Response of the root system of a winter wheat crop to waterlogging

This study was aimed at analysing and quantifying the response of the root system dynamics of a wheat crop to waterlogging. Two experiments were carried out in parallel: one under controlled conditions with semi-permanent water tables using lysimeters equipped with oxygen measurers, and the other under conditions of artificially drained plots by continually monitoring their hydraulic functioning. The root system was observed frequently using the root mapping method, and this made it possible to measure the growth of the root front, to estimate root densities, and infer growth indices from them. The results showed that the anoxic medium for wheat roots consisted of a water-saturated soil with an oxygen concentration of below a critical threshold estimated to be 0.12 mol m^–3 water. The results also showed that the area which was unfavourable to root growth corresponded to the water table topped with a capillary zone of approximately 6 cm. Once the critical threshold had been reached, it was the water-table duration that explained root behaviour and the first effects were perceptible after approximately 48 h. On the basis of these results, two stress variables were analysed: water-table duration in the root zone (WTD) and proportion of roots in the water table (RPWT). The RPWT variable gave the best results within the two experimental contexts. In the case of the permanent regime, this variable made it possible to consider the root proliferation observations made above the saturated zone. Equations linking the stress variable RPWT to the growth indices are proposed that offer new perspectives to modelling waterlogging effects.     

Continuous measurement of oxygen concentration in citrus soil by means of a waterproof zirconia oxygen sensor

A limiting-current type of zirconia oxygen sensor has been developed and its efficiency was tested for the determination of oxygen in soil air. This oxygen sensor is waterproof and has a very short response time. By the use of the sensor, changes in soil oxygen concentration, due to undecomposed organic material and waterlogging, were observed. The sensor was found to be highly stable in the soil and suitable for continuous oxygen monitoring in the field.     

黄土旱塬区冬小麦土壤水库动态

土壤水库是旱作农业区粮食稳产和可持续发展的基础.本文结合长期田间定位试验,通过对黄土高原南部长武旱塬2012—2015年冬小麦土壤水分变化的研究,分析了土壤水库的年际与年内变化特征和动态规律.结果表明: 研究区冬小麦田间平均土壤含水量垂直分布曲线均呈“双峰双谷”形,第1处峰点在10～20 cm土层,第1处谷点在50 cm左右,第2处峰点在100 cm左右,第2处谷点在280 cm左右.无论何种降水年型下,土壤水库对降水的响应滞后且滞后的程度一致.降水年型对土壤水库的年际与年内动态变化影响较大.与丰水年相比,枯水年、平水年土壤水库对大气干旱的调节能力降低,表现为主要供水层上移;枯水年、平水年降水量虽少,但对土壤水分的补充作用较丰水年明显;丰水年土壤水库有较大盈余(84.2 mm),水分平衡出现正补偿,枯水年土壤水库稍有亏缺(1.5 mm),水分平衡出现负补偿,平水年土壤水库稍有盈余(9.5 mm),水分平衡出现正补偿.长武旱塬冬小麦田间土壤水分动态可分为4个时期:苗期耗水期、缓慢消耗期、大量消耗期、收获期,整体蒸散耗水大小顺序为:大量消耗期>苗期耗水期>收获期>缓慢消耗期.     

氮肥和6-BA对花后受渍冬小麦抗渍性的调控效应

渍水是黄淮南部麦区和长江中下游麦区冬小麦生育后期的主要气象灾害因子,试验以小麦品种‘烟农19’为材料,采用裂区设计研究氮肥和6-BA对花后受渍冬小麦抗渍性的调控效应。结果显示:(1)花后渍害显著降低冬小麦根系活力、总吸收面积、活跃吸收面积、旗叶叶绿素含量、旗叶净光合速率,极显著降低穗粒数、千粒重和籽粒产量,而对穗数无显著影响。(2)受渍后叶面喷施氮肥+6-BA、氮肥、6-BA均能显著提高冬小麦花后抗渍性,其根系活力分别提高18.7%、14.6%、12.0%,根系总吸收面积分别提高31.9%、22.1%、19.6%,根系活跃吸收面积分别提高32.5%、21.7%、18.1%,叶绿素含量分别提高16.2%、9.4%、10.3%,净光合速率分别提高32.6%、23.3%、23.3%,穗粒数分别提高13.8%、9.3%、8.5%,千粒重分别提高17.3%、11.5%、10.5%,籽粒产量分别提高35.9%、23.5%、20.9%。研究表明,氮肥和6-BA正交互作用显著,即花后同时喷施氮肥和6-BA缓解小麦渍害的效果更佳。     

The effect of soil moisture on the tolerance of Lupinus pilosus genotypes to a calcareous soil

Commercial narrow-leafed lupins (Lupinus angustifolius L.) grown on calcareous soils commonly display chlorotic symptoms resembling Fe deficiency. The severity of chlorosis increases with concurrent increases in soil moisture content. Our research has indicated that the rough-seeded lupin species, Lupinus pilosus Murr., has a range of adaptation to calcareous soils, from tolerant to intolerant. A pot experiment was conducted comparing a tolerant, a moderately tolerant and a moderately intolerant genotype of L. pilosus. Plants were grown for 35 days in a calcareous soil (50% CaCO₃) at three moisture contents (80%, 100% and 120% of field capacity); the growth was compared with that on a fertile black cracking clay control soil at 70% of field capacity. Visual chlorosis score, chlorophyll meter readings, number of leaves and shoot dry weights were recorded at 14, 21, 28 and 35 days after sowing. Concentrations of chlorophyll, active Fe and nutrients in the youngest fully expanded leaves were also measured. Results showed that increased soil moisture increased the severity of chlorotic symptoms (increased chlorosis score) in all genotypes. The tolerant genotype showed significantly less symptoms than other genotypes at all moisture contents. All genotypes were able to recover from chlorosis symptoms at 80% moisture in the calcareous soil. Chlorosis score negatively correlated with chlorophyll meter readings, chlorophyll concentration and foliar active and total Fe, and Mn concentrations. Visual chlorosis score appeared to be a cost effective, accurate and efficient method enabling classification of the tolerance of genotypes. The chlorotic symptoms were likely to be due to HCO₃ ^- induced nutrient deficiencies or a direct effect of HCO₃ ^- on chlorophyll synthesis. This study indicates that the most probable mechanism of tolerance is related to an ability to prevent uptake of HCO₃ ^- or efficiently sequester it once inside the root which prevents increases in internal pH and transport to the shoots.     

Phosphorus benefits of different legume crops to subsequent wheat grown in different soils of Western Australia

Certain legume crops, including white lupin (Lupinus albus L.), mobilise soil-bound phosphorus (P) through root exudates. The changes in the rhizosphere enhance P availability to these crops, and possibly to subsequent crops growing in the same soil. We conducted a pot experiment to compare phosphorus acquisition of three legume species with that of wheat, and to determine whether the legume crops influence growth and P uptake of a subsequent wheat crop. Field pea (Pisum sativum L.), faba bean (Vicia faba L.), white lupin (Lupinus albus L.) and wheat (Triticum aestivum L.) were grown in three different soils to which we added no or 20 mg P kg^–1 soil (P0, P20). Growth, P content and rhizosphere carboxylates varied significantly amongst crops, soils and P levels. Total P content of the plants was increased with applied phosphorus. Phosphorus content of faba bean was 3.9 and 8.8 mg/pot, at P0 and P20, respectively, which was about double that of all other species at the respective P levels. Field pea and white lupin had large amounts of rhizosphere carboxylates, whereas wheat and faba bean had negligible amounts in all three soils at both P levels. Wheat grew better after legumes than after wheat in all three soils. The effect of the previous plant species was greater when these previous species had received P fertiliser. All the legumes increased plant biomass of subsequent wheat significantly over the unplanted pots in all the soils. Faba bean was unparalleled in promoting subsequent wheat growth on all fertilised soils. This experiment clearly demonstrated a residual benefit of the legume crops on the growth of the subsequent wheat crop due to enhanced P uptake. Faba bean appeared to be a suitable P-mobilising legume crop plant for use in rotations with wheat.     

The effect of soil drought on the composition of carbohydrates in yellow lupin seeds and triticale kernels

Carbohydrate analysis was made of yellow lupin seeds (cv. Juno) and triticale kernels (cv. Dagro), produced by plants exposed to drought stress for 21 days after the initial flowering of the first node of lupin and initial earing of triticale. The seeds of all experimental variants were harvest at full maturity, dried and stored in linen bags at 18–20 °C. Soluble carbohydrates were extracted and analysed as described by Horbowicz and Obendorf (1994). Gas chromatographic separation of carbohydrates showed that raffinose family oligosaccharides (RFO) were dominant in lupin seeds. The other carbohydrates present were sucrose (10 %), cyclitols and galactosyl cyclitols (12–13 %). Soil drought resulted in higher levels of verbascose, but decreased the quantities of the other carbohydrates in lupine seeds. In triticale kernels, over 50 % of soluble sugars were composed of sucrose and maltose, while 17.7 % were raffinose and stachyose. In response to drought the content of mono- and oligosaccharides declined. The decrease of soluble carbohydrates content in seeds of lupin and triticale kernels has no effect on the seed germination and vigour. It is assumed that the changes in the concentration of soluble sugars observed under drought may impair the storability of triticale kernels, but improve it for lupine seeds.     

渍害胁迫下小麦生长的响应机理及调控措施研究进展

全球气候变化导致近年来渍害频发,而旱地作物小麦对渍害敏感.受气候、土壤、轮作制度等因素的影响,我国长江中下游小麦主产区的渍害灾情严重.渍害引起的土壤溶氧量降低可以导致小麦根系生长受到抑制,进而限制植株生长,最终降低小麦产量和品质.本文基于国内外相关研究,从根系呼吸代谢、水分传导、矿质养分吸收、光合作用、氧化还原代谢等方...     

渗漏型蒸渗仪对梭梭和柠条蒸腾蒸发的研究

利用非称量蒸渗仪对梭梭、柠条的蒸散进行了研究,结果表明：3年生的梭梭的单株蒸散量是515．3mm,3年生柠条的单株蒸散量是499．1mm。供水量和蒸散量之间存在着一定的正相关关系。3年生和2年生梭梭的单株平均蒸腾量分别是105．8mm和202.77mm;3年生和2年生柠条的单株平均蒸腾量分别为120．67mm和128．72mm。在3种供水条件下,柠条的蒸腾量都是梭梭的81％左右。在水分充足的情况下,梭梭和柠条的蒸腾量呈单峰曲线;在土壤水分亏缺的情况下,它们的蒸腾量呈双峰曲线。在干旱胁迫情况下,柠条和梭梭的蒸腾量与土壤含水率之间存在着极显著的线性关系,它们分别是:ET＝－33．29＋3217.93x（r＝0.8643）和ET＝－35．63＋1674．42x（r＝0．8273）。全年的沙面蒸发量是104.6mm-131．6mm,6－9月份的沙面蒸发量占全年沙面蒸发量的76．84％。沙面蒸发呈明显的双峰曲线。在供水条件下,沙面蒸发量随供水量的增加而增大。在无供水条件下,降水量的90．88％用于蒸发,9．12％保留于土壤中。对3年3个不同供水量蒸渗仅实测值进行多因子回归分析,得出沙面蒸发量与环境因子的关系：Ee＝－42．5131＋730．2497x1＋0．7422x2＋0．5494x3．其中Ee为月蒸发量,x1为0—40cm沙层月均含水率,x2为月均日辐射强度,x3为某月日平     

江淮地区小麦涝渍灾害风险评估与区划

基于灾害风险分析理论,根据历年气候资料,小麦生长发育、种植面积和产量资料,对江淮地区各县小麦涝渍脆弱性、自然气候风险、灾损风险和抗灾能力等方面进行分析评估,建立了包括涝渍脆弱度、气候风险指数、灾损风险指数、涝渍综合风险评估系数等不同的涝渍风险表征模型,并构建了涝渍综合风险评估系数作为区划指标,对江淮地区小麦涝渍灾害风险进行了空间区域划分。结果表明:涝渍脆弱度、气候风险指数、灾损风险指数和抗灾力系数4个因子的组合,可以较好地反映江淮地区小麦涝渍风险特征;按照高、较高、中和低4个等级对小麦涝渍综合风险进行了区划;安徽省江淮南部为高风险区;沿淮中部以及江淮中部南部、沿洪泽湖区域为涝渍较高风险区;河南省33°N以南区域、以及安徽、江苏省淮北中部区域为涝渍中风险区;33°N以北地区为涝渍低风险区。     

基于高光谱和数字图像特征指数的受渍冬小麦SPAD估算

为了探索基于高光谱和数字图像技术的受渍冬小麦SPAD最优监测方法,本研究基于排灌可控的微区试验,通过分析常用的15个高光谱特征指数和14个数字图像特征指数与受渍冬小麦叶绿素相对含量(SPAD)的相关关系,构建了基于最优监测特征指数的BP神经网络模型,对受渍冬小麦的SPAD进行估算.结果 表明:与正常小麦相比,短期渍水(...     

Review of prospects for germplasm improvement for waterlogging tolerance in wheat,barley and oats

A review is presented for prospects of germplasm improvement for waterlogging tolerance in wheat, barley and oats using a mechanistic approach based on adaptive physiological traits. In `The waterlogged environments for crop production' section, the extent of waterlogging is reviewed commencing with determination of environmental factors which may limit plant growth and development in waterlogging prone regions. This highlights that different types of waterlogging may exist, there may be large spatial and temporal variation in waterlogging, and that waterlogging may be confounded in field experiments with additional environmental factors. Environmental characterisation is therefore a key step to using mechanistic approaches for germplasm improvement for target environments, for extrapolation to other environments, and for development of screening protocols under controlled conditions that accurately reflect the field environment. In the `Information on key components required for germplasm improvement' section, the genetic diversity in wheat, barley and oats for waterlogging tolerance is confirmed. Physiological mechanisms for waterlogging tolerance are diverse and can be grouped into adaptive traits relating to (1) phenology, (2) morphology and anatomy, (3) nutrition, (4) metabolism including anaerobic catabolism and anoxia tolerance, and (5) post anoxic damage and recovery. For wheat and barley, there is some genetic diversity for waterlogging tolerance at the germination stage, however the full potential seems yet to be exploited. Varietal differences in tolerance at the germination stage often differ from tolerance at later stages of development, and this supports the view that different mechanisms of tolerance exist at the whole plant and tissue level. Limited work from genetic studies indicates a high heritability for waterlogging tolerance. It is concluded that the best opportunities for germplasm improvement are for further exploration and utilisation of genetic diversity by improving selection criteria including the use of marker assisted selection. Additional opportunities are described for increasing genetic diversity using wide hybridisations and development of transgenic plants.     

The impact of temperature variability on wheat yields

With current annual production at over 600 million tonnes, wheat is the third largest crop in the world behind corn and rice, and an essential source of carbohydrates for millions of people. While wheat is grown over a wide range of environments, it is common in the major wheat‐producing countries for grain filling to occur when soil moisture is declining and temperature is increasing. Average global temperatures have increased over the last decades and are predicted to continue rising, along with a greater frequency of extremely hot days. Such events have already been reported for major wheat growing regions in the world. However, the direct impact of past temperature variability and changes in averages and extremes on wheat production has not been quantified. Attributing changes in observed yields over recent decades to a single factor such as temperature is not possible due to the confounding effects of other factors. By using simulation modelling, we were able to separate the impact of temperature from other factors and show that the effect of temperature on wheat production has been underestimated. Surprisingly, observed variations in average growing‐season temperatures of ±2 °C in the main wheat growing regions of Australia can cause reductions in grain production of up to 50%. Most of this can be attributed to increased leaf senescence as a result of temperatures >34 °C. Temperature conditions during grain filling in the major wheat growing regions of the world are similar to the Australian conditions during grain filling. With average temperatures and the frequency of heat events projected to increase world‐wide with global warming, yield reductions due to higher temperatures during the important grain‐filling stage alone could substantially undermine future global food security. Adaptation strategies need to be considered now to prevent substantial yield losses in wheat from increasing future heat stress.     

花后盐与渍水逆境对小麦籽粒产量及蛋白质和淀粉积累的影响

采用盆栽试验,研究了花后渍水、盐胁迫和盐渍处理对2个小麦品种（扬麦12和淮麦17）籽粒产量及蛋白质和淀粉积累与组分的影响.结果表明：与对照相比,花后渍水、盐胁迫和盐渍处理显著降低了小麦花前贮藏氮素（花前贮藏干物质）转运量和花后同化氮素（花后同化物）输入籽粒量,从而导致小麦籽粒产量、蛋白质和淀粉产量显著降低,其中盐胁迫和盐渍处理表现更为明显.与对照和渍水处理相比,盐胁迫和盐渍处理显著降低了小麦籽粒蛋白质积累量及谷/醇蛋白比,显著提高了蛋白质组分含量;同时降低了小麦籽粒淀粉积累量、淀粉组分含量及直/支链淀粉比;盐胁迫处理对扬麦12的影响较盐渍处理明显,而盐渍处理对淮麦17的影响较盐胁迫处理明显.渍水条件下小麦籽粒蛋白质和淀粉积累量均下降,除淮麦17谷蛋白和清蛋白含量有所提高外,淮麦17其他蛋白组分含量和扬麦12各蛋白组分含量均下降.     

不同水分条件下氮素供应对小麦植株氮代谢及籽粒蛋白质积累的影响

土壤水分逆境是限制小麦籽粒品质形成的重要生态因子,明确土壤水分逆境下小麦籽粒品质形成的生理机制及调优技术途径,对于深化小麦品质生理生态研究和指导小麦调优栽培具有重要的理论意义和应用前景。在防雨池栽条件下,设置渍水、干旱和对照3个水分处理,每个水分处理下再设置120和240 kg.hm-2两个施氮水平,研究了花后渍水和干旱逆境下氮素对两个籽粒蛋白质含量不同的小麦品种植株氮代谢和籽粒蛋白质积累的影响。结果表明,与正常水分处理相比,花后干旱和渍水均降低旗叶硝酸还原酶活性、叶片总氮含量和游离氨基酸含量。干旱处理提高了茎鞘总氮与游离氨基酸含量以及籽粒蛋白质含量,而渍水处理则使其降低。水分逆境下增施氮肥提高旗叶硝酸还原酶活性、叶片与茎鞘总氮和游离氨基酸含量以及籽粒游离氨基酸和蛋白质含量。花后干旱和渍水均显著降低了小麦籽粒产量和蛋白质产量。增施氮肥提高适宜水分和水分亏缺条件下小麦籽粒产量,但不利于渍水下小麦产量的提高。这说明,花后渍水和干旱逆境下施用氮肥对小麦植株氮代谢和籽粒蛋白质积累有明显的调节效应。     

Groundwater dynamics along forest-marsh transects in a southeastern salt marsh,USA: Description,interpretation and challenges for numerical modeling

Long-term and spatially dense time series of total head measured alongthree forest-marsh piezometer transects across a finger marsh basin,together with bimonthly groundwater salinity measurements, reveal dynamicfeatures that present challenges to the interpretation and modeling of thisshallow water table aquifer. These include:1. Rapid response of forest water table to rain events.2. Daytime lowering (drawdown) of the water table in the forest and highmarsh due to evapotranspiration and its recovery due to rain, seepage ortidal inundation.3. Upward gradients in head along the western margin of the marsh butdownward gradients in the eastern, more seaward, high marsh and forest.4. Rapid head responses to the tide in parts of the high marsh andforest that are not actually inundated.5. Asymmetrical distribution of salinity with higher values in theeastern marsh and forest than in the west.6. Sharp salinity gradients across the tidal creek that bisects the basin. We discuss modeling issues related to these features because acomprehensive understanding of them may have a bearing on patterns ofbotanical zonation and primary production, the transport of nutrients andcontaminants, and the response of this system to sea level rise.