Browsing by Subject "Transpiration"

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Abgabe von bodenbürtigem Lachgas über Pflanzen
(2003) Ferch, Norbert-Jakob; Römheld, Volker
The aim of this work was to explore and to rank the different ways and forms of transition of N2O through plants (dissolved in water and transported with the transpiration or gaseous through aerenchyma). To achieve this goal an experimental set-up had to be realized that allowed the determination of possible N2O emissions by plants, the determination of different ways of transition of N2O through the plant and the determination of different influencing factors (e.g. N2O concentration) on the N2O emissions. In the beginning experiments with closed chambers and with ?controlled opened chambers? were conducted in comparison to each other. In the experiments with closed chambers samples were drawn by means of molecular sieves and vacutainers. N2O concentrations of the samples were measured with a GC (gas chromatograph type HP 5890) equipped with an ECD (electron capture detector). Besides the two methods mentioned above in order to determine the N2O concentrations within the experiments with the ?controlled opened chambers? a third method was used for N2O measurement by means of a photo acoustic online measuring machine. The accuracy of the photo acoustic measurement was evaluated with the GC. For the questions of interest the photo acoustic measurement showed to be the best to determine differences of N2O emissions between different experimental treatments. The experiments that were taken in consideration were conducted in a ?controlled opened system? because in closed chambers CO2 concentration decreased rapidly. Additionally, the air in the closed chambers became saturated in water vapour within a few minutes. These two factors lead to inhibited growth of the plants and to undesired influences on the N2O measurements. The ?controlled opened system? consisted of a root and a shoot compartment. Both compartments were separated airtight from each other and from the surroundings. The root compartments were enriched with a definite amount of N2O. The N2O concentrations measured in the shoot compartments of the systems with N2O enrichment in the root compartment were compared with measurements of systems without N2O enrichment and measurements of ambient air. The necessity to divide the root compartment from the shoot compartment airtight was realised with a material on the basis of silicone that is usually used to make prints of teeth (Optosil, from Haereus) and a sealing mass (Prestik AE hellgrau, from Bostik GmbH). To determine the different factors potentially influencing the N2O emission through plants a hydroponical culture system was established that allowed controlling the following factors: concentration of nutrients, pH-factor, concentration of different water soluble gases (e. g. N2O, CO2) and the ratio between water and gas filled space in the root compartment. As experimental plants sunflower (Helianthus annuus cv. Frankasol), barley (Hordeum vulgare cv. Scarlet), rice (Oryza sativa cv. 94D-22) and corn (Zea mays cv. Helix) were used. For the experiment with sunflower (no aerenchyma, N2O dissolved in water available only) a relationship between N2O concentration in the root compartment, the emitted amount of N2O by the shoots and the intensity of transpiration in a diurnal pattern was found. In systems with gaseous availability of N2O in the root compartment the observed emissions were higher than in systems with availability of N2O dissolved only in water. From this it could be concluded, that gaseous N2O is better available for plants than N2O dissolved in water. Similar results were obtained from experiments with barley. The only difference was that the highest N2O emissions were observed in systems with availability of N2O dissolved in water only. The possible N2O emission through aerenchyma was checked with rice plants. In these experiments a pronounced diurnal pattern of the N2O emissions was also found. This lead to the conclusion that aerenchyma only have a small influence on the N2O emissions out of the root compartment through rice plants. Because the N2O emission in the three experiments described above followed the diurnal pattern of the transpiration, it was concluded that N2O was transported with the transpiration water flow from the root (compartment) to the shoot (compartment). The experiments with corn showed for all treatments (control and availability of N2O in gaseous form or dissolved in water) a net N2O depletion in the shoot compartment for night (darkness) and day (light) respectively, thus leading to the conclusion that N2O can be metabolised and used as a nitrogen source. All in all the experiments showed that the main way of transition of N2O through plants is water dissolved with the transpiration water flow and not gaseous (through aerenchyma).
Chamber‐based system for measuring whole‐plant transpiration dynamics
(2022) Pieters, Alejandro; Giese, Marcus; Schmierer, Marc; Johnson, Kristian; Asch, Folkard
Most of our insights on whole‐plant transpiration (E) are based on leaf‐chamber measurements using water vapor porometers, IRGAs, or flux measurements. Gravimetric methods are integrative, accurate, and a clear differentiation between evaporation and E can be made. Water vapor pressure deficit (VPD) is the driving force for E but assessing its impact has been evasive, due to confounding effects of other climate drivers. We developed a chamber‐based gravimetric method, in which whole plant response of E to VPD could be assessed, while keeping other environmental parameters at predetermined values. Stable VPD values (0.5–3.7 kPa) were attained within 5 min after changing flow settings and maintained for at least 45 min. Species differing in life form and photosynthetic metabolism were used. Typical runs covering the range of VPDs lasted up to 4 h, preventing acclimation responses or soilborne water deficit. Species‐specific responses of E to VPD could be identified, as well as differences in leaf conductance. The combined gravimetric‐chamber‐based system presented overcomes several limitations of previous gravimetric set ups in terms of replicability, time, and elucidation of the impact of specific environmental drivers on E, filling a methodological gap and widening our phenotyping capabilities.
Vergleichende Betrachtung von Mikroklima, Struktur und aus dem Xylemsaftfluss von Bäumen hochskalierter Transpiration eines tropisch-montanen Regenwaldes und eines Wolkenwaldes in Südost-Ecuador
(2010) Ohlemacher, Christian; Küppers, Manfred
In a tropical montane rain forest 1990 m a.s.l. and a cloud forest 2240 m a.s.l. in the Andes of Southeast Ecuador, tree stand structure (tree height, tree basal area, tree sapwood area, tree crown ground projection area and leaf area index (LAI)) was registered and the sap flow rate of trees, the microclimate (photosynthetically active radiation, temperature, air moisture) inside and above the canopy, and short term stem radius changes were measured. The period of measurement was one year, and synchronous measurements exist from 7 months. To investigate, whether the stand conductance for water differs between the two sites, their stand structure, xylem sap flow and microclimate were compared. Annual stand transpiration was calculated by means of upscaling the xylem sap flow, under inclusion of the site specific microclimate, with the basal area as scaling parameter. Mean radial stem growth was derived from stem radius changes. Radial stem growth is higher in the montane rain forest than in the cloud forest by a factor 3-5. No clear hints were found for different conductivity of trees between the investigated stands. The lower annual stand transpiration of the higher sited cloud forest (238 mm/a^-1) than that of the lower sited montane rain forest (438 mm/a^-1) is caused by a lower stand and foliage density (LAI = 1,6 in the cloud forest vs. LAI = 3,7 in the montane rain forest) and the higher air moisture at the higher sited stand. The crown area-related sap flow rate of single trees is approximately equal at both stands.