Patterns and determinants of soil CO2 efflux in major forest types of Central Himalayas, India

Soil CO₂ efflux (F_soil) is a significant contributor of labile CO₂ to the atmosphere. The Himalayas, a global climate hotspot, condense several climate zones on account of their elevational gradients, thus, creating an opportunity to investigate the F_soil trends in different climate zones. Presently, the studies in the Indian Himalayan region are localized to a particular forest type, climate zone, or area of interest, such as seasonal variation. We used a portable infrared gas analyzer to investigate the F_soil rates in Himalayan tropical to alpine scrub forest along a 3100-m elevational gradient. Several study parameters such as seasons, forest types, tree species identity, age of trees, distance from tree base, elevation, climatic factors, and soil physico-chemical and enzymatic parameters were investigated to infer their impact on F_soil regulation. Our results indicate the warm and wet rainy season F_soil rates to be 3.8 times higher than the cold and relatively dry winter season. The tropical forest types showed up to 11 times higher F_soil rates than the alpine scrub forest. The temperate Himalayan blue pine and tropical dipterocarp sal showed significant F_soil rates, while the alpine Rhododendron shrubs the least. Temperature and moisture together regulate the rainy season F_soil maxima. Spatially, F_soil rates decreased with distance from the tree base (ρ =  - 0.301; p < 0.0001). Nepalese alder showed a significant positive increase in F_soil with stem girth (R² = 0.7771; p = 0.048). Species richness (r, 0.81) and diversity (r, 0.77) were significantly associated with F_soil, while elevation and major edaphic properties showed a negative association. Surface litter inclusion presented an elevation-modulated impact. Temperature sensitivity was exorbitantly higher in the sub-tropical pine (Q₁₀, 11.80) and the alpine scrub (Q₁₀, 9.08) forests. We conclude that the rise in atmospheric temperature and the reduction in stand density could enhance the F_soil rates on account of increased temperature sensitivity.

Interaction of abiotic factor on soil CO2 efflux in three forest communities in tropical deciduous forest from India

Environmental factors along with soil physico-chemical properties play a significant role on the diurnal trend of soil CO₂ efflux. Soil CO₂ efflux in Indian tropical forests is poorly studied. We studied the soil CO₂ efflux in a representative tropical deciduous forest at Katerniaghat Wildlife Sanctuary (KWLS), Uttar Pradesh. The three forest communities namely dry mixed (DMF), Sal mixed (SMF), and Teak plantation (TPF) were selected for measuring soil CO₂ efflux in the summer season during April to May 2017 using automated LI-COR 8100 soil CO₂ flux system. Soil physico-chemical parameters were also studied in the three abovementioned forest communities. We also measured the different microclimatic variables at forest understorey in all three communities during the summer season. Total day time soil CO₂ efflux of 826.70, 1089.24, and 828.94 (μmolCO₂ m^-2d^-1) was observed in TPF, SMF, and DMF respectively. Soil CO₂ efflux observed significant differences (P < 0.01) among the three forest communities studied for the summer season in tropical deciduous forest of Terai Himalaya. Average soil CO₂ efflux rate (μmol CO₂ m^-2 s^-1) of 4.06 ± 0.36, 5.03 ± 0.45, and 4.37 ± 0.79 was observed in TPF, SMF, and DMF, respectively, which is positively correlated with total organic carbon (TOC) and water holding capacity (WHC) among soil physico-chemical variables. Among microclimatic variables, soil temperature (ST, °C) and air temperature (AT, °C) observed strong positive correlation with day time soil CO₂ efflux in all three communities. Significant increase in soil CO₂ flux was observed with increasing air and soil temperature (AT and ST) in DMF and SMF. Maximum TOC of 19.23 g Kg^-1 was observed in SMF among all communities in the summer season. The result showed that soil CO₂ efflux is closely associated with TOC, WHC, AT, and ST for Indian deciduous forest ecosystems.

Intensive ground vegetation growth mitigates the carbon loss after forest disturbance

AIMS

Slow or failed tree regeneration after forest disturbance is increasingly observed in the central European Alps, potentially amplifying the carbon (C) loss from disturbance. We aimed at quantifying C dynamics of a poorly regenerating disturbance site with a special focus on the role of non-woody ground vegetation.

METHODS

Soil CO₂ efflux, fine root biomass, ground vegetation biomass, tree increment and litter input were assessed in (i) an undisturbed section of a ~ 110 years old Norway spruce stand, (ii) in a disturbed section which was clear-cut six years ago (no tree regeneration), and (iii) in a disturbed section which was clear-cut three years ago (no tree regeneration).

RESULTS

Total soil CO₂ efflux was similar across all stand sections (8.5 ± 0.2 to 8.9 ± 0.3 t C ha^-1 yr.^-1). The undisturbed forest served as atmospheric C sink (2.1 t C ha^-1 yr.^-1), whereas both clearings were C sources to the atmosphere. The source strength three years after disturbance (-5.5 t C ha^-1 yr.^-1) was almost twice as high as six years after disturbance (-2.9 t C ha^-1 yr.^-1), with declining heterotrophic soil respiration and the high productivity of dense graminoid ground vegetation mitigating C loss.

CONCLUSIONS

C loss after disturbance decreases with time and ground vegetation growth. Dense non-woody ground vegetation cover can hamper tree regeneration but simultaneously decrease the ecosystem C loss. The role of ground vegetation should be more explicitly taken into account in forest C budgets assessing disturbance effects.