Crop row spacing and its influence on the partitioning of evapotranspiration by winter-grown wheat in Northern Syria

A study was conducted during the 1996–97 crop growth season at ICARDA in northern Syria, to investigate the influence of wheat canopy architecture on the partitioning of moisture between soil evaporation and crop transpiration, on a soil with high hydraulic conductivity. The study was conducted on the long-term two course wheat-lentil rotation trial, established on a swelling clay soil (Calcixerollic xerochrept). The wheat canopy architecture was manipulated by sowing the crop at either of two row-spacings, 0.17 or 0.30 m, both at a constant sowing rate equivalent to 120 kg ha^–1. In this study, evapotranspiration from the crop was inferred from changes in soil moisture content over time, evaporation and rainfall interception were measured daily using microlysimetry, drainage was estimated as being the difference between potential daily evapotranspiration, and the evapotranspiration estimated from the soil water deficit. Between sowing and day 80 (tillering stage), evapotranspiration was calculated to consist mainly of soil evaporation. However, after day 80, transpiration became an increasingly dominant component of evapotranspiration. For both row-spacings, cumulative evapotranspiration over the season was approximately 373 mm. In the narrow-row crop, transpiration and soil evaporation were approximately 185 mm and 183 mm of water respectively. Conversely for the wide row-spaced crop, 172 mm of water was transpired while about 205 mm of water evaporated from the soil surface. While green leaf area index did not differ between row-spacings, the architecture of the crops as a result of sowing affected solar radiation penetration such that more incident radiation was intercepted at the soil surface of the wide row-spaced crop. This is likely to have made some contribution to the elevated levels of evaporation from the soil beneath the canopy of the wide-sown crop.     

春小麦田喷灌的水量分布及小气候效应

春小麦喷灌的田间观测表明,在灌浆初期,春小麦冠层的截留水量可达25％－30％,冠层截留水量可使冠层下方的均匀系数比冠层上方提高10.1%-12.7%。喷灌的水分飘移蒸发损失可达总水量的20％－25％。春小麦喷灌可以降低空气和土壤温度,增加空气实际水汽压和相对湿度,这对抑制作物蒸腾将起一定作用。     

黄土旱塬区土壤水分状况与作物生长、降水的关系

土壤水分研究是统筹农业生产和生态环境建设的关键环节.本研究结合4年田间定位试验,通过对黄土高原南部长武旱塬冬小麦和春玉米2012—2015年土壤水分状况的研究,分析农田土壤干层形成情况、土壤水分对作物生长的影响、降水对土壤水库的影响以及作物对土壤水分状况的影响.结果表明: 降水年型是冬小麦地土壤干层形成的主导因素,年内降水分布不均是春玉米地土壤干层形成的主导因素.长武旱塬区冬小麦和春玉米一年一季的种植制度不会导致永久性干层的产生;相较于春玉米,冬小麦根系生长习性更符合黄土旱塬区土壤水分循环特征,黄土旱塬区土壤水分有效性可保证作物产量稳定;降水作用下,冬小麦土壤水库充、放水过程呈现收获期、休闲期和苗期连续充水、缓慢消耗期和大量消耗期连续失水相互交替的特点.0～300和300～600 cm土层土壤水库不一致性现象明显,以最大根深作为野外监测试验中土壤含水量的取样深度时,由于深层土壤水库负反馈作用,不同降水年型下,休闲期和苗期的蒸散均会被高估,缓慢消耗期和大量消耗期的蒸散均会被低估.冬小麦田间过渡层存在的范围为140～360 cm;作物生长的时间跨度影响土壤水库效应的发挥,土壤水库对冬小麦供水表现为年际间的调节作用,土壤水库对春玉米供水表现为季节间的调节作用.     

Plants as Sources of Airborne Bacteria, Including Ice Nucleation-Active Bacteria

Vertical wind shear and concentration gradients of viable, airborne bacteria were used to calculate the upward flux of viable cells above bare soil and canopies of several crops. Concentrations at soil or canopy height varied from 46 colony-forming units per m³ over young corn and wet soil to 663 colony-forming units per m³ over dry soil and 6,500 colony-forming units per m³ over a closed wheat canopy. In simultaneous samples, concentrations of viable bacteria in the air 10 m inside an alfalfa field were fourfold higher than those over a field with dry, bare soil immediately upwind. The upward flux of viable bacteria over alfalfa was three- to fourfold greater than over dry soil. Concentrations of ice nucleation-active bacteria were higher over plants than over soil. Thus, plant canopies may constitute a major source of bacteria, including ice nucleation-active bacteria, in the air.     

被动式夜间增温设施设计及其增温效果

为了建立一套简便节能的野外夜间增温设施,参照国际上夜间被动式增温系统（passive nighttime warming, PNW）,在江苏丹阳设计了稻麦系统夜间被动式增温设施.结果表明：该系统可以保证15.75 m²的有效采样区域,温度增幅均匀,水稻冠层全生育期夜间平均温度升高1.1 ℃,冬小麦冠层和5 cm土层全生育期夜间平均温度分别提高1.3 ℃和0.8 ℃;该增温系统在运行期间,水稻和冬小麦全生育期的冠层和土壤温度的日变化趋势与非增温对照区基本一致.该系统使麦田土壤含水量略微降低,但对小麦生长的影响不明显.将该系统在我国水稻和冬小麦主要产区应用时发现,该夜间增温系统可以使水稻和冬小麦始花期分别平均提前3 d和5 d.该系统的增温效果在不同区域和季节存在一定的差异,但综合考虑该系统的增温均匀性和增温区域有效性,及其对稻麦生育期的影响效果,该设施不仅节能,而且可以满足野外增温试验研究的基本要求.     

Recent biometeorological applications to crops

The paper demonstrates how standard climatological data can effectively be exploited by making use of biometeorological knowledge and modern data processing facilities in studies concerned with the evaluation of crop-weather relationships and the analysis of climatic resources. In analyzing potential biological yield of wheat at Normandin (Quebec), it was found that the potential yield was reduced by approximately 45% because of variations in temperature and radiation whereas the actual yield was reduced by 70%. In mesoscale analyses, the error between soil moisture observations and estimates from a climatological soil moisture budget was in the same order as the standard deviation of 3-times replicated 38 soil moisture samples taken over five years at Swift Current (Sask.). An analysis of crop-weather relationships at Lacombe (Alta.) indicated that the 1957 wheat yield was reduced from the potential 3,300 kg/ha to 2,004 kg/ha or by 40% because of a severe cold spell during the soft dough developing stage resulting in improper filling of the kernels. In macroscale analyses, relative winter hardiness indices for woody ornamental plants together with site suitability indices for winter survival were used in the development of a map of plant hardiness zones in Canada. In the application of this research to forage crops average winter survival percentage of legumes and grasses by classes of hardiness together with selected regional climatic averages were developed for six regions of southern Canada. Long-term research into the relationships between Canadian Prairie crop yields and development (wheat, oats and barley) and selected climatic and soil variables has been used successfully for estimating regional crop production, for determining climatic limitations of the area suitable for the cultivation of these crops, and for assessing the impact of postulated climatic changes on crop production.Contribution No 862 of the Chemistry and Biology Research Institute.     

耕层调控与有机肥处理下麦田土壤和小麦冠层结构特性及其相互关系

本研究基于5年的耕作定位试验,设置深耕(DT)、深耕有机肥(DTF)、浅耕(ST)、浅耕有机肥(STF)、免耕(NT)和免耕有机肥(NTF)处理,以期通过改良耕层土壤结构,优化小麦冠层结构特性.结果表明: 同一耕作处理下,增施有机肥可降低土壤容重、提高土壤孔隙度,提高20～40 cm土层2～5和0.25～2 mm粒级土壤团聚体含量,降低>5 mm粒级团聚体含量、>0.25 mm粒级团聚体的平均质量直径(MWD)和几何平均直径(GMD).与其他处理相比,NTF处理改善了0～20 cm土层土壤容重、增加土壤孔隙度;DTF处理降低了40～60 cm土壤容重和>0.25 mm粒级机械团聚体的稳定性,增加了土壤透气性.花后各时期,有机肥处理的叶片角度指数降低,叶面积指数(LAI)和旗叶净光合速率(P_n)提高.STF处理的角度指数最低,DTF处理的P_n最高,显著大于其他处理.通径分析表明,自变量容重、孔隙度、>0.25 mm粒级团聚体的数量(R_0.25)和MWD对因变量角度指数、LAI和P_n的直接通径系数均达到极显著水平.0～20 cm土层,MWD值增大有利于P_n和LAI的提高;20～40 cm土层,土壤容重在一定范围内的增加可优化叶夹角,提高冠层透光率;40～60 cm土层,高的土壤容重和低的孔隙度限制了LAI和P_n的增加.综上,豫中补灌区增施有机肥下的深耕或浅耕处理有利于改良土壤结构、增加土壤通透性,优化冠层结构,提高冠层受光率、叶面积指数和光合速率.     

不同耕作方式对陇中旱农区春小麦和豌豆根系空间分布及产量的影响

依托陇中旱农区长期的保护性耕作定位试验,对不同耕作方式下春小麦和豌豆根系空间分布特征及作物产量进行研究,以探索耕作措施影响作物产量的机制.结果表明: 随着生育期的推进,春小麦和豌豆的总根长、根表面积呈先增后减的趋势,开花期达到最大;春小麦根系苗期以0～10 cm最多,花期、成熟期10～30 cm最多;而豌豆根系苗期和成熟期均以0～10 cm最多,花期10～30 cm最多.免耕秸秆覆盖和免耕覆膜增加了根长和根表面积,春小麦和豌豆各生育时期的根长较传统耕作增加了35.9%～92.6%,根表面积增加了43.2%～162.4%.免耕秸秆覆盖和免耕覆膜优化了春小麦和豌豆根系分布,与传统耕作相比,增加了春小麦和豌豆苗期0～10 cm土层根长和根表面积分布比例,花期和成熟期深层次根系分布也显著增加,免耕秸秆覆盖在开花期30～80 cm土层根长和根表面积的分布比例分别比传统耕作提高了3.3%和9.7%.春小麦各生育期的总根长、根表面积与产量呈显著正相关,豌豆各生育期的总根长与豌豆产量呈极显著正相关.免耕秸秆覆盖和免耕覆膜较传统耕作春小麦和豌豆产量增加23.4%～38.7%,水分利用效率提高了13.7%～28.5%.在陇中旱农区,免耕秸秆覆盖和免耕覆膜可以增加作物根长和根表面积,优化了根系在土壤中的空间分布,增强作物根层吸收能力,从而提高作物产量和水分高效利用.     

Effects of wheat volunteers and blackgrass in set-aside following a winter wheat crop on soil infectivity and soil conduciveness to take-all

Two experiments were carried out in France in which disease indices were used to evaluate the effects of wheat volunteers and blackgrass (Alopecurus myosuroides) on soil infectivity and soil conduciveness to take-all caused by Gaeumannomyces graminis var. tritici. Soil infectivity was evaluated by measuring the disease index on susceptible wheat plants grown on soil samples collected from the field. Soil conduciveness to the disease was obtained by measuring disease indices on plants grown on soil samples to which different amounts of take-all fungus inoculum were added. One experiment (Expt. 1) was carried out using soils from farmers' fields (two fields in 1994 and two in 1995); soil infectivity and soil conduciveness were evaluated for three experimental situations: bare soil, soil with wheat volunteers and soil with blackgrass plants. In 1994 the soil infectivity was zero in bare soil, high with the wheat cover, and intermediate with the blackgrass cover. In 1995 the soil infectivity was uniformly low for all three conditions. Soils bearing wheat were less conducive than bare soil, soils bearing blackgrass and bare soils were similarly conducive. A second experiment (Expt. 2) carried out in 1995 compared the soil infectivity and soil conduciveness to take-all of soils planted with wheat or blackgrass in set-aside land after periods of wheat monoculture of 0–6 yr. The soil infectivity was low for all treatments. The soil was more conducive after blackgrass than after wheat. In both cases, the soil conduciveness was less when the monoculture had continued for more than 4 yr. The decline was less after blackgrass than after wheat. Thus, whenever set-aside is set up during the increase phase of the disease in fields with cereal successions, abundant wheat volunteers might hinder the expected positive effect of a break in cereal successions on take-all development. The presence of blackgrass in a set-aside field, with significant soil infectivity and high soil conduciveness, might increase the risks of take-all development in a wheat crop following set-aside.     

Stomatal control of transpiration from a developing sugarcane canopy

Abstract. Stomatal conductance of single leaves and transpiration from an entire sugarcane (Saccharum spp. hybrid) canopy were measured simultaneously using independent techniques. Stomatal and environmental controls of transpiration were assessed at three stages of canopy development, corresponding to leaf area indices (L) of 2.2, 3.6 and 5.6. Leaf and canopy boundary layers impeded transport of transpired water vapour away from the canopy, causing humidity around the leaves to find its own value through local equilibration rather than a value determined by the humidity of the bulk air mass above the canopy. This tended to uncouple transpiration from direct stomatal control, so that transpiration predicted from measurement of stomatal conductance and leaf-to-air vapour pressure differences was increasingly overestimated as the reference point for ambient vapour pressure measurement was moved farther from the leaf and into the bulk air. The partitioning of control between net radiation and stomata was expressed as a dimensionless decoupling coefficent ranging from zero to 1.0. When the stomatal aperture was near its maximum this coefficient was approximately 0.9, indicating that small reductions in stomatal aperture would have had little effect on canopy transpiration. Maximum rates of transpiration were, however, limited by large adjustments in maximum stomatal conductance during canopy development. The product of maximum stomatal conductance and L. a potential total canopy conductance in the absence of boundary layer effects, remained constant as L increased. Similarly, maximum canopy conductance, derived from independent micrometeorological measurements, also remained constant over this period. Calculations indicated that combined leaf and canopy boundary layer conductance decreased with increasing L such that the ratio of boundary layer conductance to maximum stomatal conductance remained nearly constant at approximately 0.5. These observations indicated that stomata adjusted to maintain both transpiration and the degree of stomatal control of transpiration constant as canopy development proceeded.     

华北平原冬小麦农田蒸散量

以华北平原冬小麦农田为研究对象,采用涡度相关技术和热红外遥感技术,研究了不同环境条件下土壤含水量与农田蒸散量及作物冠层温度的关系.结果表明,冬小麦在农田郁闭(LAI≥3)、晴天和土壤相对含水量低于田间持水量65%的情况下,蒸发比值日变化正午前后出现相对较低且平稳的变化趋势.在晴天情况下,农田潜热通量与作物冠层温度日变化和季节变化均呈极显著的非线性相关关系,而冠气温差、农田相对蒸散量则与0～100 cm土层的土壤相对含水量密切相关.以13:30～14:00的平均冠层温度值T_c、日最高气温T_{a max}和日净辐射总量Rn_d为统计数据,确立了冬小麦农田日蒸散量ET_d （mm）估算简化模式参数.     

Coordination of stomatal,hydraulic, and canopy boundary layer properties: Do stomata balance conductances by measuring transpiration?

A striking coordination is observed in sugarcane between prevailing levels of stomatal opening and the hydraulic capacity of the soil, roots and stem to supply the leaves with water. This coordination of vapor phase and liquid phase conductances is associated with decreases in stomatal conductance on a leaf area basis that compensate for increasing leaf area during canopy development, causing transpiration to approach a maximum value on a per plant or ground area basis rather than increase linearly with leaf area. The resulting balance between water loss and water transport capacity maintains leaf water status remarkably constant over a wide range of plant. sizes and growing conditions. These changes in stomatal conductance during development are determined by changes in the composition of the xylem sap rather than by changes in leaf properties. Changes in boundary layer conductance resulting from non-developmental changes in canopy structure such as loding cause additional changes in stomatal conductance mediated by altered humidity at the leaf surface. These maintain a constant level of total canopy vapor phase conductance (stomatal and boundary layer in series) and a constant level of canopy transpiration. These patterns indicate that stomata exert an active role in regulating transpiration even in dense canopies. This control function is consistent with stomatal metering of transpiration, mediated by fluxes of root-derived materials in the xylem sap.     

Elevated CO2 effects on canopy and soil water flux parameters measured using a large chamber in crops grown with free-air CO2 enrichment

An arable crop rotation (winter barley-sugar beet-winter wheat) was exposed to elevated atmospheric CO(2) concentrations ([CO(2) ]) using a FACE facility (Free-Air CO(2) Enrichment) during two rotation periods. The atmospheric [CO(2) ] of the treatment plots was elevated to 550 ppm during daylight hours (T>5°C). Canopy transpiration (E(C) ) and conductance (G(C) ) were measured at selected intervals (>10% of total growing season) using a dynamic CO(2) /H(2) O chamber measuring system. Plant available soil water content (gravimetry and TDR probes) and canopy microclimate conditions were recorded in parallel. Averaged across both growing seasons, elevated [CO(2) ] reduced E(C) by 9%, 18% and 12%, and G(C) by 9%, 17% and 12% in barley, sugar beet and wheat, respectively. Both global radiation (Rg) and vapour pressure deficit (VPD) were the main driving forces of E(C) , whereas G(C) was mostly related to Rg. The responses of E(C) and especially G(C) to [CO(2) ] enrichment were insensitive to weather conditions and leaf area index. However, differences in LAI between plots counteracted the [CO(2) ] impact on E(C) and thus, at least in part, explained the variability of seasonal [CO(2) ] responses between crops and years. As a consequence of lower transpirational canopy water loss, [CO(2) ] enrichment increased plant available soil water content in the course of the season by ca. 15 mm. This was true for all crops and years. Lower transpirational cooling due to a [CO(2) ]-induced reduction of E(C) increased canopy surface and air temperature by up to 2 °C and 0.5 °C, respectively. This is the first study to address effects of FACE on both water fluxes at canopy scale and water status of a European crop rotation.     

黑河地区绿洲生态条件下麦田生物气象若干特征

观测分析了ＨＥＩＦＥ地区绿洲中麦田的微气候特征,结果表明ＳＰＡＣ中水５势随高度呈显著梯度分布,在土壤－植物以及植物－大气界面,水势值存在两个大的跳跃;水势廓线存在明显的日变化;ＳＰＡＣ各部分水势变化的起伏顺序是大气〉植物〉土壤,说明水势变化受植物水分代谢进程直到气象因子的强烈影响和控制。冠层上方近地面风温湿的时间剖而显示出白天与夜晚相比,大气混合得较好。日出前则大气较为稳定。在典型晴天条件下,麦田     

开放式空气CO2浓度增高条件下旱地土壤气体CO2浓度廓线测定

设计了一套适合于FACE(free airCO2 enrichment)平台的旱地土壤气体CO2 浓度廓线测定方法 ,并将其应用于田间实验 .在江苏省无锡市郊区具有太湖地区典型水稻土的稻麦轮作农田 ,对FACE和对照麦田以及裸土 0～ 30cm土层的土壤气体CO2 浓度廓线进行了观测研究 .结果表明 ,所采用的方法满足进行旱地农田土壤气体CO2 浓度廓线研究的要求 ;在 0～ 30cm土层中 ,上层土壤气体中的CO2 向上垂直扩散要比下层土壤快 ;在作物旺盛生长期 ,大气CO2 浓度升高 2 0 0± 4 0 μmol·mol-1使 0～ 30cm土层的土壤气体CO2 浓度显著提高 14 %± 5 % (t 检验P <0 .0 0 1) .     

A mesoscale analysis of floristic patterns in the south-west Finnish Archipelago

Aim To identify the ecological gradients based on the flora on a mesoscale in an archipelago. To interpret the results of the ordination and the classification of a grid cell‐based botanical data set, with several environmental and geographical attributes. To compare the mesoscale distribution patterns of vascular plants with patterns previously observed on an island scale, and to develop a floristic zonation of the study area. Location The south‐west Finnish Archipelago. Methods Vascular plant species‐lists from over 1500 localities were assigned to 5 × 5 km grid cells. The grid cell‐based floristic data were subjected to both unconstrained [detrended correspondence analysis (DCA)] and constrained [detrended canonical correspondence analysis (DCCA)] gradient analyses. The results of DCA were interpreted with calculated weighted averages of Ellenberg's indicator values for vascular plants, the number of occurring taxa and indices for the strength of human influence and the occurrence of limestone. The results of DCCA were interpreted with geographical attributes of the grid cells and the occurrence of limestone. The grid cells were clustered using two‐way indicator species analysis (twinspan ). Results Both the unconstrained and the constrained ordinations gave consistent and interpretable results. The main ecological gradient runs from the grid cells containing species‐rich islands with high human impact to grid cells containing species‐poor islands with low human impact. This gradient also represents the continuum from areas with large islands near the mainland, to the outermost areas at the edge of the open sea. The secondary gradient was shown to be a gradient of soil reaction. twinspan gave a clustering primarily based on the location of the grid cells on an inner–outer archipelago gradient, but the occurrence of limestone also influenced the classification. The archipelago was divided into five non‐homogeneous areas based on the twinspan clusters. The detected gradients correspond well with the gradients detected in a similar island‐level analysis. Main conclusions The two major ecological gradients in the study area seem to be robust, which is indicated by the similar results obtained both on an island and on a mesoscale. A shift from local and regional processes to broader geographical gradients probably starts to occur at the applied scale. The distribution patterns are strongly affected by the inner–outer archipelago gradient and the occurrence of limestone.     

麦蚜和寄生蜂对农业景观格局的响应及其关键景观因子分析

大量研究表明多样性的农业景观格局能够影响蚜虫及寄生蜂的分布。本文利用并设计了两种尺度的麦田农业景观格局,依据麦蚜种群发生特点,分为迁入期、增长期与高峰期三个时期,论述了不同尺度下农业景观元素对麦蚜及寄生蜂系统的影响,通过逐步回归筛选了不同时期麦蚜及寄生蜂分布的关键景观元素,最后通过CANOCO软件模拟了麦蚜及寄生蜂的分布排序格局。结果表明不同景观因子对麦蚜及寄生蜂种群影响不同,迁入期两种尺度下裸地最有利于两种有翅蚜的迁飞入田,塑料大棚对有翅蚜种群的入田有抑制作用。增长期草地与林地生境对麦蚜种群增长率促进最大,塑料大棚同样抑制了麦蚜的种群增长率;但塑料大棚、草地与林地对蚜茧蜂的种群增长率有促进作用,非麦类作物生境对蚜茧蜂种群增长率抑制作用最大;草地与林地有利于重寄生蜂的种群增长率;高峰期裸地比例大的农业景观下麦蚜的最大种群密度较大,草地与林地对蚜茧蜂与重寄生蜂的最大种群密度均有促进作用。两种尺度下的研究结果一致。不同麦物种的对不同景观元素反应与形态学与生活史特征有关,而且景观结构中特定的植物种类、非作物植物的密度与物候期都可能影响寄生蜂群落的多样性与功能。     

The effect of growing alfalfa on subseouent cotton plant development and on nitrate formation in peat soil

Summary When cotton was grown in Hula peat soil following alfalfa, the germination, growth and yield were lower than when it followed wheat or bare soil. Results indicated that the formation of N-NO₃ in the soil was reduced by alfalfa crop growth, or when alfalfa root leachate was applied to bare soil. The inhibition of nitrification appeared to be due to substances originating in the plant and released by the roots. It is suggested that saponine, which is known to be released by alfalfa roots, may be responsible for this effect. Contribution from the Volcani Center, A.R.O., 1977 series, no. 206-E.     

Analysis and modelling of effects of leaf rust and Septoria tritici blotch on wheat growth

A model to predict Septoria tritici blotch (STB) and leaf rust effects on wheat growth was constructed and evaluated in two steps. At the leaf scale, Bastiaans' approach that predicts the relative photosynthesis of a wheat leaf infected with a single disease, was extended to the case of two diseases, one biotrophic and one necrotrophic by considering the leaf rust-STB complex. A glasshouse experiment with flag leaves inoculated either singly with one disease or with two diseases combined was performed to check the leaf damage model. No interaction of the two diseases on photosynthesis loss was observed when they occurred simultaneously on the same leaf. In a second step, the single-leaf model was extended to the canopy scale to model the effects of the leaf rust-STB complex on the growth of a wheat crop. The model predicts the effects of disease on the growth of an affected crop relative to the growth of a healthy crop. The canopy model accounted for different contributions to photosynthetic activity of leaf layers, derived from their position in the canopy and their natural leaf senescence. Treatments differing in nitrogen fertilization, microclimatic conditions, and wheat cultivars were implemented in a field experiment to evaluate the model. The model accurately estimated the effect of disease on crop growth for each cultivar, with differences from experimental values lower than 10%, which suggests that this model is well suited to aid an understanding of disease effects on plant growth. A reduction in green leaf area was the main effect of disease in these field experiments and STB accounted for more than 70% of the reduction in plant growth. Simulations suggested that the production of rust spores may result in a loss of biomass from diseased crops and that stem photosynthesis may need to be considered in modelling diseased crop growth.     

Modelling wheat growth and yield losses from late epidemics of foliar diseases using loss of green leaf area per layer and pre-anthesis reserves

BACKGROUND AND AIMS: Crop protection strategies, based on preventing quantitative crop losses rather than pest outbreaks, are being developed as a promising way to reduce fungicide use. The Bastiaans' model was applied to winter wheat crops (Triticum aestivum) affected by leaf rust (Puccinia triticina) and Septoria tritici blotch (STB; Mycosphaerella graminicola) under a range of crop management conditions. This study examined (a) whether green leaf area per layer accurately accounts for growth loss; and (b) whether from growth loss it is possible to derive yield loss accurately and simply. Methods Over 5 years of field experiments, numerous green leaf area dynamics were analysed during the post-anthesis period on wheat crops using natural aerial epidemics of leaf rust and STB. Key Results When radiation use efficiency (RUE) was derived from bulk green leaf area index (GLAI), RUE(bulk) was hardly accurate and exhibited large variations among diseased wheat crops, thus extending outside the biological range. In contrast, when RUE was derived from GLAI loss per layer, RUE(layer) was a more accurate calculation and fell within the biological range. In one situation out of 13, no significant shift in the RUE(layer) of diseased crops vs. healthy crops was observed. A single linear relationship linked yield to post-anthesis accumulated growth for all treatments. Its slope, not different from 1, suggests that the allocation of post-anthesis photosynthates to grains was not affected by the late occurring diseases under study. The mobilization of pre-anthesis reserves completely accounted for the intercept value. Conclusions The results strongly suggest that a simple model based on green leaf area per layer and pre-anthesis reserves can predict both growth and yield of wheat suffering from late epidemics of foliar diseases over a range of crop practices. It could help in better understanding how crop structure and reserve management contribute to tolerance of wheat genotypes to leaf diseases.