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Articles 57841 - 57870 of 58447
Full-Text Articles in Entire DC Network
Analytical Studies Of Some Acyloin-Oximes., Hans A. Suter
Analytical Studies Of Some Acyloin-Oximes., Hans A. Suter
LSU Historical Dissertations and Theses
No abstract provided.
A Study Of Line-Width Photographic Photometry For Use In Spectrochemical Analysis., John A. Perry
A Study Of Line-Width Photographic Photometry For Use In Spectrochemical Analysis., John A. Perry
LSU Historical Dissertations and Theses
No abstract provided.
A Study Of Some Nitroso Compounds., Cilton Watson Tate
A Study Of Some Nitroso Compounds., Cilton Watson Tate
LSU Historical Dissertations and Theses
No abstract provided.
The Cosmic-Ray Transition Curve In Lead., Bartow Hodge
The Cosmic-Ray Transition Curve In Lead., Bartow Hodge
LSU Historical Dissertations and Theses
No abstract provided.
Studies Of The Reactions In Alcoholic Solution Of Gold(Iii) And Alpha-Naphthylamine., Theo Conner Mccoy
Studies Of The Reactions In Alcoholic Solution Of Gold(Iii) And Alpha-Naphthylamine., Theo Conner Mccoy
LSU Historical Dissertations and Theses
No abstract provided.
Electrokinetic And Light Scattering Study Of Alumina Sols., James Porter Craig
Electrokinetic And Light Scattering Study Of Alumina Sols., James Porter Craig
LSU Historical Dissertations and Theses
No abstract provided.
Foraminifera Of The Type Section Of The Archusa Marl Of Mississippi (Eocene, Claiborne Group, Wautubbee Formation), Nathan Eugene Crockett
Foraminifera Of The Type Section Of The Archusa Marl Of Mississippi (Eocene, Claiborne Group, Wautubbee Formation), Nathan Eugene Crockett
Masters Theses
"The type locality of the Archusa marl member of the Wautubbee formation is situated south of Quitman, Clarke County, Mississippi. Stratigraphically, the unit falls within the middle Eocene Claiborne group, being roughly equivalent to the upper part of the Lisbon formation of Alabama and the lower part of the Cook Mountain. The marl falls within the Ostrea sellaefonnis zone and the zone of "Ceratobulimina eximia.” The type section consists of 48 feet of sandy marls, with a thin oyster bed near the middle.
The Archusa foraminifera fauna consists of 87 species and varieties, belonging to 49 genera and …
The Mineralogy Of The Grassy Creek And Saverton Formations, Dirk Pieter Van Duym
The Mineralogy Of The Grassy Creek And Saverton Formations, Dirk Pieter Van Duym
Masters Theses
"A study of the mineralogy of the Grassy Creek and Saverton formations of Northeast Missouri was undertaken to determine whether a division is justified, as proposed by some stratigraphers, of these argillaceous beds into two formations. The formations were sampled systematically at surface exposures on the northeast limb of the Lincoln Arch in the vicinity of Hannibal and Louisiana, Missouri. The samples were investigated mineralogically in the laboratory. Previous studies showed that the fossils of the Grassy Creek and Saverton beds were virtually identical. The present study demonstrates that the Grassy Creek and Saverton beds are too near alike in …
Determination Of The Thermal Conductivity Of Sodium Chloride At Elevated Temperatures, Harold Robert Weisbrod
Determination Of The Thermal Conductivity Of Sodium Chloride At Elevated Temperatures, Harold Robert Weisbrod
Masters Theses
"The purpose of this research is to investigate possible methods of determining the thermal conductivity of small poorly conducting samples at elevated temperatures, and, further, to assemble a suitable apparatus, followed by measurement of thermal conductivity of one or more cubic lattice samples.
Basic requirements of the apparatus are few. It is first required that the measurement of thermal conductivity be made over a considerable range temperature. It is also preferred that the basic apparatus be placed in a vacuum where undesirable heat flow by convection is eliminated and air corrodible samples are preserved.
The apparatus must use only the …
Geology Of The South Half Of The Meramec Spring Quadrangle, Missouri, Howard Joseph Yorston
Geology Of The South Half Of The Meramec Spring Quadrangle, Missouri, Howard Joseph Yorston
Masters Theses
"This report is a continuation of the work initiated by Mueller in his mapping of the north half of the Meramec Spring Quadrangle. The completion of this work provides not only a geologic map of the whole quadrangle but also completes the mapping of the geology of a strip of quadrangles extending from Rolla to the Mississippi River. In addition to being a step closer to the goal of complete geologic coverage for the state, this work will be of value to those concerned with the prediction of depths of wells drilled in search for water, which in view of …
The Formal Science Background Of Students Enrolled In General Science Classes In Dewitt High School, Charles O. Foreman
The Formal Science Background Of Students Enrolled In General Science Classes In Dewitt High School, Charles O. Foreman
Dissertations and Theses @ UNI
No abstract provided.
Biological Oxidation Of Copper Sulfide Minerals, Delmar Boyd Davis
Biological Oxidation Of Copper Sulfide Minerals, Delmar Boyd Davis
Theses and Dissertations
This work represents a study of the biological oxidation of copper sulfide minerals. The principal objective of the study was to determine the extent of bacterial oxidation on copper containing sulfide minerals. It was also desired to determine if the bacteria could oxidize copper sulfides in the absence of iron. A better understanding of the nitrogen requirements of the organisms was desired. Minerals used in this study were Bingham Canyon Float Concentrate, chalcopyrite, covellite, calcocite, bornite, tetrahedrite, and reagent grade copper sulfide. The bacteria used were obtained from the mine waters of Bingham Canyon, Utah. To study the problem the …
A Statistical Evaluation Of Various Determinations Of Germanium, Kenneth William Bartz
A Statistical Evaluation Of Various Determinations Of Germanium, Kenneth William Bartz
Bachelors’ Theses
Germanium first came to the author's attention under the heading of "A Study of the Excited States of Matter." The various and diverse, not to mention peculiar properties of this element aroused my interest. But upon further studying of this unusual element my concern switched from its properties to the methods of analysis. It is the purpose of this paper to discuss and correlate the numerous and varied analytical determinations. However, actual determinations are limited to instrumental procedures only.
For the evaluation and interpretation of the date, Statistical Analysis is used. The author's qualification in Statistical Analysis include a year …
Mechanism Of Adsorption Of Cations By Silicate Minerals, Milton Glen Armstrong
Mechanism Of Adsorption Of Cations By Silicate Minerals, Milton Glen Armstrong
Theses and Dissertations
Adsorption of cations by clays has been a subject of investigation for many years. Many proposals have been advanced to explain this process of adsorption. Two proposals have been prominent in recent years. The Marshall "charged lattice" theory attributes adsorption of cations by clays to an electrostatic attration of the clay particles for cations. This charge on the clay particles is attributed to various isomorphic substitutions in the lattice of the clay which result in an unbalanced charge on the particle. This isomorphic substitution can take place either in the silicon-oxygen tetrahedra of the silicate structure or with the aluminum …
Collector-Depressant Equilibria In The Selective Flotation Of Sulfide Ores, Heber Ross Olson
Collector-Depressant Equilibria In The Selective Flotation Of Sulfide Ores, Heber Ross Olson
Theses and Dissertations
This dissertation presents the results of a collector - depressant equilibria study of the flotation systems potassium n-amyl xanthate - sodium cyanide - molybdenite and ethyl zanthate sodium sulfide - molybdenite and the study of conditions necessary for the selective flotation of covellite, tetra-hedrite, bornite, chalcopyrite, molybdenite, marcasite and pyrite in the system ethyl xanthate and sodium cyanide; the conditions necessary for the selective flotation of pyrite, covellite, bornite, galena, chalcopyrite, active sphalerite, and molybdenite in the system potassium ethyl xanthate and sodium sulfide; the conditions necessary for the selective flotation of molybdenite and pyrite in the system of potassium …
An Investigation Of Some Changes In The Chemical Composition Of Arterial Tissue Which Correlate With The Development Of Arteriosclerosis, Richard Dee Strickland
An Investigation Of Some Changes In The Chemical Composition Of Arterial Tissue Which Correlate With The Development Of Arteriosclerosis, Richard Dee Strickland
Chemistry and Chemical Biology ETDs
Arteriosclerosis is one of the major health problems confronting people of middle and advanced age. The disorder, commonly called "hardening of the arteries", is a contributing factor in more deaths than any other ailment.
An Investigation Of The Collision Lengths Of Penetrating-Shower-Producing Radiation In Various Materials, James Francis Kenney
An Investigation Of The Collision Lengths Of Penetrating-Shower-Producing Radiation In Various Materials, James Francis Kenney
Physics & Astronomy ETDs
The purpose of this paper is to compile and tabulate some of the experimental data that have been obtained on penetrating showers, and to compare these data with the results that should be expected from the various theories that have been advanced.
Estimates For The Zeros Of Ultraspherical Polynomials, Frank B. Correia
Estimates For The Zeros Of Ultraspherical Polynomials, Frank B. Correia
Mathematics & Statistics ETDs
In this work an attempt is made to develop a new method for estimating the zeros of the Ultraspherical Polynomials. This method presupposes knowledge of the differential equation that these polynomials satisfy. However the method is applicable to a much wider class of functions since it may also be applied to estimating the zeros of the solutions of any homogeneous linear differential equation of the second order which satisfies certain initial conditions.
Geology Of East Grants Ridge, Valencia County, New Mexico, Herbert C. Johnston Jr.
Geology Of East Grants Ridge, Valencia County, New Mexico, Herbert C. Johnston Jr.
Earth and Planetary Sciences ETDs
The field investigation for this report was initiated in October 1952 and was continued intermittently until February 1953. The area was mapped on the scale of 1/31680 with the aid of aerial photographs and Soil Conservation Service planimeteric base map 173. This scale was later enlargened to 1/15840. Rock and mineral specimens were studied with the aid of a hand lens, and the oil immersion method was used to identify some minerals. No thin sections were made. Sedimentary rocks were mapped to complete the geologic picture. No detailed sedimentary sections were measured as emphasis was placed on the Cenozoic igneous …
The Crystal Structure Of Ceni, Joseph J. Finney
The Crystal Structure Of Ceni, Joseph J. Finney
Earth and Planetary Sciences ETDs
X-ray diffraction methods were used to determine the cell constants and structure of CeNi. The unit cell is orthohombic. The spcae group is probably Cmcm with aO=3.77 +/- 0.01, bO=10.46 +/- 0.02, cO=4.37+/- 0.01 A. The cell formula is Ce4Ni4. The observed density if 7.51 grams/cm3 and the calculated density is 7.65 grams/cm3, a deviation of 1.8%.
Studies In The Cinnoline Series, David B. Cox
Studies In The Cinnoline Series, David B. Cox
Chemistry and Chemical Biology ETDs
Recent work by Castle and Kruse (16) has partially elucidated the range of reactivity of the chlorine atom in the compounds 4-chlorocinnoline and 4-chloro-6,7-dimethoxycinnoline. Condensations between the chlorinated cinnolines and certain phenylacetonitriles were found to proceed readily; however, condensations with compounds of the malonic ester type were unsuccessful. It was found that hydrolysis of the condensation product obtained from 4-chlorocinnoline and phenylacetontrile by hot 60% sulfuric acid caused decarboxylation of the intermediate acid, the final product being 4-benzylcinnoline. This compound has a formal resemblance to the basic ring structure of papaverine.
Paleontology And Stratigraphy Of The Upper Cretaceous Rocks Between Mount Taylor And The Rio Puerco, New Mexico, Kenneth D. Sharp
Paleontology And Stratigraphy Of The Upper Cretaceous Rocks Between Mount Taylor And The Rio Puerco, New Mexico, Kenneth D. Sharp
Earth and Planetary Sciences ETDs
The area covered in this report lies between Mt. Taylor and the Rio Puerco, and embraces approximately 675 square miles. Much of it is readily accessible by either paved highways or improved roads. The general region is a land of numerous mesas, the largest of which is Mesa Chivato. Sandstones form prominent ridges while shales and alluvium form the valleys. Many volcanic plugs stand out as landmarks.
Stratigraphy And Paleontology Of The Carboniferous Rocks Of The Cedro Canyon Area, Manzanita Mountains, Bernalillo County, New Mexico, Ernest Szabo
Earth and Planetary Sciences ETDs
The discovery of an extension into the Cedro Canyon area, in the northern Manzanita Mountains, Bernalillo County, New Mexico, of strata similar in lithology and stratigraphic position to known pre-Pennsylvanian rocks of nearby areas is included in this report. No diagnostic fossils have been found in these newly discovered strata and therefore definite age assignment can not be made.
The Pennsylvanian strata are dominantly marine and exhibit unusual lighologic variations. These variations are attributed to the environment of a transgressing sea on an unstable shelf.
Measured sections indicate that it is possible to subdivide these strata according to series on …
Stratigraphic Relationships Of Cretaceous And Early Tertiary Rocks Of A Part Of Northwestern San Juan Basin, Elmer H. Baltz Jr.
Stratigraphic Relationships Of Cretaceous And Early Tertiary Rocks Of A Part Of Northwestern San Juan Basin, Elmer H. Baltz Jr.
Earth and Planetary Sciences ETDs
No abstract provided.
Geology And Mineralogy Of The Fierro-Hanover District, Grant County, New Mexico., Robert B. O'Sullivan
Geology And Mineralogy Of The Fierro-Hanover District, Grant County, New Mexico., Robert B. O'Sullivan
Earth and Planetary Sciences ETDs
The primary purpose of this report is to describe the petrography of the contact pyrometasomatic ores and rocks from the metamorphic aureole near Fierro. In the course of this work the literature pertaining to the area was read in order to compare the features of metamorphism about Fierro with those about Hanover. One two-day reconnaissance was made in the area.
Stratigraphic Analysis Of The Upper Cretaceous Pictured Cliffs Sandstone In Northeastern San Juan County, New Mexico, John W. Caldwell
Stratigraphic Analysis Of The Upper Cretaceous Pictured Cliffs Sandstone In Northeastern San Juan County, New Mexico, John W. Caldwell
Earth and Planetary Sciences ETDs
The San Juan Basin is located in northwestern New Mexico and southern Colorado and is physiographically a part of the Colorado Plateau province.
The Upper Cretaceous Pictured Cliffs sandstone is exposed around the perimeter of the San Juan Basin and is present throughout the greater part of the Basin in the subsurface. This economically important gas-bearing sandstone is situated in the structural basin in which the strata are upturned on the basinward flanks of the nearby Laramide cliffs.
Five possible origins for the Pictured Cliffs gas are presented: from the underlying Lewis shale, from within the Pictured Cliffs sandstone, from …
The Variegated Member Of The Morrison Formation In The Southeastern Part Of The San Juan Basin, Valencia County New Mexico, William L. Chenoweth
The Variegated Member Of The Morrison Formation In The Southeastern Part Of The San Juan Basin, Valencia County New Mexico, William L. Chenoweth
Earth and Planetary Sciences ETDs
The strata now designated as Morrison in western New Mexico have been known by a variety of names since the beginning of geological exploration in the West. The nomenclature has become confused due to the many facies that are present. Recent exploration for uranium has renewed interest in the stratigraphy of the Morrison formation.
Chelation Of The Rare Earth Elements As A Function Of Ph Using Thenoyltrifluoroacetone, Hugh James Bronaugh
Chelation Of The Rare Earth Elements As A Function Of Ph Using Thenoyltrifluoroacetone, Hugh James Bronaugh
Chemistry and Chemical Biology ETDs
The rare Earth elements, or lanthanides, having atomic numbers 57 through 71 occupy only one space in the periodic chart of the elements. These fifteen elements, which have extraordinarily similar chemical and physical properties, are placed in group three of the periodic table, between barium of group two and hafnium of group four. This series of elements has been the subject of extensive study in the past. The development of atomic energy has significantly increased the interest in the rare earths in the past ten years.
The Structural Geology Of The Cerrillos Hills Area, New Mexico, Alan E. Disbrow
The Structural Geology Of The Cerrillos Hills Area, New Mexico, Alan E. Disbrow
Earth and Planetary Sciences ETDs
The earliest major structural deformation recorded in rocks exposed in the Cerrillos area occurred during the Laramie uplift of the Sangre de Cristo Mountains. This resulted in an erosional wedging of Upper Cretaceous strata at a rate of 130 feet per mile. Subsequent deposition of the Eocene Galisteo sand, clay, and gravel overstepped this surface in a sourceward direction.
At the beginning of work on this project the major problem was to determine the geological structure of the Cerrillos Hills. It was felt that a large-scale geologic map of an area extensive enough to reveal the structurally complex center of …
The Huego (Gym) Limestone, Luna County, New Mexico, Lowell E. Bogart
The Huego (Gym) Limestone, Luna County, New Mexico, Lowell E. Bogart
Earth and Planetary Sciences ETDs
Southwestern New Mexico is characterized by Basin and Range Physiography. Nearly level bolson plains are interrupted irregularly by linear mountain ranges. Sedimentary rocks ranging in age from Cambrian and recent crop out in the mountain areas. Darton (1916) mapped and described a limestone formation, about 1,000 feet thick, which he named Gym limestone. He thought the Gym was restricted in outcrop to Luna County and was distinct from previously described Paleozoic formations. The Gym was originally thought to be Pennsylvanian in age but later on was regarded as Permian. In the restudy of the Gym limestone was the basis of …