On our property, one of several dynamic cone penetrometer tests was conducted; I ran this through ChatGPT.
The analysis of the results for the dynamic cone penetrometer test RKS 13 provides the following information:
1. Layer structure at RKS 13
• Topsoil (up to 0.6 m below ground surface, GOK):
• The upper layers consist of medium sand (mS), fine sand (fS), and silt (u). These materials are loosely to moderately dense.
• Middle depth (up to approx. 4.4 m below GOK):
• Predominantly silt (U) with shares of fine sand (fS). These layers are plastic and poorly permeable to water.
• Deep layers (from approx. 4.4 m below GOK):
• The marl (KM) begins here. It is strongly weathered in the upper part but becomes firmer at depth. Marl is load-bearing but poorly permeable to water.
2. Groundwater
• The measured groundwater level is at 2.24 m below GOK (73.65 m NHN). This value indicates that the location is moderately moist.
• No hydrostatic groundwater was detected that could pose construction challenges.
3. Recommendations for site RKS 13
1. Load-bearing capacity of the building ground:
• The building ground is load-bearing. A standard slab-on-grade can be used without any problems. Additional stabilization is not required.
2. Drainage:
• Due to the poorly permeable marl layer, temporary water accumulations may occur during heavy rain. Drainage may be advisable to divert water away from the slab-on-grade.
3. Sealing:
• Sealing against rising moisture is recommended for the slab-on-grade since the silt in the upper layers can retain moisture.
Conclusion for site RKS 13
• The site is suitable for the construction of a slab-on-grade without a basement.
• Temporary waterlogging is possible but can be easily managed with appropriate drainage and sealing.
• There are no indications of contaminated sites or other hazards.