Tuttle Creek Lake
| Tuttle Creek Lake | |
|---|---|
 Tuttle Creek Dam | |
  Tuttle Creek Lake | |
 | |
| Location | Pottawatomie / Riley / Marshall counties in Kansas |
| Coordinates | 39°15′25″N 96°35′32″W / 39.25694°N 96.59222°W |
| Type | Reservoir |
| Primary inflows | Big Blue River |
| Primary outflows | Big Blue River to Kansas River |
| Catchment area | 25,000 km2 (9,600 mi2)[1] |
| Basin countries | United States |
| Max. length | 25 km (16 mi)[1] |
| Max. width | 2 km (1.3 mi) |
| Surface area | 50 km2 (19 mi2)[1] |
| Max. depth | 15 m (50 ft)[2] |
| Water volume | 0.41 km3 (0.098 cu mi) (normal level)[1] |
| Shore length1 | 160 km (100 mi)[1] |
| Surface elevation | 328 m (1075 ft)[1] |
| Settlements | Manhattan |
| References | [3][1][2] |
| 1 Shore length is not a well-defined measure. | |
Tuttle Creek Lake is a reservoir on the Big Blue River 5 miles (8 km) north of Manhattan, in the Flint Hills region of northeast Kansas. It was built and is operated by the Army Corps of Engineers for the primary purpose of flood control. Secondary functions of the project include release of water stores to maintain barge traffic on the Mississippi River during seasons of drought, maintenance of a multi-use conservation pool for fish and wildlife enhancement and recreation (fishing, hunting, and boating), and release of sufficient water in droughts to maintain water quality for downstream communities.[4]
The base of the dam is bordered by Tuttle Creek State Park, which features 1,200 acres (4.9 km2) of recreational areas, including nature trails, camping sites, and an artificial beach.[5] The state park also hosted the Country Stampede Music Festival every summer from 1996 to 2018.
Geography
[edit]Excluding the 8.5 miles (13.7 km) of narrow valley below the dam, the project manages the drainage of the entire watershed of the Big Blue River, an area of 9,628 square miles (24,940 km2)[6] that ranges from just north of Manhattan to the Platte River.
The border between Riley County (on the west) and Pottawatomie County (on the east) is submerged underneath the lake. The dam is roughly two miles north of Manhattan, Kansas, and is crossed by Kansas Highway 13. Near the river delta at the lake's northern end, a bridge carrying Kansas Highway 16 spans the lake.
History
[edit]From 1903 to 1959, 25 floods damaged the areas of the Kansas River at Topeka; but, over the same period, there were also times of critical drought. With the growth of population and industry, there was envisioned projects to both contain excessive floodwaters and conserve water for release in drought.[7]
The Flood Control Act of 1938 authorized construction of Tuttle Creek Reservoir, and funds for initial planning were authorized in 1944. The construction of Tuttle Creek Dam as a Corps of Engineers project was given particular impetus by the Great Flood of 1951, which inundated downtown Manhattan, Topeka, and the West Bottoms of Kansas City. Total losses in the Kansas cities and farmland exceeded $725,000,000.[8] Nevertheless, the project met with heavy opposition from landowners whose land faced flooding by the lake's construction. Residents of the Blue Valley organized opposition under the phrase "Let's quit this dam foolishness," and the campaign led to victory for Democrat Howard Shultz Miller in the U.S. House of Representatives in 1952.[9] Although the opposition was heated, it failed to ultimately stop the dam.
Construction began on 1952. Closure of the dam (still under construction) occurred July 4, 1959 with diversion of the river though the completed intake tower ("The Tubes"). In 1960, dam contained a record snow melt; even though not yet finished, the dam was credited at that time with preventing $15,243,000 in damages. During this event, the tubes discharged 29,000 cubic feet per second (820 m3/s),[8] a record amount for the intake tower that was not matched or exceeded until the tower's estimated 30,000 cubic feet per second (850 m3/s) release on May 31, 2019.[10]
When the dam was completed and the lake began filling up in 1962, it affected ten towns and entirely submerged four of them (from north to south): Cleburne at 39°31′49″N 96°38′6″W / 39.53028°N 96.63500°W, Randolph, Garrison Cross and Stockdale. The only town to rebuild elsewhere was Randolph, where the streets are named after the submerged towns.[11] The remnants of "Old Randolph", as it's known locally, can still be seen partially submerged to this day.[12]
The value of the dam was particularly proven during the Great Flood of 1993, when floodwaters reaching up to 63 feet (19 m) above normal were held back. However, when the dam reached capacity in July 1993, it necessitated the first release of the spillway since its installation. All 18 gates on the spillway were raised 4 feet (1.2 m) during the peak of the flood, producing a flow rate of 60,000 cubic feet per second (1,700 m3/s) (with the tubes closed at that time). While this controlled flow rate resulted in flooding of low-lying homes and cropland, it was significantly less than the estimated peak flow of 96,000 cubic feet per second (2,700 m3/s) the downstream communities would have experienced on June 30 had the dam not been in place, an amount that would have topped the Big Blue River Levee and flooded downtown Manhattan.[13] The roar of the water was audible half a mile (800 m) away and some people in nearby Manhattan reported hearing the noise.
2019 flood
[edit]During 2019 there was a period consisting of a few days where there was heavy rain. The water levels rose and preparations were made in the event that the spillway was to be opened. The nearby RV park and other areas near the dam's main wall were evacuated, and those in the path of the spillway's flooding and destruction radius, if it were to be opened, were evacuated as well. The rain continued and more water than usual leaked out of the spillway's gates as a result, but the spillway was not opened. In the days following the event, there was some recovery from flash floods as a result of the rain.
1993 spillway chute erosion and repair
[edit]
After three weeks of release in 1993, the spillway gates were closed, revealing over 32 acres (13 ha) of freshly exposed rock formations. This attraction became known locally as the Little Grand Canyon[14] or "The Canyon".
Erosion
[edit]Below the gates lies 600 feet (180 m) of concrete-lined chute followed by about 7,000 feet (2,100 m) of unlined chute, originally maintained with grass cover. Erosion of the unlined chute during a spillway release was a factor of the design. As expected, the released water had rapidly scoured away all soil on the floor of the unlined chute and then quickly removed a few feet of loose, weathered rock, exposing solid, durable limestone shelves. Each of these limestone ledges experienced head cutting, where the underlying soft shale was eroded away; weakening, collapsing, and washing away some horizontal distance of the limestone at a rate much slower than the first removal of the looser material.[15]
Each of these headcuts have a relatively resistant limestone bed on top and easily erodible rock (shale) underneath. Two particularly resistant limestone formations formed notable shelves: The limestone beds of the Red Eagle Formation topped a 26 feet (7.9 m) cliff (pictured), and from the base of that cliff stretched out 4.5 acres (1.8 ha) of the Long Creek limestone bed of the Foraker Formation (now covered by a beaver dam).
Geologic study
[edit]This area is of interest to geologists due to its superb exposure of the 300 million year old rocks of the upper-Carboniferous and lower-Permian underlying the Flint Hills. In this one location, five formations can be studied that are rarely exposed in great extent singly, let alone all together in an extended horizontal presentation.[16]
These strata attest to a flat, arid paleoenvironment along the western margin of Pangaea with intermittent marine transgressions from the Panthalassa Ocean. Conditions there may have been analogous to the modern-day Persian Gulf coast of the Arabian Peninsula. As sea levels rose and fell over the course of many millennia, so too did the depositional environment change, resulting in repeating sequences of rock strata distinctive to the late paleozoic. In periods of high sea-level, limestone and shale were deposited, while periods of low sea-level resulted in the deposition of red and green clays and paleosols, giving the exposures at the spillway "canyon" a colorful "layer cake" appearance.
Spillway chute repair
[edit]
Impressiveness of the 1993 geologic display aside, there was concern about the durability of the spillway in future releases. The structure and strength of the spillway's bedrock was studied to determine any necessary course of repair, reinforcement, or replacement. During the 1993 spillway release, daily photographs were taken of the rushing water at nine different locations to measure the speed of the expected head cutting. Analysis determined that the spillway could still survive 10 times the intensity of the 1993 release (the maximum 612,000 cubic feet per second (17,300 m3/s) the spillway was designed to release).[15]
However, the previously unexposed Roca Shale, which had demonstrated remarkable durability during the release, was expected to undergo rapid severe deterioration if left open to the effects of the Kansas climate. So, it was determined that minimal repair was to be made to the upper length of the chute. Weaker and fractured limestone shelves were grouted and then buttressed with shotcrete, and then the area was covered with terraced soil and returned to grass. Soil pH was adjusted to further protect the reburied rock.[15] The rock formations of the lower portion were left exposed.
Earthquake threat and mitigation
[edit]
Хотя Канзас не широко известен как сейсмически активный, линия разлома Гумбольдта , связанная с хребтом Немаха, проходит через восточный Канзас, и, вероятно, наиболее активный регион на этой линии находится в непосредственной близости от озера. Исследования, начавшиеся в 1980-х годах, показали, что геология этого района потенциально может вызвать землетрясение, плотины способное вызвать разрушение , что может поставить под угрозу жизни тысяч людей, живущих ниже по течению в долинах рек Блю-Ривер и Канзас .
Чтобы устранить эту угрозу, Инженерный корпус армии в июле 2010 года завершил проект, в рамках которого плотина была укреплена более чем 350 бетонными стенами, чтобы перекрыть каналы в нижележащем карсте , и оснащена датчиками предупреждения .
См. также
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Ссылки
[ редактировать ]- ^ Jump up to: а б с д и ж г «Озеро Таттл-Крик» . Инженерный корпус армии США, округ Канзас-Сити. Архивировано из оригинала 18 декабря 2006 года . Проверено 15 января 2007 г.
- ^ Jump up to: а б «Водохранилище Таттл-Крик» . Департамент дикой природы и парков Канзаса. Архивировано из оригинала 27 сентября 2007 года . Проверено 15 января 2007 г.
- ^ «Плотина Таттл-Крик» . Информационная система географических названий . Геологическая служба США , Министерство внутренних дел США . 13 октября 1978 года . Проверено 16 января 2021 г.
- ^ «Послестроительная история» . www.nwk.usace.army.mil . Инженерный корпус армии США . Проверено 1 июня 2019 г.
Основной целью регулирования озера Таттл-Крик является борьба с наводнениями. Второстепенными целями являются навигация, качество воды, отдых, а также улучшение рыбной ловли и дикой природы. Эти цели будут достигаться, насколько это практически возможно, без ущерба для основной цели.
- ^ «Государственный парк Таттл-Крик» . Департамент дикой природы и парков Канзаса . Проверено 22 января 2008 г.
- ^ «Краткий обзор качества воды в озере Таттл-Крик за 2007–2016 годы» . Инженерный корпус армии США, Секция экологических ресурсов, Канзас-Сити, Миссури . Проверено 1 июня 2019 г.
- ^ «Наводнения и засухи» . www.nwk.usace.army.mil . Инженерный корпус армии США . Проверено 1 июня 2019 г.
- ^ Jump up to: а б «История» . www.nwk.usace.army.mil . Инженерный корпус армии США . Проверено 1 июня 2019 г.
- ^ «Республиканская 83-я» . ВРЕМЯ . 17 ноября 1952 года. Архивировано из оригинала 12 сентября 2012 года.
- ^ «Очередной скачок в стоке из плотины Таттл-Крик, планов по открытию водосбросных ворот по-прежнему нет» . www.wibw.com . 31 мая 2019 года . Проверено 1 июня 2019 г.
- ^ «Список названий улиц в Рэндольфе, штат Канзас» . www.geographic.org . Проверено 25 января 2015 г.
- ^ «Карты Google» . Карты Гугл . Проверено 25 января 2015 г.
- ^ Брайан Макналти, руководитель оперативного проекта, Tuttle Creek Lake – Lake Operations and current Construction Activity (PDF) , Инженерный корпус армии США , округ Канзас-Сити, стр. 30, 35–37 , получено 1 июня 2019 г.
- ^ «[название неразборчиво]» . Коллегия штата Канзас . 11 октября 1995 года . Проверено 1 июня 2019 г.
Маленький Большой Каньон Манхэттена похож на Большой Каньон в Аризоне.
- ^ Jump up to: а б с Дэвид Мэтьюз, Влад Г. Перлеа, Франке К. Уолберг, Дуглас Р. Андерсон (Инженерный корпус армии США, Канзас-Сити, Миссури) (1998). «Эрозия и ремонт желоба для водосброса без облицовки, выкопанного в скале» . Международная конференция по практическим примерам в области геотехнической инженерии . Миссурийский университет науки и технологий . Проверено 1 июня 2019 г.
В случае с водосбросом Таттл-Крик считается, что первые две фазы [поверхностная эрозия] имели относительно короткую продолжительность по сравнению с третьей фазой [срезание головы].
{{cite journal}}: CS1 maint: несколько имен: список авторов ( ссылка ) - ^ Р.Р. Вест, факультет геологии, Университет штата Канзас. «Вклад в геологию горных пород, обнаженных в результате «Наводнения 93 года» на водосбросе водохранилища Таттл-Крик недалеко от Манхэттена, Канзас» . Отчет в открытом файле . 94-36. Канзасская геологическая служба .
{{cite journal}}: CS1 maint: несколько имен: список авторов ( ссылка )
Внешние ссылки
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- Охраняемые территории округа Маршалл, штат Канзас
- Охраняемые территории округа Поттаватоми, штат Канзас
- Водоемы в Канзасе
- Охраняемые территории округа Райли, штат Канзас
- Государственные парки Канзаса
- Плотины в Канзасе
- Плотины Инженерного корпуса армии США
- Водоемы округа Маршалл, штат Канзас
- Водоемы округа Поттаватоми, штат Канзас
- Водоемы округа Райли, штат Канзас