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Articles 1 - 11 of 11
Full-Text Articles in Physical Sciences and Mathematics
Laboratory Scale Seismic Analysis Of A Spatially Variable Hydrological Surface In Unconfined, Unconsolidated Sand, David E. Smolkin
Laboratory Scale Seismic Analysis Of A Spatially Variable Hydrological Surface In Unconfined, Unconsolidated Sand, David E. Smolkin
LSU Master's Theses
The ability to measure the depth to the water table can provide information such as reservoir characteristics, soil conditions for agriculture, and actions to be taken with contaminant flow and removal. We attempt to detect this boundary in a larger-than-lab scale experiment. We attempt to simulate a spatially variable water level and attempt to image changes in the depth of this water level. We try to reduce the normally complex natural conditions to those of a nominally homogeneous and isotropic, unconfined sand volume for modeling. These simplified conditions help isolate the effects of remaining complexities such as the variable saturation …
Provenance And Origin Of Holocene Beach Ridge And Modern Beach Sands From The Costa De Nayarit, Western Mexico, Ruben Abe Cisneros
Provenance And Origin Of Holocene Beach Ridge And Modern Beach Sands From The Costa De Nayarit, Western Mexico, Ruben Abe Cisneros
LSU Master's Theses
The Costa de Nayarit in western Mexico is a classic modern example of the progradation of a coastline in a wave-dominated depositional environment. Throughout the Pleistocene, sediments have been brought to the Costa De Nayarit via three major river systems, the Rio Grande de Santiago, the Rio San Pedro and the Rio Acaponeta. These river systems obtain their sediments from two distinctly different volcanic provinces within central Mexico, the Sierra Madre Occidental (SMO), a volcanic province characterized by its predominance of felsic volcanism (rhyolites) and pyroclastic flows (welded ash flow tuff and ignimbrite), and the Trans-Mexican Volcanic Belt (TMVB), which …
West Antarctic Ice Sheet Retreat Chronology Of Two Middle-Shelf Grounding-Zone Wedges In Eastern Basin, Ross Sea, Antarctica, Lenora Nicole Copeland
West Antarctic Ice Sheet Retreat Chronology Of Two Middle-Shelf Grounding-Zone Wedges In Eastern Basin, Ross Sea, Antarctica, Lenora Nicole Copeland
LSU Master's Theses
This study isolated a small number of large, in situ and reworked foraminifera from diamicts deposited in two grounding zone wedges on the middle continental shelf in Eastern Basin, Ross Sea, Antarctica. All samples were of sufficient weight to yield Holocene dates if the samples were indeed of Holocene age. Of the twelve small samples sent for radiocarbon analysis, the two heaviest were for reworked foraminifera which yielded dates of >22,200 14C BP and >22,500 14C BP. None of the other ten samples yielded radiocarbon dates. The lack of Holocene radiocarbon dates for the six in situ and four reworked …
Miscible Column Studies Of Unfractured And Saturated Cores Of Topopah Spring Tuff From Yucca Mountain, Nevada Using Hydrophobic Organic Pollutants, Kody V. Kramer
LSU Master's Theses
Miscible displacement column studies were conducted on unfractured cores of Topopah Spring Tuff to quantify transport characteristics of bromide&44; pentafluorobenzoic acid &40;PFBA&41;&44; trichloroethylene &40;TCE&41;&44; and naphthalene. Three 5 cm diameter by 2 cm long cores were flushed with pulses of simulated groundwater containing these tracers&44; followed by tracer&45;free solution. Effective porosities were gravimetrically measured as 11&37;&44; 10.6&37;&44; and 9.5&37;. The tracers achieved full breakthrough in an order correlating to their hydrophobicities. Bromide and PFBA sorbed least&44; achieving full breakthrough in fewer than 10 pore volumes. As water analogues&44; both exhibited no quantifiable sorption. Delay to full breakthrough was contributed to …
A Palynological And Sequence Stratigraphic Study Of Santonian - Maastrichtan Strata From The Upper Magdalena Basin, Sandra Garzon
A Palynological And Sequence Stratigraphic Study Of Santonian - Maastrichtan Strata From The Upper Magdalena Basin, Sandra Garzon
LSU Master's Theses
This manuscript presents a biostratigraphic and sequence stratigraphic interpretation of palynological data from two outcrop sections on the NE flank of the Upper Magdalena Valley (UMV) basin comprising the Santonian to Lower Maastrichtian interval. The objectives of this study where: a) to characterize the lithologically similar Lower Lidita, Upper Lidita, and El Cobre, Buscavidas formations and b) to provide a better understanding of important correlation horizons in the northeastern part of the UMV basin and to confirm the age assignment of stratal units. A cyclic pattern of palynomorph distribution was recognized in both sections and tied to the different stages …
Evaluating The Duration Of Post-Lgm Grounding Events In The Glomar Challenger Basin Paleotrough, Eastern Basin Antarctica, Using Sediment Flux Calculations, Boluwatife Owolana
Evaluating The Duration Of Post-Lgm Grounding Events In The Glomar Challenger Basin Paleotrough, Eastern Basin Antarctica, Using Sediment Flux Calculations, Boluwatife Owolana
LSU Master's Theses
Previously acquired geological and geophysical data from the eastern Ross Sea outer shelf support the view that the West Antarctic Ice Sheet (WAIS) deposited three large-volume grounding zone wedges (GZWs) during the relatively short time since the onset of ice sheet retreat began at approximately 11 ka 14C BP. Here, GZW sediment volumes were estimated from seismic data correlations to evaluate the different possible durations of the individual grounding events. The two end-member fluxes used correspond to 1) a modern flux active at Whillans Ice Stream and 2) a larger flux accounting for the larger size of the drainage basin …
Geothermal And Geopressure Assessment With Implications For Carbon Dioxide Sequestration, A Regional Scale Study, Lower Tuscaloosa Formation, Louisiana, Timmon Drumm
LSU Master's Theses
The Massive Sand member of the lower Tuscaloosa formation in Louisiana has the potential to be a prolific reservoir for carbon dioxide sequestration. Proximity to near-term anthropogenic carbon dioxide sources and existing infrastructure in the area make Louisiana a viable prospect for carbon capture and storage projects. The geothermal and geopressure conditions of the reservoir indicate that high carbon dioxide densities can be maintained throughout the study area, and substantial sand thicknesses were located. Subsurface depths of the top of the Massive Sand member range from roughly -2500 ft (-762 m) to over -21,000 ft (-6400 m) with a regional …
Antarctic Plant And Phytoplankton Response To The First Phase Of The Mid Miocene Climatic Optimum At South Mcmurdo Sound, Lee Foersterling
Antarctic Plant And Phytoplankton Response To The First Phase Of The Mid Miocene Climatic Optimum At South Mcmurdo Sound, Lee Foersterling
LSU Master's Theses
The Antarctic Drilling Program (ANDRILL) recovered 1138.54 m of sub-seafloor marine sediments with 98% core recovery at the AND2-2A drill site in South McMurdo Sound. Biostratigraphy, magnetostratigraphy, and isotopic dating (Acton et al., 2008) indicated that an Early to Middle Miocene section (223-1138.54 mbsf) was recovered. This study focuses on an interval with high concentrations of palynomorphs, located between 460.57 and 403.48 mbsf and dated to 16.7 Ma to 16.2 Ma according to the updated Acton et al. (2008) ANDRILL SMS age model. Palynological results show a pronounced increase in organic microfossils between 434.01 and 431.91 mbsf, compared to levels …
Soft Sediment Relay Zones: A High Resolution Seismic Survey Livingston Parish, Louisiana, Erin T. Elliott
Soft Sediment Relay Zones: A High Resolution Seismic Survey Livingston Parish, Louisiana, Erin T. Elliott
LSU Master's Theses
The southern coast of the United States, bordering the Gulf of Mexico, is home to several down-to-the-south, listric, normal fault systems striking parallel to the coast. One of these, the Baton Rouge–Tepetate Fault System located in southern Louisiana, consists of a series of near-surface, reactivated growth faults and relay ramps– a broad area of ductile strain, with contemporaneous sedimentation. Evidence of recent fault and relay ramp movement is seen in surficial fault line scarps and offset roads. This thesis utilizes two near-surface (<500 >m), high-resolution (10 - 300 Hz), continuous seismic reflection profiles (360 m and 480 m long, 3 …
Geomicrobiology Of Louisiana Coastal Marshes Before And After The Deepwater Horizon Oil Spill, Chang Liu
Geomicrobiology Of Louisiana Coastal Marshes Before And After The Deepwater Horizon Oil Spill, Chang Liu
LSU Master's Theses
The 2010 Deepwater Horizon oil spill in the Gulf of Mexico not only impacted open ocean and shoreline geochemical and ecological environments, but it served to promote research of microbial ecosystems in poorly studied habitats, such as Louisiana marshes. Sediment and water samples from four main marshes in southern Louisiana were collected in May 2010 (pre-oil), September 2010 (oiled), and June 2011 (post-oil). Sites near the Mississippi River had exceptionally low salinity in the immediate months following the oil spill due to freshwater diversion efforts; salinity increased by an order of magnitude one year later. Microbial diversity was evaluated from …
Investigation Into The Cause Of Earthen Embankment Instability Along The "V-Line" Artificial Levee In Marrero, Louisiana, Usa, Jason Hicks
LSU Master's Theses
The “V-line” levee, located in Marrero, LA, has a crack along its crest, measuring approximately 100 meters in length, 30 centimeters in depth, and 30 centimeters in width. This crack is a sign of levee instability. Seismic shear wave, CPT, and laboratory shear strength data were collected and processed to identify the cause of the instability. A zone of low seismic shear wave velocity was interpreted approximately 3 meters deep from the berm of the levee. Because of the large spacing between laboratory shear strength test sampling and CPT sites, a similar zone of low shear strength was not found …