CTU small portable rainfall simulator (9550)
Katedra hydromeliorací a krajinného inženýrství, Fakulta stavební ČVUT v Praze
Zdroj financování: Půdoochranky SOPLAS
dry
precipitation start:
14:18
winter rape
- Exp. plot:
- #179
- Zal.:
- 22.09.2022
- Plot inclination [%]:
- 9%
soil moisture
[0;0] is in top left corner (viewed from the bottom), X is width, Y lenght
| time | plot X coordinate [m ] | plot Y coordinate [m ] | volumetric soil moisture [%V] | Note |
|---|
Derived from record(s) #5026
average value from point measurements within the experimental plot
| time | volumetric soil moisture [%V] | Note |
|---|
surface run-off
runoff measured with volumetric method in 2,5 minute step
| time | flow rate [l.min-1] | Note |
|---|
sediment load
lab results for samples collected during simulation run
collected samples were weighed, dried out and wieghed again, resulting sediment mass is related to the original volume of the sample
| time | suspended solids concentration [g.l-1] | Note |
|---|
Derived from record(s) #5229 #5230
total mass of suspended solids within timestep derived from measured flow rate and sediment concentration data
| time | sediment delivery [kg] | Note |
|---|
Derived from record(s) #5229 #5230
one value interpolated
| time | sediment delivery [kg] | Note |
|---|
precipitation
| time | rainfall intensity [mm.h-1] | Note |
|---|
dry
very wet
precipitation start:
15:08
winter rape
- Exp. plot:
- #179
- Zal.:
- 22.09.2022
- Plot inclination [%]:
- 9%
soil moisture
[0;0] is in top left corner (viewed from the bottom), X is width, Y lenght
| time | plot X coordinate [m ] | plot Y coordinate [m ] | volumetric soil moisture [%V] | Note |
|---|
Derived from record(s) #5058
average value from point measurements within the experimental plot
| time | volumetric soil moisture [%V] | Note |
|---|
surface run-off
runoff measured with volumetric method in 2,5 minute step
| time | flow rate [l.min-1] | Note |
|---|
sediment load
lab results for samples collected during simulation run
collected samples were weighed, dried out and wieghed again, resulting sediment mass is related to the original volume of the sample
| time | suspended solids concentration [g.l-1] | Note |
|---|
Derived from record(s) #5235 #5236
total mass of suspended solids within timestep derived from measured flow rate and sediment concentration data
| time | sediment delivery [kg] | Note |
|---|
Derived from record(s) #5235 #5236
moving average
| time | sediment delivery [kg] | Note |
|---|
precipitation
| time | rainfall intensity [mm.h-1] | Note |
|---|