ESPM 131 Lecture Notes - Lecture 2: Humus, Protozoa, Hydrolysis

• School: Berkeley
• Department: Environmental Science, Policy, And Management
• Course: ESPM 131
• Professor: Mary Firestone

Document Summary

Different took ecology relies on models due to complexity provides top - down approaches for temporal fpatial dynamics. Prop . gaspigvioysdidfanesfco@nn. fhngyoti-nsos. lidsenr01. p precipitation res kai yhzd minerals derived thru weathering phys breakdown in site. Chem alteration in composition t reactivity chen : dissolution re alt . of surface by hydrolysis. Ions usually clay + bacteria are the same size can have mineral coatings importantfor hzo holding capacity organic matter humus : traditional term. Dx ant of c in the atmosphere. 10 - 10005 yrs old particles + aggregates pore space : deep . on size of. 0% q an inside of aggregate , diffusion is tough microbes use more then cliff supplies. Oxidized metal on outside reduced on inside. ^ hietarehy of forces : in organics + bio processes that bind small large: polysaccharides - made by bacteria + roots. 2) hyphae - fungal e actin bacteria (filamentous)