Attributes | Values |
---|
rdf:type
| |
Description
| - Tile drainage water temperatures and discharge rates were measured in highland watersheds mostly underlain by acid crystalline rock. The aim was to evaluate water temperature as a means of determining the source and pathway of drainage runoff during high-flow events. Rapid increase in drainage discharge was accompanied by rapid change in water temperature. In winter, the risik/falling limb of the hydrograph was accompanied by a decrease/increase in temperature. In summer, the trends were reversed. These data suggest that the water temperature changes are caused by water from a precipitation event or snowmelt, which can be separated from the remainder of the hydrograph. Measurements indicate that the major portion of the event water infiltrates in the watershed recharge zone where soils are permeable, enters the weathered bedrock, flows preferentially and rapidly down the slope along disjoint fissures in the bedrock, emerging as ascending springs and intercepted by the tile drainage systems.
- Tile drainage water temperatures and discharge rates were measured in highland watersheds mostly underlain by acid crystalline rock. The aim was to evaluate water temperature as a means of determining the source and pathway of drainage runoff during high-flow events. Rapid increase in drainage discharge was accompanied by rapid change in water temperature. In winter, the risik/falling limb of the hydrograph was accompanied by a decrease/increase in temperature. In summer, the trends were reversed. These data suggest that the water temperature changes are caused by water from a precipitation event or snowmelt, which can be separated from the remainder of the hydrograph. Measurements indicate that the major portion of the event water infiltrates in the watershed recharge zone where soils are permeable, enters the weathered bedrock, flows preferentially and rapidly down the slope along disjoint fissures in the bedrock, emerging as ascending springs and intercepted by the tile drainage systems. (en)
|
Title
| - Drainage water temperature as a basis for verifying drainage runoff composition on slopes
- Drainage water temperature as a basis for verifying drainage runoff composition on slopes (en)
|
skos:prefLabel
| - Drainage water temperature as a basis for verifying drainage runoff composition on slopes
- Drainage water temperature as a basis for verifying drainage runoff composition on slopes (en)
|
skos:notation
| - RIV/60460709:41210/11:52661!RIV13-MSM-41210___
|
http://linked.open...avai/riv/aktivita
| |
http://linked.open...avai/riv/aktivity
| - P(QH82095), Z(MSM6046070901), Z(MZE0002704902)
|
http://linked.open...iv/cisloPeriodika
| |
http://linked.open...vai/riv/dodaniDat
| |
http://linked.open...aciTvurceVysledku
| |
http://linked.open.../riv/druhVysledku
| |
http://linked.open...iv/duvernostUdaju
| |
http://linked.open...titaPredkladatele
| |
http://linked.open...dnocenehoVysledku
| |
http://linked.open...ai/riv/idVysledku
| - RIV/60460709:41210/11:52661
|
http://linked.open...riv/jazykVysledku
| |
http://linked.open.../riv/klicovaSlova
| - drainage water temperature, drainage runoff, preferential flow, spring, recharge zone (en)
|
http://linked.open.../riv/klicoveSlovo
| |
http://linked.open...odStatuVydavatele
| |
http://linked.open...ontrolniKodProRIV
| |
http://linked.open...i/riv/nazevZdroje
| |
http://linked.open...in/vavai/riv/obor
| |
http://linked.open...ichTvurcuVysledku
| |
http://linked.open...cetTvurcuVysledku
| |
http://linked.open...vavai/riv/projekt
| |
http://linked.open...UplatneniVysledku
| |
http://linked.open...v/svazekPeriodika
| |
http://linked.open...iv/tvurceVysledku
| - Kaplická, Markéta
- Kvítek, Tomáš
- Zajíček, Antonín
- Žlábek, Pavel
- Bystřický, Václav
- Doležal, František
- Kulhavý, Zbyněk
|
http://linked.open...n/vavai/riv/zamer
| |
issn
| |
number of pages
| |
http://localhost/t...ganizacniJednotka
| |