CLIMATIC AND TOPOGRAPHIC RELATIONS OF 3 GREAT-PLAINS SOILS .2. CARBON, NITROGEN, AND PHOSPHORUS

被引：36

作者：

HONEYCUTT, CW

HEIL, RD

COLE, CV

机构：

[1] COLORADO STATE UNIV, COLORADO AGR EXP STN, FT COLLINS, CO 80523 USA

[2] COLORADO STATE UNIV, USDA ARS NAT RESOURCE ECOL LAB, FT COLLINS, CO 80523 USA

来源：

SOIL SCIENCE SOCIETY OF AMERICA JOURNAL | 1990年 / 54卷 / 02期

关键词：

D O I：

10.2136/sssaj1990.03615995005400020031x

中图分类号：

S15 [土壤学];

学科分类号：

0903 ; 090301 ;

摘要：

Organic-C concentrations were highest in the surface horizons and declined with depth, but relatively high concentrations of organic P were found in the subsoils studied. The depth of this organic P-accumulation zone varied in patterns indicative of climatic and topographic controls on the leaching process. Both the total contents and vertical distributions of organic C and P, therefore, suggest that stoichiometric relationships between C and P should not be assumed, as both climate and topography may influence soil C and P levels to different extents and through different processes. -from Authors

引用

页码：476 / 483

页数：8

共 32 条

[1] COMPARISON OF HUMIC FRACTIONS OF CHERNOZEMIC AND LUVISOLIC SOILS BY ELEMENTAL ANALYSES, UV AND ESR SPECTROSCOPY [J].