110,119 research outputs found
Water purification by reverse osmosis using heterocyclic polymer membranes
Pyrrone (polyimidazopyrrolone) polymers are a new class of thermally stable, radiation and chemical resistant aromatic-heterocyclic polymers featuring a greater chemical and mechanical durability than cellulose acetate
Canonical Structure of Locally Homogeneous Systems on Compact Closed 3-Manifolds of Types , Nil and Sol
In this paper we investigate the canonical structure of diffeomorphism
invariant phase spaces for spatially locally homogeneous spacetimes with
3-dimensional compact closed spaces. After giving a general algorithm to
express the diffeomorphism-invariant phase space and the canonical structure of
a locally homogeneous system in terms of those of a homogeneous system on a
covering space and a moduli space, we completely determine the canonical
structures and the Hamiltonians of locally homogeneous pure gravity systems on
orientable compact closed 3-spaces of the Thurston-type , \Nil and
\Sol for all possible space topologies and invariance groups. We point out
that in many cases the canonical structure becomes degenerate in the moduli
sectors, which implies that the locally homogeneous systems are not canonically
closed in general in the full diffeomorphism-invariant phase space of generic
spacetimes with compact closed spaces.Comment: 62 pages, LaTe
Challenges for an Ontology of Artificial Intelligence
Of primary importance in formulating a response to the increasing prevalence and power of artificial intelligence (AI) applications in society are questions of ontology. Questions such as: What “are” these systems? How are they to be regarded? How does an algorithm come to be regarded as an agent? We discuss three factors which hinder discussion and obscure attempts to form a clear ontology of AI: (1) the various and evolving definitions of AI, (2) the tendency for pre-existing technologies to be assimilated and regarded as “normal,” and (3) the tendency of human beings to anthropomorphize. This list is not intended as exhaustive, nor is it seen to preclude entirely a clear ontology, however, these challenges are a necessary set of topics for consideration. Each of these factors is seen to present a 'moving target' for discussion, which poses a challenge for both technical specialists and non-practitioners of AI systems development (e.g., philosophers and theologians) to speak meaningfully given that the corpus of AI structures and capabilities evolves at a rapid pace. Finally, we present avenues for moving forward, including opportunities for collaborative synthesis for scholars in philosophy and science
Alaska DOT&PF Pile Extension Pier Pushover Software Version 1.0 – Installation Instructions and Theory Documentation
Conjugacy classes in maximal parabolic subgroups of general linear groups
We compute conjugacy classes in maximal parabolic subgroups of the general
linear group. This computation proceeds by reducing to a ``matrix problem''.
Such problems involve finding normal forms for matrices under a specified set
of row and column operations. We solve the relevant matrix problem in small
dimensional cases. This gives us all conjugacy classes in maximal parabolic
subgroups over a perfect field when one of the two blocks has dimension less
than 6. In particular, this includes every maximal parabolic subgroup of
GL_n(k) for n < 12 and k a perfect field. If our field is finite of size q, we
also show that the number of conjugacy classes, and so the number of
characters, of these groups is a polynomial in with integral coefficients.Comment: 23 pages, 6 figures. See also
http://zaphod.uchicago.edu/~murray/research/index.html . Submitted to Journal
of Algebr
The Use of Credit Card Debt by New Firms
Examines Kauffman Firm Survey data for credit card debt characteristics of small startups and whether and to what extent they affect the firms' survival rates. Explores average balances over three years and links between debt amounts and survival rates
Federal Income Taxation of Estates and Beneficiaries. By M. Carr Ferguson, James G. Freeland, Richard B. Stephens
Mars geologic mapping program: Review and highlights
The Mars Geologic Mapping (MGM) Program was introduced by NASA in 1987 as a new initiative in the Planetary Geology and Geophysics (PGG) Program. The overall purpose of the program is to support research on topical science problems that address specific questions. Among the objectives of the project are: (1) to produce highly detailed geologic maps that will greatly increase the knowledge of the materials and processes that have contributed to the evolutionary history of Mars; (2) to define areas of special interest for possible future investigation by planned missions (Mars Observer, Mars Sample Return); and (3) to maintain the interest of the planetary community in the development of new concepts and the re-evaluation of Martian geology as new data in usable form become available. Some interesting highlights of the geologic mapping indicate that multiple flood episodes occurred at different times during the Hesperian Period in both Kasei and Maja Valles. Studies of small channels in the Memnonia, Mangala, and Tharsis regions show that fluvial events appear to have occurred during the Amazonian Period at equatorial latitudes. Flood waters occurred during the Amazonian Period at equatorial latitudes. Flood waters from Mangala Valles may have seeped into surficial materials with the subsequent development of numerous sapping channels and debris flows; this suggests that the ancient highland terrain consists of relatively unconsolidated materials. Multiple layers were observed for the first time in the ridged plains lava flows covering large areas of Lunae Planum; some wrinkle ridges in this area are associated with grabens and collapse volcanic units at Hadriaca and Tyrrhena Paterae indicates that the units may have been emplaced by gravity-driven pyroclastic flows. Unlike the north polar layered deposits, those in the south polar region show no angular unconformities or evidence of faulting and folding. Water ice in the south polar layered deposits may be protected from solar heating and sublimation by a weathering rind or lag deposit on the surface
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