Astm D338518 Pdf -

Infiltration occurs when water at the soil surface enters the pores of the soil matrix. The rate at which this occurs is influenced by soil texture, structure, bulk density, initial moisture content, and the presence of vegetation or cracks. Initially, when soil is dry, the infiltration rate is high due to capillary suction (matric potential). As the soil saturates, gravity becomes the dominant force, and the infiltration rate stabilizes, approaching the saturated hydraulic conductivity ($K_sat$) of the soil.

is the recognized international standard for determining the infiltration rate of soils in the field using a double-ring infiltrometer . This method is essential for geotechnical and environmental engineering, providing data for septic tank design, irrigation planning, and groundwater recharge studies. Core Objectives of ASTM D3385-18 astm d338518 pdf

: To measure the rate at which a liquid (typically water) enters the soil surface. Infiltration occurs when water at the soil surface

ASTM D3385-18 standard provides a field procedure for measuring the infiltration rate As the soil saturates, gravity becomes the dominant