally occurring arsenic and iron oxides and the condition of the groundwater in the study area are fairly typical of many geologic settings across the nation, suggesting that the process of arsenic mobilization that was observed in the presence of hydrocarbons is not geographically limited.
This research was supported by the USGS Toxic Substances Hydrology Program and Hydrologic Research and Development Program, the Virginia Polytechnic Institute and State University, and the National Crude Oil Spill Fate and Natural Attenuation Research Site, a collaborative venture of the USGS, the Enbridge Energy Limited Partnership, the Minnesota Pollution Control Agency, and Beltrami County, Minnesota. By law, the USGS, a science bureau of the U.S. Department of the Interior, does not have any regulatory authority or responsibility.
Jon Campbell ( Phone: 703-648-4180 );
Improved global topographic (elevation) data are now publicly available for most of Asia (India, China, southern Siberia, Japan, Indonesia), Oceania (Australia, New Zealand), and western Pacific Islands. See diagram below for geographic coverage.
The data are being released following the President’s commitment at the United Nations to provide assistance for global efforts to combat climate change. The broad availability of more detailed elevation data across the globe through the Shuttle Radar Topography Mission (SRTM) will improve baseline information that is crucial to investigating the impacts of climate change on specific regions and communities.
“We are pleased to offer improved elevation data to scientists, educators, and students worldwide. It’s free to whomever can use it,” said Suzette Kimball, acting USGS Director, at the initial release of SRTM30 data for Africa in September. “Elevation, the third dimension of maps, is critical in understanding so many aspects of how nature works. Easy access to reliable data like this advances the mutual understanding of environmental challenges by citizens, researchers, and decision makers around the globe.”
The SRTM30 datasets resolve to 30-meters and can be used worldwide to improve environmental monitoring, advance climate change research, and promote local decision support. The previous global resolution for this data was 90-meters.
SRTM30 elevation data are increasingly being used to supplement other satellite imagery. In India, for example, SRTM30 elevation data can be used to track changes to the Gangotri Glacier, a major source of water for the Ganges River. Changes to this glacier, which has retreated 345 meters over the past 25 years, directly affect the water resources for hundreds of millions of people on the Indian subcontinent.
The National Aeronautics and Space Administration (NASA) and the National Geospatial-Intelligence Agency (NGA) worked collaboratively to produce the enhanced SRTM data, which have been extensively reviewed by relevant government agencies and deemed suitable for public release. SRTM flew aboard the Space Shuttle Endeavour in February 2000, mapping Earth's topography between 56 degrees south and 60 degrees north of the equator. During the 11-day mission, SRTM used imaging radar to map the surface of Earth numerous times from different perspectives.
The USGS, a bureau of the U.S. Department of the Interior, distributes SRTM30 data free of charge via its user-friendly Earth Explorer website. NASA also distributes SRTM data versions through the Land Processes Distributed Active Archive Center (LPDAAC) operated by USGS along with descriptions of the various versions and processing options.
Enhanced 30-meter resolution SRTM data for the remainder of the globe (at less than 60 deg. latitude) are scheduled to be released in the last of four releases in August 2015.Shaded grid over most of Asia, Japan, and Australia indicates the coverage of the third of four releases of improved topographic (elevation) data now publicly available through USGS archives. (High resolution image)
Some media are reporting that the Asian H5N1 strain of highly pathogenic avian influenza has now entered the United States. This is incorrect. The avian flu that was recently found in a green-winged teal in Washington state is a different strain and is not known to harm humans nor has it been found in domestic poultry. This Washington state strain incorporates genes from North American waterfowl-associated viruses. Unlike the Asian H5N1 strain that has been found in Asia, Europe, and Africa, this Washington state strain has only been found in wild waterfowl and has not been associated with human illness, nor has this new Washington state strain been found in domestic poultry.
Catherine Puckett, USGS ( Phone: 352-377-2469 );
BOZEMAN – Pallid sturgeon come from a genetic line that has lived on this planet for tens of millions of years; yet it has been decades since anyone has documented any of the enormous fish successfully producing young that survive to adulthood in the upper Missouri River basin.
Now, fisheries scientists with the U.S. Geological Survey, Montana State University and the U.S. Fish and Wildlife Service have shown why, detailing for the first time the biological mechanism that has caused the long decline of pallid sturgeon in the Missouri River and led to its being placed on the endangered species list 25 years ago.
In a paper published this week in the journal Fisheries, the scientists show that oxygen-depleted dead zones between dams in the upper Missouri River are directly linked with the failure of endangered pallid sturgeon hatched embryos to survive to adulthood.
“This research is a notable breakthrough in identifying the reason why pallid sturgeon in the Missouri River have been declining for so many decades,” said Suzette Kimball, acting director of the USGS. “By pinpointing the biological mechanism responsible for the species’ decline, resource managers have vital information they can use as a focus of pallid sturgeon conservation.”
“We certainly think this is a significant finding in the story of why pallid sturgeon are failing to recruit in the upper Missouri River,” said Christopher Guy, the assistant unit leader with the USGS Montana Cooperative Fishery Research Unit and the MSU professor who was the lead author on the paper. “We’re basically talking about a living dinosaur that takes 20 years to reach sexual maturity and can live as long as the average human in the U.S. After millions of years of success, the pallid sturgeon population stumbled and now we know why. From a conservation perspective, this is a major breakthrough.”
The study is the first to make a direct link among dam-induced changes in riverine sediment transport, the subsequent effects of those changes on reduced oxygen levels and the survival of an endangered species, the pallid sturgeon.
“This research shows that the transition zone between the freely flowing river and reservoirs is an ecological sink – a dead zone – for pallid sturgeon,” Guy said. “Essentially, hatched sturgeon embryos die in the oxygen-depleted sediments in the transition zones.”
Guy said fisheries biologists long suspected that the Missouri River’s massive reservoirs were preventing hatched embryonic pallid sturgeon from surviving to the juvenile stage. But early attempts to tie the problem to low levels of dissolved oxygen were unsuccessful.
“The reason for that is we hadn’t sampled deep enough,” Guy said. “It wasn’t until we sampled water down at the bottom, where those sediments are being deposited, that we found there was no dissolved oxygen. Because hatched pallid sturgeon embryos are negatively buoyant, they tend to sink into that hostile environment.”
“The lack of oxygen is a function of high microbial activity in the sediment laden area,” said co-author Eric Scholl, a Ph.D. student at Montana State University and a co-author on the study.
Hilary Treanor, an MSU research associate working with Guy, said they were able to show just how hostile these transition zones between riverine environment and reservoir could be to hatched sturgeon embryos.
In experiments at the U.S. Fish and Wildlife Fish Technology Center in Bozeman with coauthors Molly Webb, Kevin Kappenman, and Jason Ilgen, Treanor said different aged hatched embryos were treated with water of varying levels of dissolved oxygen. The lowest level they could recreate – 1.5 milligrams of oxygen per liter of water – was still higher than samples pulled from the bottom at the upper end of Fort Peck Reservoir.
At those depleted levels, the hatched sturgeon embryos suffered almost immediately.
“We saw changes in their behavior fairly quickly. They became disoriented and weren’t able to move the way they should have,” Treanor said. “Within an hour we started to see mortality. By the end of the experiment they were all dead.”
"Pallid sturgeon, native to the Missouri and Mississippi rivers, were listed as an endangered species in 1990. The species has a lifespan of as much as a century. According to the U.S. Fish and Wildlife Service, fewer than 175 wild-spawned pallid sturgeon – all adults – live in the free-flowing Missouri River above Lake Sakakawea. Since 1990, not a single wild-spawned pallid sturgeon is known to have survived to a juvenile, despite intensive searching.
In the past 5 years, researchers identified the most important reason for pallid sturgeon population declines in the Upper Missouri River: the lack of survival of naturally produced hatched sturgeon embryos.
Guy said this most recent study of sturgeon built on research conducted by USGS fisheries biologist Patrick Braaten, which demonstrated not enough available drift distance exists between the reservoirs for hatched pallid sturgeon embryos before entering the reservoirs in the upper Missouri River.
Before dams, hatched pallid sturgeon embryos would drift for hundreds of miles, eventually settling out of the river’s current in areas with low flow where they matured enough to negotiate the river’s flow.
“This team has shown how much we can do when we have a collaboration between MSU, USGS and world-renowned reproductive physiologists Molly Webb and Kevin Kappenman with the U.S. Fish and Wildlife Service,” Guy said. “In the process of doing this research, we’ve trained a dozen MSU graduate students and a number of undergraduate field and lab techs.”
Given what the new research shows about how no oxygen is available to hatched pallid sturgeon embryos, the authors of the paper propose that officials will need to consider innovative approaches to managing Missouri River reservoirs for pallid sturgeon conservation to have a chance. It also could provide some guiding principles for the construction of new dams around the world, Guy said.
EATONTOWN, N.J. -- In the two years and three months since Hurricane Sandy scored a direct hit on New Jersey, the Federal Emergency Management Agency has remained engaged in the recovery effort, providing $6.9 billion to date to help the state recover and rebuild.Language English
SPOKANE, Wash. — In cooperation with the Polish Geological Institute — National Research Institute, U.S. Geological Survey scientists have published a new assessment of copper resources in Poland and Germany. This investigation is part of the U.S. Geological Survey’s Global Mineral Resource Assessment. The study synthesizes available information on known resources and estimates the location and quantity of undiscovered copper associated with the well-known late Permian (approximately 255 million years old), carbon-enriched shale, the Kupferschiefer, of the Southern Permian Basin in Europe.
The ore deposits associated with the Kupferschiefer in Germany and Poland have been mined for over 800 years and are world-famous among geologists because research on these deposits played a significant role in the scientific debates on ore genesis. The largest Kupferschiefer copper deposit occurs in the Lubin-Sieroszowice mining area, Poland. It is the largest copper deposit in Europe and one of the largest copper deposits on the Earth.
Most of the known copper resource and almost all of the estimated undiscovered copper resources occur in southwestern Poland and adjacent parts of eastern Germany. Since 1958, about 15 million metric tons of copper have been produced, and about 30 million metric tons of discovered copper remains to be developed. The USGS estimates a mean value of 110 million metric tons of copper may be undiscovered to a depth of 2.5 km below the surface in this area. Most of the undiscovered resource in southwestern Poland would be deeper than 1.5 km, where virgin rock temperatures exceed 50 degrees C (122 degrees F).
In 800 years of mining, about 2.6 million metric tons of copper were produced from Kupferschiefer deposits in east-central Germany. The areas near the deposits in east-central Germany have been well explored; less than one million metric tons of discovered copper remain in identified deposits. Mean undiscovered copper estimates for this area are about 20 million metric tons.
This USGS study supports previous findings by the Polish Geological Institute for the amount of undiscovered copper in Poland. Mean values from the USGS study are remarkably similar to the values estimated by Polish geologists. The USGS study differs from the Polish study in that two different methods are used to probabilistically estimate the amount of undiscovered copper and maps are included to show where undiscovered resources are likely to occur.
The full report, USGS Scientific Investigations Report 2010–5090–U, “Assessment of undiscovered copper resources associated with the Permian Kupferschiefer, Southern Permian Basin, Europe,” by Michael Zientek and others, is available online.
Additional USGS mineral resource assessment results and reports, including previous volumes of this publication series, and an estimate of undiscovered copper resource of the world in 2013, are online.
The U.S. Geological Survey (USGS) has released a convenient and informative new method for the analysis of groundwater and surface-water hydrologic data called the Groundwater (GW) Toolbox. The GIS-driven graphical and mapping interface is a significant advancement in USGS software for estimating base flow (the groundwater-discharge component of streamflow), surface runoff, and groundwater recharge from streamflow data.
The GW Toolbox brings together several analysis methods previously developed by the USGS and Bureau of Reclamation. Each of the methods included with the GW Toolbox use daily streamflow data automatically retrieved from the USGS National Water Information System (NWIS) for more than 26,000 streamgage sites across the United States. In addition to streamflow data, the GW Toolbox facilitates the retrieval of groundwater-level and precipitation time-series data from the NWIS database.
The GW Toolbox will be of use to engineers, academia, and government agencies at all levels for the analysis of many of the water-budget components of a typical watershed. The intensively visual interface will help shed light on water availability and hydrologic trends in response to climate and land-use changes and variability in these watersheds.
The GW Toolbox runs in a Microsoft Windows environment and includes the Base Flow Index (BFI), HYSEP, and PART hydrograph-separation methods to estimate base flow and surface runoff and the RORA and RECESS methods to estimate groundwater recharge.
WASHINGTON – The Federal Emergency Management Agency (FEMA) today announced it is seeking applicants for its Youth Preparedness Council. The Council supports FEMA’s commitment to involving youth in preparedness-related activities and provides an opportunity for young people to offer their perspectives, feedback and insights on how to help make America more resilient.Language English
WASHINGTON – The U.S. Department of Homeland Security’s Federal Emergency Management Agency (FEMA) seeks experienced individuals who are interested in serving on the National Advisory Council (NAC) to apply. All applications must be received by 5 p.m. ET on Monday, February 16, 2015.Language English
ANCHORAGE, Alaska Melting glaciers are not just impacting sea level, they are also affecting the flow of organic carbon to the world’s oceans, according to new research that provides the first ever global-scale estimates for the storage and release of organic carbon from glaciers.
The research, published in the Jan. 19 issue of Nature Geoscience, is crucial to better understand the role glaciers play in the global carbon cycle, especially as climate warming continues to reduce glacier ice stores and release ice-locked organic carbon into downstream freshwater and marine ecosystems.
“This research makes it clear that glaciers represent a substantial reservoir of organic carbon,” said Eran Hood, the lead author on the paper and a scientist with the University of Alaska Southeast (Juneau). “As a result, the loss of glacier mass worldwide, along with the corresponding release of carbon, will affect high-latitude marine ecosystems, particularly those surrounding the major ice sheets that now receive fairly limited land-to-ocean fluxes of organic carbon.”
Polar ice sheets and mountain glaciers cover roughly 11 percent of the Earth’s land surface and contain about 70 percent of Earth’s fresh water. They also store and release organic carbon to downstream environments as they melt. Because this glacier-derived organic carbon is readily metabolized by microorganisms, it can affect productivity in aquatic ecosystems.
“This research demonstrates that the impacts of glacier change reach beyond sea level rise,” said U.S. Geological Survey research glaciologist and co-author of the research Shad O’Neel. “Changes in organic carbon release from glaciers have implications for aquatic ecosystems because this material is readily consumed by microbes at the bottom of the food chain.”
Due to climate change, glacier mass losses are expected to accelerate, leading to a cumulative loss of nearly 17 million tons of glacial dissolved organic carbon by 2050 — equivalent to about half of the annual flux of dissolved organic carbon from the Amazon River.
These estimates are the first of their kind, and thus have high uncertainty, the scientists wrote, noting that refining estimates of organic carbon loss from glaciers is critical for improving the understanding of the impacts of glacier change. The U.S. Department of the Interior Alaska Climate Science Center and USGS Alaska Science Center plan to continue this work in 2015 and beyond with new efforts aimed at studying the biophysical implications of glacier change.
This project highlights ongoing collaboration between academic and federal research and the transformative results that stem from such funding partnerships. Other institutions involved in the research include Ecole Polytechnique Fédérale de Lausanne and Florida State University.
The work was supported by the National Science Foundation, the USGS Alaska Science Center, and the DOI Alaska Climate Science Center. The Alaska Climate Science Center provides scientific information to help natural resource managers and policy makers respond effectively to climate change.