On soil genesis in temperate humid climate. IV. The "low humus podzols".
DOI:
https://doi.org/10.18174/njas.v12i4.17515Abstract
"Low humus podzols" do not possess a spodic horizon; podzol formation in conjunction with predominantly reducing conditions give rise to an eluviated profile. Low humus podzols have an umbric epipedon, the Fe and Al contents of the B horizon are intermediate between those of the A and C horizon, and their humus is mostly dispersed. Psammic Umbraquepts is proposed as a fifth subgroup for these soils. (Abstract retrieved from CAB Abstracts by CABI’s permission)Downloads
Published
1964-11-01
Issue
Section
Papers