EFFECT OF PLANT ROOTS ON CHEMICAL AND BIOCHEMICAL PROPERTIES OF SURROUNDING DISCRETE SOIL ZONES
- 1 May 1988
- journal article
- research article
- Published by Canadian Science Publishing in Canadian Journal of Soil Science
- Vol. 68 (2), 233-242
- https://doi.org/10.4141/cjss88-023
Abstract
The chemical and biochemical properties within and immediately adjacent to the root zone of two grass species were studied over a 5-wk period. The experiment utilized a simple container comprising five sandwiched compartments giving a center or "rhizosphere" zone, two intermediate zones, and two outer zones. Soil samples were taken from an Orthic Brown, Dark Brown, and Black Chernozemic Ah horizon and from the Orthic Dark Brown Chernozemic Ap horizons of the unfertilized part of a continuous wheat field and the fallow field of a wheat-fallow rotation, both under cultivation for 70 yr. The two grasses were blue grama (Bouteloua gracilis (H.B.K.) Lag.) and rye (Secale céréale L. 'Frontier'). High root densities were achieved by the end of the study, especially with the blue grama. Changes in pH over time were slight but consistent; they decreased in the Black Chernozemic soil and increased in the other soils. A redistribution of labile phosphorus was caused by the presence of the plant roots. The Orthic Dark Brown Ah and Ap horizon soils reacted differently to the conditions of the study. Monosaccharides always increased in the rhizosphere zone and generally decreased in the zone adjacent to the rhizosphere zone in the case of rye and in the outside zone in the case of blue grama. The ratio galactose + mannose/arabinose + xylose always increased towards the outer zone. Although the presence of roots influenced the measured chemical properties of the soil surrounding them, there were no overall common trends. The results, even in this simplified system, demonstrated complex and interrelated effects (P < 0.01) of soil type, plant species, and time on the biochemical dynamics in and near the rhizosphere. The properties of rhizosphere soil are system specific. To interpret the processes within the system, detailed knowledge of the soil organic matter, the physiology of the species root, and the effect on each other is obligatory. Key words: Rhizosphere, Chernozemic Ah/Ap horizons, blue grama, rye, monosaccharidesThis publication has 11 references indexed in Scilit:
- Transformations and movement of P in the rhizospherePlant and Soil, 1987
- Root‐induced changes in the rhizosphere: Importance for the mineral nutrition of plantsJournal of Plant Nutrition and Soil Science, 1986
- MONOSACCHARIDES IN HYDROLYSATES OF WATER-STABLE AGGREGATES AFTER 67 YEARS OF CROPPING TO SPRING WHEAT AS DETERMINED BY CAPILLARY GAS CHROMATOGRAPHYCanadian Journal of Soil Science, 1984
- SUBSTRATE FLOW AND UTILIZATION IN THE RHIZOSPHERE OF CEREALSNew Phytologist, 1983
- Chemical properties of soil and water-stable aggregates after sixty-seven years of cropping to spring wheatPlant and Soil, 1983
- Seasonal effects on photoassimilated carbon-14 in the root system of blue grama and associated soil organic matterSoil Biology and Biochemistry, 1983
- Suppression of decomposition of 14C‐labelled plant roots in the presence of living roots of maize and perennial ryegrassEuropean Journal of Soil Science, 1982
- Changes in Inorganic and Organic Soil Phosphorus Fractions Induced by Cultivation Practices and by Laboratory IncubationsSoil Science Society of America Journal, 1982
- Changes of pH across the rhizosphere induced by rootsPlant and Soil, 1981
- A comparison of methods for soil microbial population and biomass studiesJournal of Plant Nutrition and Soil Science, 1979