小麦开花期根系电容量预测产量

IF 2 4区 农林科学 Q2 AGRONOMY International Agrophysics Pub Date : 2021-06-10 DOI:10.31545/INTAGR/136711
I. Cseresnyés, P. Mikó, Bettina Kelemen, A. Füzy, I. Parádi, T. Takács
{"title":"小麦开花期根系电容量预测产量","authors":"I. Cseresnyés, P. Mikó, Bettina Kelemen, A. Füzy, I. Parádi, T. Takács","doi":"10.31545/INTAGR/136711","DOIUrl":null,"url":null,"abstract":"Larger root system size (RSS) is critical for increased early vigour and water use, it contributes to enhanced grain yield (GY) in crops (Fageria, 2013), thus emphasizing the importance of applying field root phenotyping techniques in breeding programmes (Postic et al., 2019). Nevertheless, as conventional root investigation methods are generally laborious and destructive, and the isolation of the intact root system from field soil is practically impossible, the investigation of roots is often neglected compared to those of shoots. The measurement of root electrical capacitance (CR) is a promising, rapid in situ technique capable of screening numerous plants at different growth stages. Moreover, the sampled plants can be harvested at maturity to determine GY and can also be used for reproduction (Středa et al., 2020). The CR method was successfully applied in the field to evaluate the effect of dwarfing genes on the RSS of barley (Chloupek et al., 2006), in order to select barley and wheat genotypes for higher RSS and drought tolerance (Chloupek et al., 2010; Svačina et al., 2014; Heřmanská et al., 2015), to assess the root diversity and water use of wheat varieties (Středa et al., 2012; Nakhforoosh et al., 2014), and to estimate canola RSS in relation to lodging resistance (Wu and Ma, 2016). Some of these studies demonstrated significant relationships between the CR-based root size and individual GY, particularly in dry environments. © 2021 Institute of Agrophysics, Polish Academy of Sciences I. CSERESNYÉS et al. 160 The measurement technique is based on the correlation between RSS variables and the CR detected between a ground electrode (inserted into the soil) and a plant electrode (fixed on the stem) using a low-frequency alternating current (AC) signal (Chloupek, 1972). Conceptual models consider the roots to be imperfect cylindrical capacitors, in which the amount of electric charge stored by the polarizable membrane dielectrics depends on the root-soil interfacial area (Dalton, 1995). Even though some of the underlying biophysical principles are still unclear and there are uncertainties about the relative contribution of proximal and distal (fine) roots to the magnitude of the CR detected (Dietrich et al., 2012; Ellis et al., 2013; Cseresnyés et al., 2020; Peruzzo et al., 2020), several pot and field trials have convincingly demonstrated the efficiency of the capacitance method (Středa et al., 2020). One advantage of the technique is that, as the CR value is affected not only by the size but also by the histological properties of the roots (e.g. suberization), the method characterizes both root physiological status and its functionality (Ellis et al., 2013; Cseresnyés et al., 2018). Even though the measured capacitance is very sensitive to soil water content (SWC), this effect can be taken into account by converting the measured CR to saturation (apparent) capacitance, CR*, which was detected in experiments on water-saturated soil (Cseresnyés et al., 2018). This adaptation allows us to compare the field data collected at different dates (under different SWC), which was previously considered to be a serious limitation for the capacitance technique (Chloupek et al., 2010; Středa et al., 2012). In this manner, field monitoring revealed that CR, as a proxy of root activity, peaked during flowering in maize and soybean (Cseresnyés et al., 2018). Minirhizotron and soil core studies verified that wheat root biomass and root length reached a maximum around anthesis, in parallel with the peaks of leaf area, transpiration and water use, and were also significantly correlated with stand GY (Wang et al., 2014; Yang et al., 2018; Postic et al., 2019). A methodological field study involving three winter wheat cultivars is presented here. As intercropping systems have gained increasing attention in organic farming worldwide due to more efficient, complementary resource use (Bedoussac and Justes, 2011; Lithourgidis et al., 2011), wheat-pea mixtures were tested to compare them with wheat sole crops. Focusing on wheat, RSS was assessed merely on the basis of CR* measured in situ at anthesis. The specific aims of the study were (i) to study the correlation of the individual CR* values with the total aboveground biomass (TAB) at maturity and also with GY for each wheat cultivar in order to validate the stand-scale results, (ii) to evaluate the effect of pea intercropping with halved wheat density on mean CR* and the corresponding GY using a stand scale over a three-year period, and (iii) to analyse the relationship between mean CR* and GY across the cropping systems and years. In brief, the study examined the relevance of the capacitance method in the field, or more precisely, the efficiency with which wheat grain yield may be predicted by measuring the saturation root capacitance (CR*) at anthesis under different cultivation and climatic conditions. MATERIALS AND METHODS The field study was conducted during three winter wheat growing seasons from 2017 to 2020 (referred to as harvest years 2018, 2019 and 2020) in a certified organic field in Martonvásár, Central Hungary (N 47°18’, E 18°47’, 109 m a.s.l.). The soil was a Haplic Chernozem (36% sand, 41% silt, 23% clay) with a pH value of 7.66, 1.61% CaCO3, 3.22% humus, 1887/361/445 mg kg total N/P/K and 0.309 cm cm water content at field capacity. The climate is continental with a mean (1987-2016) annual temperature of 11.0°C (January: –1.0°C, July: 21.2°C) and annual precipitation of 548 mm, of which 193 mm falls during the main crop growing season (March-June; Fig. 1). There were optimal rainfall conditions in 2018. By contrast, late-winter and Fig. 1. Monthly rainfall (mm, columns) and mean air temperature (°C, lines) at the experimental site (Martonvásár, Hungary) during the winter wheat growing seasons. The long-term (1987–2016) average is displayed as a reference. WHEAT YIELD PREDICTION BY ROOT ELECTRICAL CAPACITANCE 161 spring droughts occurred in the next two seasons with sufficient precipitation only occurring from early May (flowering stage) in 2019 and from late May (milk stage) in 2020. Winter wheat (Triticum aestivum L.) cultivars ‘Mv Nádor’ (“N”) and ‘Mv Kolompos’ (“K”) and the YQCCP composite population (“C”) were sown in October each year in 6 × 1 m plots with 12 cm row spacing as sole crops (“0”) at a density of 300 seeds m, and at half that density (150 seeds m) intercrops (“P”) with winter pea (Pisum sativum L., cv. Aviron; 50 seeds m). The three replications of each treatment were randomly arranged in the same field, with each one being surrounded by a 1 m border strip, but in slightly different places each year. Natural fertilizers and artificial chemicals were not used directly, which latter is even banned in organic agriculture. At the time of anthesis (in early to mid-May, depending on the cultivar and year) 15 wheat plants were randomly selected from the inner rows of each plot. SWC was measured in the 0-12 cm layer 5 cm away from each sample plant (equal to the depth and position of the CR ground electrode) with a calibrated CS620 portable TDR meter (Campbell Sci. Ltd., Loughborough, UK). The relative water saturation (θrel) value was calculated by dividing the measured volumetric SWC values (cm cm) by the predetermined saturation water content of 0.476 cm cm (Cseresnyés et al., 2018). Thereafter, parallel CR was recorded for the selected plants with a U1733C handheld LCR meter (Agilent Co. Ltd., Penang, Malaysia) at 1 kHz, 1 V AC. The ground electrode was a stainless steel rod 15 cm in length and 6 mm in diameter (303S31; RS Pro GmbH., Gmünd, Austria), pushed vertically into the soil 5 cm from the stem to a depth of 12 cm. The plant electrode was clamped to all of the basal parts of the plant 15 mm above the soil (Svačina et al., 2014) after smearing them with conductivity gel. In order to eliminate the SWC effect, all of the CR data were converted into CR*, according to the empirical function: CR* = CR 5.807erel, using the relevant θrel values (for a detailed calculation, see Cseresnyés et al., 2018). After the CR measurements were complete, five randomly selected wheat plants per plot were cut at ground level, and oven-dried at 70°C until a constant weight was achieved in order to determine shoot dry mass (SDM; ±0.001 g). In the last year (2020) the plants chosen for measuring CR were individually tagged. At maturity (in early July), the tagged plants were hand harvested and oven-dried to determine TAB, after which they were hand threshed to obtain plant GY. Thereafter, the plots were harvested mechanically, and the wheat grains were separated from the peas and weighed. The mean plant GY was determined for each plot on the basis of wheat seedling density. The data were analysed with Statistica 13.0 software (StatSoft Inc., Tulsa, OK, USA). The unpaired t-test or one-way ANOVA with Tukey’s posthoc test was performed to compare the means of CR*, SDM and GY (p < 0.05). If the F-test or Bartlett’s test indicated unequal variances, Welch’s t-test or Kruskal-Wallis with Dunn’s posthoc test was used. Linear regression analysis was applied to relate CR* to TAB, SDM and GY. The resultant regressions were compared using a linear analysis of covariance (ANCOVA).","PeriodicalId":13959,"journal":{"name":"International Agrophysics","volume":"35 1","pages":"159-165"},"PeriodicalIF":2.0000,"publicationDate":"2021-06-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"Prediction of wheat grain yield by measuring root electrical capacitance at anthesis\",\"authors\":\"I. 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The CR method was successfully applied in the field to evaluate the effect of dwarfing genes on the RSS of barley (Chloupek et al., 2006), in order to select barley and wheat genotypes for higher RSS and drought tolerance (Chloupek et al., 2010; Svačina et al., 2014; Heřmanská et al., 2015), to assess the root diversity and water use of wheat varieties (Středa et al., 2012; Nakhforoosh et al., 2014), and to estimate canola RSS in relation to lodging resistance (Wu and Ma, 2016). Some of these studies demonstrated significant relationships between the CR-based root size and individual GY, particularly in dry environments. © 2021 Institute of Agrophysics, Polish Academy of Sciences I. CSERESNYÉS et al. 160 The measurement technique is based on the correlation between RSS variables and the CR detected between a ground electrode (inserted into the soil) and a plant electrode (fixed on the stem) using a low-frequency alternating current (AC) signal (Chloupek, 1972). Conceptual models consider the roots to be imperfect cylindrical capacitors, in which the amount of electric charge stored by the polarizable membrane dielectrics depends on the root-soil interfacial area (Dalton, 1995). Even though some of the underlying biophysical principles are still unclear and there are uncertainties about the relative contribution of proximal and distal (fine) roots to the magnitude of the CR detected (Dietrich et al., 2012; Ellis et al., 2013; Cseresnyés et al., 2020; Peruzzo et al., 2020), several pot and field trials have convincingly demonstrated the efficiency of the capacitance method (Středa et al., 2020). One advantage of the technique is that, as the CR value is affected not only by the size but also by the histological properties of the roots (e.g. suberization), the method characterizes both root physiological status and its functionality (Ellis et al., 2013; Cseresnyés et al., 2018). Even though the measured capacitance is very sensitive to soil water content (SWC), this effect can be taken into account by converting the measured CR to saturation (apparent) capacitance, CR*, which was detected in experiments on water-saturated soil (Cseresnyés et al., 2018). This adaptation allows us to compare the field data collected at different dates (under different SWC), which was previously considered to be a serious limitation for the capacitance technique (Chloupek et al., 2010; Středa et al., 2012). In this manner, field monitoring revealed that CR, as a proxy of root activity, peaked during flowering in maize and soybean (Cseresnyés et al., 2018). Minirhizotron and soil core studies verified that wheat root biomass and root length reached a maximum around anthesis, in parallel with the peaks of leaf area, transpiration and water use, and were also significantly correlated with stand GY (Wang et al., 2014; Yang et al., 2018; Postic et al., 2019). A methodological field study involving three winter wheat cultivars is presented here. As intercropping systems have gained increasing attention in organic farming worldwide due to more efficient, complementary resource use (Bedoussac and Justes, 2011; Lithourgidis et al., 2011), wheat-pea mixtures were tested to compare them with wheat sole crops. Focusing on wheat, RSS was assessed merely on the basis of CR* measured in situ at anthesis. The specific aims of the study were (i) to study the correlation of the individual CR* values with the total aboveground biomass (TAB) at maturity and also with GY for each wheat cultivar in order to validate the stand-scale results, (ii) to evaluate the effect of pea intercropping with halved wheat density on mean CR* and the corresponding GY using a stand scale over a three-year period, and (iii) to analyse the relationship between mean CR* and GY across the cropping systems and years. In brief, the study examined the relevance of the capacitance method in the field, or more precisely, the efficiency with which wheat grain yield may be predicted by measuring the saturation root capacitance (CR*) at anthesis under different cultivation and climatic conditions. MATERIALS AND METHODS The field study was conducted during three winter wheat growing seasons from 2017 to 2020 (referred to as harvest years 2018, 2019 and 2020) in a certified organic field in Martonvásár, Central Hungary (N 47°18’, E 18°47’, 109 m a.s.l.). The soil was a Haplic Chernozem (36% sand, 41% silt, 23% clay) with a pH value of 7.66, 1.61% CaCO3, 3.22% humus, 1887/361/445 mg kg total N/P/K and 0.309 cm cm water content at field capacity. The climate is continental with a mean (1987-2016) annual temperature of 11.0°C (January: –1.0°C, July: 21.2°C) and annual precipitation of 548 mm, of which 193 mm falls during the main crop growing season (March-June; Fig. 1). There were optimal rainfall conditions in 2018. By contrast, late-winter and Fig. 1. Monthly rainfall (mm, columns) and mean air temperature (°C, lines) at the experimental site (Martonvásár, Hungary) during the winter wheat growing seasons. The long-term (1987–2016) average is displayed as a reference. WHEAT YIELD PREDICTION BY ROOT ELECTRICAL CAPACITANCE 161 spring droughts occurred in the next two seasons with sufficient precipitation only occurring from early May (flowering stage) in 2019 and from late May (milk stage) in 2020. Winter wheat (Triticum aestivum L.) cultivars ‘Mv Nádor’ (“N”) and ‘Mv Kolompos’ (“K”) and the YQCCP composite population (“C”) were sown in October each year in 6 × 1 m plots with 12 cm row spacing as sole crops (“0”) at a density of 300 seeds m, and at half that density (150 seeds m) intercrops (“P”) with winter pea (Pisum sativum L., cv. Aviron; 50 seeds m). The three replications of each treatment were randomly arranged in the same field, with each one being surrounded by a 1 m border strip, but in slightly different places each year. Natural fertilizers and artificial chemicals were not used directly, which latter is even banned in organic agriculture. At the time of anthesis (in early to mid-May, depending on the cultivar and year) 15 wheat plants were randomly selected from the inner rows of each plot. SWC was measured in the 0-12 cm layer 5 cm away from each sample plant (equal to the depth and position of the CR ground electrode) with a calibrated CS620 portable TDR meter (Campbell Sci. Ltd., Loughborough, UK). The relative water saturation (θrel) value was calculated by dividing the measured volumetric SWC values (cm cm) by the predetermined saturation water content of 0.476 cm cm (Cseresnyés et al., 2018). Thereafter, parallel CR was recorded for the selected plants with a U1733C handheld LCR meter (Agilent Co. Ltd., Penang, Malaysia) at 1 kHz, 1 V AC. The ground electrode was a stainless steel rod 15 cm in length and 6 mm in diameter (303S31; RS Pro GmbH., Gmünd, Austria), pushed vertically into the soil 5 cm from the stem to a depth of 12 cm. The plant electrode was clamped to all of the basal parts of the plant 15 mm above the soil (Svačina et al., 2014) after smearing them with conductivity gel. In order to eliminate the SWC effect, all of the CR data were converted into CR*, according to the empirical function: CR* = CR 5.807erel, using the relevant θrel values (for a detailed calculation, see Cseresnyés et al., 2018). After the CR measurements were complete, five randomly selected wheat plants per plot were cut at ground level, and oven-dried at 70°C until a constant weight was achieved in order to determine shoot dry mass (SDM; ±0.001 g). In the last year (2020) the plants chosen for measuring CR were individually tagged. At maturity (in early July), the tagged plants were hand harvested and oven-dried to determine TAB, after which they were hand threshed to obtain plant GY. Thereafter, the plots were harvested mechanically, and the wheat grains were separated from the peas and weighed. The mean plant GY was determined for each plot on the basis of wheat seedling density. The data were analysed with Statistica 13.0 software (StatSoft Inc., Tulsa, OK, USA). The unpaired t-test or one-way ANOVA with Tukey’s posthoc test was performed to compare the means of CR*, SDM and GY (p < 0.05). If the F-test or Bartlett’s test indicated unequal variances, Welch’s t-test or Kruskal-Wallis with Dunn’s posthoc test was used. Linear regression analysis was applied to relate CR* to TAB, SDM and GY. 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引用次数: 3

摘要

较大的根系大小(RSS)对于提高早期活力和水分利用至关重要,它有助于提高作物的粮食产量(GY)(Fageria,2013),从而强调了在育种计划中应用田间根系表型技术的重要性(Postic等人,2019)。然而,由于传统的根系调查方法通常是费力和破坏性的,并且几乎不可能将完整的根系从田间土壤中分离出来,因此与对枝条的调查相比,对根系的调查往往被忽视。根电容(CR)测量是一种很有前途的快速原位技术,能够筛选不同生长阶段的大量植物。此外,采样的植物可以在成熟时收获以确定GY,也可以用于繁殖(Středa等人,2020)。CR方法已成功应用于田间评估矮化基因对大麦RSS的影响(Chlopek等人,2006),以选择具有更高RSS和耐旱性的大麦和小麦基因型(Chloppek等人,2010;Svačina等人,2014;Heřmanská等人,2015),评估小麦品种的根系多样性和水分利用(Středa et al.,2012;Nakhforoosh et al.,2014),并估计油菜RSS与抗倒伏性的关系(Wu和Ma,2016)。其中一些研究表明,基于CR的根系大小与个体GY之间存在显著关系,尤其是在干燥环境中。©2021波兰科学院土壤物理研究所I.CSRESNYÉS等人160测量技术基于RSS变量与使用低频交流(AC)信号在接地电极(插入土壤)和植物电极(固定在茎上)之间检测到的CR之间的相关性(Chlopek,1972)。概念模型认为根部是不完美的圆柱形电容器,其中可极化膜电介质存储的电荷量取决于根部-土壤界面面积(Dalton,1995)。尽管一些基本的生物物理原理仍然不清楚,近端和远端(细)根对检测到的CR大小的相对贡献也存在不确定性(Dietrich等人,2012;Ellis等人,2013;Csersnyés等人,2020;Peruzzo等人,2020),几次现场试验令人信服地证明了电容法的有效性(Středa等人,2020)。该技术的一个优点是,由于CR值不仅受根的大小影响,还受根的组织学特性(如木栓化)影响,该方法表征了根的生理状态及其功能(Ellis等人,2013;Csersnyés等人,2018)。尽管测量的电容对土壤含水量(SWC)非常敏感,但可以通过将测量的CR转换为饱和(表观)电容CR*来考虑这种影响,这是在水饱和土壤的实验中检测到的(Csersnyés等人,2018)。这种适应性使我们能够比较在不同日期(在不同SWC下)收集的现场数据,这在以前被认为是电容技术的严重限制(Chlopek等人,2010;Středa等人,2012年)。通过这种方式,田间监测显示,CR作为根系活性的代表,在玉米和大豆开花期间达到峰值(Csersnyés等人,2018)。Minirhizotron和土壤核心研究证实,小麦根系生物量和根长在开花前后达到最大值,与叶面积、蒸腾和水分利用的峰值平行,并且与林分GY显著相关(Wang et al.,2014;杨等人,2018;Postic等人,2019)。本文介绍了一项涉及三个冬小麦品种的方法学实地研究。由于更有效、互补的资源利用,间作系统在全球有机农业中越来越受到关注(Bedousac和Justes,2011;Lithourgidis等人,2011),对小麦-豌豆混合物进行了测试,将其与小麦单一作物进行比较。以小麦为重点,仅根据开花时原位测量的CR*来评估RSS。本研究的具体目的是:(i)研究每个小麦品种成熟时个体CR*值与地上总生物量(TAB)以及GY的相关性,以验证林分尺度的结果;(ii)使用林分尺度评估小麦密度减半的豌豆间作对三年内平均CR*和相应GY的影响,以及(iii)分析不同种植制度和年份的平均CR*和GY之间的关系。简言之,该研究考察了电容法在田间的相关性,或者更准确地说,通过测量不同栽培和气候条件下开花时的饱和根电容(CR*)来预测小麦产量的效率。 材料和方法在2017年至2020年的三个冬小麦生长季节(称为收获年2018年、2019年和2020年),在匈牙利中部Martonvásár的一块经认证的有机地(北纬47°18',东经18°47',海拔109米)进行了实地研究,1887/361/445 mg/kg总N/P/K和0.309 cm cm含水量。气候为大陆性气候,(1987-2016)年平均气温为11.0°C(1月:-1.0°C,7月:21.2°C),年降水量为548毫米,其中193毫米在主要作物生长季节(3-6月;图1)。2018年有最佳降雨条件。相比之下,晚冬和图1。在冬小麦生长季节,试验地点(匈牙利Martonvásár)的月降雨量(毫米,柱)和平均气温(°C,线)。长期(1987–2016)平均值显示为参考值。根电容预测小麦产量161春季干旱发生在接下来的两个季节,降水充足的时间仅发生在2019年5月初(开花期)和2020年5月下旬(泌乳期)。冬小麦(Triticum aestivum L.)品种Mv Nádor(“N”)和Mv Kolompos(“K”)以及YQCCP复合群体(“C”)于每年10月播种在6×1m的地块上,行距12cm,作为唯一作物(“0”),密度为300种子m,与冬豌豆(Pisum sativum L.,cv.Aviron;50种子m)以该密度的一半(150种子m)进行间作(“P”)。每种处理的三个复制品被随机安排在同一块田地里,每个复制品都被1米的边界带包围,但每年在稍微不同的地方。天然肥料和人工化学品没有直接使用,后者甚至在有机农业中被禁止。在开花时(5月初至中旬,取决于品种和年份),从每个地块的内排中随机选择15株小麦。使用校准的CS620便携式TDR测量仪(Campbell Sci.有限公司,Loughborough,UK)在距离每个样品植物5cm(等于CR接地电极的深度和位置)的0-12cm层中测量SWC。相对水饱和度(θrel)值是通过将测得的体积SWC值(cm cm)除以0.476 cm cm的预定饱和含水量来计算的(Csersnyés等人,2018)。此后,用U1733C手持式LCR测量仪(安捷伦有限公司,马来西亚槟城)在1 kHz,1 V AC下记录所选植物的平行CR。接地电极是一根长15厘米、直径6毫米的不锈钢棒(303S31;RS Pro GmbH,Gmünd,Austria),从树干垂直推入土壤5厘米,深度12厘米。在用导电凝胶涂抹植物电极后,将其夹在土壤上方15 mm的植物所有基底部分(Svačina等人,2014)。为了消除SWC效应,根据经验函数将所有CR数据转换为CR*:CR*=CR 5.807erel,使用相关θrel值(详细计算,见Csersnyés等人,2018)。CR测量完成后,在地面上对每个地块随机选择五株小麦植株进行切割,并在70°C下烘干,直到达到恒定重量,以确定茎干质量(SDM;±0.001 g)。去年(2020年),选择用于测量CR的植物被单独标记。成熟时(7月初),用手收割标记的植物并烘干以确定TAB,然后用手脱粒以获得植物GY。此后,用机械收割地块,将小麦粒与豌豆分离并称重。根据小麦幼苗密度确定每个地块的平均植株GY。使用Statistica 13.0软件(美国俄克拉荷马州塔尔萨市StatSoft股份有限公司)对数据进行分析。对CR*、SDM和GY的平均值进行了非配对t检验或单因素方差分析(p<0.05)。如果F检验或Bartlett检验表明方差不相等,则使用Welch t检验或Kruskal-Wallis与Dunn的后验检验。应用线性回归分析将CR*与TAB、SDM和GY联系起来。使用协方差线性分析(ANCOVA)对所得回归进行比较。
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Prediction of wheat grain yield by measuring root electrical capacitance at anthesis
Larger root system size (RSS) is critical for increased early vigour and water use, it contributes to enhanced grain yield (GY) in crops (Fageria, 2013), thus emphasizing the importance of applying field root phenotyping techniques in breeding programmes (Postic et al., 2019). Nevertheless, as conventional root investigation methods are generally laborious and destructive, and the isolation of the intact root system from field soil is practically impossible, the investigation of roots is often neglected compared to those of shoots. The measurement of root electrical capacitance (CR) is a promising, rapid in situ technique capable of screening numerous plants at different growth stages. Moreover, the sampled plants can be harvested at maturity to determine GY and can also be used for reproduction (Středa et al., 2020). The CR method was successfully applied in the field to evaluate the effect of dwarfing genes on the RSS of barley (Chloupek et al., 2006), in order to select barley and wheat genotypes for higher RSS and drought tolerance (Chloupek et al., 2010; Svačina et al., 2014; Heřmanská et al., 2015), to assess the root diversity and water use of wheat varieties (Středa et al., 2012; Nakhforoosh et al., 2014), and to estimate canola RSS in relation to lodging resistance (Wu and Ma, 2016). Some of these studies demonstrated significant relationships between the CR-based root size and individual GY, particularly in dry environments. © 2021 Institute of Agrophysics, Polish Academy of Sciences I. CSERESNYÉS et al. 160 The measurement technique is based on the correlation between RSS variables and the CR detected between a ground electrode (inserted into the soil) and a plant electrode (fixed on the stem) using a low-frequency alternating current (AC) signal (Chloupek, 1972). Conceptual models consider the roots to be imperfect cylindrical capacitors, in which the amount of electric charge stored by the polarizable membrane dielectrics depends on the root-soil interfacial area (Dalton, 1995). Even though some of the underlying biophysical principles are still unclear and there are uncertainties about the relative contribution of proximal and distal (fine) roots to the magnitude of the CR detected (Dietrich et al., 2012; Ellis et al., 2013; Cseresnyés et al., 2020; Peruzzo et al., 2020), several pot and field trials have convincingly demonstrated the efficiency of the capacitance method (Středa et al., 2020). One advantage of the technique is that, as the CR value is affected not only by the size but also by the histological properties of the roots (e.g. suberization), the method characterizes both root physiological status and its functionality (Ellis et al., 2013; Cseresnyés et al., 2018). Even though the measured capacitance is very sensitive to soil water content (SWC), this effect can be taken into account by converting the measured CR to saturation (apparent) capacitance, CR*, which was detected in experiments on water-saturated soil (Cseresnyés et al., 2018). This adaptation allows us to compare the field data collected at different dates (under different SWC), which was previously considered to be a serious limitation for the capacitance technique (Chloupek et al., 2010; Středa et al., 2012). In this manner, field monitoring revealed that CR, as a proxy of root activity, peaked during flowering in maize and soybean (Cseresnyés et al., 2018). Minirhizotron and soil core studies verified that wheat root biomass and root length reached a maximum around anthesis, in parallel with the peaks of leaf area, transpiration and water use, and were also significantly correlated with stand GY (Wang et al., 2014; Yang et al., 2018; Postic et al., 2019). A methodological field study involving three winter wheat cultivars is presented here. As intercropping systems have gained increasing attention in organic farming worldwide due to more efficient, complementary resource use (Bedoussac and Justes, 2011; Lithourgidis et al., 2011), wheat-pea mixtures were tested to compare them with wheat sole crops. Focusing on wheat, RSS was assessed merely on the basis of CR* measured in situ at anthesis. The specific aims of the study were (i) to study the correlation of the individual CR* values with the total aboveground biomass (TAB) at maturity and also with GY for each wheat cultivar in order to validate the stand-scale results, (ii) to evaluate the effect of pea intercropping with halved wheat density on mean CR* and the corresponding GY using a stand scale over a three-year period, and (iii) to analyse the relationship between mean CR* and GY across the cropping systems and years. In brief, the study examined the relevance of the capacitance method in the field, or more precisely, the efficiency with which wheat grain yield may be predicted by measuring the saturation root capacitance (CR*) at anthesis under different cultivation and climatic conditions. MATERIALS AND METHODS The field study was conducted during three winter wheat growing seasons from 2017 to 2020 (referred to as harvest years 2018, 2019 and 2020) in a certified organic field in Martonvásár, Central Hungary (N 47°18’, E 18°47’, 109 m a.s.l.). The soil was a Haplic Chernozem (36% sand, 41% silt, 23% clay) with a pH value of 7.66, 1.61% CaCO3, 3.22% humus, 1887/361/445 mg kg total N/P/K and 0.309 cm cm water content at field capacity. The climate is continental with a mean (1987-2016) annual temperature of 11.0°C (January: –1.0°C, July: 21.2°C) and annual precipitation of 548 mm, of which 193 mm falls during the main crop growing season (March-June; Fig. 1). There were optimal rainfall conditions in 2018. By contrast, late-winter and Fig. 1. Monthly rainfall (mm, columns) and mean air temperature (°C, lines) at the experimental site (Martonvásár, Hungary) during the winter wheat growing seasons. The long-term (1987–2016) average is displayed as a reference. WHEAT YIELD PREDICTION BY ROOT ELECTRICAL CAPACITANCE 161 spring droughts occurred in the next two seasons with sufficient precipitation only occurring from early May (flowering stage) in 2019 and from late May (milk stage) in 2020. Winter wheat (Triticum aestivum L.) cultivars ‘Mv Nádor’ (“N”) and ‘Mv Kolompos’ (“K”) and the YQCCP composite population (“C”) were sown in October each year in 6 × 1 m plots with 12 cm row spacing as sole crops (“0”) at a density of 300 seeds m, and at half that density (150 seeds m) intercrops (“P”) with winter pea (Pisum sativum L., cv. Aviron; 50 seeds m). The three replications of each treatment were randomly arranged in the same field, with each one being surrounded by a 1 m border strip, but in slightly different places each year. Natural fertilizers and artificial chemicals were not used directly, which latter is even banned in organic agriculture. At the time of anthesis (in early to mid-May, depending on the cultivar and year) 15 wheat plants were randomly selected from the inner rows of each plot. SWC was measured in the 0-12 cm layer 5 cm away from each sample plant (equal to the depth and position of the CR ground electrode) with a calibrated CS620 portable TDR meter (Campbell Sci. Ltd., Loughborough, UK). The relative water saturation (θrel) value was calculated by dividing the measured volumetric SWC values (cm cm) by the predetermined saturation water content of 0.476 cm cm (Cseresnyés et al., 2018). Thereafter, parallel CR was recorded for the selected plants with a U1733C handheld LCR meter (Agilent Co. Ltd., Penang, Malaysia) at 1 kHz, 1 V AC. The ground electrode was a stainless steel rod 15 cm in length and 6 mm in diameter (303S31; RS Pro GmbH., Gmünd, Austria), pushed vertically into the soil 5 cm from the stem to a depth of 12 cm. The plant electrode was clamped to all of the basal parts of the plant 15 mm above the soil (Svačina et al., 2014) after smearing them with conductivity gel. In order to eliminate the SWC effect, all of the CR data were converted into CR*, according to the empirical function: CR* = CR 5.807erel, using the relevant θrel values (for a detailed calculation, see Cseresnyés et al., 2018). After the CR measurements were complete, five randomly selected wheat plants per plot were cut at ground level, and oven-dried at 70°C until a constant weight was achieved in order to determine shoot dry mass (SDM; ±0.001 g). In the last year (2020) the plants chosen for measuring CR were individually tagged. At maturity (in early July), the tagged plants were hand harvested and oven-dried to determine TAB, after which they were hand threshed to obtain plant GY. Thereafter, the plots were harvested mechanically, and the wheat grains were separated from the peas and weighed. The mean plant GY was determined for each plot on the basis of wheat seedling density. The data were analysed with Statistica 13.0 software (StatSoft Inc., Tulsa, OK, USA). The unpaired t-test or one-way ANOVA with Tukey’s posthoc test was performed to compare the means of CR*, SDM and GY (p < 0.05). If the F-test or Bartlett’s test indicated unequal variances, Welch’s t-test or Kruskal-Wallis with Dunn’s posthoc test was used. Linear regression analysis was applied to relate CR* to TAB, SDM and GY. The resultant regressions were compared using a linear analysis of covariance (ANCOVA).
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来源期刊
International Agrophysics
International Agrophysics 农林科学-农艺学
CiteScore
3.60
自引率
9.10%
发文量
27
审稿时长
3 months
期刊介绍: The journal is focused on the soil-plant-atmosphere system. The journal publishes original research and review papers on any subject regarding soil, plant and atmosphere and the interface in between. Manuscripts on postharvest processing and quality of crops are also welcomed. Particularly the journal is focused on the following areas: implications of agricultural land use, soil management and climate change on production of biomass and renewable energy, soil structure, cycling of carbon, water, heat and nutrients, biota, greenhouse gases and environment, soil-plant-atmosphere continuum and ways of its regulation to increase efficiency of water, energy and chemicals in agriculture, postharvest management and processing of agricultural and horticultural products in relation to food quality and safety, mathematical modeling of physical processes affecting environment quality, plant production and postharvest processing, advances in sensors and communication devices to measure and collect information about physical conditions in agricultural and natural environments. Papers accepted in the International Agrophysics should reveal substantial novelty and include thoughtful physical, biological and chemical interpretation and accurate description of the methods used. All manuscripts are initially checked on topic suitability and linguistic quality.
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