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This page offers a description of the vegetation instruments and measurements available during the campaign. |
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INSTRUMENTATION A large amount of ground measurements will be collected in the Barrax study area during the SEN2FLEX campaign, covering LAI, fCover, Leaf Chlorophyll a+b, Leaf water content and leaf biomass, together with other complementary data. All the available ground measurements will be cross-checked with GPS measurements. The sampling strategy to be followed in choosing measurement points has been designed according to statistical criteria. Nevertheless, most times experimental constraints become critical, and finding a balance between what is mathematically optimal and what is experimentally possible requires some compromise. According to statistical requirements, till 4 to 15 areas have to be sampled to fully characterize a crop (its size and heterogeneity). These areas will be chosen randomly, but it is not operationally very often (high plant densities, very wet soils or tall plants may cause moving across the cross be very hard). So, the aim is to perform random sampling in crops where it will be possible, but restrict sampling to crop geometrical constraints when it will be not. For example, taking samples in 1.80 meters high corn crops following the circular track made by irrigation pivot wheel could be a good idea. Once sampling areas wil be chosen, a strategy to take samples inside each area will be again needed. The above considerations on the choice of areas will be again useful in point sampling within the sampling area: random criterion is mathematically supported, so it will be the one to be followed when field crop configuration allows it; however, it will be sometimes difficult to move around one measurement point to take samples randomly, so mobility requirements shall be taken into account in such cases, and a sampling strategy that made sampling easier shall be be followed. Biophysical parameters that will be used in the characterization of the different crops: a. Dry Matter content (DM)
The LAI-2000 (Li-Cor inc., Lincoln, NE, in fig. 6.1) uses a fish-eye lens with an hemispheric field of view (?148º). The detector is composed of five concentric rings (sensitive to radiation below 490nm). Each ring responds over a different range of zenith angles. Light attenuation through the canopy is measured and light transmittance is calculated as the ratio of below: above canopy readings for each of the 5 angles. This ratio is used to calculate several variables, including leaf area index, gap fraction, and mean tilt angle (a number representing the foliage orientation).
Figure 6.1 LAI2000 Plant Canopy Analyser
The Garmin GPS 12CX color-display Personal Navigator (figure 5.1) provides satellite navigation you can count on.
Figure 6.2. GARMIN´s GPS 12CX
Hemispherical canopy photography is a technique for studying plant canopies via photographs acquired through a hemispherical (fisheye) lens from beneath the canopy (oriented towards zenith) or placed above the canopy for downwards looking. Therefore, it can be used for any canopy type. A hemispherical photograph allows you to derive, among others, vegetation structural characteristics such as, gap fraction, leaf area index (LAI) and average leaf inclination angle (ALA). It provides a permanent record and is therefore a valuable information source for position, size, density, and distribution of canopy gaps. The view angle is equal to 183º and allows the gap fraction to be evaluated in all viewing directions, which increases the accuracy of the derived biophysical variables (LAI, ALA). Fig 6.3. NIKON Coolpix5000 with the NIKON FC-E8 fisheye converter.
Time-Domain Reflectometry (TDR) The main components of a typical TDR instrumentation are schematically drawn in figure 6.4. The electronic apparatus includes a control unit, needed for the synchronisation of the pulse generator and the receiver, and the output device (generally a LCD monitor) and related peripherals (communication port and/or dot matrix printer). The apparatus is connected with a coaxial cable to the transmission line (TDR probe), which may have different shapes and configurations.
Figure 6.4. Schematic view of TDR apparatus (adapted from Topp and Davis, 1985)
Figure 6.5. Example of TDR output with a balanced parallel line in a wetted soil.
The returning signals are superimposed to the emitted ones and they are detected by the receiving unit, with a voltage decrease or increase depending on the phase of the reflection. By means of its built-in hardware and firmware, the receiving unit samples and records the returning signal at very small time steps; in the same time, the output device provides a graph of the reflected voltage versus time.
Figure 6.6. Balanced probes of different length. A widely used TDR equipment is the Tektronix cable tester Mod.1502 C, which has been conceived as a portable measuring device and it can be easily connected to a personal computer through its communication port. In this case, the step-pulse is characterised by an amplitude of 300 mV, a rise time of 0.2 ns and a duration of 25 ms corresponding to a theoretical frequency range from 20 kHz and 1.75 GHz. The effective frequency bandwidth is certainly restricted by attenuation effects induced by cable connections; the extent of this attenuation, which mainly affects the higher frequencies range, largely depends on the quality and on the length of cables. From the analysis of several estimates of soil dielectric permittivity on different types of soils by means of TDR, Heimovaara et al. (1994) estimated a frequency range between 200 MHz and 1 GHz, thus confirming the assumptions reported in previous section. Figure 6.7. Parallel balanced (a) and unbalanced (b) TDR probes (from Whalley, 1993) The probe inserted into the soil constitutes the pulse transmission line which can be electrically balanced or unbalanced. The balanced lines (figure 6.6) are more widely used and they are made of parallel and cylindrical metallic conductors; the soil between them is the dielectric medium (figure 6.7-a). The probe is connected to the TDR unit by means of a coaxial cable or a parallel shielded cable; every connection represents an impedance mismatching which causes a partial reflection of energy. Figure 6.8. Unbalanced three-wire probe (L=14 cm) with coaxial cable and connector.
Chlorophyll Content Meter The New CCM-200 Chlorophyll Content Meter (fig. 6.4.) from Opti-Sciences
accurately determines chlorophyll content in plants and crops. Especially
useful for improving Nitrogen management programs, the CCM-200 is also
an ideal instrument for research and teaching. The CCM-200 provides agronomists,
researchers, and teachers with reliable, repeatable chlorophyll content
readings. The ample on-board data storage and hand-held design make the
CCM-200 the most field efficient, affordable chlorophyll content meter
on the market. Fig. 6.4 Chlorophyll Content Meter CCM-200
Table 6.1- CCM-200 Technical Specifications Chlorophyll Meter SPAD-502 The SPAD-502 is a compact meter designed to help users improve crop quality and increase crop yeild by providing an indication of the amount of chlorophyll present in plant leaves.
Figure 6.10 Chlorophyll Meter SPAD-502 GPS Trimble Pathfinder Pro XRS Versatile GPS receiver that offers submeter accuracy in real time, and centimeter level postprocessed accuracy. It is used with TSCe controller, rugged and adaptable handheld data collector that provides exceptional control of Trimble GPS and optical sensors.
Key features:
Chlorophyll Measurements
MEASUREMENT PROTOCOLS Crop phenology A phenological state is the growth stage during which the plants exhibit particular physiological and/or morphological characteristics. It can be determined by comparing the plant morphology to stages defined for that crop (figure 6.11). The stage in which is the 50% of the plants is usually assumed.
Figure 6.5 Standard crop phenology scale, for cereals and legumes.
The minimum sample size is one in case of a uniform stand. The identification of different growth stages and the associated proportions of the canopy are important especially for larger, heterogeneous areas and at certain growth stages when the canopy changes very rapidly. Green vegetation cover fraction It will be evaluated from a digital picture, taken from the vertical
direction and at a constant height, with the Sun in such a position that
shadows proportion is minimal. In order to obtain the green vegetation
cover fraction a classification of the registered image will be performed. This is the mass of plant material within a defined area divided by the area size (kg•m-2). For taking the measurements, cut all of the plants from a pre-defined area. If applicable, separate plants into components (stems, leaves, fruits) and place into separate containers (plastic, bags, etc.). Weigh each component within a few hours (preliminary test can be used to determine permissible elapsed time). Dry the plants at 70ºC until constant weight is reached and weigh again. From the two masses and the known sampled area, wet and dry biomass can be calculated. Water content is calculated as the percentage of wet (or dry) mass, or per unit area (volume) when biomass (biomass and height) are known. Sample size depends on the size of the individual plants and available
drying facilities. A minimum of 150 grams of matter for small crops or
plant components should be in one sample. The minimum number of samples
is five. This parameter is the mass of water in a plant sample divided by the mass of the entire plant sample before drying (i.e. on a wet biomass basis). Units are percent or dimensionless, although when plant height and/or biomass are known, water content can also be expressed in kg/m3 or kg/m2, respectively). It is given from the biomass evaluation procedure directly, for each one of plant components. Leaf Area Index It will be calculated by means of the LICOR 3000 device in the laboratory, from destructive samples. Comparative measurements will be done with other systems in the field (SUNSCAN, TRAC, LICOR 2000, hemispherical camera…), in order to validate those from the laboratory. Leaf Chlorophyll The leaf chlorophyll content will be measured with the CCM-200 Chlorophyll Content Meter (figure 6.4). However, it performs relative measurements, so calibration measurements must be made before using laboratory analysis methods. Leaf disks will be cut with a calibrated cork borer, wrapped in aluminum foil, frozen in liquid-nitrogen, and stored (still wrapped in foil) at -20 °C. Leaf pigments will be later extracted with acetone in the presence of Na ascorbate and stored as described previously (Abadía and Abadía 1993). Pigment extracts will be thawed on ice, filtered through a 0.45 µm filter and analyzed by an isocratic HPLC method based on that developed by De las Rivas et al. (1989). Two steps (instead of three) will be used: mobile phase A (acetonitrile:methanol,7:1,v:v) will be pumped for 3.5 min, and then mobile phase B (acetonitrile :methanol: water: ethyl acetate, 7:0.96:0.04:8 by volume) will be pumped for 4.5 min. To both solvents 0.7% (v:v) of the modifier triethylamine (TEA) will be added (Hill and Kind 1993) to improve pigment stability during separation. All chemicals used will be HPLC quality. The column will be equilibrated before injecting each sample by flushing with mobile phase A for 5 min. The analysis time for each sample will be 13 min, including equilibration time. Plant density This is the number of plant stems per unit area. For row crops, the method consists in counting the number of stems along the row and converting it into density using the average row width. For randomly distributed plants, count the number of stems within a predefined area. One or several stems may be originated from a root system of one plant. Sample size varies with the crop. The area included in one sample should be large enough to contain a minimum of 30 (for large, e.g. corn) or 60 (smaller crops, e.g. cereals) stems. For rice, a sample area of 25x25 cm can be sufficient. A minimum of three samples should be taken in a homogeneous canopy, but the number should be increased for heterogeneous canopies and/or for larger areas. Plant height This is the distance between the canopy component of interest and the soil surface for non flooded fields. For the measurement, it must be placed a measuring stick near selected plants. Take a sufficient number of measurements to obtain a representative value. Several height parameters are useful; in the general order of decreasing importance they are: • Total maximum height (to the top of the canopy). A minimum of five measurements is recommended for relativity uniform canopies. This number should be increased as canopy variability and/or the area measured increase. Plant row direction It can be defined as the orientation of the plant rows, given in degrees or geographic direction. It must be identified the row direction of the plants, if any, and relate it to the North direction. This can be done in situ or from aerial photographs with a scale large enough, so that the row direction can be recognized. Note that plant row direction may not coincide with tillage direction. Only one observation is needed if the row direction remains constant. However, it is important to ascertain that this is the case, as FOW direction may vary due to the field shape, cultivation pattern and natural obstacles (topography, woody, vegetation, etc…). In these instances, aerial photographs are the preferred method. Canopy structure This is the three dimensional location and orientation of plants and plant components in the canopy. A direct measurement would involve a reconstruction of the three-dimensional distribution of the canopy. Although very desirable, not rapid and effective method has been developed yet. The following approach can be used to characterize the leaf distribution: leaf position is determined by placing a gridded horizontal plate beneath the canopy (x, y coordinates) and by measuring its height (z) above the plate; leaf inclination angle (in degrees) is measured with an inclinometer; leaf azimuth angle is determined (for 45º increments) using a small plate equipped with a circular bubble level and a dowel attached perpendicularly to the face of the plate. To measure the relevant physical dimensions of each canopy component (leaves, stems, heads), one should first select an appropriate geometric model for that component (e.g., cylinder, ellipsoidal disk, plate) and then measure the length, width, diameter or axes as appropriate for the assumed model (for stems, diameters at bottom and top should be measured). Among the numerous parameters describing canopy structure, two types deserve special attention: leaf dimensions and the orientation of leaves and stems. It is also helpful to Xerox plant components for a permanent record. For a qualitative characterization of the canopy, photographs can be taken showing the vertical profile of one plant or one group of plants, preferably with a gridded background plate put vertically behind a plant row. Soil moisture It is defined as the amount of water held in a unit mass (gravimetric basis) of soil. The weight of water in a soil sample is divided by the weight of the sample after drying. Units are g•g-1 (gravimetric basis). Bulk density should also be determined where gravimetric samples are taken. Although various methods for measuring soil water content are available, the destructive sampling method has been widely used because of its simplicity. A sample of soil is taken from a layer of the soil profile to be characterized. This can be accomplished using a spatula for gravimetric moisture content. The moist samples should be weighed as soon as possible and then dried at 105ºC to a constant weight (generally 24 hours or less). Alternatively, drying in a microwave oven can produce good results and take much less time (less than 1 hour depending on sample size); a preliminary test should be carried out to calibrate this method of drying against the above standard. Using wet and dry soil masses and the volume (if known) water content values can be calculated. It is recommended for ASAR/ENVISAT that the layer 0 to 5 cm in depth always be sampled and reported to ensure comparability of results among different studies. To obtain representative mean values, it is recommended as a general guideline that 5 or more (minimum 3) individual samples be taken. Soil roughness Soil roughness is the shape of the soil-air interface in three dimensions. The roughness components are clods or soil aggregates random, furrows or rows (periodic), and slope or inclination of the surface (monotonic). In practice, it can be described by the spatial correlation function of surface roughness in two perpendicular directions. Optimally, the measurements technique should produce data with horizontal and vertical resolutions of one-tenth of the radar wavelength studied. In addition, measurements should be made over a consecutive length of up to 10 times the largest roughness periodicity (e.g. across 10 rows of a crop). For distinct periodic surfaces (e.g. plowed) these measurements should provide slope angle distribution as well. Some methods are photographs of a gridded metal panel inserted into the soil and levelled which are subsequently digitized, water resistant paper attached to the metal plate and the cross section sprayed with a colour spray paint. It is important that surface roughness is not changed during the panel insertion or spraying. This is impossible to achieve under some conditions, e.g. for a loose, dry soil where this approach should be avoided.
Sampling for each crop is currently being defined, as well as the measurements that must be made simultaneous with satellite/aircraft overpasses (chlorophyll and water, surely) and which not (LAI and FCV). Figure 6.12 shows the RGB LANDSAT-5 image composition reported by IDR corresponding to may-26 of 2005 overlaped to the INTA and DLR flights configurations planned to Mission 1 of SEN2FLEX campaign. Figure 6.12.
Flight configuration for Mission 1 of SEN2FLEX campaign. The RGB LANDSAT-5
image composition reported by IDR corresponding to may-26 of 2005.
Program of activities planned for the SEN2FLEX campaign
A monitoring system for soil water content, based on a TDR system (Tektronix) that will be operating continuously from June 2nd to July 18th, will be installed. Randomly distributed soil water content measurements will also be performed during the flights. In addition, it will be performed some LAI measurements in selected points (for validation only) and if needed spectro-radiometer measurements. Table 6.2- Planned activities for the
Mission 1 of SEN2FLEX campaign.
UNIVERSITY OF VALENCIA Characterisation of the biophysical parameters that will be used in the characterization of the different crops: a. Dry Matter content (DM) b. Water Content (WC) c. Leaf Area Index (LAI) from LAI-Licor d. Fractional Vegetation Cover (FVC) from hemispherical photographs e. Chlorophyll Content (CC) Table 6.3- Planned activities
for the Mission 1 of SEN2FLEX campaign.
Figure 6.13. Vegetation sampling for the SEN2FLEX campaign Mission-1 overlaped to the RGB LANDSAT-5 image composition reported by IDR corresponding to may-26 of 2005.
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by GPDS Group University of Valencia (Spain) |
Last Updated: July
29th - 14:40h LT |