Detection of cavitation and construction of hydraulic vulnerability curves using acoustic emission signals

Protocol

Authors

Daniel M. Johnson1, Stefan Mayr2, Sabine Rosner3 Kathy Steppe4

Author affiliations

1Warnell School of Forestry and Natural Resources, University of Georgia, Athens GA 30606 USA

2Department of Botany, University of Innsbruck, Sternwartestr. 15, 6020 Innsbruck

3Institute of Botany, BOKU Vienna, Gregor Mendel Str. 33, A-1180 Vienna, Austria

4Laboratory of Plant Ecology, Ghent University, Coupure links 653, 9000 Gent, Belgium

 Overview

Plant water transport occurs in a metastable state bearing the risk of hydraulic failure. Hydraulic conductivity loss is induced by cavitation, i.e. the breakage of the water column inside the small conduits. When a water column breaks, a small amount of energy is released. This energy is detectable with acoustic emission (AE) sensors operating in the ultrasonic frequency range (above 20 kHz). AE can thus be used in situ to assess cavitation in plants growing in the field or greenhouse or for generating vulnerability curves. A vulnerability curve is a plot of the hydraulic dysfunction versus decreasing water potential in the (secondary) xylem. Constructing vulnerability curves by means of acoustic emission (AE) and point measurements of water potential is based on the assumption that information extracted from AE signals is correlated with hydraulic dysfunction.

Background

Acoustic emissions (AE) in the ultrasonic frequency range provide a non- to minimally-invasive tool to measure xylem embolism in plant organs. Previous work has shown a close correspondence between the number of AE and percent loss of hydraulic conductivity in stems and leaves of many species. Milburn & Johnson (1966) were the first to detect cavitation events in plants using sound transducers and amplifiers in the audible low-frequency range (< 20 kHz). In 1983, Tyree and Dixon applied a technique from engineering (e.g. pressure vessel testing) for detection of cavitations at frequencies between 100 and 2000 kHz, which led to the development of the Physical Acoustics Drought Stress Monitor (DSM) (Physical Acoustics Corporation, Princeton, NJ, USA) (Tyree & Sperry, 1989). In the ultrasonic frequency range, background noise can be successfully filtered out. The DSM counts AE/time and operates in the frequency range where maximum amplitudes are found, thus detecting cavitations in xylem non-destructively. During the past decades, professional AE testing equipment has been vastly improved, and quite cheaply available single or dual channel AE systems give waveform information for each single AE.

AE can be used in situ to assess cavitation in plants growing in the field or in greenhouse, or for generating vulnerability curves. Construction of vulnerability curves based on AE data works well in conifer branches and some angiosperm species (Cochard 1992, Lo Gullo and Salleo 1991, Mayr & Rosner 2011, Vergeynst et al. 2015), but can be quite tricky in many woody angiosperm branches or shoots (Rosner 2015). The main difficulty is to define the threshold of 100% conductivity loss, since AE of dehydrating branches comes from cavitation in vessels and fibers, shrinkage processes or mechanical failure of the wood (Kawamoto & Williams 2002). Even dehydrating bark tissue can produce AE in the high frequency range (Kikuta 2003).

AE analysis has also been used to monitor freeze-thaw induced cavitation (e.g. Weiser and Wallner 1988, Kikuta and Richter 2003, Mayr et al. 2007) and to study freezing in xylem (e.g. Charrier et al. 2014a).

Materials/Equipment

Physical Acoustics Corporation (Mistras Group), Vallen Systeme, Dakel and KRN Services, Inc. offer a wide range of sensors, detectors and software tools.

  • AE transducers

The most commonly used sensor for detection of xylem embolism has been the Physical Acoustics Corporation R15, which has a frequency detection range of 50-200 kHz. This frequency range is suitable to detect cavitation (Tyree & Sperry 1989). Multiple response sensors, such as WD (frequency range 100-1000 kHz) from Physical Acoustics (Rosner 2012), and point-contact broadband sensors, such as KRNBB-PC from KRN Services (Vergeynst et al. 2015), enable the analysis of the frequency spectrum of AE. Transducers that come with an integral preamplifier are larger in size than those that need a separate preamplifier. Transducers are also available from other companies such as Vallen Systeme or Dakel.

  • AE acquisition hardware

A wide range of detectors that accept up to 80 AE transducers are available. These detectors must be installed as a PCI board in a computer or in an external chassis. Smaller systems may be assembled via USB-based components (node system, Physical Acoustics Corporation), and quite affordable single- or dual channel hand-held instruments are also available from Physical Acoustics Corporation (Pocket AE Acoustic Emission (AE) system) and from Vallen Systeme (ASCO-DAQ2).

  • AE Software for data acquisition and post processing

Detection systems are provided with modular software packages for data acquisition, post processing or replay. The software packages can be customized for the specific demands of the user. Physical Acoustic Corporation comes with the AEwinTM Software; VisualAE and VisualTR are the data analysis tools of the Vallen AE-Suite Software. Both companies offer software for advanced data analysis: NOESISTM Software from Physical Acoustics Corporation and VisualClass Software from Vallen Systeme analyse waveforms based on e.g. pattern recognition. The advantage of the Vallen AE-Suite Software is its compatibility with the AEwinTM Software.

Units, terms, definitions

Amplitude –    Largest voltage peak in the AE signal waveform; expressed in decibels relative to one microvolt at the sensor output (dBAE)

Counts –          Number of times the AE signal crosses the detection threshold

Duration –       Time from the first threshold crossing to the end of the last threshold crossing of the AE signal

Energy –          Total elastic energy released by an acoustic emission event, e.g. by a cavitating conduit (unit in attojoules)

Frequency       The number of cycles occurring in unit time of an oscillating signal.

Procedure

Transducer coupling/mounting

The AE sensor is attached to the organ or tissue of interest (e.g., branch, leaf, etc.) on which a droplet of silicon-based grease has been applied. When pressing the sensor onto the organ or tissue surface, the grease is spread and covers the whole contact surface. The sensor can be placed on top of the sample if the sample is flat (e.g. on leaves), or clamped to the sample (Fig. 1). The surface of branches or stems must be smooth in order to guarantee reliable AE detection. For most species, it is preferable to remove the bark. Smooth and parallel surfaces can be achieved using a wood rasp file with different coarseness. Poor sensor coupling or air spaces between sensor and wood surface may lead to a lower AE detection rate and weaker (lower amplitude) AE signals. Movement of sensors will cause artificial AE. Wounds near the AE sensor are covered with silicone grease and parafilm (Pechiney Plastic Packaging, Chicago, IL, USA) (Fig. 1). The sensor should be attached carefully to avoid damage, and a second rehydration may be necessary after attachment (the rehydration process is described below in the chapter “Bench top dehydration…”).

On leaves, sensors are positioned on the upper side (i.e. adaxial) of the leaf, at the proximal third of the leaf midrib (Kikuta et al. 1997).

 

Fig. 1 Sensor mounting on stems: Wounds are sealed with parafilm.

 

Data acquisition

When the sensor is mounted, it is connected to the AE detector. Prior to data acquisition, the amplitude threshold for AE detection and the levels of signal amplification for the sensor used has to be set in the AE acquisition software. A detection threshold of 35 dB is sufficient to filter out background noise under laboratory conditions (Mayr & Rosner 2012). Under field conditions, a threshold of 45 dB is suggested in order to avoid signals arising from plant organ movement due to wind (Steppe et al. 2009). After the plastic bag (shelter against transpiration as described below in the chapter “Bench top dehydration…”) is removed from the plant, data acquisition is started. The detector will continue collecting data until it is stopped. Detection time is dependent on the size of the plant material and on the species. Experiments may therefore take some hours up to several days. Once data collection is finished, the data can be exported to a spreadsheet and can be analyzed for number of AE signals, amplitude of each signal, signal duration, signal energy etc.

Bench top dehydration of whole branches, shoots or single leaves for vulnerability analysis

Bench top dehydration is performed on quite intact systems such as whole branches or shoots on which the water potential can be measured directly. Detached branches or shoots are harvested at pre-dawn and rehydrated over night. If possible, sensors are mounted on well watered plants or detached branches one day before the acoustic measurements take place. If (for some reason) the sensor has to be mounted shortly before the measurements, all cut ends have to be carefully sealed with parafilm or with plastic foil. During sensor mounting and before measurements, leaves shall be covered by a black plastic bag in order to avoid transpiration.

While AE data are continuously recorded during dehydration on the lab bench, point measurements (Scholander technique, e.g. Mayr and Rosner 2011) or continuous measurements (psychrometry, e.g. Wolkerstorfer et al. 2012, stem shrinkage with dendrometers, e.g. Vergeynst et al. 2015) of water potential take place. The frequency of water potential point measurements depends on the size of the branch/shoot, the number of leaves available and the total duration of dehydration (leaf wilting). Vergeynst et al. (2015) recently found for grapevine that loss in water potential is linearly related to stem shrinkage. Additional dendrometer measurements can thus decrease the number of harvested leaves needed for point measurements of water potential. This may help to keep a more “intact system” during dehydration. The relationship between water potential and stem shrinkage should however be validated. In any case, wounds induced due to leaf sampling should be sealed immediately by silicone grease.

The AE method can also be used for the construction of hydraulic vulnerability curves of single (isolated) leaves (e.g. Johnson et al. 2009). As leaves dehydrate, the water potential of nearby (on the lab bench) leaves is measured as an approximation of the leaf water potential of the leaves to which an AE sensor is attached. The nearby leaves should be treated with silicon-based grease to mimic the conditions of the leaves to which the sensors are attached.

Construction of vulnerability curves

Both the cumulative number and cumulative amplitude or energy of acoustic emissions have been reported in the literature as proxies for loss in hydraulic conductivity (e.g. Tyree & Dixon 1983; Lo Gullo and Salleo 1991, Kikuta et al. 1997; Rosner et al. 2006, Johnson et al. 2009, Mayr and Rosner 2011, Vergeynst et al. 2015).

  • AE counting method

The cumulative number of AE is a good estimate for conductivity loss in plant material where the conduits have a quite similar size, e.g. in conifer branches (Cochard 1992). In plant material where 100% cumulated AE corresponds to 100% conductivity loss, cumulated AE can be used as a proxy for the percent loss of conductivity. The percent cumulative AE is plotted against the water potential, thereafter P50 or P12 and P88 (i.e. water potential inducing 50% or 12% and 88% conductivity loss, respectively) can be calculated.

However, in many angiosperm species, 100% cumulative AE does not correspond to 100% conductivity loss (Rosner 2015). Nolf et al. (2014) recently developed an AE counting method where the AE rate peak is used as a proxy for 50% conductivity loss. The method is appropriate for diffuse- as well for ring-porous angiosperm species. P50 values assessed with classical hydraulic methods and P50 calculated from AE testing data were significantly linearly related.

  • AE amplitude/energy methods

The amplitude or energy of AE is closely correlated with conduit diameter in leaf xylem across species (Johnson et al. 2009) and in conifer branch- or trunkwood (Mayr and Rosner 2011, Ponomarenko et al. 2014). This relationship can be used for construction of vulnerability curves in plant parts where xylem conduits show a quite high variability in diameter (Rosner et al. 2006). The method has been tested so far on isolated conifer wood and conifer branches. The cumulated AE energy as a proxy for hydraulic conductivity loss is related to the water potential, which is either measured directly on branches (Mayr & Rosner 2011) or calculated from the relationship between relative water loss and water potential of a parallel sample set (Rosner et al. 2006).

If the AE amplitude of single signals plotted against time shows distinct clusters, AE sources of interest (related to conductivity loss) can be easily separated from other AE sources (cavitation in ray tracheids, shrinkage processes, mechanical failure). This clustering method has been applied successfully in small isolated conifer sapwood samples, where the water potential was measured by psychrometers (Wolkerstorfer et al. 2012). Cumulated AE are collected from the first AE cluster solely and are thereafter related to the water potential.

Dehydration of isolated sapwood specimen

The AE method has been used for the construction of hydraulic vulnerability curves of isolated wood material (Kikuta et al. 2003). AE sensors are attached to samples and are intermittently weighed while collecting AE data. Relative water loss is measured in parallel samples as they dry (Rosner et al. 2006) or in small samples along with water potential using screen-cage psychrometers (Wolkerstorfer et al. 2012). Once the relationship between relative water content and water potential has been established, the weights of the AE samples can be converted into water potentials for the construction of the vulnerability curve. Attaching the sensor to wood samples also requires stripping the bark, which can damage xylem and allow for dehydration, and may explain the discrepancies between AE and percent loss of conductivity observed in well-hydrated samples with few embolisms (Mayr & Rosner 2011).

Recently, AE and visual analyses on isolated sapwood specimen were also used to study the cavitation process in single tracheids (Mayr et al. 2014, Ponomarenko et al. 2014).

AE analyses during freeze-thaw stress

Sensors attached to freezing branches revealed AE activity predominantly on freezing but not on thawing, which is in contradiction to the “thaw expansion hypothesis” (Mayr and Sperry 2010). Experiments demonstrated a close link between drought and freezing stress (Mayr et al. 2007, Zublasing and Mayr 2007, Charrier et al. 2014b). For AE analyses it has to be considered that acoustic properties change when water turns into ice. However, this may be used to detect ice formation (Charrier et al. 2014a).

Notes and troubleshooting tips

  • After sensor attachment to an unstressed sample (e.g. before start of bench dehydration), AE activity should be negligible. More than a few signals per minute indicate sensor movements. Lead break tests enable validation of the coupling.
  • Fluorescent lights are often a source of RFI (radio frequency interference) that is detected by the sensor. Best results have been obtained by acoustically shielding samples inside a ~1cm thick corrugated cardboard box lined with 6-8cm thick packing foam.
  • AE in leaves can be more difficult to measure than in woody tissues, due to the often small conduit dimensions in leaf xylem. Also, the correlation between leaf AE and loss of hydraulic conductivity is not as strong, in some species, as it is in woody tissues. This is likely due to the much more complex pathway of water transport through the leaf as compared to wood. Johnson et al. (2009) calculated a minimum conduit size of about 4.5 µm for which embolism is detectable by acoustic emissions, which may make this method unsuitable for some species.
  • The Pocket AE software begins overwriting data after 24 hours.

Links to resources and suppliers

http://www.pacndt.com/

http://www.vallen.de/

http://www.krnservices.com/

http://www.dakel.cz

Literature references

Cochard H (1992) Vulnerability of several conifers to air embolism. Tree Physiollogy 11, 73–83.

Johnson DM, Meinzer FC, Woodruff DR, McCulloh KA (2009) Leaf xylem embolism, detected acoustically and by cryo-SEM, corresponds to decreases in leaf hydraulic conductance in four evergreen species. Plant, Cell and Environment 32, 828–836.

Charrier G, Charra-Vaskou K, Benoit L, Améglio T, Mayr S (2014a) Changes in ultrasound velocity and attenuation indicate freezing of xylem sap. Agricultural and Forest Meteorology 185, 20-25.

Charrier G, Charra-Vaskou K, Kasuga J, Cochard H, Mayr S, Améglio T (2014b) Freeze-thaw stress. Effects of temperature on hydraulic conductivity and ultrasonic activity in ten woody angiosperms. Plant Physiology 164, 992-998.

Kawamoto S, Williams RS. 2002. Acoustic emission and acousto-ultrasonic techniques for wood and wood-based composites A Review. . Madison, WI: Gen. Techn. Rep. FPL-GTR-134. U.S. Department of Agriculture, Forest Service, Forest Products Laboratory.

Kikuta SB (2003) Ultrasound acoustic emissions from bark samples differing in anatomical characteristics. Phyton 43, 161-176.

Kikuta SB, Lo Gullo MA, Nardini A, Richter H, Salleo S (1997) Ultrasound acoustic emissions from dehydrating leaves of deciduous and evergreen trees. Plant, Cell and Environment 20, 1381–1390.

Kikuta SB, Hietz P, Richter H (2003) Vulnerability curves from conifer sapwood sections exposed over solutions with known water potentials. Journal of Experimental Botany 54, 2149–55.

Kikuta SB, Richter H (2003) Ultrasound acoustic emissions from freezing xylem. Plant, Cell and Environment 26, 383-388.

Lo Gullo MA, Salleo S. 1991. Three different methods for measuring xylem cavitation and embolism: a comparison. Annals of Botany 67, 417–424.

Mayr S, Cochard H, Améglio T, Kikuta S (2007) Embolism formation during freezing in the wood of Picea abies. Plant Physiology 143, 60-67.

Mayr S, Kartusch B, Kikuta S (2014) Evidence for air-seeding: watching the formation of embolism in conifer xylem. Journal of Plant Hydraulics 1, e0004.

Mayr S, Rosner S (2011) Cavitation in dehydrating xylem of Picea abies: energy properties of ultrasonic emissions reflect tracheid dimensions. Tree Physiology 31, 59-68.

Mayr S, Sperry JS (2010) Freeze-thaw induced embolism in Pinus contorta: centrifuge experiments validate the “thaw-expansion hypothesis” but conflict with ultrasonic emission data. New Phytologist 185, 1016-1024.

Mayr S, Zublasing V (2010) Ultrasonic emissions from conifer xylem exposed to repeated freezing. Journal of Plant Physiology 167, 34-40.

Millburn JA, Johnson RPC (1966) The conduction of sap. I. Detection of vibrations produced by sap cavitation in Ricinus xylem. Planta 69, 43–52.

Nolf M, Beikircher B, Mayr S (2014) Hydraulic vulnerability to drought induced embolism in eight co-occurring temperate shrubs. In: Proceedings of the 20. Meeting of the Austrian Society of Plant Biology (ATSPB), Lunz am See, Austria, June 19-21. ISBN 978-3-900932-17-6, p. 26.

Ponomarenko A, Vincent O, Pietriga A, Cochard H, Badel E, Marmottant P (2014) Ultrasonic emissions reveal individual cavitation bubbles in water-stressed wood. J R Soc Interface. http://dx.doi.org/10.1098/rsif.2014.0480.

Rosner S (2012) Waveform features of acoustic emission provide information about reversible and irreversible processes during spruce sapwood drying. BioResources 7, 1253-1263.

Rosner S. (2015) A new type of vulnerability curve: Is there truth in vine? Tree Physiology. doi: 10.1093/treephys/tpu080.

Rosner S, Klein A, Wimmer R, Karlsson B (2006) Extraction of features from ultrasound acoustic emissions: a tool to assess the hydraulic vulnerability of Norway spruce trunkwood? New Phytologist 171, 105-116.

Steppe K, Zeugin F, Zweifel R (2009) Low-decibel ultrasonic acoustic emissions are temperature-induced and probably have no biotic origin. New Phytologist 183, 928-931.

Tyree MT, Dixon MA (1983) Cavitation events in Thuja occidentalis. Ultrasonic acoustic emissions from the sapwood can be measured. Plant Physiology 72, 1094–1099.

Tyree MT, Sperry JS (1989) Characterization and propagation of acoustic emission signals in woody plants: towards an improved acoustic emission counter. Plant Cell and Environment 12, 371–382.

Vergeynst LL, Dierick M, Bogaerts J, Cnudde V, Steppe K (2015) Cavitation: A blessing in disguise? New method to establish vulnerability curves and assess hydraulic capacitance of woody tissues. Tree Physiology. doi:10.1093/treephys/tpu056

Weiser RL, Wallner SJ (1988) Freezing woody plant stems produces acoustic emissions. Journal of the American Society of Horticultural Science 113, 636-639

Wolkerstorfer S, Rosner S, Hietz P (2012) An improved method and data analysis for ultrasound acoustic emissions and xylem vulnerability in conifer wood. Physiologia Plantarum 146:185-191.

Health, safety & hazardous waste disposal considerations

No health, safety or hazardous disposal problems are caused by the method described.

Search terms and classification

This protocol has been tested on woody species such as Norway spruce (Picea abies) and poplar (Populus alba, Populus tremula).

Detection of AE is probably restricted to plant species or plant organs with a conduit size of more than 4.5 µm (Johnson et al. 2009).