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Fig. 1 | Annals of Forest Science

Fig. 1

From: Changes in the non-growing season soil heterotrophic respiration rate are driven by environmental factors after fire in a cold temperate forest ecosystem

Fig. 1

Non-growing season soil temperature, soil moisture at a depth of 5 cm, and depth of snowpack measured at non-trenched (a, c, and e) and trenched (b, d, and f) plots in control and burned stands. Error bars represent standard deviations, and the shadowed period indicates the spring freeze-thaw cycle (FTC). Values represent the average of three technical replications and repeated measurements

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Annals of Forest Science

ISSN: 1297-966X