Li 1600
The LI-1600 is a portable environmental monitoring device designed for research applications. It is capable of measuring and recording various environmental parameters, such as temperature, humidity, and solar radiation. The LI-1600 is compact, lightweight, and easy to use, making it suitable for field studies and environmental data collection.
10 protocols using li 1600
Leaf Physiological Responses to Infestation
Acclimation of Plant Water Relations
In order to quantify eventual acclimation of water relation parameters in terms of leaf water potential at the turgor loss point (Ψtlp), osmotic potential at full turgor (π0) and bulk modulus of elasticity (ɛmax), leaf water potential isotherms of leaves of at least one plant per module per experimental group were determined from pressure–volume (P–V) curves (Tyree and Hammel 1972 (link)). Measurements were performed before starting the treatment and repeated at the end of the 10-week period, respectively.
Evaluating Grapevine Drought Response
where Tcanopy (°C) was the temperature deduced from the thermal images of six sun-exposed mature leaves per vine, Tdry (°C) and Twet (°C) were the temperatures detected on the cardboard “reference surfaces”. Stomatal conductance (gs) and transpiration were measured with a steady state porometer (Licor Li-1600) in the third experimental year.
Leaf Transpiration and Stomatal Conductance
Leaf Water Dynamics and Hydraulic Conductance
Leaf hydraulic conductance (KLeaf) was calculating according to Ohm’s law following the formula:
It has been assumed that Ψsoil is in equilibrium with Ψp and the lowest diurnal Ψleaf is equal to Ψm [66 ,67 (link),99 (link)]. However, sometimes the first assumption may lead to overestimation of Kplant [100 (link)]. Additionally, values of KLeaf reflect the capacity of evergreen and deciduous plants, grown under ambient conditions, for water exploitation during a period of soil drying.
Measuring Leaf Xylem pH, Stomatal Resistance, and Water Use Efficiency
Daily water dissipation by transpiration and the evaporation from soil surface was determined by weighing every day. At the beginning of this measurement, the plant weight per pot was determined to avoid prejudicing the amount of water use per pot. The cumulative amount of water dissipation by transpiration per pot d−1 during the whole experiment was the total water dissipation by transpiration of the potted plants. The water use efficiency of biomass production (WUE) was determined for each potted plant by dividing the total biomass production (above- plus belowground biomass) by cumulative water use throughout the test period (i.e. the total water dissipation by transpiration).
The water potential of top third fully expanded leaf were measured by pressure chamber (Model: 3005, Soil Moisture Equipment Co. U.S.A) as described above. The soil water content per pot was measured by HH2 Moisture Meter (Cambridge, England).
Stomatal Conductance Measurement Protocol
Leaf Physiological Measurements in Plants
Specific leaf weight (SLW) in g cm−2 was calculated according to Pearce et al. (1968) using the formula:
Relative water content (RWC %) was calculated based on Gonzalez and Gonzalez (2001) using the formula: where: FW = the sample fresh weight, TW = the turgid weight & DW = the dry weight.
Leaf chlorophyll fluorescence was measured using chlorophyll fluorometer (OS-30, opti sciences, inc. The USA) to calculate the maximum quantum yield of photo-system ll (PSll) by the formula of Maxwell and Johnson (2000) (link) as follow: where: Fv/Fm = the maximal quantum efficiency of PSll (MQE), Fm = the maximal chlorophyll fluorescence, and Fo = minimum chlorophyll fluorescence (in the dark).
Leaf temperature (°C): During the mid-day time, and in the absence of cloud cover, a portable steady state the promoter (LI-COR model LI- 1600) was used to measure leaf temperature on a central portion of fully extended flag leaves from three randomly selected plants in each plot.
Stomatal Conductance Measurement Protocol
Measuring Plant Transpiration and Stomatal Conductance
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