The Trinity River, Water Management, and the City
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Stormwater Management Program 2013-2018 Appendix A
Appendix A 2012 Texas Integrated Report - Texas 303(d) List (Category 5) 2012 Texas Integrated Report - Texas 303(d) List (Category 5) As required under Sections 303(d) and 304(a) of the federal Clean Water Act, this list identifies the water bodies in or bordering Texas for which effluent limitations are not stringent enough to implement water quality standards, and for which the associated pollutants are suitable for measurement by maximum daily load. In addition, the TCEQ also develops a schedule identifying Total Maximum Daily Loads (TMDLs) that will be initiated in the next two years for priority impaired waters. Issuance of permits to discharge into 303(d)-listed water bodies is described in the TCEQ regulatory guidance document Procedures to Implement the Texas Surface Water Quality Standards (January 2003, RG-194). Impairments are limited to the geographic area described by the Assessment Unit and identified with a six or seven-digit AU_ID. A TMDL for each impaired parameter will be developed to allocate pollutant loads from contributing sources that affect the parameter of concern in each Assessment Unit. The TMDL will be identified and counted using a six or seven-digit AU_ID. Water Quality permits that are issued before a TMDL is approved will not increase pollutant loading that would contribute to the impairment identified for the Assessment Unit. Explanation of Column Headings SegID and Name: The unique identifier (SegID), segment name, and location of the water body. The SegID may be one of two types of numbers. The first type is a classified segment number (4 digits, e.g., 0218), as defined in Appendix A of the Texas Surface Water Quality Standards (TSWQS). -
Houston-Galveston, Texas Managing Coastal Subsidence
HOUSTON-GALVESTON, TEXAS Managing coastal subsidence TEXAS he greater Houston area, possibly more than any other Lake Livingston A N D S metropolitan area in the United States, has been adversely U P L L affected by land subsidence. Extensive subsidence, caused T A S T A mainly by ground-water pumping but also by oil and gas extraction, O C T r has increased the frequency of flooding, caused extensive damage to Subsidence study area i n i t y industrial and transportation infrastructure, motivated major in- R i v vestments in levees, reservoirs, and surface-water distribution facili- e S r D N ties, and caused substantial loss of wetland habitat. Lake Houston A L W O Although regional land subsidence is often subtle and difficult to L detect, there are localities in and near Houston where the effects are Houston quite evident. In this low-lying coastal environment, as much as 10 L Galveston feet of subsidence has shifted the position of the coastline and A Bay T changed the distribution of wetlands and aquatic vegetation. In fact, S A Texas City the San Jacinto Battleground State Historical Park, site of the battle O Galveston that won Texas independence, is now partly submerged. This park, C Gulf of Mexico about 20 miles east of downtown Houston on the shores of Galveston Bay, commemorates the April 21, 1836, victory of Texans 0 20 Miles led by Sam Houston over Mexican forces led by Santa Ana. About 0 20 Kilometers 100 acres of the park are now under water due to subsidence, and A road (below right) that provided access to the San Jacinto Monument was closed due to flood- ing caused by subsidence. -
Habitat Restoration in the Middle Trinity River Basin When It Comes to Water, the Trinity River Is the Life Blood of People in Dallas/Fort Worth (DFW) and Houston
APRIL 2011 Habitat Restoration in the Middle Trinity River Basin When it comes to water, the Trinity River is the life blood of people in Dallas/Fort Worth (DFW) and Houston. Compromised flow, water quality impairments, and increasing water demands have forced municipalities within the Trinity River Basin to consider long-term solutions for clean water supply often from outside entities (e.g., purchase and transfer of water from other regions of the state). 1 Trinity River—Perspective of History When it comes to water, the Trinity River is the It must have been something to see the Trinity River life blood of people in Dallas/Fort Worth (DFW) prior to European settlement, when Native Americans and Houston. Compromised flow, water quality traveled its bends. One’s imagination can transport impairments, and increasing water demands have you to another time to see the river through the eyes forced municipalities within the Trinity River Basin of French explorer, René Robert La Salle, who stood on to consider long-term solutions for clean water supply its banks in 1687 and was inspired to call it the River often from outside entities (e.g., purchase and transfer of Canoes. of water from other regions of the state). There Rivers were once the highways of frontiersmen, are likely multiple strategies for water supply, but as these waterways afforded the easiest travel, linking maintaining a healthy Trinity River ecosystem is one land with sea and therefore becoming avenues of that is often overlooked. commerce. Over the years as commerce increased, the modest cow town of Fort Worth on the river’s Population Trends and Importance of the northern end combined with neighboring Dallas to Trinity River become one of the top 10 fastest growing metropolitan The population in Texas will expand significantly in areas in the nation. -
Figure 12. Map Location of Elm Fork of the Trinity River (Denton County)
Adapted from TxDOT County Maps of Texas, Denton, Texas. 1998. Figure 12. Map Location of Elm Fork of the Trinity River (Denton County) Figure 13. Elm Fork of the Trinity River north of FM 428 20 Elm Fork of the Trinity River (Denton County) The Elm Fork of the Trinity River begins one mile northwest of Saint Jo in eastern Montague County and flows southeasterly about 85 miles to its junction with the West Fork of the Trinity River, where it forms the Trinity River about five miles northwest of Dallas (TPWD, 1998). This section of the Elm Fork meanders through heavily wooded areas of the Eastern Cross Timbers region of Texas from Lake Ray Roberts to Lake Lewisville. Along the banks of the Elm Fork of the Trinity River between the two reservoirs is a unique 10-mile multi-use trail system called the Greenbelt Corridor. The Greenbelt Corridor provides access to the Elm Fork at three trailheads for equestrians, hikers, bikers, canoeists, anglers, and other outdoor enthusiasts (TPWD, 2000). A partial plant list from Lake Ray Roberts State Park includes sumac holly, prickly pear, rough leaf dogwood, eastern red cedar, persimmon, black hickory, black walnut, red bud, honey mesquite, eastern cottonwood, black willow, and numerous oak and elm species. Mammals found in the area include opossum, cave bat, nutria, plains pocket gopher, eastern flying squirrel, California jackrabbit, eastern cottontail, white-tail deer, mink, spotted skunk, red fox, coyote, and bobcat. Numerous reptiles and amphibians have also been found in the area, including various snakes, such as copperhead, cottonmouth, bullsnake, and diamondback rattlesnake (TPWD, 2000). -
Chapter 1 Description of the Region
Chapter 1 Description of the Region The East Texas Regional Water Planning Area (ETRWPA) is one of sixteen areas established by the 1997 Texas legislature Senate Bill 1 for the purpose of State water resource planning at a regional level on five- year planning cycles. The first regional water plan was adopted in 2001. Since that time, it was updated in 2006, 2011, and 2016. This plan, the 2021 Regional Water Plan (2021 Plan), is the result of the 5th cycle of regional water planning. Pursuant to the formation of the ETRWPA, the East Texas Regional Water Planning Group (ETRWPG or RWPG), was formed and charged with the responsibility to evaluate the region’s population projections, water demand projections, and existing water supplies for a 50-year planning horizon. The RWPG then identifies water shortages under drought of record conditions and recommends water management strategies. This planning is performed in accordance with regional and state water planning requirements of the Texas Water Development Board (TWDB). This chapter provides details for the ETRWPA that are relevant to water resource planning, including: a physical description of the region, climatological details, population projections, economic activities, sources of water and water demand, and regional resources. A discussion of threats to the region’s resources and water supply, a general discussion of water conservation and drought preparation in the region, and a listing of ongoing state and federal programs in the ETRWPA that impact water planning efforts in the region are also provided. 1.1 General Introduction The ETRWPA consists of all or portions of 20 counties located in the Neches, Sabine, and Trinity River Basins, and the Neches- Trinity Coastal Basin. -
Lower Galveston Bay Watershed Legend
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Zapruder Film
Zapruder film From Wikipedia, the free encyclopedia Jump to: navigation, search Frame 150 from the Zapruder Film The Zapruder film is a silent, 8 mm color home movie shot by Abraham Zapruder in Dallas, Texas, in Dealey Plaza while standing near "the grassy knoll" during the assassination of President John F. Kennedy on November 22, 1963. It is the definitive, most authoritative footage of the assassination. Contents [hide] • 1 Background • 2 History • 3 Use in "JFK" • 4 External links [edit] Background Zapruder filmed the scene with a Model 414 PD Bell & Howell Zoomatic Director Series Camera that operated via a spring-wound mechanism at an average tested speed of 18.3 frames-per-second. The entire Dealey Plaza exposed film frames lasts 26.6 seconds, with the presidential assassination sequence occupying 19.3 seconds. There are 486 frames altogether. The sequence is recorded on Kodak Kodachrome II 8 mm movie safety film. Zapruder, who suffered from vertigo, made the film while being steadied by his receptionist, Marilyn Sitzman, standing on the most western of two concrete pedestals which extend from the John Neely Bryan north pergola cement structure, overlooking Elm street in Dealey Plaza. President Kennedy's automobile was below and almost exactly in front of Zapruder on Elm Street, at the time of his fatal wound to the head. The film has been used by the Warren Commission and all subsequent investigations of the assassination. The Zapruder frames used by the Commission consist of exhibits 889–899 plus exhibits 901 and 902 (totaling less than 1 second of the actual 26.6 second film), published in the commission supporting volume XVIII. -
TPWD Strategic Planning Regions
River Basins TPWD Brazos River Basin Brazos-Colorado Coastal Basin W o lf Cr eek Canadian River Basin R ita B l anca C r e e k e e ancar Cl ita B R Strategic Planning Colorado River Basin Colorado-Lavaca Coastal Basin Canadian River Cypress Creek Basin Regions Guadalupe River Basin Nor t h F o r k of the R e d R i ver XAmarillo Lavaca River Basin 10 Salt Fork of the Red River Lavaca-Guadalupe Coastal Basin Neches River Basin P r air i e Dog To w n F o r k of the R e d R i ver Neches-Trinity Coastal Basin ® Nueces River Basin Nor t h P e as e R i ve r Nueces-Rio Grande Coastal Basin Pease River Red River Basin White River Tongue River 6a Wi chita R iver W i chita R i ver Rio Grande River Basin Nor t h Wi chita R iver Little Wichita River South Wichita Ri ver Lubbock Trinity River Sabine River Basin X Nor t h Sulphur R i v e r Brazos River West Fork of the Trinity River San Antonio River Basin Brazos River Sulphur R i v e r South Sulphur River San Antonio-Nueces Coastal Basin 9 Clear Fork Tr Plano San Jacinto River Basin X Cypre ss Creek Garland FortWorth Irving X Sabine River in San Jacinto-Brazos Coastal Basin ity Rive X Clea r F o r k of the B r az os R i v e r XTr n X iityX RiverMesqu ite Sulphur River Basin r XX Dallas Arlington Grand Prai rie Sabine River Trinity River Basin XAbilene Paluxy River Leon River Trinity-San Jacinto Coastal Basin Chambers Creek Brazos River Attoyac Bayou XEl Paso R i c h land Cr ee k Colorado River 8 Pecan Bayou 5a Navasota River Neches River Waco Angelina River Concho River X Colorado River 7 Lampasas -
A Preliminary Evaluation of Trinity River Sediment and Nutrient Loads Into Galveston Bay, Texas, During Two Periods of High Flow
A PRELIMINARY EVALUATION OF TRINITY RIVER SEDIMENT AND NUTRIENT LOADS INTO GALVESTON BAY, TEXAS, DURING TWO PERIODS OF HIGH FLOW Michael T. Lee, Hydrologist - U.S. Geological Survey, Texas Water Science Center, 19241 David Memorial Drive, Suite 180, Conroe, TX 77385, ph. 936-271-5313, fax 936-271-5399, [email protected] INTRODUCTION Background: The amount of nutrients and sediment delivered to an estuary affects water- quality and the coastal ecosystem. Excess nutrients and suspended sediment in the environment can be detrimental to aquatic ecosystems and to the health of organisms living in and using the coastal waters. Nutrients are required to sustain life, but excess nutrient loads can upset the nutrient cycle balance resulting in changes in water quality harmful to aquatic organisms (Aldous and others, 2005). Nitrogen and phosphorus compounds occur naturally in coastal streams and rivers but also are commonly applied to land as commercial fertilizers and livestock waste to increase agricultural production (Crain, 2006). Nitrogen is present in water as nitrite and nitrate anions, in cationic form as ammonium (all inorganic nitrogen), and as part of organic solutes (Hem, 1992). Phosphorus is not as abundant in the environment as nitrogen and often is the limiting element for plant growth (East and others, 1998). Usually phosphorus is present as phosphate in natural waters and much of the phosphorus in streams attaches to particulate matter and is unavailable for uptake by plants. Orthophosphate species are the predominant dissolved phosphorus forms in most streams (Terrio, 1995). Nutrients that are not utilized by crops or stored in the soil can runoff to streams in overland flow or infiltrate with groundwater recharge; water quality in estuaries that receive surface-water inflows or groundwater discharge containing excess amounts of nutrients is often degraded. -
A G a T E W a Y T 0 T H E C I T Y 0 F DALLAS , TEXAS a County Government Center a Thesis Submitted in Partial Fulfillment Of
A G A T E W A Y T 0 T H E C I T Y 0 F DALLAS , TEXAS A County Government Center A Thesis Submitted In Partial Fulfillment of the Requirements for the Degree of Master In Architecture Massachusetts Institute of Technology Cambridge, Massachusetts August 13, 1958 Respectfully submitted _ John Crews Rainey, B. Arch. University of Texas 6- ) Lawrence B. Anderson, Head Department of Architecture Massachusetts Institute of Technology Room 14-0551 77 Massachusetts Avenue Cambridge, MA 02139 Ph: 617.253.2800 MITLibraries Email: [email protected] Document Services http://libraries.mit.edu/docs DISCLAIM ER Page has been ommitted due to a pagination error by the author. ( page 34 ) III A GATEWAY TO THE CITY OF DALLAS A County Government Center John Crews Rainey Submitted for the degree of M. Arch. in the Department of Architecture on August 13, 1958. The city of Dallas, Texas, population 600,000, is air capital of the Southwest, a wholesale and manufacturing center, a quality retailing center, one of the largest insurance centers in the nation and an industrial giant. The city, just over one hundred years old, was founded in 1841 by John Neely Bryan on a bluff overlooking the Trinity River Valley. Bryan's cabin still remains on the bluff as a testament of Dallas' amazing growth. In the past fifty years the center of downtown activity has moved eastward from the area surrounding Bryan's cabin. Due to the recently completed Dallas-Ft. Worth expressway, and because of an existing ring of traffic around the down- town area limiting expansion beyond it, the downtown area will, in the immediate future, expand back to its original location. -
Sediment Characterization of the San Luis Pass Flood Tidal Delta Carolina Ramon-Duenas, Julia S
Sediment characterization of the San Luis Pass flood tidal delta Carolina Ramon-Duenas, Julia S. Wellner with Will Sager and others University of Houston ASBPA Texas Chapter 2018 Symposium April 24rd, 2018 August 22, 2017 August 31, 2017 Galveston Bay Entrance during Harvey Side-scan, Bolivar Roads San Luis Pass during Harvey August 31, 2017 San Luis Pass Gulf of Mexico Flood tidal deltas Flood tidal delta - Accumulation of sand on the shoreward side of an inlet Maintained by flood currents FitzGerald et al. 2012 Why San Luis Pass? • One of few natural tidal deltas in Texas • Migrating westward flood delta • San Luis Pass (SLP) tidal delta is the primary sink for most of the sand eroded from updrift parts of Galveston Island Modified Texas General Land Office Methods • 2D High Resolution Seismic (CHIRP) R/V Mishipeshu • Seafloor samples Grain size (CILAS) Smear slides • Publicly available cores and databases 200 um How Chirp is Collected Convert .JSF to .SEGY Extract Navigation using SeiSee Processing (Gain- Smoothing) Load Navigation and SEGY to Kingdom software How Samples are Collected • Water depth • Ripples height • Ripples wavelength • Geometry description • Progradation direction Delta Evolution Evolution SLP flood tidal delta Formation inlet Migration 3-4 m/yr Current position ~2100 yr BP GI – Galveston Island FI – Follets Island Wallace & Anderson 2013 Lateral and vertical lithofacies San Luis Pass Brazos river Davis & Dalrymple 2012 after Israel 1987 Chirp data • 65 km Summer 2017 • 22 km Fall 2017 • 87 km in total Chirp data • 65 km Summer 2017 • 22 km Fall 2017 • 87 km in total A B` A` B Chirp data A A` 12 12 meters Chirp data A A` 12 12 meters Pleistocene-Holocene SB 12 meters Chirp data B B` 9 9 meters Chirp data B B` 9 9 meters Pleistocene-Holocene SB Chirp data B B` Pleistocene- Holocene SB 7.5 meters Pleistocene-Holocene SB Paleo-channel locations -5 m Wallace & Anderson 2013 -20 m River paths from Dellapenna et. -
Mas Rtt Wastiiiigt3u,Fie Mm
COMMERCE STREET VIADUCT HAER No. TX-35 Texas Historic Bridges Recording Project Spanning Trinity River at Commerce Street M Ac. » Mas rtT Dallas County ' fcA Texas S^. ^fl^ C- BLACK AND WHITE PHOTOGRAPHY XEROGRAPHIC COPIES OF COLOR TRANSPARENCIES WRITTEN HISTORICAL AND DESCRIPTIVE DATA HISTORIC AMERICAN ENGINEERING RECORD National Park Service Department of the Interior 1849CSt,NW wastiiiigt3u,fie mm V«fc«i&le.-...^<L''"*:2j HISTORIC AMERICAN ENGINEERING RECORD &y- ML. COMMERCE STREET VIADUCT HAERNo.TX-35 Location: Spanning Trinity River at Commerce Street, Dallas, Dallas County, Texas. UTM: 14/704240/3628300 USGS: Dallas, Texas, quadrangle. Date of Construction: Circa 1930. Designer: Francis Dey Hughes, consulting engineer, Dallas, Texas. Builder: Austin Bridge Company, Dallas, Texas; Mosher Steel and Machinery Company, Dallas, Texas, steel fabricator. Present Owner: City of Dallas. Present Use: Vehicular bridge. Significance: The Commerce Street Viaduct, a major viaduct over the Trinity River in Dallas, featured the largest steel girders fabricated in Texas at the time of its construction. Historian: Robert W. Jackson, August 1996. Project Information: This document was prepared as part of the Texas Historic Bridges Recording Project performed during the summer of 1996 by the Historic American Engineering Record (HAER). The project was sponsored by the Texas Department of Transportation (TxDOT). I:ii-„ ■_'*,!.. ..JL':AIJI , COMMERCE STREET VIADUCT HAERNo.TX-35 (Page 2) Introduction: Site Development The Commerce Street Viaduct is one of four highway viaducts built in the early 1930s as part of a plan to relieve traffic congestion on the Dallas-Oak Cliff (Houston Street) Viaduct, which served since 1912 as the only reliable all-weather road crossing of the Trinity River at Dallas.