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Journal articles on the topic 'Breastfeeding – Texas – Fort Worth'

Author: Grafiati

Published: 1 July 2021

Last updated: 8 February 2022

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1

Pate, J'Nell L., Victoria Buenger, and Walter L. Buenger. "Texas Merchant: Marvin Leonard and Fort Worth." Journal of Southern History 66, no. 3 (August 2000): 675. http://dx.doi.org/10.2307/2587926.

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2

Jensen, Bradley K. "An Interview with Cookie Chambers CIO Texas New Mexico Power Fort Worth, Texas." Journal of Information Technology Case and Application Research 6, no. 2 (April 2004): 63–65. http://dx.doi.org/10.1080/15228053.2004.10856044.

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3

Winguth, A. M. E., and B. Kelp. "The Urban Heat Island of the North-Central Texas Region and Its Relation to the 2011 Severe Texas Drought." Journal of Applied Meteorology and Climatology 52, no. 11 (November 2013): 2418–33. http://dx.doi.org/10.1175/jamc-d-12-0195.1.

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AbstractHourly surface temperature differences between Dallas–Fort Worth, Texas, metropolitan and rural sites have been used to calculate the urban heat island from 2001 to 2011. The heat island peaked after sunset and was particularly strong during the drought and heat wave in July 2011, reaching a single-day instantaneous maximum value of 5.4°C and a monthly mean maximum of 3.4°C, as compared with the 2001–11 July average of 2.4°C. This severe drought caused faster warming of rural locations relative to the metropolitan area in the morning as a result of lower soil moisture content, which led to an average negative heat island in July 2011 of −2.3°C at 1100 central standard time. The ground-based assessment of canopy air temperature at screening level has been supported by a remotely sensed surface estimate from the Moderate Resolution Imaging Spectroradiometer (MODIS) on board the Terra satellite, highlighting a dual-peak maximum heat island in the major city centers of Dallas and Fort Worth. Both ground-based and remotely sensed spatial analyses of the maximum heat island indicate a northwest shift, the result of southeast winds in July 2011 of ~2 m s−1 on average. There was an overall positive trend in the urban heat island of 0.14°C decade−1 in the Dallas–Fort Worth metropolitan area from 2001 to 2011, due to rapid urbanization. Superimposed on this trend are significant interannual and decadal variations that influence the urban climate.

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4

Harp, Derald A., Edward L. McWilliams, Michael A. Arnold, and John F. Griffiths. "An Updated Hardiness Zone Map for Dallas-Fort Worth, Texas." HortTechnology 12, no. 4 (January 2002): 694–96. http://dx.doi.org/10.21273/horttech.12.4.694.

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The combination of concrete and asphalt surfaces, large buildings, lack of surface water, and anthropogenic heat inputs result in urban temperatures warmer than surrounding rural areas. This effect is often most pronounced with winter minimum temperatures and may cause changes in local plant hardiness zones. Local minimum temperatures were obtained for the years 1974-96 from the National Climatic Data Center and the Office of the State Climatologist of Texas for all recording stations within the Dallas-Fort Worth, Texas metropolitan area. Data were averaged and analyzed in two groups: 1974-86 and 1987-96. Contour maps were created using Surfer software. The 1974-86 local map had only one major difference from the 1990 USDA Plant Hardiness Zone map, which was the inclusion of 8a temperatures in more western portions of the metroplex. The inclusion of the years 1987-96 resulted in the westward expansion of 8a and a new 8b zone near downtown Dallas. These changes mimic the expansion of suburban development and increased urbanization over the last decade. We propose an updated plant hardiness zone map for this metropolitan area, which should more accurately reflect changes that have occurred since publication of the USDA Plant Hardiness Zone map.

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5

Dennie, Devin, R. D. Elmore, John Deng, Earl Manning, and Johari Pannalal. "Palaeomagnetism of the Mississippian Barnett Shale, Fort Worth Basin, Texas." Geological Society, London, Special Publications 371, no. 1 (2012): 89–106. http://dx.doi.org/10.1144/sp371.10.

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6

Rockers, Gary F. "FORT WORTH, TEXAS ENVIRONMENTAL MANAGEMENT SYSTEM (EMS) EXPERIENCE and UP-DATE." Proceedings of the Water Environment Federation 2002, no. 3 (January 1, 2002): 145–53. http://dx.doi.org/10.2175/193864702785302366.

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7

Moyano Pahissa, Ángela. "Reseña del libro: Gringos in Mexico, Fort Worth Texas, Simmen, Edward." Secuencia, no. 14 (January 1, 1989): 091. http://dx.doi.org/10.18234/secuencia.v0i14.262.

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<p>Narraciones de 24 viajeros norteamericanos en México que rescatan Ia cultura y la tradición del país. Las distintas descripciones, complementadas con varios cuentos, abarcan desde la época juarista hasta los años treinta del presente siglo.</p>

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8

Aitkenhead-Peterson, J. A., and M. K. Steele. "Dissolved organic carbon and dissolved organic nitrogen concentrations and exports upstream and downstream of the Dallas–Fort Worth metropolis, Texas, USA." Marine and Freshwater Research 67, no. 9 (2016): 1326. http://dx.doi.org/10.1071/mf15280.

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Concentrations and export of dissolved organic carbon (DOC) and dissolved organic nitrogen (DON) from terrestrial landscapes to near-coastal zones vary with land use. Information on (DOC) and (DON) concentrations and exports from urban ecosystems is sparse; thus, their source from within urbanised watersheds such as soil or vegetation or from permitted sewage discharge is unknown. We examined DOC and DON concentrations and exports in four gauged subwatersheds in the humid subtropical, upper Trinity River basin, upstream and downstream of the Dallas–Fort Worth metropolis in Texas, USA. Annual average DOC concentrations ranged from 5.7±0.4 to 6.4±0.8mgL–1 and DON concentrations ranged from 0.31±0.05 to 0.33±0.14mgL–1. Dissolved organic carbon exports, which included permitted sewage discharge, ranged from 522kgkm–2 year–1 above Dallas–Fort Worth to 3637kgkm–2 year–1 below Dallas–Fort Worth. Permitted effluent discharge contributed between 1 and 35% of DOC loading above and below the Dallas–Fort Worth metropolis. DON exports ranged from 27 to 179kgkm–2 year–1 above and below Dallas–Fort Worth respectively. There was difficulty apportioning permitted effluent-discharge contribution to DON because of the transformations among nitrogen-species. A moderate but significant relationship was found between DOC and sodium concentrations (R2=0.45; P<0.0001; n=40) and between DOC and potassium concentrations (R2=0.45; P<0.0001; n=40). Dissolved organic nitrogen also displayed a significant relationship with sodium (R2=0.33; P<0.001; n=40) and potassium (R2=0.59; P<0.001; n=40), suggesting that increases in these cations to aquatic ecosystems may induce increases in DOC and DON concentrations. Although DOC export was significantly correlated with medium-density urban land use (r=0.96; P<0.05: n=4), DON export was not (r=0.93; P>0.05; n=4), suggesting that land-management practices and permitted point-source discharges have a significant effect on aquatic DOC and DON concentrations and exports derived from urban watersheds.

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9

Bryant, John. "Variation of Soil Suction with Depth in Dallas and Fort Worth, Texas." Transportation Research Record: Journal of the Transportation Research Board 1615, no. 1 (January 1998): 100–104. http://dx.doi.org/10.3141/1615-14.

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The variation of soil suction and the estimate of constant soil suction with depth is used to design many slab-on-grade foundations and pavement moisture barriers. The Post-Tensioning Institute’s design procedures for slab-on-grade foundations and design of vertical pavement moisture barriers use the constant suction at depth to predict differential soil movements that influence shear, deflection, and moment magnitudes and the effective barrier depth. Constant soil suction estimates can be correlated to the climate or long-term weather conditions at any given site by using the Thornthwaite moisture index (TMI), which estimates the amount of net moisture surplus or deficit from precipitation and evapotranspiration of moisture from the ground surface. On the basis of the empirical curves, the constant value of total soil suction for the Dallas–Fort Worth, Texas (DFW) area is about 246 kPa based on an average TMI of 0. Analysis of more than 1,200 total soil suction laboratory tests performed on developed and undeveloped lots indicates that the measured average total soil suction value in the upper 6 m is closer to 979 kPa for the DFW area ranging between 55 kPa and 11,246 kPa during the 1995–1997 period. Some hypothesized reasons for the difference between the empirical and measured equilibrium (constant) soil suction values are amounts of clay, clay origin, variable plasticity indexes, soluble salt content, and equilibration curve differences.

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10

Bohan, Peter. "Cowtown Moderne: Art Deco Architecture of Fort Worth, Texas Judith Singer Cohen." Journal of the Society of Architectural Historians 50, no. 3 (September 1991): 332–33. http://dx.doi.org/10.2307/990627.

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11

Striner, Richard. "Cowtown Moderne: Art Deco Architecture of Fort Worth, Texas. Judith Singer Cohen." Winterthur Portfolio 24, no. 4 (December 1989): 297–99. http://dx.doi.org/10.1086/496453.

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12

Tiedeman, Jane L., and Alan H. Straus. "Regional Study of Value Pricing in the Dallas–Fort Worth Region, Texas." Transportation Research Record: Journal of the Transportation Research Board 1960, no. 1 (January 2006): 99–107. http://dx.doi.org/10.1177/0361198106196000113.

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13

Qi, Jie, Bo Zhang, Huailai Zhou, and Kurt Marfurt. "Attribute expression of fault-controlled karst — Fort Worth Basin, Texas: A tutorial." Interpretation 2, no. 3 (August 1, 2014): SF91—SF110. http://dx.doi.org/10.1190/int-2013-0188.1.

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Much of seismic interpretation is based on pattern recognition, such that experienced interpreters are able to extract subtle geologic features that a new interpreter may easily overlook. Seismic pattern recognition is based on the identification of changes in (1) amplitude, (2) phase, (3) frequency, (4) dip, (5) continuity, and (6) reflector configuration. Seismic attributes, which providing quantitative measures that can be subsequently used in risk analysis and data mining, partially automate the pattern recognition problem by extracting key statistical, geometric, or kinematic components of the 3D seismic volume. Early attribute analysis began with recognition of bright spots and quickly moved into the mapping of folds, faults, and channels. Although a novice interpreter may quickly recognize faults and channels on attribute time slices, karst terrains provide more complex patterns. We sought to instruct the attribute expression of a karst terrain in the western part of the Fort Worth Basin, Texas, United States of America. Karst provides a specific expression on almost every attribute. Specifically, karst in the Fort Worth Basin Ellenburger Group exhibits strong dip, negative curvature, low coherence, and a shift to lower frequencies. Geomorphologically, the inferred karst geometries seen in our study areas indicate strong structural control, whereby large-scale karst collapse is associated with faults and where karst lineaments are aligned perpendicularly to faults associated with reflector rotation anomalies.

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14

Hill, Ronald J., Etuan Zhang, Barry Jay Katz, and Yongchun Tang. "Modeling of gas generation from the Barnett Shale, Fort Worth Basin, Texas." AAPG Bulletin 91, no. 4 (April 2007): 501–21. http://dx.doi.org/10.1306/12060606063.

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15

Park, Jin-Ho, Yongsun Joo, and Jae-Guen Yang. "Cycloids in Louis I. Kahn’s kimbell art museum at fort worth, Texas." Mathematical Intelligencer 29, no. 2 (March 2007): 42–48. http://dx.doi.org/10.1007/bf02986205.

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16

Timotius, Hagayudha, and Yulinar Firdaus. "CHARACTERISTIC OF SHALE GAS RESERVOIR USING LMR (LAMBDA-MU-RHO) INVERSION: CASE STUDY BARNETT SHALE, FORT WORTH BASIN TEXAS, USA." BULLETIN OF THE MARINE GEOLOGY 28, no. 1 (February 15, 2016): 43. http://dx.doi.org/10.32693/bomg.28.1.2013.54.

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The decreasing of fossil fuel reserves in the conventional reservoir has made geologists and geophysicists to explore alternative energy source that could answer energy needs in the future. Therefore the exploration of oil and gas that is still trapped in the source rock (shale) is needed, and one of them still developed in shale gas. The method of Amplitude Versus Offset (AVO) Inversion is used for Lambda-Mu-Rho attributes, that is expected to assess values of physical parameters of shale. Fort Worth Basin is chosen to be a study area because, the Barnett Shale Formation has proven contains of oil and gas. This study using synthetic seismic data, based on geological model and well log data obtained from Vermylen (2012). It is expected from the study of Barnett Shale that related to shale gas development could be applied. Keyword: Shale gas, Barnett Shale, Fort Worth Basin, AVO Inversion, Lambda-mu-rho attributes Penurunan cadangan bahan bakar fosil pada reservoar konvensional membuat ahli geologi dan geofisika mengeksplorasi sumber energi alternatif guna menjawab kebutuhan energi di masa depan. Oleh karena itu dibutuhkan eksplorasi minyak dan gas yang masih terperangkap dalam batuan induk (serpih), dan salah satunya yang dikembangkan saat ini adalah â€œshale gasâ€. Penggunaan metode inversi Amplitudo Versus Offset (AVO) untuk atribut Lambda-Mu-Rho diharapkan dapat menghasilkan nilai-nilai parameter â€œfisis shaleâ€. Cekungan Fort Worth dipilih sebagai lokasi penelitian ini karena terdapat Formasi â€œBarnett Shaleâ€ yang telah terbukti mengandung minyak dan gas. Penelitian ini menggunakan data seismik sintetik berdasarkan model geologi serta data sumur yang diperoleh dari Vermylen (2012). Diharapkan dari penelitian tentang Barnett Shale yang berkaitan dengan pengembangan shale gas dapat diaplikasikan. Kata kunci: â€œShale gasâ€, â€œBarnett Shaleâ€, Cekungan Fort Worth, Inversi AVO, atribut Lambda-Mu-Rho

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17

Quinones, Louis Andrew, Heather R. DeShon, Maria B. Magnani, and Cliff Frohlich. "Stress Orientations in the Fort Worth Basin, Texas, Determined from Earthquake Focal Mechanisms." Bulletin of the Seismological Society of America 108, no. 3A (April 10, 2018): 1124–32. http://dx.doi.org/10.1785/0120170337.

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18

Hennings, Peter H., Jens‐Erik Lund Snee, Johnathon L. Osmond, Heather R. DeShon, Robin Dommisse, Elizabeth Horne, Casee Lemons, and Mark D. Zoback. "Injection‐Induced Seismicity and Fault‐Slip Potential in the Fort Worth Basin, Texas." Bulletin of the Seismological Society of America 109, no. 5 (July 23, 2019): 1615–34. http://dx.doi.org/10.1785/0120190017.

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Abstract The rate of seismicity in the hydrocarbon‐producing Fort Worth Basin of north‐central Texas, which underlies the Dallas–Fort Worth metropolitan area, increased markedly from 2008 through 2015, coinciding spatiotemporally with injection of 2 billion barrels of wastewater into deep aquifers. Although the rate of seismicity has declined with injection rates, some earthquake sequences remained active in 2018 and new clusters have developed. Most of this seismicity occurred away from regionally mapped faults, challenging efforts to constrain the continuing hazards of injection‐induced seismicity in the basin. Here, we present detailed new models of potentially seismogenic faults and the stress field, which we use to build a probabilistic assessment of fault‐slip potential. Our new fault map, based on reflection seismic data, tens of thousands of well logs, and outcrop characterization, includes 251 basement‐rooted normal faults that strike dominantly north‐northeast, several of which extend under populated areas. The updated stress map indicates a relatively consistent north‐northeast–south‐southwest azimuth of the maximum horizontal principal stress over seismically active parts of the basin, with a transition from strike‐slip faulting in the north to normal faulting in the southeast. Based on these new data, our probabilistic analysis shows that a majority of the total trace length of the mapped faults have slip potential that is equal to or higher than that of the faults that have already hosted injection‐induced earthquake sequences. We conclude that most faults in the system are highly sensitive to reactivation, and we postulate that many faults are still unidentified. Ongoing injection operations in the region should be conducted with these understandings in mind.

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19

Rodriguez, Norelis D., and R. Paul Philp. "Geochemical characterization of gases from the Mississippian Barnett Shale, Fort Worth Basin, Texas." AAPG Bulletin 94, no. 11 (November 2010): 1641–56. http://dx.doi.org/10.1306/04061009119.

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20

Sadeddin, Walid. "Holothurian sclerites from the Albian (Early Cretaceous) of the Fort Worth area, Texas, USA." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 200, no. 3 (July 31, 1996): 325–51. http://dx.doi.org/10.1127/njgpa/200/1996/325.

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21

Kim, Soontae, Daewon W. Byun, and Daniel Cohan. "Contributions of inter- and intra-state emissions to ozone over Dallas-Fort Worth, Texas." Civil Engineering and Environmental Systems 26, no. 1 (March 2009): 103–16. http://dx.doi.org/10.1080/10286600802005364.

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22

Chen, Si, Zi Long Ma, and Lei Cao. "Analysis of Peter Walker’s Modern-Classical Landscape Design Method." Applied Mechanics and Materials 209-211 (October 2012): 341–45. http://dx.doi.org/10.4028/www.scientific.net/amm.209-211.341.

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Influenced by Le Notre Garden, Peter Walker’s works brought forward the landscape architectural modernism movement while embracing classical elements. Most of his works have geometric and symmetrical layout with axis and specifics to sites. Modern materials, dynamic and static waterscape, geometric shaped plants and sculptures are common elements of his design. This paper analyzed the innovative style and features of Peter Walker’s five modern-classical landscape works: Burnett Park (Fort Worth, Texas, USA), Garden of Kempinski Hotel (München, German), Toyota City Museum of Art (Toyota City, Aichi, Japan), IBM Solana (Dallas, Texas, USA) and Cambridge Center Roof Garden (Cambridge, Massachusetts, USA).

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23

Harp, Derald A., and Edward L. McWilliams. "Urban Mesoclimate Effects on Winter Survival and Damage of Ornamental Species in Fort Worth, Texas." HortScience 31, no. 4 (August 1996): 661a—661. http://dx.doi.org/10.21273/hortsci.31.4.661a.

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Urban areas are typically 2 to 3°C warmer than surrounding rural areas throughout the year. Winter minimum temperatures are often 4 to 5 °C warmer in the city and, during extreme episodes may exhibit differences of 12 to 13°C. Because the USDA Hardiness Maps compile readings from individual stations in an area, temperature differences may not be apparent at the local scale. This study was conducted to compare ornamental plant damage during Winter 1995–96 in Fort Worth, Texas. AVHRR 1-km thermal satellite imagery was used to determine the warmest and coolest portions in Fort Worth, Texas. Each temperature area was divided into five 0.5-km blocks on the basis of similar landscape features and plant types. During Mar. 1996, these areas were evaluated on the basis of plant damage to several species. Asian jasmine (Trachelospermum asiaticum), indian hawthorn (Raphiolepis indica), St. augustine turf (Stenotaphrum secundatum), southern magnolia (Magnolia grandiflora), and Live Oak (Quercus virginiana) were the primary species damaged. Asian jasmine and St. Augustine turf were either completely killed or severely damaged in the coldest areas but suffered only moderate or light damage in the warmest areas. Indian hawthorn, live oak, and southern magnolia suffered leaf and stem damage in the coldest areas but little to no damage in the warmer areas.

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24

Abouelresh, Mohamed O., and Roger M. Slatt. "Lithofacies and sequence stratigraphy of the Barnett Shale in east-central Fort Worth Basin, Texas." AAPG Bulletin 96, no. 1 (January 2012): 1–22. http://dx.doi.org/10.1306/04261110116.

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25

Kuehn, Kevin A., Robert Garrison, Larry Robertson, Robert D. Koehn, Alfred L. Johnson, and William J. Rea. "Identification of Airborne Microfungal Populations from Home Environments within the Dallas-Fort Worth (Texas) Region." Indoor Environment 1, no. 5 (September 1992): 285–92. http://dx.doi.org/10.1177/1420326x9200100506.

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26

Foss, Ann W., and Yekang Ko. "Barriers and opportunities for climate change education: The case of Dallas-Fort Worth in Texas." Journal of Environmental Education 50, no. 3 (May 3, 2019): 145–59. http://dx.doi.org/10.1080/00958964.2019.1604479.

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27

Kuehn, Kevin A., Robert Garrison, Larry Robertson, Robert D. Koehn, Alfred L. Johnson, and William J. Rea. "Identification of Airborne Microfungal Populations from Home Environments within the Dallas-Fort Worth (Texas) Region." Indoor and Built Environment 1, no. 5 (1992): 285–92. http://dx.doi.org/10.1159/000463461.

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28

Pratt, Joanne H. "Why Aren’t More People Telecommuting?: Explanations from Four Studies." Transportation Research Record: Journal of the Transportation Research Board 1607, no. 1 (January 1997): 196–203. http://dx.doi.org/10.3141/1607-26.

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Despite the proven “bottom-line” benefits of telework, companies are still reluctant to implement new ways of organizing their workforces. That is particularly true of the practice of allowing employees to work from home offices. The findings of four studies that identify factors that must be considered in overcoming the barriers to telework are presented: (a) a report of the Telecommute America! public-private effort to promote awareness and understanding of telecommuting and telework; (b) a survey of Houston, Texas, employers required to submit trip reduction plans under the Clean Air Acts; (c) an evaluation of the city and county of Denver, Colorado, TRP 2000 training program, and (d) the Dallas-Fort Worth, Texas, telecommuting assistance initiative of the North Texas Clean Air Coalition.

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29

Greeley, Nansee, and Theresa Reardon Offerman. "Now & Then: Words, Words, Words: Ancient Communication." Mathematics Teaching in the Middle School 3, no. 5 (January 1998): 358–64. http://dx.doi.org/10.5951/mtms.3.5.0358.

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Now… The insightful use of words is what most people think of when they consider the work of a journalist, especially that of a reporter. However, numbers play a large part, as well. Mike Fisher, sports journalist for the Dallas Cowboys; columnist for the Fort Worth Star-Telegram; and host of the radio show, Fish for Lunch, which airs daily on KLIF radio in Dallas, Texas, knows that a good understanding of numbers, particularly statistics, is essential to being a sports journalist.

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30

Kennedy, W. J., A. S. Gale, J. M. Hancock, J. S. Crampton, and W. A. Cobban. "Ammonites and inoceramid bivalves from close to the middle-upper Albian Boundary around Fort Worth, Texas." Journal of Paleontology 73, no. 6 (November 1999): 1101–25. http://dx.doi.org/10.1017/s0022336000031012.

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The Goodland/Comanche Peak Limestone, Kiamichi Formation and basal Duck Creek Limestones around Fort Worth Texas yield a limited number of cosmopolitan ammonite and inoceramid bivalve taxa that allow precise correlation with the sequence that has been used as a standard in northwest Europe. The upper part of the Goodland/Comanche Peak Limestones yields species of Dipoloceras that show the base of the Upper Albian substage, provisionally defined as the first appearance of D. cristatum (Brongniart, 1822), to lie within this unit. Brancoceras aff. cricki Spath, 1934, Mortoniceras (Deiradoceras) beloventer new species, and Actinoceramus cf. concentricus (Parkinson, 1819) parabolicus Crampton, 1996a, co-occurs with D. cristatum in the Comanche Peak Limestone. The Kiamichi Formation yields rare Mortoniceras (Mortoniceras) pricei (Spath, 1922), M. (Deiradoceras) prerostratum Spath, 1921, M. (D.) bipunctatum Spath, 1933, and Actinoceramus sulcatus (Parkinson, 1819) morphotypes that allow correlation with the European Hysteroceras orbignyi and Hysteroceras varicosum subzones of the Mortoniceras inflatum zone. The basal Duck Creek Limestone yields Mortoniceras (Deiradoceras) sp. and Hysteroceras cf. varicosum (J. de C. Sowerby, 1824), and can also be correlated with the varicosum subzone.

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31

Leonard, Bill J. "Book Review: Living Stones: The Centennial History of Broadway Baptist Church, Fort Worth, Texas, 1882–1982." Review & Expositor 83, no. 4 (December 1986): 645–46. http://dx.doi.org/10.1177/003463738608300437.

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32

Smye, Katie M., Casee R. Lemons, Ray Eastwood, Guinevere McDaid, and Peter H. Hennings. "Stratigraphic architecture and petrophysical characterization of formations for deep disposal in the Fort Worth Basin, Texas." Interpretation 7, no. 4 (November 1, 2019): SL1—SL17. http://dx.doi.org/10.1190/int-2018-0195.1.

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Disposal of hydraulic fracturing flowback and produced water into Ordovician and Cambrian formations of the Fort Worth Basin (FWB), coupled with an increase in observed seismicity in the Dallas-Fort Worth area, necessitates an understanding of the geologic character of these disposal targets. More than 2 billion barrels (Bbbls) of wastewater have been disposed into the Ordovician Ellenburger Group of the FWB over the past 35 years. Since the implementation of the TexNet Earthquake Catalog (1 January 2017), more than 20 earthquakes of local magnitude ML2.0 or greater have been detected in the area, with depths ranging from 2 to 10 km (approximately 6500–33,000 ft). The cited mechanism for inducement of these earthquakes is reactivation of basement faults due to pore pressure changes, either directly related to proximal disposal or due to disposal volume buildup over time. Here, we present a stratigraphic and petrophysical analysis of FWB disposal targets and their relation to basement rocks. The Ellenburger consists of alternating layers of limestone and dolomite, with minor siliciclastics above the basement toward the Llano Uplift. Matrix porosity averages <5 porosity units (p.u.), with higher porosity in dolomitic layers than in limestone. Dolomite dominates at the top of the Ellenburger, which was exposed at the end of both the Lower and Upper Ordovician. Where crystalline basement rocks are penetrated, the composition ranges from granitic to chlorite-bearing metamorphosed lithology. The basement-sediment interface is frequently marked by increased porosity. An updated map of structure on top of basement indicates elevations ranging from outcrop at the Llano Uplift to more than [Formula: see text] ([Formula: see text]) subsea toward the northeast. The disposal zone pore volume is estimated from thickness and porosity maps and ranges from [Formula: see text] to [Formula: see text] billion barrels per square mile ([Formula: see text]).

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33

Milliken, Kitty L., William L. Esch, Robert M. Reed, and Tongwei Zhang. "Grain assemblages and strong diagenetic overprinting in siliceous mudrocks, Barnett Shale (Mississippian), Fort Worth Basin, Texas." AAPG Bulletin 96, no. 8 (August 2012): 1553–78. http://dx.doi.org/10.1306/12011111129.

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34

Williams, Harry F. L. "GIS-based analysis of foundation repairs and soil conditions in the Dallas-Fort Worth region, Texas." Environmental Geology 58, no. 5 (October 14, 2008): 919–28. http://dx.doi.org/10.1007/s00254-008-1571-y.

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35

Herndon, Robert M., Patricia K. Coyle, Thomas J. Murray, and Jerry S. Wolinsky. "Report of the Consensus Panel on the New International Panel Guidelines for Diagnosis of MS." International Journal of MS Care 4, no. 4 (December 1, 2002): 170–73. http://dx.doi.org/10.7224/1537-2073-4.4.170.

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The new international panel guidelines for diagnosis of multiple sclerosis (MS) raised a number of concerns regarding their use and application, particularly in relation to their impact on treatment issues and options. As a result, a consensus panel composed primarily of North American neurologists with inclusion of several members from the International Panel was convened in Fort Worth, Texas, November 30 to December 2, 2001, to discuss these concerns, resulting in the following consensus statement regarding the guidelines and their appropriate use. (Int J MS Care. 2002; 4: 170–173)

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Franţescu, Ovidiu D., Rodney M. Feldmann, and Carrie E. Schweitzer. "Cretaceous fossil Raninoida De Haan, 1839 (Crustacea, Decapoda, Brachyura) from northeast Texas." Journal of Paleontology 90, no. 6 (October 17, 2016): 1118–32. http://dx.doi.org/10.1017/jpa.2016.106.

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AbstractTwo new Raninoida crabs from the Cretaceous of Texas are described,Planocorystes robreidinew genus new species, andTexicancernew genus to accommodateNecrocarcinus renfroae. All the previously described raninoid-like decapods from the Pawpaw Formation have been reassigned according to Karasawa et al. (2014). Cretaceous raninoid-like crabs are the dominant taxa amongst the fossil decapods found in the Fort Worth, Texas, area, with hundreds of specimens collected. All of these fossils have been collected from limonitic nodules, and most of them present a good degree of preservation, with articulated pereiopods, pleons, venter and in rare occasions even the gills. The decapod fauna of the Pawpaw Formation represents a diverse population, with a large number of taxa in high abundance. One specimen ofP.robreidiappears to exhibit a lethal bite mark.

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Steiger, Scott M., Richard E. Orville, and Lawrence D. Carey. "Total Lightning Signatures of Thunderstorm Intensity over North Texas. Part II: Mesoscale Convective Systems." Monthly Weather Review 135, no. 10 (October 1, 2007): 3303–24. http://dx.doi.org/10.1175/mwr3483.1.

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Abstract Total lightning data from the Lightning Detection and Ranging (LDAR II) research network in addition to cloud-to-ground flash data from the National Lightning Detection Network (NLDN) and data from the Dallas–Fort Worth, Texas, Weather Surveillance Radar-1988 Doppler (WSR-88D) station (KFWS) were examined from individual cells within mesoscale convective systems that crossed the Dallas–Fort Worth region on 13 October 2001, 27 May 2002, and 16 June 2002. LDAR II source density contours were comma shaped, in association with severe wind events within mesoscale convective systems (MCSs) on 13 October 2001 and 27 May 2002. This signature is similar to the radar reflectivity bow echo. The source density comma shape was apparent 15 min prior to a severe wind report and lasted more than 20 min during the 13 October storm. Consistent relationships between severe straight-line winds, radar, and lightning storm cell characteristics (e.g., lightning heights) were not found for cells within MCSs as was the case for severe weather in supercells in Part I of this study. Cell interactions within MCSs are believed to weaken these relationships as reflectivity and lightning from nearby storms contaminate the cells of interest. Another hypothesis for these weak relations is that system, not individual cell, processes are responsible for severe straight-line winds at the surface. Analysis of the total lightning structure of the 13 October 2001 MCS showed downward-sloping source density contours behind the main convective line into the stratiform region. This further supports a charge advection mechanism in developing the stratiform charge structure. Bimodal vertical source density distributions were observed within MCS convection close to the center of the LDAR II network, while the lower mode was not detected at increasing range.

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Stokoe, Kenneth H., James A. Bay, Brent L. Rosenblad, Michael R. Murphy, Kenneth W. Fults, and Dar-Hao Chen. "Super-Accelerated Testing of Flexible Pavement with Stationary Dynamic Deflectometer." Transportation Research Record: Journal of the Transportation Research Board 1716, no. 1 (January 2000): 98–107. http://dx.doi.org/10.3141/1716-12.

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The Texas Department of Transportation (TxDOT), in partnership with the Center for Transportation Research, has implemented the Texas mobile load simulator (TxMLS) as a tool for accelerated testing of in-service pavements. Although the TxMLS has been used successfully to test in-service pavements in the Yoakum and Fort Worth districts, the fact that only one TxMLS machine exists limits the number of accelerated pavement tests (APT) that can be performed. Therefore, TxDOT is evaluating a modification of the rolling dynamic deflectometer (RDD) for use as a super-accelerated pavement tester. In this application, the truck-mounted dynamic loading system is operated in a stationary mode, with the loading rollers and rolling sensors of the RDD removed from operation. The servohydraulic actuator is used for application of harmonic loading to a wheel footprint on the pavement surface. Hundreds of thousands of load repetitions are applied in a matter of hours; hence the designation as super-accelerated testing. This stationary dynamic deflectometer (SDD) is being studied as a possible tool for use in expanding TxDOT’s APT program. The SDD may allow TxDOT to increase, in a cost-effective manner, the number of accelerated tests that can be performed. Preliminary tests have been performed with the TxMLS and SDD on two different pavement recycling strategies constructed on the northbound and southbound lanes of US-281 in the Fort Worth District. That the same conclusion was reached about the relative performance of the test sections with both machines indicates the potential usefulness of the SDD.

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Black, William R., Andrew Goetz, Michael Kuby, and Bruce Ralston. "Transport Geography Sessions at the Association of American Geographers Annual Meeting, 1 April 1997, Fort Worth, Texas." Journal of Transport Geography 5, no. 3 (September 1997): 221–23. http://dx.doi.org/10.1016/s0966-6923(97)89813-4.

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Stephens, William, Grete E. Wilt, Erica Adams Lehnert, NoelleAngelique M. Molinari, and Tanya Telfair LeBlanc. "A Spatial and Temporal Investigation of Medical Surge in Dallas–Fort Worth During Hurricane Harvey, Texas 2017." Disaster Medicine and Public Health Preparedness 14, no. 1 (January 30, 2020): 111–18. http://dx.doi.org/10.1017/dmp.2019.143.

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ABSTRACTObjective:When 2017 Hurricane Harvey struck the coastline of Texas on August 25, 2017, it resulted in 88 fatalities and more than US $125 billion in damage to infrastructure. The floods associated with the storm created a toxic mix of chemicals, sewage and other biohazards, and over 6 million cubic meters of garbage in Houston alone. The level of biohazard exposure and injuries from trauma among persons residing in affected areas was widespread and likely contributed to increases in emergency department (ED) visits in Houston and cities receiving hurricane evacuees. We investigated medical surge resulting from these evacuations in Dallas–Fort Worth (DFW) metroplex EDs.Methods:We used data sourced from the North Texas Syndromic Surveillance Region 2/3 in ESSENCE to investigate ED visit surge following the storm in DFW hospitals because this area received evacuees from the 60 counties with disaster declarations due to the storm. We used the interrupted time series (ITS) analysis to estimate the magnitude and duration of the ED surge. ITS was applied to all ED visits in DFW and visits made by patients residing in any of the 60 counties with disaster declarations due to the storm. The DFW metropolitan statistical area included 55 hospitals. Time series analyses examined data from March 1, 2017–January 6, 2018 with focus on the storm impact period, August 14–September 15, 2017. Data from before, during, and after the storm were visualized spatially and temporally to characterize magnitude, duration, and spatial variation of medical surge attributable to Hurricane Harvey.Results:During the study period overall, ED visits in the DFW area rose immediately by about 11% (95% CI: 9%, 13%), amounting to ~16 500 excess total visits before returning to the baseline on September 21, 2017. Visits by patients identified as residing in disaster declaration counties to DFW hospitals rose immediately by 127% (95% CI: 125%, 129%), amounting to 654 excess visits by September 29, 2017, when visits returned to the baseline. A spatial analysis revealed that evacuated patients were strongly clustered (Moran’s I = 0.35, P < 0.0001) among 5 of the counties with disaster declarations in the 11-day window during the storm surge.Conclusions:The observed increase in ED visits in DFW due to Hurricane Harvey and ensuing evacuation was significant. Anticipating medical surge following large-scale hurricanes is critical for community preparedness planning. Coordinated planning across stakeholders is necessary to safeguard the population and for a skillful response to medical surge needs. Plans that address hurricane response, in particular, should have contingencies for support beyond the expected disaster areas.

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Raisinghani, Mahesh S. "An Interview With Jonathan Overton, Director, Program Management Office, Cook Children’s Health Care System, Fort Worth, Texas." Journal of Information Technology Case and Application Research 16, no. 3-4 (October 2, 2014): 168–71. http://dx.doi.org/10.1080/15228053.2014.987615.

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Hu, Xiao-Ming, and Ming Xue. "Influence of Synoptic Sea-Breeze Fronts on the Urban Heat Island Intensity in Dallas–Fort Worth, Texas." Monthly Weather Review 144, no. 4 (March 29, 2016): 1487–507. http://dx.doi.org/10.1175/mwr-d-15-0201.1.

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Abstract When assessed using the difference between urban and rural air temperatures, the urban heat island (UHI) is most prominent during the nighttime. Typically, nocturnal UHI intensity is maintained throughout the night. The UHI intensity over Dallas–Fort Worth (DFW), Texas, however, experienced frequent “collapses” (sudden decreases) around midnight during August 2011, while the region was experiencing an intense heat wave. Observational and modeling studies were conducted to understand this unique phenomenon. Sea-breeze passage was found to be ultimately responsible for the collapses of the nocturnal UHI. Sea-breeze circulation developed along the coast of the Gulf of Mexico during the daytime. During the nighttime, the sea-breeze circulation was advected inland (as far as ~400 km) by the low-level jet-enhanced southerly flow, maintaining the characteristics of sea-breeze fronts, including the enhanced wind shear and vertical mixing. Ahead of the front, surface radiative cooling enhanced the near-surface temperature inversion in rural areas through the night with calm winds. During the frontal passage (around midnight at DFW), the enhanced vertical mixing at the leading edge of the fronts brought warmer air to the surface, leading to rural surface warming events. In contrast, urban effects led to a nearly neutral urban boundary layer. The enhanced mechanical mixing associated with sea-breeze fronts, therefore, did not increase urban surface temperature. The different responses to the sea-breeze frontal passages between rural (warming) and urban areas (no warming) led to the collapse of the UHI. The inland penetration of sea-breeze fronts at such large distances from the coast and their effects on UHI have not been documented in the literature.

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Dodds, William B., and Kenneth A. Hunt. "Legend Airlines: American Airlines Worst Nightmare?" Journal of Business Case Studies (JBCS) 8, no. 2 (February 8, 2012): 135–40. http://dx.doi.org/10.19030/jbcs.v8i2.6798.

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This case reviews the air battles American Airlines (AA) and Legend Airlines (LA) engaged in over the right to fly out of Love Field in Dallas, Texas, the home of American Airlines based at Dallas-Fort Worth International Airport.Legend Airlines was attacking the industry with a value proposition of quality flights and superior customer service with a laser focus on passengers who traveled frequently and paid top fares.The case is designed for classroom discussion and application to understand the economic consequences American Airlines faced with the up-scale entry of Legend Airlines into the heart of American Airlines market.

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Karibo, Holly M. "‘The Only Trouble is the Dam’ Heroin’: Addiction, Treatment and Punishment at the Fort Worth Narcotic Farm." Social History of Medicine 33, no. 2 (August 16, 2018): 515–38. http://dx.doi.org/10.1093/shm/hky069.

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Summary In 1929, the U.S. federal government approved two ground-breaking programs designed to treat drug addiction. Emerging at a time when many began to worry about a supposed rising tide of drug use across the country, the establishment of narcotic hospitals at Lexington, Kentucky and Fort Worth, Texas marked a watershed moment in the treatment of addiction. This article traces the institutional history of one of those facilities, the Fort Worth Narcotic Farm, and the experiences of the men who found themselves under its care. It argues that, on the surface, the creation of the farm model seemed like a hopeful alternative to strict incarceration models. Its creation reflected shifting notions of addiction: namely, that addiction is not simply a crime, but it is also a disease with serious public health implications. Yet, the establishment of the hospital as places to both treat and punish addicts was their inherent and fundamental flaw. Central to this was the concept of the “prisoner-patient,” a person forced to undergo treatment as a result of criminal charges. Not only did patients express their frustration with the prison-like setting at Fort Worth, but recidivism rates remained high throughout the facility’s operation. Ultimately, lawmakers and politicians would use these recidivism rates as part of a broader push for more punitive drug legislation in the post-World War II period. By placing the history of addiction into conversation with mass incarceration studies, this article shows that the roots of the punishment model employed in the last quarter of the twentieth century were interwoven into seemingly “progressive” treatment models dating back to at least the 1930s. Indeed, the very failures of early addiction treatment models that arose by mid-century helped to justify an expanding criminal justice model in the post-1960s era.

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Quinones, Louis, Heather R. DeShon, SeongJu Jeong, Paul Ogwari, Oner Sufri, Monique M. Holt, and Kevin B. Kwong. "Tracking Induced Seismicity in the Fort Worth Basin: A Summary of the 2008–2018 North Texas Earthquake Study Catalog." Bulletin of the Seismological Society of America 109, no. 4 (June 11, 2019): 1203–16. http://dx.doi.org/10.1785/0120190057.

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Abstract Since 2008, earthquake sequences within the Fort Worth basin (FWB), north Texas, have been linked to wastewater disposal activities related to unconventional shale‐gas production. The North Texas Earthquake Study (NTXES) catalog (2008–2018), described and included herein, uses a combination of local and regional seismic networks to track significant seismic sequences in the basin. The FWB earthquakes occur along discrete faults that are relatively far apart (>30 km), allowing for more detailed study of individual sequence development. The three largest sequences (magnitude 3.6+) are monitored by local seismic networks (<15 km epicentral distances), whereas basinwide seismicity outside these three sequences is monitored using regional distance stations. A regional 1D velocity model for the FWB reflects basinwide well log, receiver function, and regional crustal structure studies and is modified for the larger individual earthquake sequences using local well‐log and geology data. Here, we present an mb_Lg relationship appropriate for Texas and a basin‐specific ML relationship, both calculated using attenuation curves developed with the NTXES catalog. Analysis of the catalog reveals that the earthquakes generally occur within the Precambrian basement formation along steeply dipping normal faults, and although overall seismicity rates have decreased since 2016, new faults have become active. Between 2006 and 2018, more than 2 billion barrels of fluids were injected into the Ellenburger formation within the FWB. We observe strong spatial and temporal correlations between the earthquake locations and wastewater disposal well locations and injection volumes, implying that fluid injection activities may be the main driving force of seismicity in the basin. In addition, we observe seismicity occurring at greater distances from injection wells (>10 km) over time, implying that far‐field stress changes associated with fluid injection activities may be an important component to understanding the seismic hazard of induced seismicity sequences.

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Fridinger, Fred, and Beverly Dehart. "A Model for the Inclusion of a Physical Fitness and Health Promotion Component in a Chemical Abuse Treatment Program." Journal of Drug Education 23, no. 3 (September 1993): 215–22. http://dx.doi.org/10.2190/xtkp-a4y7-ppb5-wm36.

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Alcohol and other substance abuse treatment programs are focusing more on the wellbeing of the total patient rather than just targeting functional sobriety. Various explanations are offered in this article for the inclusion of a fitness and health promotion component in a chemical abuse treatment program. The treatment program at Charter Hospital of Fort Worth, Texas, is discussed in detail, including a comprehensive medical examination, fitness and nutritional screenings, and appropriate exercise activities. Educational sessions are offered on health fitness, risk reduction, stress management, smoking cessation, proper nutrition and the positive psychological aspects of exercise. The implications of a health/fitness component in the recovery process are emphasized.

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Wright, Beth S., and Beverly Louise Brown. "Giambattista Tiepolo: Master of the Oil Sketch. Kimbell Art Museum, Fort Worth, Texas. 18 September - 12 December 1993." Eighteenth-Century Studies 27, no. 3 (1994): 483. http://dx.doi.org/10.2307/2739366.

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Lewan, M. D., and M. J. Pawlewicz. "Reevaluation of thermal maturity and stages of petroleum formation of the Mississippian Barnett Shale, Fort Worth Basin, Texas." AAPG Bulletin 101, no. 12 (December 2017): 1945–70. http://dx.doi.org/10.1306/01251716053.

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Simpkins, James W., and Meharvan Singh. "Consortium for the Assessment of Research on Progestins and Estrogens (CARPE) Fort Worth, Texas August 1–3, 2003." Journal of Women's Health 13, no. 10 (December 2004): 1165–68. http://dx.doi.org/10.1089/jwh.2004.13.1165.

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Montgomery, Scott L., Daniel M. Jarvie, Kent A. Bowker, and Richard M. Pollastro. "Mississippian Barnett Shale, Fort Worth basin, north-central Texas: Gas-shale play with multi–trillion cubic foot potential." AAPG Bulletin 89, no. 2 (February 2005): 155–75. http://dx.doi.org/10.1306/09170404042.

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