An OWL ontology for an observation tower concept in an urban park. Showing the conncections between its design components.
Construction
InterlockingTiles
RetainingWallDrainage
ConstructionComponent
MainMaterial
Asphalt
receivesPressureFrom
isConnectedTo
isRetainedBy
addsPressureOn
retains
MainRamp
ViewingTowerOption1
Other
Handrail
Steel
ViewingTowerOption2
TopDeck
DesignedViewingTower
ViewingTowerComponent
ViewingTower
Column
Wood
hasDiameter
hasNumberOfColumns
hasSlope
hasRadius
hasHeight
hasWidth
hasRotationAngle
ColumnOption2
ColumnOption1
MainRampOption1
HandrailOption2
HandrailOption1
MainRampOption2
isComponentOf
isMainMaterialOf
hasComponent
hasMainMaterial
A groundwater inhibitor not storing or conducting any water. No groundwaterflow in this layer.
An underground layer of rock, which is capable of storing and conducting groundwater.
A groundwater inhibitor that restricts the flow and storage of groundwater. It has a low permeability, but it does allow a low groundwaterflow.
Sand with a hydraulic conductivity of around 10^-3 m/s.
A confined groundwater body is a groundwater body. Groundwater inhibitors are both above and below the aquifer holding the groundwater body, causing it to be under pressure so that when the aquifer is penetrated by a well, the water will rise above the top of the aquifer.
Sand with a hydraulic conductivity of around 10^-4 to 10^-5 m/s.
An aquifer consisting of solid rock which has significant fractures and and fissures trough which the groundwater flows.
A distinct volume of groundwater within an aquifer or system of aquifers, which is hydraulically isolated from nearby groundwater bodies.
An underground rock/soil layer inhibiting the flow and the storage of groundwater.
An aquifer consisting of karstified carbonate rock. The groundwater flows through karsts.
Sand with a hydraulic conductivity of around 10^-3 to 10^-4 m/s.
An aquifer consisting of unconsolidated rock or solid rock of which the pores are flown through by water. Porous aquifers typically occur in sand and sandstone.
A soil type with a high effective porosity.
A granular material composed of finely divided mineral particles.Sand has various compositions but is defined by its grain size. Sand grains are smaller than gravel and coarser than silt.
A granular material of a size between sand and clay, composed mostly of broken grains of quartz.
Sand with a hydraulic conductivity of around 10^-5 to 10^-6 m/s. Containing a certain amount of silt.
An underground layer of soil / rock.
A type of soil with certain properties.
Solid rock that may be impermeable or fractured.
Pore volume available for groundwater flow.
A property of the soil.