View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Repository of the Academy's Library Plant Soil (2020) 449:423–437 https://doi.org/10.1007/s11104-020-04505-4 REGULAR ARTICLE Root capacitance measurements allow non-intrusive in-situ monitoring of the seasonal dynamics and drought response of root activity in two grassland species Imre Cseresnyés & Kálmán Rajkai & Katalin Szitár & László Radimszky & Gábor Ónodi & György Kröel-Dulay Received: 29 October 2019 /Accepted: 18 March 2020 /Published online: 26 March 2020 # The Author(s) 2020 Abstract root activity in both species. Stipa borysthenica Background and aims In this study, the potential of non- displayed great plasticity in root activity, including intrusive root electrical capacitance (CR) measurements quick post-treatment recovery during the rainy autumn. for monitoring the seasonal changes and drought re- The changes observed in root activity were similar to sponse of root activity was tested on two grassland those previously recorded using conventional root in- species in a climate change experiment. vestigation techniques (i.e. destructive, minirhizotron, Methods CR was detected between a ground electrode ingrowth core) in temperate grasslands. inserted into the soil and a plant electrode attached to the Conclusions Root capacitance measurements proved to stem of the perennial grass Stipa borysthenica and the be adequate for monitoring root activity in situ in natural biennial herb Crepis rhoeadifolia in control and drought grassland. The method could be particularly useful in plots throughout two growing seasons. A pilot study studies where plant injury or soil disturbance need to be revealed that CR was strongly correlated with root bio- avoided. mass for a given time and soil water content. The effect of changing soil water content on the measured CR value Keywords Drought treatment . Grassland . In-situ root was accounted for by means of species-specific experi- methods . Root dynamics . Electrical capacitance . Soil mental calibrations. water content Results Root activity (CR) was found to peak at the flowering stage in late spring (S. borysthenica)orearly Abbreviations summer (C. rhoeadifolia). Both the natural shortage of CR Root electrical capacitance rainfall and the experimental summer drought reduced CR* Apparent root electrical capacitance Crel Relative root electrical capacitance LME Linear mixed effect model Responsible Editor: Rafael S. Oliveira . SWC Soil water content I. Cseresnyés (*) : K. Rajkai : L. Radimszky RDW Root dry weight Centre for Agricultural Research, Institute for Soil Sciences and θrel Relative water saturation Agricultural Chemistry, Herman Ottó út 15, Budapest H-1022, Hungary e-mail: [email protected] K. Szitár : G. Ónodi : G. Kröel-Dulay Centre for Ecological Research, Institute of Ecology and Botany, Introduction Alkotmány u. 2–4, Vácrátót H-2163, Hungary Apart from their main functions on the individual plant scale (i.e. plant anchorage, water and mineral absorption 424 Plant Soil (2020) 449:423–437 and translocation, food storage and hormonal regula- The measured CR was found to be linked to root tion), roots play a key role in ecosystem processes system size, but it could be influenced by variations in associated with material and energy flows (Hooker root tissue properties (water content, tissue density, su- et al. 2000). Root growth dynamics and belowground berization, xylem maturation, root decay) and presum- interactions strongly affect species distribution and rel- ably root–soil contact, which could vary with time and ative abundance, and thus plant community structure environmental conditions (Dalton 1995; Ellis et al. (Eissenstatetal.2013). Very few studies focus on 2013). This shows an advantage of the root capacitance collecting relevant information about root functional method: CR value seems to comprise root extension and traits especially in natural vegetation, despite their ob- physiological status, could be related to the water (and vious ecological significance (de Vries et al. 2016). nutrient) uptake activity of the whole root system (re- Many authors monitor aboveground phenology, where- ferred to as “root activity” from here) (Cseresnyés et al. as roots are only sampled destructively at the end of the 2016). On the other hand, one disadvantage of the experimental period. However, as root and shoot phe- technique is the high sensitivity of detected CR values nology are often asynchronous and are greatly influ- to external factors, including soil composition, soil wa- enced by growth conditions even in the same species, ter content (SWC), and plant electrode position (Ellis the tracking of root phenology could be critical for et al. 2013), so that data can only be compared when the evaluating whole-plant responses to the environment same species is grown in the same soil type (Chloupek (Radville et al. 2016). The lack of information on root et al. 2010). The capacitance method has mostly been systems is principally due to methodological difficulties used under controlled pot conditions to estimate root in assessing root functions directly in the soil size, and to study the phenology pattern and stress (Milchunas 2012). The conventional destructive tech- response of root growth in crops (Cseresnyés et al. niques (auger sampling, excavation, ingrowth cores) are 2016;Wuetal.2017), native grasses and herbs (Aulen inherently unsuitable for such studies. In-situ rhizotron and Shipley 2012) and tree saplings (Vamerali et al. and minirhizotron systems are widely used in plant 2009). Previous studies reported the successful applica- ecology (e.g. Pilon et al. 2013; Bai et al. 2017; Arndal tion of CR measurements in field-grown crops et al. 2018), but the installation requires soil disturbance, (Chloupek et al. 2010;Svačina et al. 2014;Heřmanská they only represent a small fraction of the root system, et al. 2015), but specific calibrations are a prerequisite and they tend to generate artefacts (Vamerali et al. for data comparison over time in the case of variable 2012). Advanced methods (e.g. tracers, X-ray imaging, SWC (Cseresnyés et al. 2018). MRI) are expensive, and have low resolution on the In spite of the promising results in pot experiments, scale of active (absorbing) fine roots (Milchunas 2012). the CR method has not yet been applied in natural plant Measuring the electrical capacitance of root–soil sys- communities. Since root production accounts for up to tems (CR) is a cheap, simple and rapid non-intrusive 70–90% of total primary production in temperate grass- method, based on the correlation between CR and the lands, particularly in arid and semiarid areas (Milchunas mass, length or surface area of the whole root system 2012), root phenology and population dynamics have a (Chloupek 1972). CR is usually detected by driving a great influence on ecosystem functioning and stress (e.g. low-frequency alternating current (1 kHz AC) between drought) adaptation, and thus on responses to the chang- a ground electrode (metal rod) inserted into the soil and a ing climate (Carrillo et al. 2014; de Vries et al. 2016). plant electrode (needle or clamp) fixed on the stem base. Perennial sand grasslands, which represent valuable According to Dalton's (1995) model, root branches act as patches of remnant vegetation in the Pannonian region lossy cylindrical capacitors connected in parallel. in Central Europe, are especially sensitive to climate Rhizodermal membranes play the role of a dielectric, change (Bartha et al. 2011). Regional climate models separating the conductive xylem and phloem sap from predict increasing temperature, severe summer droughts the conductive soil solution. Capacitance is formed by the and more frequent rainfall anomalies in the Carpathian active polarization (charge storage) of the membranes, Basin for the next few decades (Bartholy et al. 2007). and its magnitude is proportional to the area of the root– The objective of this study was to test the potential of soil interface (Fig. 1). The revised two-dielectric capacitor the CR method in monitoring the seasonal changes and model considers the capacitive behavior of the surround- drought responses of root activity in a native grassland. ing soil as well (Rajkai et al. 2005). In particular, the aim was (i) to monitor the seasonal Plant Soil (2020) 449:423–437 425 Fig. 1 Schematic illustration of root electrical capacitance mea- The plant root is represented as an axially symmetric cylindrical surements with the equivalent electrical network of the root sys- capacitor. In the equation for electrical capacitance ε and A are the tem, according to Dalton (1995) and Ellis et al. (2013). Each permittivity and surface area of the root tissue, respectively, r1 is element (i) consists of a parallel resistor–capacitor (Ri–Ci)circuit. the radius of the xylem and r2 is that of the rhizodermis patterns of root activity in a perennial grass and a bien- Materials and methods nial herb species over two consecutive years, (ii)to evaluate the response of root activity to different annual Study site and plant material rainfall patterns, and (iii) to assess root activity re- sponses to an experimental two-month summer drought. The study site is located in an inland sand dune area in Importantly, this study focused on root physiological Central Hungary, near to the village of Fülöpháza responses at the species level by sampling individual (N46°52′17″,E19°25′17″, 107 m asl.). The vegetation plants non-destructively. However, the simultaneous ap- is an open perennial sand grassland with 30–40% plant plication of this in-situ method to several coexisting coverage, dominated by Festuca vaginata W. et K. and species could contribute to a better understanding of Stipa borysthenica Klokov. The area is covered by nutri- responses at plant community level. ent-poor, coarse-textured calcaric arenosol according to 426 Plant Soil (2020) 449:423–437 Table 1 Main properties of the calcaric arenosol (0–20 cm) at the (Campbell Sci. Ltd., Loughborough, UK) calibrated to Fülöpháza study site this soil, equipped with a 20-cm-long probe.