scholarly journals The Growth Response of Pasture Brome (Bromus valdivianus Phil.) to Defoliation Frequency under Two Soil-Water Restriction Levels

Agronomy ◽  
2021 ◽  
Vol 11 (2) ◽  
pp. 300
Author(s):  
Javier García-Favre ◽  
Ignacio F. López ◽  
Lydia M. Cranston ◽  
Daniel J. Donaghy ◽  
Peter D. Kemp

Pasture brome (Bromus valdivianus Phil.) has the potential to increase current levels of herbage production and pasture persistence in New Zealand dryland, well-drained soils. However, there is little literature on the effect of defoliation management on growth of this grass under contrasting soil-water restriction levels. The growth physiology and performance of pasture brome were evaluated in pots in a glasshouse. Defoliation frequency (DF) treatments were applied based on three different accumulated growing degree-days (AGDD): 250, 500 and 1000 AGDD (high, medium, and low DF). At end of the first growing cycle (1000 AGDD), water availability was restricted to 20–25% of field capacity (FC) in half of the pots, while the other pots were maintained between 80–85% FC. Total accumulated herbage mass was positively related with the low DF and well-watered conditions (p < 0.05). At the final harvest, plants subjected to low DF had greater root mass than high and medium DF (p < 0.05). At each harvest, the leaf regrowth stage (LS) for low DF was 3.5, while for high and medium DF, the LS was 1.5 and 2.0; respectively. Tiller water-soluble carbohydrates were highest at the low DF and under 20–25% FC. Regardless of soil-water conditions, defoliation at 3.5 LS supports production, enhancing survival during a drought.

Agronomy ◽  
2021 ◽  
Vol 11 (7) ◽  
pp. 1333
Author(s):  
Javier García-Favre ◽  
Yongmei Zhang ◽  
Ignacio F. López ◽  
Daniel J. Donaghy ◽  
Lydia M. Cranston ◽  
...  

Bromus valdivianus Phil. (Bv) is a water stress-tolerant species, but its competitiveness in a diverse pasture may depend on defoliation management and soil moisture levels. This glasshouse study examined the effect of three defoliation frequencies, based on accumulated growing degree days (AGDD) (250, 500, and 1000 AGDD), and two soil water levels (80–85% of field capacity (FC) and 20–25% FC) on Bv growth as monoculture and as a mixture with Lolium perenne L. (Lp). The treatments were applied in a completely randomised block design with four blocks. The above-ground biomass of Bv was lower in the mixture than in the monoculture (p ≤ 0.001). The Bv plants in the mixture defoliated more infrequently (1000 AGDD) showed an increase in root biomass under 20–25% FC compared to 80–85% FC, with no differences measured between soil water levels in the monoculture. Total root length was highest in the mixture with the combination of infrequent defoliation and 20–25% FC. Conversely, frequent defoliation treatments resulted in reduced water-soluble carbohydrate reserves in the tiller bases of plants (p ≤ 0.001), as they allocated assimilates mainly to foliage growth. These results provide evidence that B. valdivianus can increase its competitiveness relative to Lp through the enhancement of the root growth and the energy reserve in the tiller base under drought conditions and infrequent defoliation in a mixture.


Agronomy ◽  
2021 ◽  
Vol 11 (10) ◽  
pp. 2058
Author(s):  
Iván P. Ordóñez ◽  
Ignacio F. López ◽  
Peter D. Kemp ◽  
Daniel J. Donaghy ◽  
Yongmei Zhang ◽  
...  

The increase in drought events due to climate change have enhanced the relevance of species with greater tolerance or avoidance traits to water restriction periods, such as Bromus valdivianus Phil. (B. valdivianus). In southern Chile, B. valdivianus and Lolium perenne L. (L. perenne) coexist; however, the pasture defoliation criterion is based on the physiological growth and development of L. perenne. It is hypothesised that B. valdivianus needs a lower defoliation frequency than L. perenne to enhance its regrowth and energy reserves. Defoliation frequencies tested were based on B. valdivianus leaf stage 2 (LS-2), leaf stage 3 (LS-3), leaf stage 4 (LS-4) and leaf stage 5 (LS-5). The leaf stage development of Lolium perenne was monitored and contrasted with that of B. valdivianus. The study was conducted in a glasshouse and used a randomised complete block design. For Bromus valdivianus, the lamina length, photosynthetic rate, stomatal conductance, tiller number per plant, leaf area, leaf weights, root growth rate, water-soluble carbohydrates (WSCs) and starch were evaluated. Bromus valdivianus maintained six live leaves with three leaves growing simultaneously. When an individual tiller started developing its seventh leaf, senescence began for the second leaf (the first relevant leaf for photosynthesis). Plant herbage mass, the root growth rate and tiller growth were maximised at LS-4 onwards. The highest leaf elongation rate, evaluated through the slope of the lamina elongation curve of a fully expanded leaf, was verified at LS-4. The water-soluble carbohydrates (WSCs) increased at LS-5; however, no statistical differences were found in LS-4. The LS-3 and LS-2 treatments showed a detrimental effect on WSCs and regrowth. The leaf photosynthetic rate and stomatal conductance diminished while the leaf age increased. In conclusion, B. valdivianus is a ‘six-leaf’ species with leaf senescence beginning at LS-4.25. Defoliation at LS-4 and LS-5 was optimum for plant regrowth, maximising the aboveground plant parameters and total WSC accumulation. The LS-4 for B. valdivianus was equivalent to LS-3.5 for L. perenne. No differences related to tiller population in B. valdivianus were found in the different defoliation frequencies.


1993 ◽  
Vol 73 (1) ◽  
pp. 51-59 ◽  
Author(s):  
D. A. Angers ◽  
N. Samson ◽  
A. Légère

Crop rotations and tillage practices can alter the structure of die soil through their effects on soil disturbance and mixing and on organic matter (OM) accumulation and mineralization. The objective of this study was to determine the changes in soil water-stable aggregation induced by 4 yr of different rotation and tillage practices on a Kamouraska clay at La Pocatière, Quebec. The influence of soil water content (WC) at time of sampling and of different biological and biochemical properties on soil aggregation was also examined. Two rotations (continuous barley (Hordeum vulgare L.) vs. a 2-yr barley–red clover (Trifolium pratense L.) rotation) and three tillage treatments (moldboard plowing (MP) chisel plowing (CP) and no-tillage (NT)) were compared in a split-plot design. Measurements of the size distribution of water-stable aggregates were made on surface (0–7.5 cm) soil samples taken periodically during the 4-yr period. Rotations had no effect on soil aggregation. The mean-weight diameter (MWD) of water-stable aggregates did not vary significantly with time under the NT treatment during the study but decreased significantly under the MP and CP treatments. In the fourth growing season, MWD values in NT plots were on average 40% higher than in MP and CP plots, which were both similar. The larger values in MWD under NT were attributable to a larger proportion of aggregates > 2 mm at the expense of smaller ones (< 1 mm). The MWD data showed important temporal fluctuations, which could in part be explained by the effects of WC at time of sampling. This effect of WC on MWD was less apparent under NT, which suggested that these aggregates were less susceptible to slaking. Among different OM fractions, the proportion of organic C present as hot-water-soluble carbohydrates was best correlated with MWD. Key words: Soil management, aggregation, slaking


1996 ◽  
Vol 26 (1) ◽  
pp. 53-62 ◽  
Author(s):  
R.L. Rothwell ◽  
U. Silins ◽  
G.R. Hillman

Hydrologic drainage criteria that describe the position of the water table between adjacent ditches are commonly used to assess the initial effectiveness of peatland drainage projects for tree growth improvement. However, these criteria do not reflect the soil conditions that regulate tree growth and performance after drainage. The effect of three drainage ditch spacings (30, 40, and 50 m) on the spatial variability of soil water conditions at three drained boreal Alberta peatlands was studied. Soil water content (0–30 cm depth) was found to be insensitive (p = 0.686) to drainage ditch spacing several years after drainage. Greater variation was observed between different sampling locations (p = 0.024) relative to the position of the ditch edge within similar ditch spacings. Spatial distribution of soil water in the unsaturated zone was found to be inversely related to the degree of water table lowering. Spatial patterns of soil water content were strongly associated with changes to substrate bulk density resulting from post-drainage peatland subsidence.


1989 ◽  
Vol 37 (2) ◽  
pp. 83-95
Author(s):  
J. Ellen ◽  
H. van Oene

The effects of light intensity (129, 86 and 37 W/msuperscript 2) after spikelet initiation on development, yield and chemical composition were studied in spring barley cv. Trumpf under controlled conditions. Reducing the light intensity resulted in fewer shoots/plant, prolonged the leaf area duration, lowered the specific leaf wt and delayed shoot and ear development. The light intensity strongly influenced the number of aborted spikelets, the number of grains/ear and 1000-grain wt. During leaf, stem and ear development the content and amount of water-soluble carbohydrates (WSC) in leaves plus stems decreased. At the same time there was a strong increase in content and amount of cell-wall constituents (CWC), especially in leaves and stems. This implies that the formation of CWC requires a large consumption of WSC. Reducing the light intensity diminished the production of WSC and CWC appreciably. The percentage of WSC in stems at anthesis correlated well (r = 0.68) with the number of grains/ear at final harvest, calculated over main shoot, 1st and 2nd tillers. The high amount of WSC in the stems of the plants at the 2 highest light intensities at maturity implies an insufficient storage capacity in the grains. (Abstract retrieved from CAB Abstracts by CABI’s permission)


1998 ◽  
Vol 49 (7) ◽  
pp. 1095 ◽  
Author(s):  
A. F. van Herwaarden ◽  
R. A. Richards ◽  
G. D. Farquhar ◽  
J. F. Angus

Post-anthesis drought and heat shock have been implicated in previous studies as factors contributing to ‘haying-off’ in wheat, but their relative importance has not been investigated. To separate the effects, wheat plants were grown at 2 levels of nitrogen (N) and then exposed to different levels of post-anthesis water deficit in factorial combination with the presence or absence of heat shock. The growth, yield, leaf carbon exchange, water use, and the contents of protein and soluble carbohydrate were measured and compared with the field results reported in Papers I and II of this series. The experiment consisted of wheat plants (cv. Janz) grown in 1·2-m-long tubes outdoors through winter and spring in Canberra, with either nil or 240 kg N/ha applied. The tubes were supported in a refrigerated box to maintain temperatures representative of those of soil in the field, and arranged to form mini-canopies with a density of 29 plants/m2. After anthesis, half of the plants at both levels of N were watered according to their transpiration demand and the other half at 75% of demand to reduce gradually the store of soil water so that water deficit could be initiated at the same time as heat shock. Fifteen days after anthesis, different temperatures were imposed by moving half of the plants into an adjacent glasshouse where heat shock was imposed by raising the air temperature to maxima of ~35ºC for 3 days, to simulate the pattern of temperatures experienced in the field during a heat wave. During this time, the control plants experienced daily maxima of ~25ºC. Following the heat shock, all plants were placed outside and rewatered to enable the assessment of treatment effects on potential leaf function. Both water deficit and high temperature reduced assimilation. After these measurements were taken, well-watered control plants were irrigated according to transpiration demand and the plants with imposed water deficit were watered at 50% of this amount. Yields increased in response to N at both levels of water status and both levels of temperature. That is, there was no evidence of the haying-off reported in Papers I and II of this series. Two factors are proposed to account for the difference between the field crops and the plants grown in the mini-canopy here. Firstly, the pattern of soil-water use differed from the field studies reported in Paper I, with the high-N plants using more soil water than low-N plants during grain filling. Secondly, the level of water-soluble carbohydrates (WSC) in the tube-grown plants of high-N status was greater than that for plants of low-N status, which was opposite to the pattern for field-grown plants reported in Paper II. In addition, the concentrations of WSC in the tube-grown plants were higher than those in the field-grown plants, apparently because lower spike density allowed better penetration of light into the mini-canopies and led to greater assimilate storage than by the denser field crops. The results confirm the conclusion of Paper I that high temperature is not necessary for haying-off, although it is likely that it would worsen the haying-off caused by post-anthesis drought and low WSC reserves in the field. The absence of the haying-off response in this experiment was mostly because the supply of WSC from the sparse canopy was adequate to ofiset the reduction of assimilation due to water deficit and heat shock. A contributing factor to haying-off in the field may therefore be dense canopies resulting in low levels of WSC


2018 ◽  
Author(s):  
Yonge Zhang ◽  
Xinxiao Yu ◽  
Lihua Chen ◽  
Guodong Jia ◽  
Hanzhi Li

AbstractInvestigation of δ13C of leaf and twig phloem water-soluble organic material (WSOM) is a promising approach for analysis of the effects of environmental factors on plant performance. In this study, orthogonal treatments of three CO2 concentrations (Ca) × five soil water contents (SWC) were conducted using Platycladus orientalis saplings to investigate the interaction of water stress and CO2 concentration on δ13C of leaf and twig phloem WSOM. Under the lowest SWC, the δ13C of leaf and twig phloem WSOM had the most positive values at any Ca and their values decreased as Ca increased. However, at improved soil water conditions, the greatest values of δ13C of leaf and twig phloem WSOM were mostly observed at C600. In addition, a more significant relationship between SWC and δ13C of twig phloem WSOM than that between SWC and δ13C of leaf WSOM demonstrated that δ13C of twig phloem WSOM is a more sensitive indicator of SWC. Twig phloem WSOM was generally 13C-depleted compared with leaf WSOM for potential post-photosynthetic fractionation, and the 13C discrimination from leaves to twig phloem was insensitive to the interaction between SWC and Ca. Clearly, interacting effects play a more important role in photosynthetic fractionation than in post-photosynthetic fractionation.HighlightThe δ13C of leaf and twig phloem WSOM exhibited the most positive values at C400×35%–45% FC.Post-photosynthetic fractionation from leaf to twig was not be impacted by the interacting effects.


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