Luis Lopez-Sangil

Rhizodeposition of organic carbon by plants with contrasting traits for resource acquisition: responses to different fertility regimes

Background and aimsRhizodeposition plays an important role in mediating soil nutrient availability in ecosystems. However, owing to methodological difficulties (i.e., narrow zone of soil around roots, rapid assimilation by soil microbes) fertility-induced changes in rhizodeposition remain mostly unknown.MethodsWe developed a novel long-term continuous 13C labelling method to address the effects of two levels of nitrogen (N) fertilization on rhizodeposited carbon (C) by species with different nutrient acquisition strategies.ResultsFertility-induced changes in rhizodeposition were modulated by root responses to N availability rather than by changes in soil microbial biomass. Differences among species were mostly related to plant biomass: species with higher total leaf and root biomass also had higher total rhizodeposited C, whereas species with lower root biomass had higher specific rhizodeposited C (per gram root mass). Experimental controls demonstrated that most of the biases commonly associated with this type of experiment (i.e., long-term steady-state labelling) were avoided using our methodological approach.ConclusionsThese results suggest that the amount of rhizodeposited C from plants grown under different levels of N were driven mainly by plant biomass and root morphology rather than microbial biomass. They also underline the importance of plant characteristics (i.e., biomass allocation) as opposed to traits associated with plant resource acquisition strategies in predicting total C rhizodeposition.

Individual closed chamber: an alternative method for quantifying 14C in both labeled organic and inorganic carbon substrates

Incubation of 14C-labeled substrates continues to be a widely used procedure in soil organic matter (OM) research due to its sensitiveness. When the labeling is found in liquid fractions (soil extracts, hydrolysates), 14C can be easily quantified by using an aliquot for scintillation counting. For this reason, converting a solid carbon sample into liquid form is a typical step for accurate 14C analysis. We have developed an alternative method to carry out this step, which uses standard glass hardware and does not require complex laboratory facilities. Carbon (both in organic or inorganic forms) is converted into CO2 within a reaction vessel connected to a Twisselmann’s extractor with an alkali trap inside. This forms an individual closed chamber (ICC) for each sample, thus eliminating the risk of cross-contaminations. The alkali solution adsorbs the evolved CO2 within the closed system, and the excess of pressure is easily overcome by the use of a balloon. We tested the procedure on a set of substrates and two contrasting soils, checking also the effect of different sample loads (from 20 to 160 mg C) on the CO2 recovery of the process. The percentage of carbon recovered into the alkali (i.e. the efficiency of the process) ranged from 92% for the inorganic C to 93–95% for the organic C method, the latter being sensitive to the amount of sample used for analysis. The ICC method can be successfully applied to analyze 14C-labeling in both carbonates and OM from solid samples, thus representing an alternative method to some established protocols, and it is suitable for substrates with low or very low 14C contents, in which high volumes of sample must be analyzed in order to guarantee representative results.

The Automated Root Exudate System (ARES) : a method to apply solutes at regular intervals to soils in the field

Summary Root exudation is a key component of nutrient and carbon dynamics in terrestrial ecosystems. Exudation rates vary widely by plant species and environmental conditions, but our understanding of how root exudates affect soil functioning is incomplete, in part because there are few viable methods to manipulate root exudates in situ. To address this, we devised the Automated Root Exudate System (ARES), which simulates increased root exudation by applying small amounts of labile solutes at regular intervals in the field. The ARES is a gravity‐fed drip irrigation system comprising a reservoir bottle connected via a timer to a micro‐hose irrigation grid covering c. 1 m2; 24 drip‐tips are inserted into the soil to 4‐cm depth to apply solutions into the rooting zone. We installed two ARES subplots within existing litter removal and control plots in a temperate deciduous woodland. We applied either an artificial root exudate solution (RE) or a procedural control solution (CP) to each subplot for 1 min day−1 during two growing seasons. To investigate the influence of root exudation on soil carbon dynamics, we measured soil respiration monthly and soil microbial biomass at the end of each growing season. The ARES applied the solutions at a rate of c. 2 L m−2 week−1 without significantly increasing soil water content. The application of RE solution had a clear effect on soil carbon dynamics, but the response varied by litter treatment. Across two growing seasons, soil respiration was 25% higher in RE compared to CP subplots in the litter removal treatment, but not in the control plots. By contrast, we observed a significant increase in microbial biomass carbon (33%) and nitrogen (26%) in RE subplots in the control litter treatment. The ARES is an effective, low‐cost method to apply experimental solutions directly into the rooting zone in the field. The installation of the systems entails minimal disturbance to the soil and little maintenance is required. Although we used ARES to apply root exudate solution, the method can be used to apply many other treatments involving solute inputs at regular intervals in a wide range of ecosystems.

Distinct responses of soil respiration to experimental litter manipulation in temperate woodland and tropical forest

Abstract Global change is affecting primary productivity in forests worldwide, and this, in turn, will alter long‐term carbon (C) sequestration in wooded ecosystems. On one hand, increased primary productivity, for example, in response to elevated atmospheric carbon dioxide (CO 2), can result in greater inputs of organic matter to the soil, which could increase C sequestration belowground. On other hand, many of the interactions between plants and microorganisms that determine soil C dynamics are poorly characterized, and additional inputs of plant material, such as leaf litter, can result in the mineralization of soil organic matter, and the release of soil C as CO 2 during so‐called “priming effects”. Until now, very few studies made direct comparison of changes in soil C dynamics in response to altered plant inputs in different wooded ecosystems. We addressed this with a cross‐continental study with litter removal and addition treatments in a temperate woodland (Wytham Woods) and lowland tropical forest (Gigante forest) to compare the consequences of increased litterfall on soil respiration in two distinct wooded ecosystems. Mean soil respiration was almost twice as high at Gigante (5.0 μmol CO 2 m−2 s−1) than at Wytham (2.7 μmol CO 2 m−2 s−1) but surprisingly, litter manipulation treatments had a greater and more immediate effect on soil respiration at Wytham. We measured a 30% increase in soil respiration in response to litter addition treatments at Wytham, compared to a 10% increase at Gigante. Importantly, despite higher soil respiration rates at Gigante, priming effects were stronger and more consistent at Wytham. Our results suggest that in situ priming effects in wooded ecosystems track seasonality in litterfall and soil respiration but the amount of soil C released by priming is not proportional to rates of soil respiration. Instead, priming effects may be promoted by larger inputs of organic matter combined with slower turnover rates.