ESTIMATING RESPIRATION OF ROOTS IN SOIL - INTERACTIONS WITH SOIL CO2,SOIL-TEMPERATURE AND SOIL-WATER CONTENT

Citation
Tj. Bouma et al., ESTIMATING RESPIRATION OF ROOTS IN SOIL - INTERACTIONS WITH SOIL CO2,SOIL-TEMPERATURE AND SOIL-WATER CONTENT, Plant and soil, 195(2), 1997, pp. 221-232
Citations number
36
Categorie Soggetti
Agriculture Soil Science","Plant Sciences",Agriculture
Journal title
ISSN journal
0032079X
Volume
195
Issue
2
Year of publication
1997
Pages
221 - 232
Database
ISI
SICI code
0032-079X(1997)195:2<221:ERORIS>2.0.ZU;2-G
Abstract
Little information is available on the variability of the dynamics of the actual and observed root respiration rate in relation to abiotic f actors. In this study, we describe I) interactions between soil CO2 co ncentration, temperature, soil water content and root respiration, and II) the effect of short-term fluctuations of these three environmenta l factors on the relation between actual and observed root respiration rates. We designed an automated, open gas-exchange system that allows continuous measurements on 12 chambers with intact roots in soil. By using three distinct chamber designs with each a different path for th e air flow, we were able to measure root respiration over a 50-fold ra nge of soil CO2 concentrations (400 to 25000 ppm) and to separate the effect of irrigation on observed vs. actual root respiration rate. All respiration measurements were made on one-year-old citrus seedlings i n sterilized sandy soil with minimal organic material. Root respiratio n was strongly affected by diurnal fluctuations in temperature (Q(10) = 2), which agrees well with the literature. In contrast to earlier fi ndings for Douglas-fir (Qi et al., 1994), root respiration rates of ci trus were not affected by soil CO2 concentrations (400 to 25000 ppm CO 2; pH around 6). Soil CO2 was strongly affected by soil water content but not by respiration measurements, unless the air flow for root resp iration measurements was directed through the soil. The latter method of measuring root respiration reduced soil CO2 concentration to that o f incoming air. Irrigation caused a temporary reduction in CO2 diffusi on, decreasing the observed respiration rates obtained by techniques t hat depended on diffusion. This apparent drop in respiration rate did not occur if the air flow was directed through the soil. Our dynamic d ata are used to indicate the optimal method of measuring root respirat ion in soil, in relation to the objectives and limitations of the expe rimental conditions.