Analysis of spatio-temporal variability of soil erodibility values by water erosion
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43210%2F22%3A43921417" target="_blank" >RIV/62156489:43210/22:43921417 - isvavai.cz</a>
Výsledek na webu
<a href="https://doi.org/10.11118/978-80-7509-831-3-0031" target="_blank" >https://doi.org/10.11118/978-80-7509-831-3-0031</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.11118/978-80-7509-831-3-0031" target="_blank" >10.11118/978-80-7509-831-3-0031</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Analysis of spatio-temporal variability of soil erodibility values by water erosion
Popis výsledku v původním jazyce
In current dynamic development of GIS and remote sensing methods, especially the use of accurate LiDAR data, there is a significant disproportion in the accuracy of morphological and soil data in the assessment of erosion. In current practice, the map of main soil units (MSU) is used to determine soil erodibility (expressed by K factor), which in many cases lead to a step change in values within one field or erosion closed unit (ECU). However, the soil properties included in the calculation of the K factor usually change smoothly in the direction of the slope, but also due to other morphometric characteristics. Terrain morphology should therefore be taken into account when determining the K factor values. The K factor values change dynamically both according to the terrain morphology within ECU and depending on climatic conditions that change during the year and within the geographical location in the Czech Republic (CR) and given physio-geographical conditions. In assessing the seasonal dynamics of K factor values, they appear to be key erosion rainfalls. By including this spatio-temporal variability of K factor values, it will be possible to significantly refine soil loss calculations and proposals for erosion control measures and retention elements and their intangible services for environment and increasing the landscape character and recreational potential of the site.
Název v anglickém jazyce
Analysis of spatio-temporal variability of soil erodibility values by water erosion
Popis výsledku anglicky
In current dynamic development of GIS and remote sensing methods, especially the use of accurate LiDAR data, there is a significant disproportion in the accuracy of morphological and soil data in the assessment of erosion. In current practice, the map of main soil units (MSU) is used to determine soil erodibility (expressed by K factor), which in many cases lead to a step change in values within one field or erosion closed unit (ECU). However, the soil properties included in the calculation of the K factor usually change smoothly in the direction of the slope, but also due to other morphometric characteristics. Terrain morphology should therefore be taken into account when determining the K factor values. The K factor values change dynamically both according to the terrain morphology within ECU and depending on climatic conditions that change during the year and within the geographical location in the Czech Republic (CR) and given physio-geographical conditions. In assessing the seasonal dynamics of K factor values, they appear to be key erosion rainfalls. By including this spatio-temporal variability of K factor values, it will be possible to significantly refine soil loss calculations and proposals for erosion control measures and retention elements and their intangible services for environment and increasing the landscape character and recreational potential of the site.
Klasifikace
Druh
D - Stať ve sborníku
CEP obor
—
OECD FORD obor
10508 - Physical geography
Návaznosti výsledku
Projekt
<a href="/cs/project/QK21020069" target="_blank" >QK21020069: Korekce hodnot erodovatelnosti půdy dle morfologie terénu v rámci erozně uzavřených celků pro potřeby zpřesnění identifikace erozně ohrožených ploch</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2022
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název statě ve sborníku
Public recreation and landscape protection – with environment hand in hand…: Conference proceedings
ISBN
978-80-7509-830-6
ISSN
2336-6311
e-ISSN
2336-632X
Počet stran výsledku
5
Strana od-do
31-35
Název nakladatele
Mendelova univerzita v Brně
Místo vydání
Brno
Místo konání akce
Křtiny
Datum konání akce
9. 5. 2022
Typ akce podle státní příslušnosti
WRD - Celosvětová akce
Kód UT WoS článku
—