Supporting Documentation · Jan 7, 2026
O38 Email from Nov 13 2025 to Dec 9 2025 between Mr Kleinberg and Mr Seele
b799edafc414b7e05a62c6595bcff24a3389ca3ea8f90215ebb9042a0c5dbcdeIndexed text · page 5
Show all pagesof heavy rain events on slope stability. The last Langan submittal included ‘infinite slope evaluations, but those were above the assumed phreatic surface used in the calculation. In our opinion assuming the seepage parallel to the slope and at the ground surface emphasizes the need for the recommended Planning Board development requirements outlined in our report at the last meeting. 2. Our cases accounted for a water level shape that is based on the geometrical shape of slope and considering the only source of water is from direct precipitation between the ridge line and the eastern slope, which is limited. CME Response: We have recommended that the BMP-10 and BMP-11 infiltration basin mounding discharge be controlled to limit the groundwater flow over the slope for that reason. Due to the difficulty in determining natural and forced infiltration on the slope, we have recommended the conservative assumption outlined in our response to Langan Comment No. 1. 3. The strength values used in both CME and Langan’s analysis ignore forms of cohesion as conservative cases. However, if you back calculate the minimum friction values required to achieve FS=1.0, the soil’s friction would have to be at least 45 degrees, which is not realistic in the upper few feet. Therefore, cohesion is present, likely in the form of roots. If you check the minimum root cohesion required to achieve FS=1.0 (assuming friction of 30 degrees for the upper 2 feet), cohesion would have to be at least 35 psf or slope failures would be visible after intense rainfalls, and there is no evidence of this anywhere on the site. Therefore, the root cohesion must be considerably higher. Various researchers have evaluated root cohesion and determined values typically range from 200 psf for clear cuts and natural wooded/forested land to 500 psf. The site is predominantly wooded; however, if C= 100 psf root cohesion is used, FS values would be well over 1.5 (i.e., 1.7 to 7) for the slopes in question. CME Response: We recommend that Langan provide a formal response to the Planning Board on the basis described herein, to address this issue. 4. The existing slopes are not going to be disturbed and the developer must maintain the vegetation, therefore the analyses demonstrate shallow failures are unlikely. CME Response: We agree that the existing slopes must be protected from disturbance and that the
eveloper must maintain the vegetation, therefore the analyses demonstrate shallow failures are unlikely. CME Response: We agree that the existing slopes must be protected from disturbance and that the vegetation must be maintained both by the developer and his successors. That is why we have recommended that enforceable requirements based on our review recommendations to the Board be established. | trust this addresses your concerns. Please call with any questions. Mark Mark Seel Associate Principal / Vice President LANGAN
File revisions (1)
- Sep 29, 2026
b799edafc4147,700,230 bytes