Greens Bayou Watershed Is Wholly Contained Profile No Matter Where E Ed E Ersh Within Harris County and Is a Part of the Lower Area 213 Sq

Total Page:16

File Type:pdf, Size:1020Kb

Greens Bayou Watershed Is Wholly Contained Profile No Matter Where E Ed E Ersh Within Harris County and Is a Part of the Lower Area 213 Sq Water Designated Uses Quality Contact Recreation • Limited Quality Aquatic Habitat Monitoring Agencies City of Houston Health and Human Services City of Houston Public Works and Engineering (historical) RHEINHARDT BAYOU Texas Natural Resource Conservation Commission United States Geological Survey (flow) GARNERS BAYOU 1 GREENS BAYOU Dissolved oxygen, water temperature, and bacteria LAKE Sam Houston Tollway HOUSTON levels are critical factors that impact aquatic life. These charts show the actual value of water samples taken between 1994-1999. I-45 Oxygen in the water is important to aquatic I-59 life. Generally, dissolved Fig. 1 oxygen levels are con- SHELDON sidered good for aquatic RESERVOIR organisms at 5mg/l HALLS BAYOU (or higher). Fish popu- lations can still be supported, although mg/L stressed, at levels as colonies/ °C Flood Control low as 3 mg/l. 100mL Throughout the watershed the temper- Before extensive development occurred throughout Sam Houston Tollway Temperature affects ature dissolved oxygen relationship the watershed, Greens Bayou had a relatively small 2 the quality of aquatic appears to be satisfactory. Dissolved channel with tree-lined banks and tight meanders. During flood life and also dictates oxygen readings are adequate for events, water would pond in forested and grassy areas and slowly the amount of oxygen survival of aquatic populations in the infiltrate into the soil. Hwy. 90 SPRING GULLY that can be contained 1 upper and middle sections of the in water. watershed. However, in the lower As residential development increased impervious cover, reducing In the 1990’s, other more reaches of the bayou, these levels dip infiltration and accelerating runoff, physical modifications to the channel “environmentally friendly” types of flood Coolgreen Bacteria counts are below the levels that support healthy to control flooding became a necessity. Individuals first dug ditches from damage reduction measures were implemented. Corridor important in assessing fish habitation. There is substantially suburbs to the bayou to reduce flooding problems, but these efforts soon The Harris County Flood Control District constructed a waterbody’s suitability Fig. 2 more urban development in the middle became inefficient and more substantial modifications were required to a large detention structure and a wetlands mitigation for contact recreation, and lower portions of the watershed, effectively protect the surrounding communities. bank (1450 acres) near John Ralston Road to provide temporary flood such as swimming. resulting in polluted stormwater runoff, water storage. Smaller detention basins were also created along the Fecal coliform densities which can cause lower oxygen levels. Major modifications below US HWY 59 began in 1973, and modifications bayou and its tributaries. Water is detained in these basins until the below 200 colonies/ in the upper reaches of the bayou began in the early 1980’s. With floodwaters recede and the bayou can accommodate added water. 100 ml of water are Although the stations in the middle these modifications, the bayou’s physical nature was compromised. Since these structures do not affect the bayou during non-flooding GOODYEAR CREEK considered acceptable. and lower portions of the watershed The bayou’s meanders and bends were straightened, the cross-sections events, aquatic and aesthetic properties are minimally affected. exhibit a stable or slightly decreasing were enlarged, and portions of its banks were paved. Although this 1 = Monitoring Site trend in dissolved oxygen values, the colonies/ increased hydraulic capacities, aquatic habitat was degraded due to The District, in cooperation with other federal, state, and local agencies, mg/L °C 100mL station located in the upper portion of reduction of near-stream vegetation (shade cover) and pool and riffle is also active in purchasing homes and other buildings that are frequent- i-10 the watershed shows a significant sequences, which provide diverse aquatic habitat. ly inundated during flood events. This “buyout” program has been quite = Detention Basin Fig. 1 decline in oxygen levels since 1994. Fecal coliform densities successful in Harris County, with several hundred homes having been 3 during the time frame Continued development in the upper purchased in the last decade. Participants are given fair-market value for represented were all within portions of the watershed could their property and may receive assistance in relocating. Flood-prone reportable limits. 2 continue this trend. structures are then removed, resulting in reduced flood losses. Fig. 2 Fecal coliform densities Bacteria counts throughout the water- Since flooding problems are not always the result of activities or land on 11/6/97, 12/3/97, and shed are well above contact recreation 1/7/98 were reported as uses in close proximity to a large waterbody, the District also purchases standards at each station. Typically, >160,000 colonies/100 ml; available land outside the floodplain. Depending on the landscape and To Houston Ship Channel densities on 9/2/99 were Fig. 3 these densities are higher after land use, any part of a reported as >200,000 rainstorms, which wash bacteria from watershed can be inundated colonies/100 ml. many sources into area waterways. with water as it makes it way Fig. 3 Fecal coliform numbers generally to the major drainage channel Fecal coliform densities decline rapidly after a rainfall unless on 5/4/95 and 12/6/95 during a heavy rain event. were reported as <200 there is a continuous source of bacteria Thus, watershed planning colonies/100 ml; densities present, such as a leaking septic tank in terms of flood damage on 1/7/98 were reported as or sewer line. reduction is essential in >160,000 colonies/100 ml. colonies/ protecting lives and property mg/L °C NOTE: 100mL Degree of development also impacts in a drainage basin/watershed. Trend lines do not the amount of bacteria present as necessarily correspond to actual values on the evidenced by the higher fecal densities y-axis. The slope of the in the lower portions of the watershed. trend lines exhibit the best-fit line and indicate either increasing, 3 decreasing, or no change in the corresponding para- meter over time plotted. Watershed G r The Greens Bayou watershed is wholly contained Profile No matter where e ed e ersh within Harris County and is a part of the lower Area 213 Sq. Miles ns B u Wat San Jacinto River Basin. Greens Bayou is the largest ayo tributary to Buffalo Bayou and the Houston Ship we live or work, G Rainfall Average Annual 46" Channel. Its watershed contains portions of the Coolgreen Corridor Local Residents Get Involved Elevation 20'-134' we are always r City of Houston as well as unincorporated residential The “Coolgreen Corridor” is land set aside to reduce flood damage, but is primarily intended to be a nature e areas and undeveloped brushland. d Geology Sedimentary formations preserve. The corridor connects Herman Brown Park with Greens Bayou, approximately 1.5 miles north of e consisting of materials h in a watershed – Interstate 10 in Houston. Currently, there is no official entrance to the preserve; however, visitors can e s deposited by water r access the corridor’s nature trails through a vacant lot on Pecan Grove Drive off of Coolgreen Avenue. n te Vegetation Coastal short grass prairie s a an area of land The movement to acquire the original 23-acre strip of land began in 1989 after several severe flooding W (predominant) Bayou events damaged residents’ homes. Previously, in anticipation of the completion of the NE segment of Pine-hardwood forest that drains to a Beltway 8, the Harris County Flood Control District dug ditches to alleviate flooding problems associated Soils Clay and silt, locally sandy with the highway development. The beltway was completed before detention basins could be put in, and Poorly drained stormwater from the ditches increased flow in the bayou, resulting in increased flooding problems to High moisture retention at particular creek, homes downstream. the surface Some areas with higher river, bayou or Almost a decade later, a conservation investor donated money through the Brown Foundation, allowing permeabilities serve as the land to be purchased and donated to the Houston Parks Board, and, finally, to the City of Houston. aquifer recharge zones The sale included a deed restriction requiring that the land not be developed under any circumstances. lake. As our Since that acquisition, two private landowners and Texaco USA have donated adjacent land, expanding Major Ecoregion Western Gulf Coastal Plain the corridor to over 50 acres. Currently, members of the Legacy Land Trust are contacting other property owners, mainly those with flood-prone property, in an effort to enlarge the corridor further. Their visions Cities Houston population grows, include expanding the strip to Sheldon State Park, creating a continuous wildlife corridor and refuge Humble between Herman Brown Park and Sheldon State Park. Tributaries Halls Bayou so do the risks Garners Bayou Projects involving public and private entities are extremely important when attempting to preserve or clean up the environment. When these groups Spring Gully are able to work together, partnerships can be established with multiple benefits for all involved. The Coolgreen Corridor is a prime example of a project Big Gulch to our waterways that benefits a variety of local interests as well as maintains the health of the environment. The Coolgreen Corridor serves to enhance aesthetics of the Goodyear Creek waterway and surrounding neighborhoods, to filter runoff and enhance water quality, and to reduce flooding. The land includes specific designated sites for bird habitat, and preserves a contiguous corridor in which migratory animals can move, enhancing the diversity of species and enriching the habitat. Aquifers Gulf Coast from activities in In addition, people can experience nature in the middle of a highly urban area while learning about the bayou ecosystem. Issues Flooding/high moisture History retention at surface due the watershed.
Recommended publications
  • See Our Park Map of Water Bottle Refill Stations!
    D V L B S Spotts Park O’Reilly St T Sawyer St H I E Snover St Snover Jackson Hill St Hill Jackson THEWATERWORKS H Zane and Brady Washington Glenwood N Memorial Way HOUSTONAVE SHEPHERDDR Cemetery Cemetery buffalo BAYO U EORIALDR Carruth Overlook Carruth STUDEONTST Bridge EORIALDR Green Tree to Sixth Ward Nature Area 0.40 M.D. Anderson Buffalo Bayou has been a focal point in Houston’s Foundation Stairway Cleveland Park Fonde history since the Allen brothers founded the city in 0.42 Rec. Center (weekends and evenings aer 1836. Today, the bayou is once again the centerpiece Houston Police Tapley 5pm only) Hamill Foundation Stairway Officers’ Memorial Tributary St Sabine of its development. Rosemont Bridge Rusk St » St. Thomas High School 0.18 Buffalo Bayou Partnership (BBP) is the non-profit organiza- 0.80 0.56 Shepherd Gateway Scurlock Foundation Overlook LDR ORIA Lee & Joe Jamail Hobby Center tion revitalizing and transforming Buffalo Bayou from a gi from the Radoff Family E Sabine Promenade Jackson Hill Bridge Skatepark Bridge Shepherd Drive to the Port of Houston Turning Basin. From to Memorial Park 0.39 Jane Gregory spearheading capital projects such as the 160-acre Buffalo EORIALDR Hobby 1.14 Garden Center 0.45 Bayou Park to constructing hike and bike trails, operating Neumann Family Barbara Fish Daniel comprehensive clean-up and maintenance programs and Wortham Foundation Stairway Nature Play Area Waugh Grove offering thoughtful programming, Buffalo Bayou Partnership Bat Colony ALLENPKWY Brookfield Bridge « Walker St is reclaiming Houston’s unique waterfront. JOHNNYSTEELE Federal Reserve Bank City Hall Bud Light Amphitheater Crosby McKinney St » Annex This map will guide you as you walk, run, cycle or paddle LOSTLAKE DOPARK Outfall ONTROSEBLVD TAFTST Gillette St Gillette ELEANORTINSLEYPARK Bagby St City along the waterway and visit the many parks and historic SHEPHERDDR WAUHDR Sam Houston Park Hall sites.
    [Show full text]
  • South Fox Meadow Drainage Improvement Project
    VILLAGE OF SCARSDALE WESTCHESTER COUNTY, NEW YORK COMPREHENSIVE STORM WATER MANAGEMENT SOUTH FOX MEADOW STORMWATER IMPROVEMENT PROJECT In association with WESTCHESTER COUNTY FLOOD MITIGATION PROGRAM Rob DeGiorgio, P.E., CPESC, CPSWQ The Bronx River Watershed Fox Meadow Brook Bronx River Watershed Area in Westchester 48.3 square miles (30,932 acres) 15 Sub-watersheds Percent of undeveloped land in the Watershed 3.3% (0.8 acres in Fox Meadow Brook (FMB) FMB watershed) 928 acres (5.7% of watershed) Bronx River Watershed Fox Meadow Brook George Field Park High School Duck Pond Project Philosophy and Goals •Provide flood mitigation within the Fox Meadow Brook Drainage Basin. •Reduce peak run off rates in the Bronx River Watershed through dry detention storage. •Rehabilitate and preserve natural landscapes and wetlands through invasive species management and re- construction. •Improve water quality. • Petition for and obtain County grant funding to subsidize the project. Village of Scarsdale Fox Meadow Brook Watershed SR-2 BR-4 SR-3 BR-7 BR-8 SR-5 Village of Scarsdale History •In 2009 the Village completed a Comprehensive Storm Water Management Plan. •Critical Bronx River sub drainage basin areas identified inclusive of Fox Meadow Brook (BR-4, BR-7, BR-8). •26 Capital Improvement Projects were identified, several of which comprise the Fox Meadow Detention Improvement Project. •Project included in Village’s Capital Budget. •Project has been reviewed by the NYS DEC. •NYS EFC has approved financing for the project granting Scarsdale a 50% subsidy for their local share of the costs. Village of Scarsdale Site Locations – 7 Segments 7 Project Segments 1.
    [Show full text]
  • Water Quality Monitoring in the Bayou Teche Watershed
    Water Quality Monitoring in the Bayou Teche Watershed Researchers: Dr. Whitney Broussard III Dr. Jenneke M. Visser Kacey Peterson Mark LeBlanc Project type: Staff Research Funding sources: Louisiana Department of Environmental Quality, Environmental Protection Agency Status: In progress Summary The historic Bayou Teche is an ancient distributary of the Mississippi River. Some 3,000-4,000 years ago, the main flow of the Mississippi River followed the Bayou Teche waterway. This explains the long, slow bends of the small bayou and its wide, sloping banks. The Atákapa-Ishák nation named the bayou “Teche” meaning snake because the course of the bayou looked like a giant snake had laid down to rest, leaving its mark on the land. Many years later, the first Acadians arrived in Southwestern Louisiana via Bayou Teche. They settled along its banks and used the waterway as a means of transportation and commerce. The bayou remains to this day an iconic cultural figure and an important ecological phenomenon. Several modern events have reshaped the quality and quantity of water in Bayou Teche. After the catastrophic flood of 1927, the United States Congress authorized the US Army Corps of Engineers to create the first comprehensive flood management plan for the Mississippi River. One important element of this plan was the construction of the West Atchafalaya Basin Protection Levee, which, in conjunction with the East Protection Levee, allows the Corps of Engineers to divert a substantial amount of floodwaters out of the Mississippi River into the Atchafalaya Spillway, and away from major urban centers like Baton Rouge and New Orleans.
    [Show full text]
  • Classifying Rivers - Three Stages of River Development
    Classifying Rivers - Three Stages of River Development River Characteristics - Sediment Transport - River Velocity - Terminology The illustrations below represent the 3 general classifications into which rivers are placed according to specific characteristics. These categories are: Youthful, Mature and Old Age. A Rejuvenated River, one with a gradient that is raised by the earth's movement, can be an old age river that returns to a Youthful State, and which repeats the cycle of stages once again. A brief overview of each stage of river development begins after the images. A list of pertinent vocabulary appears at the bottom of this document. You may wish to consult it so that you will be aware of terminology used in the descriptive text that follows. Characteristics found in the 3 Stages of River Development: L. Immoor 2006 Geoteach.com 1 Youthful River: Perhaps the most dynamic of all rivers is a Youthful River. Rafters seeking an exciting ride will surely gravitate towards a young river for their recreational thrills. Characteristically youthful rivers are found at higher elevations, in mountainous areas, where the slope of the land is steeper. Water that flows over such a landscape will flow very fast. Youthful rivers can be a tributary of a larger and older river, hundreds of miles away and, in fact, they may be close to the headwaters (the beginning) of that larger river. Upon observation of a Youthful River, here is what one might see: 1. The river flowing down a steep gradient (slope). 2. The channel is deeper than it is wide and V-shaped due to downcutting rather than lateral (side-to-side) erosion.
    [Show full text]
  • Topic: Drainage Basins As Open Systems 3.1.1.2 Runoff, Hydrographs & Changes in the Water Cycle Over Time
    Topic: Drainage basins as open systems 3.1.1.2 Runoff, hydrographs & changes in the water cycle over time What you need to know How runoff varies within the water cycle. How to analyse a flood hydrograph How the water cycle changes over time Introduction: Runoff (the flow of water over the Earth’s surface) can vary depending upon a range of physical and human factors. These include: • Time of year. • Storm conditions. • Vegetation cover. • Soil saturation levels. • Topography & relief. • Agricultural land use. • Urban land use. Physical factors affecting runoff: Time of year In temperate climates, where seasonal change is evident, runoff levels can vary greatly throughout the year. In summer, runoff levels can be low due to a reduction in rainfall. Soil saturation levels will be low and therefore any rainfall at this point can easily infiltrate into the ground. However, intense baking of the soil by the sun can lead to the soil becoming effectively impermeable and summer storms can lead to high levels of runoff as the rain is unable to soak in. This can lead to flash flooSAMPLEds. In winter, precipitation may be in the form of snow and the water may be stored on the ground due to low temperatures. Warmer temperatures in spring may lead to snowmelt and this can lead to the soil reaching field capacity quickly. Further meltwater will therefore run over the surface. © Tutor2u Limited 2016 www.tutor2u.net Topic: Drainage basins as open systems 3.1.1.2 Runoff, hydrographs & changes in the water cycle over time Storm conditions Intense storms with heavy rainfall can lead to soils quickly becoming saturated.
    [Show full text]
  • Louisiana's Waterways
    Section22 Lagniappe Louisiana’s The Gulf Intracoastal Waterways Waterway is part of the larger Intracoastal Waterway, which stretches some three As you read, look for: thousand miles along the • Louisiana’s major rivers and lakes, and U.S. Atlantic coast from • vocabulary terms navigable and bayou. Boston, Massachusetts, to Key West, Florida, and Louisiana’s waterways define its geography. Water is not only the dominant fea- along the Gulf of Mexico ture of Louisiana’s environment, but it has shaped the state’s physical landscape. coast from Apalachee Bay, in northwest Florida, to Brownsville, Texas, on the Rio Grande. Right: The Native Americans called the Ouachita River “the river of sparkling silver water.” Terrain: Physical features of an area of land 40 Chapter 2 Louisiana’s Geography: Rivers and Regions The largest body of water affecting Louisiana is the Gulf of Mexico. The Map 5 Mississippi River ends its long journey in the Gulf’s warm waters. The changing Mississippi River has formed the terrain of the state. Louisiana’s Louisiana has almost 5,000 miles of navigable rivers, bayous, creeks, and Rivers and Lakes canals. (Navigable means the water is deep enough for safe travel by boat.) One waterway is part of a protected water route from the Atlantic Ocean to the Map Skill: In what direction Gulf of Mexico. The Gulf Intracoastal Waterway extends more than 1,100 miles does the Calcasieu River from Florida’s Panhandle to Brownsville, Texas. This system of rivers, bays, and flow? manmade canals provides a safe channel for ships, fishing boats, and pleasure craft.
    [Show full text]
  • The Francis M. Weston Audubon Society Blackwater River State Forest Bird Survey Peggy Baker
    Spring 2013 April-June Vol. XL No. 4 The Francis M. Weston Audubon Society Blackwater River State Forest Bird Survey Peggy Baker Blackwater River State Forest has been designated The food plots planted for game wildlife also attracted by the National Audubon as an Important Bird great numbers of wintering Chipping and Vesper Area with a global priority (the highest). This Sparrows, as well as Palm, Pine and Yellow-rumped designation means this area in Northwest Florida is vital to Warblers. birds and other biodiversity. It provides essential habitat for Dead snags left standing throughout the forest have the survival of one or more species. In 2009, FMWAS attracted large numbers of woodpeckers. Along with undertook the task of surveying the birds in BRS Forest by the Red-cockaded Woodpeckers, the forest is home to conducting weekly surveys. good numbers of nesting Pileated, Red-bellied, Red- During our three-year bird survey of the 240,000 acres headed, and Downy Woodpeckers, as well as, Northern of the BRS Forest, the FMWAS team identified 181 bird Flicker. There are a good number of Yellow-bellied species. Of these, 33 species were spring and fall migrants, Sapsuckers and a few Hairy Woodpeckers during the 35 were summer visitors only, 60 were winter only, and winter season. 53 species were seen year round. And most importantly, Eastern Bluebirds have returned to nest in the natural 86 of these species nest and raise young in BRS Forest. cavities of the dead snags. Brown-headed Nuthatches are Under the Migratory Bird Program, the U. S.
    [Show full text]
  • Attoyac Bayou Wpp Development Attoyac.Tamu.Edu
    attoyac bayou wpp development attoyac.tamu.edu The Attoyac Bayou, a sub-watershed within the Upper Neches River Watershed, extends approximately 82 miles through Rusk, Nacogdoches, San Augustine and Shelby counties before emptying into Sam Rayburn Reservoir. With several rural communities in the area, the majority of the land in the watershed is used for cattle and poultry operations, forestry or recreational and wildlife uses. The bayou is one of many rural watersheds listed as Objectives an impaired water body on the Texas Integrated Report • Assess the current water quality conditions and for Clean Water Act Sections 305(b) and 303(d) due to impairments through targeted water quality high levels of E. coli, the non-pathogenic indicator sampling and analysis bacteria found in birds and mammals used by the state to evaluate a water body’s ability to support contact • Conduct a watershed source survey and develop a recreation. Three monitoring stations managed by the comprehensive GIS inventory Angelina & Neches River Authority, U.S. Geological • Analyze water quality data using load duration Survey, and Texas Commission on Environmental Quality curves and spatially explicit modeling have provided water quality data on the bayou for a • Conduct bacteria source tracking and evaluate number of years. Beginning in 2000, data collected for the sources of E. coli present in the watershed E. coli have consistently shown elevated E. coli levels that contributing to the bayou’s bacteria load exceed the applicable Texas Water Quality Standards. • Conduct a Recreational Use Attainability Analysis Studies done to understand bacteria and nutrient and determine the most appropriate water quality loading in the area seem to justify the Attoyac’s standard for the bayou impairment listing, but the limited flow data documented make it difficult to calculate loading rates and identify • Establish and provide direction for a stakeholder sources of E.
    [Show full text]
  • Table of Contents 3.6 Clear Creek
    3.5 Master Drainage Plan ............................................................................................................. 6 Table of Contents 3.6 Clear Creek .............................................................................................................................. 6 1. Introduction ................................................................................................................................... 1 3.6.1 Magnolia Creek ............................................................................................................... 6 1.1 Purpose and Scope ................................................................................................................. 1 3.6.2 Newport – Landing Ditch Basin ....................................................................................... 6 1.2 Use of Report ......................................................................................................................... 1 3.6.3 Corum Ditch .................................................................................................................... 7 1.3 Data Sources .......................................................................................................................... 1 3.6.4 Interurban Ditch .............................................................................................................. 7 1.3.1 LiDAR .............................................................................................................................. 1 3.6.5 Robinsons
    [Show full text]
  • River Network Rearrangements in Amazonia Shake Biogeography and Civil Security
    Preprints (www.preprints.org) | NOT PEER-REVIEWED | Posted: 10 September 2018 doi:10.20944/preprints201809.0168.v1 River Network Rearrangements in Amazonia Shake Biogeography and Civil Security Authors K Ruokolainen1,2*, G Massaine Moulatlet2,3, G Zuquim2, C Hoorn3,4, H Tuomisto2 Affiliations 1 Department of Geography and Geology, University of Turku, 20014 Turku, Finland. 2 Department of Biology, University of Turku, 20014 Turku, Finland. 3 Universidad Regional Amazónica IKIAM, km 7 Via Muyuna, Parroquia Muyuna, Tena, Napo, Ecuador. 4 Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, P.O. Box 94248, 1090 GE Amsterdam, The Netherlands. *Corresponding author. Email: [email protected] Key words: avulsion, civil defence, dispersal barrier, flood, Rio Madeira, rain forest, species distribution Abstract The scene for regional biogeography and human settlements in Central Amazonia is set by the river network, which presumably consolidated in the Pliocene. However, we present geomorphological and sediment chronological data showing that the river network has been anything but stable. Even during the last 50 kyr, the tributary relationships have repeatedly changed for four major rivers, together corresponding to one third of the discharge of the Amazon. The latest major river capture event converted the Japurá from a tributary of the Rio Negro to a tributary of the Amazon only 1000 years ago. Such broad-scale lability implies that rivers cannot have been as efficient biogeographical dispersal barriers as has generally been assumed, but that their effects on human societies can have been even more profound. Climate change and deforestation scenarios predict increasing water levels during peak floods, which will likely increase the risk of future river avulsions.
    [Show full text]
  • Drainagebasin Characteristics
    350 TRANSACTIONS, AMERICAN GEOPHYSICAL UNION DRAINAGE-BASIN CHARACTERISTICS Robert E. Horton Factors descriptive of a drainage-basin as related to its hydrology may be classi­ fied broadly as s (1) Morphologic—These factors depend only on the topography of the land forms of which the drainage-basin is composed and on the form and extent of the stream-system or drainage-net within It. (2) Soil factors—This group includes factors descriptive of the materials form­ ing the groundwork of the drainage-basin, including all those physical properties in­ volved in the moisture-relations of soils. (3) Geologic-structural factors—These factors relate to the depths and charac­ teristics of the underlying rocks and the nature of the geologic structures in so far as they are related to ground-water conditions or otherwise to the hydrology of the drainage-basin. (4) Vegetational factors—These are factors which depend wholly or in part on the vegetation, natural or cultivated, growing within the drainage-basin. (5) Climatic-hydrologic factors--Climatic factors include: Temperature, humid­ ity, rainfall, and evaporation, but as humidity, rainfall, and evaporation may also be considered as hydrologic, the two groups of factors have been combined. Hydrologic factors relate specially to conditions dependent on the operation of the hydrologic cycle, particularly with reference to runoff and ground-water. One of the central problems of hydrology is the correlation of the hydrologic characteristics of a drainage-basin with its morphology, soils, and vegetation. The problem is obviously complex. In some cases, as, for example, with reference to geologic structure, it is obviously difficult, if not impossible, to express the characteristics of the drainage-basin in simple, numerical terms.
    [Show full text]
  • The Development of International Water Resources : the "Drainage Basin Approach"
    THE DEVELOPMENT OF INTERNATIONAL WATER RESOURCES : THE "DRAINAGE BASIN APPROACH" C. B. BOURNE* Vancouver With the growth of modern technology, states sharing a drainage basin could affect each other far more seriously than ever before by the utilization of its waters in their territories. This fact has inevitably influenced the evolution of legal rules for solving inter- national water conflicts. As the interdependence of co-basin states became clearer, the inadequacy of the old theories, particularly the theory of territorial sovereignty that a state may do as it pleases with the water in its territory without any legal responsi- bility for the injury it may inflict on neighbouring states, was recognized. A new theory that would take account of this inter- dependence was therefore sought, and soon the notions of com- munity and of good neighbourship were being advocated as the proper foundation for the rules of international water law. An early manifestation of this new theory was an emphasis on the drainage basin. Before long the basin was being spoken of as a unit which should form the basis for planning the develop ment of international water resources. This emphasis is under- standable. For the effects of a work on an international river in one state are usually more noticeable in co-basin states within the drainage basin than outside it, even though its effects outside the basin may in fact be serious. It is one thing, however, to assert that international law, recognizing the interdependence of co-basin states, imposes an obligation on them to take heed of the injury their utilizations of water may inflict on each other; it is another to claim that inter- *C.
    [Show full text]