Splitting complex temporal questions for question answering systems

This paper presents a multi-layered Question Answering (Q.A.) architecture suitable for enhancing current Q.A. capabilities with the possibility of processing complex questions. That is, questions whose answer needs to be gathered from pieces of factual information scattered in different documents. Specifically, we have designed a layer oriented to process the different types of temporal questions. Complex temporal questions are first decomposed into simpler ones, according to the temporal relationships expressed in the original question. In the same way, the answers of each simple question are re-composed, fulfilling the temporal restrictions of the original complex question. Using this architecture, a Temporal Q.A. system has been developed. In this paper, we focus on explaining the first part of the process: the decomposition of the complex questions. Furthermore, it has been evaluated with the TERQAS question corpus of 112 temporal questions. For the task of question splitting our system has performed, in terms of precision and recall, 85% and 71%, respectively.

Partial collapse of a ventilated stone façade: Diagnosis and analysis of the anchorage system

The mechanical behaviour of transventilated façades performed by natural stone is necessarily based on the correct execution of both anchoring elements on the stone cladding as in the ones corresponding to the enclosure support, either with brick masonry walls or reinforced concrete walls. In the case studied in the present work, the origin of the damages suffered on the façade of a building located in Alcoy has been analyzed, where the detachment of part of the outer enclosure occurred. This enclosure is a transventilated façade formed by Bateig Blue stone tiles. To this end, “in situ” tests of the anchoring systems employed have been performed, as well as laboratory tests of mechanical characterization of the material and of different types of anchor, comparing these results with those obtained in both the simplified analytical models of continuum mechanics as developed by the Finite Element Method (FEM).

Analysis of the reproductive system of female vampire squid

Analysis of the reproductive system of female vampire squid to determine reproductive strategy and fecundity of vampire squid, accessioned in the Santa Barbara Museum of Natural History and collected in 60, 70s from off southern California.

Feasibility of changeable message signs and highway advisory radio for freeway maintenance. Final report.

Texas State Department of Highways and Public Transportation, Transportation Planning Division, Austin

IVHS institutional issues and case studies. Analysis and lessons learned. Final report.

Federal Highway Administration, Washington, D.C.

San Antonio Alcohol Safety Action Project - analytic study no. 4: final analysis of the judicial system 1972 through 1974.

National Highway Traffic Safety Administration, Washington, D.C.

Puerto Rico Alcohol Safety Action Project: an anlaysis of the impact of ASAP on the traffic safety system (final analysis of the judicial system). Section II: analytic study IV 1972-1975. Final report.

Alcohol Safety Action Project--Puerto Rico, San Juan

An analysis of the rehabilitation system. Analytic study no. 6.

National Highway Traffic Safety Administration, Washington, D.C.

The English language : a brief history of its grammatical changes and its vocabulary : with exercises on synonyms, prefixes and suffixes, word-analysis and word building : a text-book for high schools and colleges /

Mode of access: Internet.

English grammar, by lectures: comprehending the principles and rules of syntactical parsing on a new and highly approved system; intended as a text book for students; containing exercises in syntax, rules for parsing by transposition, critical notes, and a lecture on rhetoric. /

Checklist Amer. imprints

The transportation system of our Nation, message relative to the transportation system of our Nation.

Mode of access: Internet.

The dollar; a study of the "new" national and international monetary system,

"First edition."

Federal mine safety and health amendments of 1975, S. 1302 : bill text, summary, section-by-section analysis, and introductory remarks : prepared for the Subcommittee on Labor of the Committee on Labor and Public Welfare, United States Senate.

At head of title: 94th Congress, 1st session. Committee print.

Locating a strand of the Seattle Fault Zone in southeast Seattle, Washington through topographic analysis, borehole analysis and ground penetrating radar

Contributing to the evaluation of seismic hazards, a previously unmapped strand of the Seattle Fault Zone (SFZ), cutting across the southwest side of Lake Washington and southeast Seattle, is located and characterized on the basis of bathymetry, borehole logs, and ground penetrating radar (GPR). Previous geologic mapping and geophysical analysis of the Seattle area have generally mapped the locations of some strands of the SFZ, though a complete and accurate understanding of locations of all individual strands of the fault system is still incomplete. A bathymetric scarp-like feature and co-linear aeromagnetic anomaly lineament defined the extent of the study area. A 2-dimensional lithology cross-section was constructed using six boreholes, chosen from suitable boreholes in the study area. In addition, two GPR transects, oblique to the proposed fault trend, served to identify physical differences in subsurface materials. The proposed fault trace follows the previously mapped contact between the Oligocene Blakeley Formation and Quaternary deposits, and topographic changes in slope. GPR profiles in Seward Park and across the proposed fault location show the contact between the Blakeley Formation and unconsolidated glacial deposits, but it does not constrain an offset. However, north-dipping beds in the Blakely Formation are consistent with previous interpretations of P-wave seismic profiles on Mercer Island and Bellevue, Washington. The profiles show the mapped location of the aeromagnetic lineament in Lake Washington and the inferred location of the steeply-dipping, high-amplitude bedrock reflector, representing a fault strand. This north-dipping reflector is likely the same feature identified in my analysis. I characterize the strand as a splay fault, antithetic to the frontal fault of the SFZ. This new fault may pose a geologic hazard to the region.