Uptake of subsoil water below 2 m fails to alleviate drought response in deep-rooted Chicory (Cichorium intybus L.)
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Deep-rooted agricultural crops can potentially utilize deep soil moisture to reduce periods where growth is water limited. Chicory (Cichorium intybus L.) is a deep-rooted species, but the benefits of deep roots to water uptake has not been studied. The aim of this study was to investigate the value of deep roots (>2 m) under topsoil water limitation.
Chicory grown in 4 m deep soil-filled rhizotrons was exposed to either topsoil drought or resource competition from the shallow-rooted species ryegrass (Lolium perenne L.) and black medic (Medicago lupulina L.). The effect on deep water uptake was assessed using non-destructive measurements of roots, soil water and tracers.
Water uptake occurred below 1.7 m depth in 2016, and below 2.3 m depth in 2017 and contributed significantly to chicory water use. However, neither surface soil drying nor intercropping increased deep water uptake to relieve water deficit in the shoots.
Chicory benefits from deep-roots during drought events, as it acceses deep soil moisture unavailable to more shallow rooted species, yet deep water uptake was unable to compensate for the reduced topsoil water uptake due to soil drying or crop competition.
KeywordsCichorium intybus L. Deep water uptake Drought response Intercropping Hydrological tracer
Minimizing water limitation during growth of agricultural crops is crucial to achieve full yield potential. Crop yield losses vary according to the timing and severity of water limitations, but even short-term drought can be a major cause of yield losses (Zipper et al. 2016). Deep-rooted crops can potentially utilize otherwise inaccessible deep-water pools as a source of water for transpiration during periods where crop production is water limited. In areas where precipitation is sufficient to rewet the soil profile during a wet season, more shallow-rooted crops still experience water limitation during the growing season, as they do not have access to the water stored deeper in the profile.
The potential influence of deep roots on water uptake has been highlighted numerous times (e.g. Canadell et al. 1996; Lynch and Wojciechowski 2015), yet information about the contribution of deep roots to water uptake remains scarce. Maeght et al. (2013) suggest that this is related to the absence of tools to measure deep root activity with sufficient throughput and standardization at affordable costs, and to the widespread assumption that as deep roots only represent a small fraction of the overall root system, their contribution to root system function is marginal. Deep root growth under field conditions has been suggested to be restricted by high soil strength, and unfavourable conditions such as e.g. hypoxia, acidity, and low nutrient availability, to substantially benefit the crop (Lynch and Wojciechowski 2015; Gao et al. 2016).
While some soils can restrict deep root growth, others allow roots to grow in the deeper soil layers (Sponchiado et al. 1989; Thorup-Kristensen and Rasmussen 2015). In addition, even though the majority of the root biomass is found in the topsoil, deep roots can contribute significantly to water supply in crops, as there is little connection between root biomass and root activity (Mazzacavallo and Kulmatiski 2015). Gregory et al. (1978) found that in the field, winter wheat had less than 5% of its root biomass below 1 m depth, and as long as the water supply was sufficient in the 0–1 m layer, the biomass reflected the water uptake well. However, when the topsoil dried, the roots between 1 and 2 m depth supplied the plants with up to 20% of the total water use. It has also been demonstrated that relatively small amounts of subsoil water can be highly valuable to wheat grain yield under moderate post-anthesis drought stress (Kirkegaard et al. 2007).
Indirectly, deeper root growth in crops has also been associated with deep-water uptake, as rooting depth has been shown to correlate positively with yield under drought in the field in wheat (Lopes and Reynolds 2010), bean (Sponchiado et al. 1989; Ho et al. 2005), rice (Uga et al. 2013) and maize (Zhu et al. 2010). In addition, modelling studies indicate that selection for deeper roots in grain crops could significantly improve deep-water acquisition and yield in dry seasons (Manschadi et al. 2006; Lilley and Kirkegaard 2011). Common to most of these studies is that deep root growth is considered to be in the range of 0.5 to 2 m depth. But several agricultural crops have the capability to grow roots below 2 m depth or even deeper within a season (Canadell et al. 1996; Ward et al. 2003; Thorup-Kristensen 2006; Rasmussen et al. 2015), and thereby access an extra pool of water originating from wet season surplus precipitation stored in the soil. For example, lucerne has shown to decrease the soil water content at 5 m depth (Fillery and Poulter 2006).
Hydrological isotope tracer techniques have over the last two decades become an increasingly popular tool to acquire information on temporal and spatial water use patterns in plants (e.g. Bishop and Dambrine 1995; Peñuelas and Filella 2003; Beyer et al. 2016). Injection of tracer into specific soil depths has proven to be a precise method to detect the relative water uptake from the chosen depth (Kulmatiski et al. 2010; Kulmatiski and Beard 2013; Bachmann et al. 2015; Beyer et al. 2016). The hydrological tracer techniques utilize the fact that no isotopic fractionation against isotope forms of hydrogen or oxygen occurs during soil water uptake by roots (Wershaw et al. 1966; Dawson and Ehleringer 1991; Bariac et al. 1994; Mensforth and Walker 1996).
The anthropocentric discussion of the importance of deep root growth for crop production is put into perspective by the fact that some plant species have evolved the potential to grow deep roots. Under what circumstances is that strategy beneficial? In this study, we hypothesize that deep root growth can help plants escape topsoil drought. Using chicory as a case study species, we aimed to test the following hypotheses; 1) Chicory can grow roots below 3 m depth within a single growing season. 2) Chicory has significant water uptake from the deeper part of the root zone despite low root intensity. 3) When chicory is exposed to either topsoil drying or resource competition from shallow-rooted species, deep water uptake can increase to compensate for the decreased topsoil water uptake.
Chicory is commonly grown in pasture mixtures for animal fodder or as a cash crop to produce chicons. It is known to be able to reach at least 2.5 m depth (Thorup-Kristensen and Rasmussen 2015) and to be drought resistant (Monti et al. 2005; Skinner 2008; Vandoorne et al. 2012a). To test the hypotheses, we grew chicory as a sole crop and in an intercrop with two shallow-rooted species – ryegrass (Lolium perenne L.) and black medic (Medicago lupulina L.) in 4 m deep rhizotrons. We allowed extensive root development before imposing a drought, as our focus was on the potential of deep roots to acquire water during drought, rather than on deep root growth during drought.
Materials and methods
Main characteristics of the soil used in the rhizotrons
Organic mattera (%)
Fine sand (%)
Coarse sand (%)
We constructed rainout shelters to control water supply. In 2016, we covered the soil in the drought stressed treatment with a transparent tarpaulin that had a hole for each plant stem. The tarpaulins were stretched out and fixed with a small inclination to let the water run off. It turned out that this design failed to keep out water during intense precipitation events, which happened twice during the season. In 2017, we designed barrel roof rainout shelters instead, using the same clear tarpaulin and placed them on all rhizotrons. The rain-out shelters were open at the ends and on the sides to allow air circulation but were wider than the rhizotrons to minimize the water that reached the chambers during precipitation under windy conditions. The barrel roof rainout shelters covered all treatments.
We installed a drip irrigation pipe (UniRam™ HCNL) with a separate tap in each chamber. The pipe supplied 5 l hour−1, equivalent to 14 mm hour−1 according to the surface area of the growth chambers.
We had two treatments in 2016 and four in 2017. In both years we grew chicory (C. intybus L., 2016: cv. Spadona from Hunsballe frø. 2017: cv. Chicoree Zoom F1 from Kiepenkerl) in monoculture under well-watered (WW) and drought stressed (DS) conditions. In 2017, we also grew chicory intercropped with either ryegrass (L. perenne L.) or black medic (M. lupulina L.), both in a WW treatment. For chicory, we chose to work with a hybrid vegetable type cultivar in the second year to reduce the variation among plants in size and development speed observed in the forage type used the first year. In 2016, we transplanted four chicory plants into each chamber. In 2017, we increased the number to six in order to reduce within-chamber variation. For the two intercrop treatments in 2017, we transplanted five plants of ryegrass or black medic in between the six chicory plants.
Timeline of the experiments in 2016 and 2017
Onset of drying out
H2 tracer study
Water uptake calculations
We grew all treatments in three randomized replicates. The soil inside the six chambers not used for the experiment in 2016 but included in 2017 had also sunken during the 2015/2016 winter and the same procedure was used to top up soil in these chambers before transplanting the chicory plants.
In 2016, we fertilized all chambers with NPK 5–1-4 fertilizer equivalent to 100 kg N ha−1, half on 1 April and the other half on 21 June. In 2017, we fertilized all chambers on 3 May and 1 June following the same procedure.
In 2016, we pruned the plants at 0.5 m height, several times between 24 May and 12 July to postpone flowering and induce leaf and root growth.
We started drying out the DS treatments on 26 June in 2016 and on 13 July in 2017, where we stopped irrigation and mounted the rainout shelters. In 2016, we repeatedly irrigated the WW treatments. In 2017, where the rainout shelters excluded precipitation in all chambers we repeatedly irrigated all treatments apart from the DS. However, we chose to supply the same amount of water in all the irrigated chambers, which led to different levels of soil water content. We irrigated regularly to ensure sufficient water supply.
Biomass and 13C
We harvested aboveground biomass on 28 July in 2016 and on 11 September in 2017. We dried the biomass at 80 °C for 48 h. Belowground biomass could not be harvested, as the plants were used for further experiments after regrowth. The biomass was analysed for 13C/12C ratio on an elemental analyser interfaced to a continuous flow isotope ratio mass spectrometer (IRMS) at the University of California Stable Isotope Facility (Davis, California, USA). Isotope values are expressed in delta notation (δ) in per mill [‰] following the definition of Coplen (2011):
where Rsample is the ratio of the less abundant to the more abundant isotope (13C/12C) in the sample and Rstandard the ratio in a standard solution. For δ13C the international standard Vienna PeeDee Belemnite (Rstandard = 11180.2 × 10−6) was used. Analytical precision (σ) was 0.2‰.
The 13C/12C ratio in plants is directly related to the average stomatal conductance during growth, as discrimination between 12CO2 and 13CO2 during photosynthesis is greatest when stomatal conductance is high. When stomates are partially or completely closed, a greater part of the CO2 inside the leaf is absorbed resulting in less fractionation and thereby higher δ13C values of the plant tissue (Farquhar and Richards 1984; Farquhar et al. 1989).
We documented the development in root growth by taking photos of the soil-rhizotron interface through the transparent acrylic glass panels. For this purpose, we designed a “photo box” that could be slid on the metal rails in place of the foamed PVC panels, and thereby excluded the sunlight from the photographed area. We placed a light source consisting of two bands of LED’s emitting light at 6000 K in the photo box. We used a compact camera (Olympus Tough TG 860). For each 1.2 m wide panel we took four photos to cover the full width of the panel. We photographed the roots on 21 June and 18 July 2016 and on 6 July, 16 August and 12 September 2017, corresponding to the time of drought initiation in the DS treatment, 2H tracer injection (see below) and for 2017, harvest. In 2017, harvest was postponed until 20 days after the 2H tracer-experiment, due to measurements of nutrient uptake later in the season (Rasmussen et al. 2019)
We recorded the roots using the line intersects method (Newman 1966) modified to grid lines (Marsh 1971; Tennant 1975) to calculate root intensity, which is the number of root intersections m−1 grid line in each panel (Thorup-Kristensen 2001). To make the counting process more effective we adjusted the grid size to the number of roots, i.e. we used coarser grids when more roots were present and finer grids for images with only a few roots. This is possible because root intensity is independent of the length of gridline. We used four grid sizes: 10, 20, 40 and 80 mm. To minimize the variance of sampled data we used grid sizes that resulted in at least 50 intersections per panel (Ytting 2015).
Soil water content
We installed time-domain reflectometry sensors (TDR-315/TDR-315 L, Acclima Inc., Meridian, Idaho) at two depths to measure volumetric water content (VWC) in the soil. In 2016, the sensors were installed at 0.5 and 1.7 m depth. In 2017, the sensors were installed at 0.5 and 2.3 m depth. Soil water content was recorded every 5 min in 2016 and every 10 min in 2017 on a datalogger (CR6, Campbell Scientific Inc., Logan, Utah). Discrepancies in measured VWC among the sensors at field capacity (FC) let us conclude that the sensors were precise but not particularly accurate, meaning that the change over time in VWC was reliable but not the measured actual VWC. We have therefore estimated a sensor reading for each sensor at FC and reported changes in VWC from FC. We estimated FC as the mean VWC over a 48-h interval after wetting. In 2017, the measurement was made in the autumn after excess water from a heavy rainfall had drained. In the autumn, there is little evaporation and no plant transpiration to decrease VWC below FC, making it an optimal time to estimate FC. We did not have data from autumn 2016, so instead, we estimated FC in early spring.
We estimated water uptake from the VWC readings. We assume that water movement in the soil is negligible when VWC is below FC. Hence, the decrease in VWC can be interpreted as plant water uptake. Water uptake is therefore estimated as the mean decrease in VWC over a given time interval. We attempted to use intervals corresponding to the time of the 2H tracer studies. In 2016, the interval was a postponed a few days and in 2017, the time interval did not cover the first two days of the tracer study.
For the period from onset of drought to harvest 2017, we tested whether the daily water uptake at 2.3 m depth was affected by daily mean VWC at 0.5 m depth across all treatments. For this period, the VWC at 2.3 m depth was close to FC in all treatments and therefore the water content in 2.3 m itself was unlikely to affect the water uptake. As transpiration demand is high at this time of the year and plants are large, we assumed that topsoil water limitations would limit total water uptake unless it is balanced by an increased water uptake lower in the profile. We excluded days in which the chambers were irrigated and one day after irrigation events to exclude periods with large soil water movement.
We used 2H labeled water injected into 2.3 m depth to trace water uptake from this depth. We mixed 90% 2H2O tracer with tap water 1:1, to achieve an enrichment of δ 5,665,651 ‰ and injected 100 ml per chamber. We removed one of the acrylic panels in each chamber temporarily to allow tracer injection and distributed it over 100 injection points in the soil. The injections were made at two horizontal rows of each 10 equally distributed holes 5 cm above and below 2.3 m depth respectively. In each of these 20 holes, we injected 5 ml tracer distributed between five points: 5, 10, 15, 20 and 25 cm from the horizontal soil surface. Tracer injection was made on 19 July 2016 and 15 August 2017.
We captured the tracer signal by collecting transpiration water using plastic bags. For studies using tracers, collecting transpiration water is considered valid, as the tracers increase the enrichment level several orders of magnitudes, which make the fractionation negligible (Thorburn and Mensforth 1993; Beyer et al. 2016). We sampled the transpiration water one day before tracer injection as a control and one, two, three, four and six days after in 2016, and three and six days after in 2017. We fixed a plastic bag over each plant with an elastic cord that minimized air exchange with the surroundings. Transpiration water condensed on the inside of the plastic bag, which was folded inwards under the elastic cord to create a gutter for the water drops. Plastic bags were mounted on the plants two hours before noon and removed at noon.
We removed the plastic bags one by one, shook them to unite the drops, and transferred each sample to a closed plastic beaker. Later we filtered the samples through filter paper to remove soil and debris contamination and transferred the samples to glass vials.
We collected water from all plants and in most cases mixed the individual plant samples before analysis. Plastic bags could not be removed without a certain loss of water, thus the total water collected was not a measure of total transpiration. Therefore we chose to mix equal amounts of water from each sample. Day 2 in 2016 and day 6 in 2017, we analysed the samples from each plant separately to get data on within chamber variation.
The samples were analysed for 2H at Centre for Isotope Research, University of Groningen, The Netherlands on a continuous flow isotope ratio mass spectrometer (IRMS, Isoprime 10) combined with a chromium reduction system (Europa PyrOH, Gehre et al. 1996).
Isotope values are expressed in delta notation (δ) as given in eq. 1. Rsample is the 2H/1H ratio in the sample and Rstandard for δ 2H is Vienna standard mean ocean water (Rstandard ≈ 1/6412). Analytical precision (σ) was 0.7 ‰.
In order to identify whether tracer was present in a sample, we adapted the criteria proposed by Kulmatiski et al. (2010). If a sample had a δ 2H-value at least two standard deviations higher than the control samples, tracer was assumed to be present.
Data analyses were conducted in R version 3.4.4 (R Core team 2018). The effect of treatment on aboveground biomass of chicory, black medic and ryegrass was tested in a mixed effects one-way ANOVA. Separate harvest of single plants allowed the inclusion of chamber as random effect to account for the fact that the two intercropped species are not independent.
The effect of soil depth and treatment on root intensity was tested in a mixed effects two-way ANOVA. We included chamber as random effect to account for the fact that the different depths are not independent. To meet assumptions of normality, depths where at least one of the treatments had no roots in any of the replicates, were excluded from the model. Separate analyses were made for each date.
The effect of soil depth and treatment on water uptake during a given time interval was tested in a mixed effect three-way ANCOVA with time as covariate. In 2016, we excluded the sensors from one replicate of the DS treatment because water reached it during a cloudburst. In 2017, we excluded two of the sensors at 0.5 m depth from the analysis, one in a chicory and ryegrass intercrop treatment and one in a chicory and black medic intercrop treatment. The first due to noise in the readings and the second due to readings showing a pattern in VWC that did not resemble the pattern of any of the other sensors.
The effect of treatment and time on 2H concentration in transpiration water was tested in a mixed effect two-way ANOVA. We log-transformed the response variable to meet the assumptions of homoscedasticity.
The effect of treatment on δ13C was tested in a one-way ANOVA. For 2017, the model is a mixed effects model because samples for each plant were analysed separately.
In all cases, separate analyses were made for each year. All models met the assumptions of normality and homoscedasticity. Differences were considered significant at P < 0.05. Tukey test P-values for pairwise comparisons were adjusted for multiplicity, by single step correction to control the family-wise error rate, using the multcomp package (Hothorn et al. 2008). For root intensity, we decided to control the family-wise error rate for each root depth. For the 2H concentration, we only made pairwise comparisons for the last date.
Plants grew well in both years, and as hypothesized, roots were observed below 3 m depth by the end of the growing season. Both the uptake of 2H tracer and sensor readings showed that chicory acquired water from 2.3 m depth. However, our results do not suggest that compensation takes place, i.e. deep water uptake was not increased to balance the decreased topsoil water uptake during drought.
Root growth showed a similar pattern across the four treatments; however intercropping decreased total root intensity down to around 2 m depth (only significant in few depths), except for 0.11 m depth, where the chicory and ryegrass intercrop treatment had a significantly higher root intensity than the other treatments. Roots of intercropped species could not be distinguished and the reported root intensities are thus the sum of two species in the intercrop treatments. The month-long summer drought did not influence root intensity in any depths.
Soil moisture and water uptake
Although chicory WW and the two intercrop treatments in 2017 received the same amount of water, less water reached the sensors at 0.5 m in the chicory and black medic intercropping than in the WW and the chicory and ryegrass intercropping. This indicates that the soil above the sensors was drier and therefore could withhold more water compared to the two other irrigated treatments. At the time of the tracer-experiment, soil water content under the chicory and black medic intercropping was similar to the DS treatment, which was lower in comparison to two other treatments (Fig. 4c and d).
We did not find any effect of mean daily soil VWC at 0.5 m depth on water uptake at 2.3 m depth, giving no indication of compensatory deep water uptake (Data not shown).
In 2016, the 2H concentration in chicory plants in the DS treatment tended to be higher compared to the WW treatment, but the difference was not significant. In 2017, no differences were seen in tracer concentration among chicory plants across the treatments. Black medic and ryegrass plants revealed significantly lower 2H enrichment in comparison to intercropped chicory.
Deep root growth
In accordance with our hypothesis, chicory demonstrated its capability to grow roots below 3 m depth and did so within 4.5 months. However, root intensity decreased markedly below 2 m in 2016 and below 2.5 m depth in 2017. The root intensity below 2 m depth at drought initiation, 2.5 m depth at tracer injection and 3.5 m depth at harvest in 2017 was very low and could be a result of roots from the 2016 crop still visible on the rhizotron surface. Studies covering a longer growing season have found extensive root growth in chicory down to 2.5 m, where equipment limitations prevented observations deeper down (Thorup-Kristensen 2006; Thorup-Kristensen and Rasmussen 2015). In the field, factors such as high soil strength (Stirzaker et al. 1996; Gao et al. 2016), biopores (Han et al. 2015), and hypoxia might restrict deep root growth, which is less likely in our facility with drained repacked soil. However, we did use field soil with a soil bulk density comparable to field soils.
Both intercrop treatments decreased total root intensity especially from 0.5 to 2 m depth. This has to be seen in the light of a total aboveground biomass that was twice as high as in the WW sole crop treatment. Observing that chicory biomass, on the other hand, was reduced to almost half when intercropped, suggests that both black medic and ryegrass had much lower root intensity below 0.3 m depth than sole cropped chicory and that the interspecific competition reduced both above- and belowground growth of chicory. Black medic and ryegrass are both shallow rooted and are unlikely to reach below 1 m depth (Kristensen and Thorup-Kristensen 2004; Thorup-Kristensen and Rasmussen 2015), thus the deep roots observed in the intercrop treatments are assumed to be chicory roots.
Deep water uptake
The sensors documented water uptake in both treatments from 1.7 m depth in 2016 and 2.3 m depth in 2017. In fact, the sensors showed that in the WW treatment in 2016, chicory water uptake at 1.7 m depth was c. 30% of its water uptake at 0.5 m depth. In 2017, chicory water uptake at 2.3 m depth was c. 10% of its uptake at 0.5 m depth when well-watered. In absolute terms, water uptake from 1.7 m depth in 2016 was in the range of 1.5 mm m−1 soil column day−1 and from 2.3 m depth in 2017, it was 0.5 mm m−1 soil column day−1. Due to the small-sized plot placed at a windy position at 4 m height, evapotranspiration have certainly been substantially higher than the potential evapotranspiration measured nearby of 3.3 and 2.1 mm day−1 for the same periods in 2016 and 2017 respectively. Crop plants in the field provide wind protection for each other thereby reduce the evapotranspiration. Still it is clear that the water uptake from the deeper part of the root zone substantially contributed to the total plant water balance.
The 2H tracer uptake by chicory from 2.3 m depth both years support the sensor-based water uptake calculations. Furthermore, the tracer study confirmed that neither black medic nor ryegrass had roots deep enough to acquire water from 2.3 m depth. This is a clear example of resource complementarity in root competition in intercropping (Tilman et al. 2001; Postma and Lynch 2012).
Response to water stress and intercropping
Water uptake from 0.5 m depth was significantly reduced in the DS treatment compared to the WW treatment indicating that the soil water potential was low enough to limit plant water uptake in the DS treatment. Contrary to our expectations, we did not find a higher water uptake neither at 1.7 m depth in 2016 nor at 2.3 m depth in 2017 when plants were water limited in the topsoil. As biomass was not significantly reduced, whereas water uptake was reduced by 59 and 74%, the reduction in water uptake cannot be explained by a reduced water need. Both years the drought had little effect on aboveground biomass. The drought was initiated late in the season after chicory had established its aboveground biomass and concluded aboveground biomass accumulation in favour of belowground biomass accumulation in the taproot. For this reason, aboveground biomass is not a good indicator of the severity of the drought. On the other hand the equal biomass in the WW and DS treatments secured equal water uptake potential in the two treatments, and thereby revealed that the drought increased the water use efficiency, as less water was taken up per aboveground biomass in the DS than in the WW treatment.
Although not significant, the 2H tracer study indicated a higher 2H concentration in the transpiration water in the DS compared to the WW treatment in 2016. This suggests a higher relative water uptake from 1.7 m depth. A higher relative uptake from a certain depth can logically be explained by an increase in water uptake from the given depth, a decrease in water uptake somewhere else in the soil profile or a combination of both. As the water uptake based on the sensor calculations show a significantly lower water uptake from 0.5 m depth in the DS than in the WW treatment in 2016, it is likely that what we observed was the effect of decreased uptake in the topsoil.
We only observed a significant increase in 13C concentration in chicory when intercropped with black medic. Samples were taken from the total aboveground biomass, and not from plant parts developed during the drought, which might explain why the treatment effects were only captured in the chicory and black medic intercropping, where black medic appeared to have induced drought stress in chicory before onset of the drought stress we induced.
Intercropping reduced total root intensity at 0.5 m depth by over 40%. Still, water uptake from this depth was only slightly decreased indicating that the lower root intensity did not restrict water uptake in well-watered conditions. Root density in upper soil layers of well-established crops does not correlate well with water uptake (Anblin and Tennant 1987; Katayama et al. 2000), which can be explained by the high mobility of water in the soil, making a dense root system superfluous. Following the logic behind Walter’s two-layer hypothesis (Walter 1939, 1971; Walker and Noy-Meir 1982), intercropping would lead to a vertical niche partitioning resulting in increased water uptake by the deep-rooted chicory when intercropped with a shallow-rooted species. However, we did not observe an increase in deep water uptake.
Absence of a deep water compensation effect
We suggest three possible explanations for why we did not observe the hypothesized increase in deep water uptake during drought or intercropping.
1) The hydraulic resistance is too high to increase deep water uptake. Theoretically, the ability of root systems to extract water from deep roots depends not only on root system depth but also on root system hydraulics (Javaux et al. 2013). Root hydraulic conductivity limits the potential water uptake, and differs among species, but also among different roots in a root system (Ahmed et al. 2018; Meunier et al. 2018). The ability of a root system to compensate, i.e. extract water where it is easily available, for instance from deeper soil depths, is, therefore, a function of (1) the xylem conductance between the roots in the extraction zone and the root crown and (2) the radial root conductance in the wet zone. Compensation has been observed in chicory below 0.6 m depth, but this was in a study allowing root growth down to only 1.5 m depth (Vandoorne et al. 2012a). In our experiment, the xylem conductance might simply have been too low in the deeper part of the root zone to allow compensation, possibly because the deep soil measurements were made in a zone with a low density of young roots (McCully 1995; Meunier et al. 2018). However, chicory had 31% fewer roots in the chicory and black medic intercropping than in the WW treatment at 2.3 m, with no reduction in water uptake, not supporting such a relationship between root density and water uptake.
2) Insufficient water supply in the topsoil induces root-to-shoot signalling causing stomatal closure, despite sufficient water supply in deeper soil layers. Signals by phytohormones like Abscisic acid (ABA), produced when parts of the root system are under low water potential, might reduce plant transpiration and consequently root water uptake also from deeper depths by triggering stomatal closure (Zhang and Davies 1990a, 1990b; Tardieu et al. 1992; Dodd et al. 2008). Split-root experiments, where one side of the root system is under low water potential, have found reduced stomata conductance, despite sufficient water supply (Blackman and Davies 1985; Zhang and Davies 1990b). However, experiments with vertical heterogeneity in soil water content yield ambiguous results (Puértolas et al. 2015; Saradadevi et al. 2016). The hormonal signalling during topsoil drying has not been tested for chicory. But chicory does show an isohydric behaviour, decreasing stomatal conductance and maintaining leaf water potential during moderate drought stress (Vandoorne et al. 2012b).
3) Deep water uptake compensation might have occurred, but was not captured in this experimental set-up. Water uptake compensation could have happened between or below the depths covered by the sensors. At the end of the drought in 2016, VWC was not only lower at 0.5 m depth in the DS treatment compared to the WW treatment but also in 1.7 m depth, which could have impaired the water uptake from this depth, too. There is however, no indication of an increasing water uptake from 1.7 m at any point in time during the drought. As the soil is drying out from the top, the depth of a possible compensation would at some point have been at exactly 1.7 m, which was not the case.
Water uptake could also have been confounded with water redistribution in the soil column, leading to an underestimation of water uptake in depths where water is moving to, and an overestimation in depths where water is moving from. We however assume that the water redistribution is small compared to the daily water uptake, and thus can be neglected.
In summary, chicory can grow roots down to 3 m depth within 4.5 months and benefit from a significant water uptake from below 2 m depth both during well-watered and drought conditions. Our study highlights the benefit of deep root growth for crop water uptake, but questions whether further compensation in deep water uptake takes place when water is limited in the topsoil. A compensation might however, be pronounced for other crop species or for crops which have had more time to establish a deep root system.
We thank statisticians Signe Marie Jensen and Helle Sørensen for advice regarding the statistical data analyses, technician Jason Allen Teem for his contribution to the experimental work, student helper Sunniva Melhus for counting roots and Engineer’s assistant Sebastian Nielsen for building the photo box and for constructive discussions on the design of it. All are affiliated with University of Copenhagen. We thank Villum Foundation (DeepFrontier project, grant number VKR023338) for financial support for this study.
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