Origin of solids
Solids entry through extraneous water (3)
Image: Erosion of cohesive soils as a result of a leaking gravity sewer located within the ground water zone [Stein00f] [Jones84a].
Image: Erosion of cohesive soils as a result of a leaking gravity sewer located within the ground water zone [Stein00f] [Jones84a].
With cohesive soils specified by DIN 1054 (clays, clayey silts and silts mixtures with non-cohesive soils), if the proportion of particles sized < 0.06 mm is more than 15%, the solid entry at the pipe failure is mainly caused by the soil erosion through the internal stresses within the pipe. This occurs in cracks with a width ≥ 6 mm and a leak size > 60 cm² [[DIN1054:2010]] [Dohma2004a] [Dohma99] [[ASTM D2487-17]] (Refer to relevant standard(s) in your jurisdiction).
DIN 1054: Subsoil - Verification of the safety of earthworks and foundations - Supplementary rules to DIN EN 1997-1 (12.2010)
Dohmann, M.; Hennerkes, J. (2004): Untersuchung des Einflusses undichter Abwasserkanäle auf die Standsicherheit des umgebenden Bodenkörpers, Abschlussbericht zum Forschungsvorhaben des MUNLV NRW, Institut für Siedlungswasserwirtschaft der RWTH Aachen
ASTM D2487-17e1: Standard Practice for Classification of Soils for Engineering Purposes (Unified Soil Classification System), ASTM International, West Conshohocken, PA, 2017, www.astm.org)
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