<p>Comparison of mean CO<sub>2</sub> concentrations across three depths and flux between and within upland (n = 23) and riparian (n = 9) plots during wet (Weeks 1–3), transition (Weeks 4–6), and dry (Weeks 7–9) periods of the 2013 growing season. Asterisks (*) indicate significant differences between groups (p<0.05, Welch’s ANOVA). Bars indicate standard errors of the mean.</p
The stable carbon isotopic composition of CO2 (δ13C-CO2) has been studied as an indicator of changes...
<p>Different letters in superscript indicate statistically significant differences (p<0.05) among se...
Effects of soil temperature (°C) and soil water content (%) on CO2 and N2O fluxes over the study per...
<p>Note: asterisk (*) indicating significant differences at α = 0.05 level between elevation interva...
<p>Soil water parameters vs. CO<sub>2</sub> concentrations at 10 cm and 30 cm depths, plotted as dai...
<p>Comparison of mean values of key carbon and water fluxes, and key meteorological drivers for each...
<p>Seasonal variations of soil CO<sub>2</sub> efflux (<i>R</i><sub><i>S</i></sub>) (A), soil tempera...
<p>Seasonal variation of soil CO<sub>2</sub> fluxes in the alpine steppe during the growing season. ...
<p>Values represent the Means± SE. C: control plots; N: N addition; E: elevated CO<sub>2</sub>; EN: ...
<p>Soil carbon and nitrogen, snow depth and ranges, average CO<sub>2</sub> fluxes, and contribution ...
<p>Volumetric water content was a significant predictor of the variability of δ<sub>P</sub> across u...
<p>(a) Soil CO<sub>2</sub> efflux, (b) soil temperature (10 cm depth), and (c) soil water content (8...
<p>The surface elevation relative to the highest point along transects is shown in blue and elevatio...
Soil organic carbon (SOC) stocks are a function of the SOC concentration and the bulk density of the...
<p>Error bars are standard error of means (n = 3). Different letters denote significant differences ...
The stable carbon isotopic composition of CO2 (δ13C-CO2) has been studied as an indicator of changes...
<p>Different letters in superscript indicate statistically significant differences (p<0.05) among se...
Effects of soil temperature (°C) and soil water content (%) on CO2 and N2O fluxes over the study per...
<p>Note: asterisk (*) indicating significant differences at α = 0.05 level between elevation interva...
<p>Soil water parameters vs. CO<sub>2</sub> concentrations at 10 cm and 30 cm depths, plotted as dai...
<p>Comparison of mean values of key carbon and water fluxes, and key meteorological drivers for each...
<p>Seasonal variations of soil CO<sub>2</sub> efflux (<i>R</i><sub><i>S</i></sub>) (A), soil tempera...
<p>Seasonal variation of soil CO<sub>2</sub> fluxes in the alpine steppe during the growing season. ...
<p>Values represent the Means± SE. C: control plots; N: N addition; E: elevated CO<sub>2</sub>; EN: ...
<p>Soil carbon and nitrogen, snow depth and ranges, average CO<sub>2</sub> fluxes, and contribution ...
<p>Volumetric water content was a significant predictor of the variability of δ<sub>P</sub> across u...
<p>(a) Soil CO<sub>2</sub> efflux, (b) soil temperature (10 cm depth), and (c) soil water content (8...
<p>The surface elevation relative to the highest point along transects is shown in blue and elevatio...
Soil organic carbon (SOC) stocks are a function of the SOC concentration and the bulk density of the...
<p>Error bars are standard error of means (n = 3). Different letters denote significant differences ...
The stable carbon isotopic composition of CO2 (δ13C-CO2) has been studied as an indicator of changes...
<p>Different letters in superscript indicate statistically significant differences (p<0.05) among se...
Effects of soil temperature (°C) and soil water content (%) on CO2 and N2O fluxes over the study per...