覆土浅埋滴灌玉米分阶段亏水条件下AquaCrop与Dual Crop Coefficient模型精度对比研究

近年来,西辽河流域地下水超采问题日益突出,改进灌溉技术降低农业用水可有效解决这一问题,但该技术缺乏科学的水分管理方法及适宜的理论模型。基于单阶段及多阶段亏水情形试验,对比同类农田水分模型精度,优选阶段性亏水管理辅助模型。研究设置7个玉米分阶段亏水调控处理,于2018、2019年进行田间小区试验,取得2个同类模型的本地化参数并比较其模拟精度。结果表明,AquaCrop和双作物系数模型可相近表达玉米冠层发育到最大而未开始衰减期间土壤水分的消耗过程,而对快速生长期与后期1m土层贮水量的模拟差异大。AquaCrop模型在土壤贮水量偏低时高估其实测值,其他情形正负偏差分布相对均匀,双作物系数模型多数情形低估其实测值。AquaCrop模型描述玉米各阶段蒸散量因亏水情形而变化能力优于双作物系数模型。AquaCrop模型和双作物系数模型的标准均方根误差平均值在模拟1 m土层贮水量时分别为4.494%~8.443%、6.017%~8.626%,在模拟蒸散量时分别为8.158%~9.510%、5.980%~15.022%。综合来看,AquaCrop模型表现更好,推荐作为适宜西辽河流域覆土浅埋滴灌玉米水分管理模型。研究可为该区域覆土浅埋滴灌种植玉米选出适宜的水分管理模型,理解新技术条件下玉米分阶段亏水调控机制及田间灌溉管理优化提供参考。

Evaluation of Actual Evapotranspiration and Crop Coefficient in Carrot by Remote Sensing Methodology Using Drainage and River Water to Overcome Reduced Water Availability

Searching for alternative methods for traditional irrigation is World trend at days due to a reduction in water and increased of drought due to climate changes therefore farmers need use modern methods of scheduling water and minimizing water losses while also increasing yield. To meet the future increasing demands water and food there is a need to utilize alternative methods to reduce evaporation, transpiration and deep percolation of water. Any countries use recycled water (drain and sewage) and desalination water from the sea or drains to irrigate crops plus computing actual crop evapotranspiration (ETc) so as to calculate the amount of water to apply to a crop. The paper aims to assess the actual evaporation and evaporation coefficient of carrots, by planting carrots in a field and the crop was exposed to several sources of water (DW and RW) and comparing ETc, Kc and production among plots of three sites (A, B and C). The study used two types of irrigation water (drain water (DW) and river water (RW)). The results were to monthly rate and accumulated actual evapotranspiration to C (irrigation by RW only) more than A (67% RW and 33% DW) and B (17% RW and 83% DW) via 7% and 58%, respectively. The yield to C more than A and B by 17% and 75%, respectively. In conclusion the use of DW can cause a reduction in crop consumptive of carrot crops also causes a reduction in yield, crop length, root length, root size, canopy of crop, number of leaves and biomass of the plant therefore, the drainage water needs to treated before irrigating crops And making use of it to irrigate the fields and fill the shortfall in the amount of water from the river. The drain water helped on filling the water shortage due to climate changes and giving production of carrot crop but less than river water.

Difference between Responses of Potato Plant Height to Corrected FAO-56-recommended Crop Coefficient and Measured Crop Coefficient

This study was conducted to establish a simple convenient method for calculating crop coefficient, and provide a certain basis for the research of the empirical formula for calculating crop coefficient with plant height which could be measured conveniently with regional differences, especially for the establishment of accurate irrigation schedule of potato in Yunnan. By the field experiment on potato under the condition of drip irrigation, it was found that the models of plant height with corrected FAO-56-recommended K and measured K were a quartic polynomial and a cubic polynomial, respectively, and the polynomial of potato plant height with measured crop coefficient was simpler with higher degree of fitting; and the differences between the period with the highest change rate of potato plant height and the periods with the greatest FAO-56-recommended K and measured K exhibited a differences of 3 d. In conclusion： In the future study of simple or empirical formula calculation of crop coefficient, plant height should be considered as a main dependent variable in that the calculation result would be closer to the measured crop coefficient with the problem of regional difference existing in the FAO method solved and the formula might be simpler; and the irrigation time of potato should be 3 d earlier than the irrigation time determined according to the corrected FAO-56-recommended crop coefficient, especially in the key water requirement stages of potato.

Evapotranspiration, Yield and Crop Coefficient of Irrigated Maize Under Straw Mulch

Maize (Zea mays L.), a staple crop grown from June to September during the rainy season on the North China Plain,is usually inter-planted in winter wheat (Triticum aestivum L.) fields about one week before harvesting of the winterwheat. In order to improve irrigation efficiency in this region of serious water shortage, field studies in 1999 and 2001, twodry seasons with less than average seasonal rainfall, were conducted with up to five irrigation applications to determineevapotranspiration, calculate the crop coefficient, and optimize the irrigation schedule with maize under mulch, as well asto establish the effects of irrigation timing and the number of applications on grain yield and water use efficiency (WUE)of maize. Results showed that with grain production at about 8 000 kg ha-1 the total evapotranspiration and WUE ofirrigated maize under mulch were about 380-400 mm and 2.0-2.2 kg m-3, respectively. Also in 2001 WUE of maizewith mulch for the treatment with three irrigations was 11.8% better than that without mulch. In the 1999 and 2001seasons, maize yield significantly improved (P = 0.05) with four irrigation applications, however, further increases werenot significant. At the same time there were no significant differences for WUE with two to four irrigation applications.In the 2001 season mulch lead to a decrease of 50 mm in the total soil evaporation, and the maize crop coefficient undermulch varied between 0.3-1.3 with a seasonal average of 1.0.

Determining Crop and Pan Coefficients for Cauliflower and Red Cabbage Crops Under Cool Season Semiarid Climatic Conditions

The aim of this study was to estimate the evapotranspiration of cauliflower and red cabbage crops grown under cool season semiarid climatic conditions from Class A pan evaporation. Actual evapotranspiration （ETc） of cauliflower and red cabbage crops was calculated according to the water balance approach. Reference evapotranspiration （ETo） was calculated with FAO Penman-Monteith equation. Pan evaporation （Epan） was measured by using Class A pan. Seasonal ETc was determined as 475 mm for cauliflower and 556 nun for red cabbage. Seasonal pan coefficient （kp=ETo/Epan） was determined as 0.82, and the seasonal crop coefficient （kc=ETc/ETo） was determined as 0.84 for cauliflower and 0.83 for red cabbage. So the evapotranspiration of cauliflower and red cabbage crops was estimated as 70% Class A pan evaporation.

Estimating Crop Coefficient in Intermittent Irrigation Paddy Fields Using Excel Solver

The current study proposes a novel method using Excel Solver to estimate, from limited data, crop coefficient （Kc） in paddy fields under intermittent irrigation （11）. The proposed method was examined in a field experiment conducted at Karang Sari Village, Bekasi, West Java, Indonesia during the first rice season of 2007/2008 （December 2007 to April 2008） in the rainy season. As the control, continuous flooding irrigation （CF） was applied to the conventional rice cultivation fields. Based on the observed water storage, Excel Solver was used to estimate crop evapotranspiration. Estimated crop evapotranspiration was used to compute Kc value, then the average Kc values at each growth stage were compared with that for the CF treatment. The estimation method was evaluated by comparing estimated crop evapotranspiration and the crop evapotranspiration derived by the well established FAO procedure. Excel Solver estimated crop evapotranspiration accurately with R2 values higher than 0.81. Accordingly, more than 81% of the FAO crop evapotranspiration was described by the proposed method. Thus, Kc value could be well determined from those estimated crop evapotranspiration. Under the II treatment, the average Kc values were 0.70, 1.06, 1.24 and 1：22 for the initial, crop development, reproductive and late stages, respectively. These values were lower than those under the CF treatment for initial and crop development stages because of a minimal soil evaporation and intense dryness during these stages. However, average Kc values under the II treatment were higher than those under the CF treatment at the reproductive and late stages, indicating that the II treatment promoted more plant activity particularly for dry biomass production as indicated by a greater number of tillers per hill.

Water requirements and single and dual crop coefficients of sugarcane grown in a tropical region, Brazil

A field experiment was conducted throughout 2009/2010 in a sugarcane field of a commercial distillery located on the coastal area of Paraiba state, Brazil. The objectives were to determine sugarcane water requirements and to test the single and dual crop coefficients by comparing the calculated values of ET with measured ones. Crop evapotranspiration was determined by field water balance, reference evapotranspiration (ETo) by the Penman-Monteith approach, while single and dual crop coefficients were computed through the standard FAO-56 methodology. The experimental area was cultivated with irrigation applied weekly by a centre pivot system in addition to rainfall and the irrigation scheduling was based on 100% ETo. Three statistical tests, mean bias difference (MBD), normalized root mean square difference (NRMSD) and regression analysis, were used to evaluate the performance of single and dual crop coefficients. Results showed that there was a notable symmetry between ET measured and ET calculated by Kc dual. The ET values, calculated from Kc single, underestimated those obtained from soil water balance measurements by 36%.

Spectral Crop Coefficient Approach for Estimating Daily Crop Water Use

While the amount of water used by a crop can be measured using lysimeters or eddy covariance systems, it is more common to estimate this quantity based on weather data and crop-related factors. Among these approaches, the standard crop coefficient method has gained widespread use. A limitation of the standard crop coefficient approach is that it applies to “standard conditions” that are invariant from field to field. In this article, we describe a method for estimating daily crop water use (CWU) that is specific to individual fields. This method, the “spectral crop coefficient” approach, utilizes a crop coefficient numerically equivalent to the crop ground cover observed in a field using remote sensing. This “spectral crop coefficient” Ksp is multiplied by potential evapotranspiration determined from standard weather observations to estimate CWU. We present results from a study involving three farmers' fields in the Texas High Plains in which CWU estimated using the Ksp approach is compared to observed values obtained from eddy covariance measurements. Statistical analysis of the results suggests that the Ksp approach can produce reasonably accurate estimates of daily CWU under a variety of irrigation strategies from fully irrigated to dryland. These results suggest that the Ksp?approach could be effectively used in applications such as operational irrigation scheduling, where its field-specific nature could minimize over-irrigation and support water conservation.

Determination of Upland Rice Cultivar Coefficient Specific Parameters for DSSAT (Version 4.7)-CERES-Rice Crop Simulation Model and Evaluation of the Crop Model under Different Temperature Treatments conditions

To develop basis for strategic or arranged decision making towards crop yield improvement in Thailand, a new method in which crop models could be used is essential. Therefore, the objective of this study was to measure cultivar specific parameters by using DSSAT (v4.7) Cropping Simulation Model (CSM) with five upland rice genotypes namely Dawk Pa-yawm, Mai Tahk, Bow Leb Nahng, Dawk Kha 50 and Dawk Kahm. Experiment was laid out in a Completely Randomized Design (CRD) with split plot design. Results showed that five upland rice genotypes had significantly affected each other by different temperature treatments (28°C, 30°C, 32°C) with grain yield, tops weight, harvest index, flowering, and maturity date. At the same time, all the phenological traits had highly significant variation with the genotypes. The cultivar specific parameters obtained by using a temperature tolerant cultivar (Basmati 385) with five upland genotypes involved in the DSSAT4.7-CSM. Model evaluation results indicated that utilizing the estimated cultivar coefficient parameters, model simulated well with varying temperature treatments as indicated by the agreement index (d-statistic) closer to unity. Hence, it was estimated that model calibration and evaluation was realistic in the limits of test cropping seasons and that CSM fitted with cultivar specific parameters can be used in simulation studies for investigation, farm managing or decision making. This electronic document is a “live” template. The various components of your paper [title, text, heads, etc.] are already defined on the style sheet, as illustrated by the portions given in this document.

Seasonal variation of evapotranspiration,Priestley-Taylor coefficient and crop coefficient in diverse landscapes

Priestley-Taylor equation(PT)and the Penman-Monteith equation(PM)are commonly used methods for regional evapotranspiration monitoring,using the PT coefficient(α_(a))and PM crop/vegetation coefficient(K_(c)).This paper investigates the seasonal changes inα_(a)and K_(c)at five sites in Australia and China,to understand the relation-ship between environmental conditions and evapotranspiration when applying different evaporation estimation methods.The research shows that higher actual evapotranspiration does not lead to higherα_(a)and K_(c)values.α_(a)and K_(c)perform similarly in cropland and forest environments in both China and Australia.Bothα_(a)and K_(c)continuously increase to a peak during the growing season and then decrease to their lowest values during the winter season.Considering K_(c)’s similar performance toα_(a)and its greater data processing requirements,K_(c)has few advantages for estimating regional evapotranspiration.Applying the Priestley-Taylor equation with a regional𝛼indicator will enhance the accuracy and reduce the workload when estimating regional evapotranspiration for similar landcover types based on remote sensing.

The Joule–Thomson effect of (CO_(2)+H_(2)) binary system relevant to gas switching reforming with carbon capture and storage(CCS)

The Joule-Thomson effect is one of the important thermodynamic properties in the system relevant to gas switching reforming with carbon capture and storage(CCS). In this work, a set of apparatus was set up to determine the Joule-Thomson effect of binary mixtures(CO_(2)+ H_(2)). The accuracy of the apparatus was verified by comparing with the experimental data of carbon dioxide. The Joule-Thomson coefficients(μ_(JT)) for(CO_(2)+ H_(2)) binary mixtures with mole fractions of carbon dioxide(x_(CO_(2))= 0.1, 0.26, 0.5,0.86, 0.94) along six isotherms at various pressures were measured. Five equations of state EOSs(PR,SRK, PR, BWR and GERG-2008 equation) were used to calculate the μ_(JT)for both pure systems and binary systems, among which the GERG-2008 predicted best with a wide range of pressure and temperature.Moreover, the Joule-Thomson inversion curves(JTIC) were calculated with five equations of state. A comparison was made between experimental data and predicted data for the inversion curve of CO_(2). The investigated EOSs show a similar prediction of the low-temperature branch of the JTIC for both pure and binary systems, except for the BWRS equation of state. Among all the equations, SRK has the most similar result to GERG-2008 for predicting JTIC.

拱架送/回风方式对日光温室冬季作物冠层区热环境的影响

传统日光温室被动的热环境调控模式难以满足温室作物冠层区空气温度和速度调控需求,且能源利用效率低下。为了改进日光温室热环境精准调控方法和提高温室能源利用效率,该研究结合日光温室围护结构特点,提出了一种日光温室拱架的送/回风方法,并基于温室作物多孔介质模型,建立了拱架送/回风系统温室的数值传热模型。采用空气温度与速度不均匀系数、气流速度适宜区面积比、能量利用系数以及累计有效积温等评价参数,研究了下送上回、中间回风和上送下回等3种温室拱架送/回风方式对日光温室冬季作物冠层区热环境的影响。结果表明,与中间回风和上送下回通风方式相比,下送上回通风方式对不同作物冠层高度处的空气温度和速度调控的结果最优,且不同作物冠层高度处气流速度适宜区面积比和累计有效积温都最大。当采用下送上回通风方式时,与送风干管风速为9、11和12 m/s相比,送风干管风速为10 m/s的能量利用系数最大,在作物冠层高度0.4、0.6、0.8和1.0 m处的能量利用系数分别为0.976、0.982、0.985和0.987,并且不同作物冠层高度处的空气温度不均匀系数和速度不均匀系数也都最小。因此,下送上回通风方式的推荐送风干管风速为10 m/s。该研究可为日光温室热环境的精准调控提供参考。

湖北省农作物碳汇的阶段性特征、空间差异与动态演进——基于1997—2022年湖北省农作物数据

湖北省是我国农业大省,科学测算湖北省农作物碳汇,摸清本底,对碳汇交易和农业低碳发展具有重要意义。对湖北省1997—2022年的农作物碳汇量进行测算,运用Dagum基尼系数、Kernel密度估计和Markov链,探讨湖北省农作物碳汇量的地区差异和动态演进特征。结果表明:1997—2022年,湖北省农作物碳汇量呈现“W”形波动上升的态势,平均值为12085.30万t,其中粮食作物为湖北省农作物碳汇的主要贡献来源。“双碳”背景下对湖北省的三大地区及各市(州、林区)展开分析,发现1997—2022年鄂东地区农作物碳汇量位于湖北省三大地区的第一位。Dagum基尼系数分析显示湖北省农作物碳汇存在一定的地区差异,其差异主要来自于超变密度,平均贡献率为53.58%,湖北省农作物碳汇总量具有较强的稳定性,具有一定的俱乐部趋同特征。最后提出相关对策建议,如开发农作物碳汇核算方法学和标准,制定差异化的农业碳汇增汇政策,探索农业碳汇交易机制及价值实现。

基于单作物系数法的温室秋季生菜蒸散量估算及验证

【目的】基于单作物系数法估算温室秋季生菜蒸散量。【方法】通过2021—2022年温室秋季生菜试验,根据各生育期影响因素修正FAO-56推荐作物系数值,即生育前期根据ET0值和灌溉频率修正,生育中期和生育后期根据气象因素和株高修正,并采用单作物系数法对温室生菜蒸散量进行估算,以称重式蒸渗仪实测蒸散量ETcm为标准值对蒸散量估算值ETcs进行验证。【结果】不同试验年度逐日ET0均呈逐渐降低变化趋势,介于1.18~2.44 mm/d。温室生菜作物系数修正值(Kc adj)和实测值(K_(c loc))均在生育前期最高,2 a均值分别为0.74±0.13和0.76±0.13;进入快速发育期后二者均呈降低趋势,并在生育中后期逐渐稳定在0.5~0.6。各生育阶段的Kc adj较FAO推荐值(Kc FAO)更接近实测值(K_(c loc)),Kc adj和K_(c loc)相对误差介于-6.7%~5.4%。应用修正单作物系数法估算温室秋季生菜ETcs与实测ETcm的日均值分别为1.310 mm/d和1.283 mm/d,决定系数(R^(2))、平均绝对误差(MAE)、均方根误差(RMSE)、一致性指数(d)分别为0.975、0.176 mm/d、0.222 mm/d、0.955。【结论】修正单作物系数法能够较为准确的估算温室秋季生菜蒸散量。

模拟CCS技术CO_2泄漏对C_3、C_4作物土壤化学性质的影响

为确定CCS技术中封存的CO2是否发生泄露及估算泄漏量,分别选取绿豆、荞麦（C3作物）和高粱、玉米（C4作物）作为研究材料,采用实验室CO2人工气候箱中盆栽实验的方法,模拟CCS技术中CO2泄露情况。通过测定土壤pH、无机离子（K＋、Na＋、Ca2＋、Mg2＋、Cl-、HCO3-、SO42-）及肥力指标（TN、AHN、TP、AP、AK、OM、CEC）,研究不同高浓度CO2对C3和C4作物土壤化学性质及肥力的影响。研究结果表明：（1）高浓度CO2对C3、C4作物土壤pH的影响不显著,pH变化值仅在（-0.03）~0.06之间;（2）同种类型作物土壤离子浓度变化的整体趋势基本相同：CO2浓度相对较低时,土壤离子含量降低;CO2浓度升高时,土壤离子含量增加。对相同离子而言,C3作物土壤中离子含量变化幅度比C4作物大;（3）高浓度CO2对C3、C4作物土壤AHN、AK、AP、CEC指标的影响情况相异,但对TN、TP、OM含量的影响情况相同。可通过监测作物土壤中离子及肥力指标的含量变化,判断CCS项目中CO2是否发生泄露及估算泄漏量,减轻CO2泄漏带来的危害。

水足迹视角下黄土丘陵区农业水土资源匹配格局——以山西省和顺县为例

从水足迹视角出发,运用CROPWAT及标准差椭圆模型分析2010—2019年山西省和顺县乡镇域主要农作物生产水足迹和耕地面积的时空变化,运用基尼系数及空间失配指数深入研究2010年、2014年、2019年乡镇域农业水土资源时空匹配格局,并明确调控方向。结果表明,研究期间,和顺县作物生产水足迹、蓝水足迹、绿水足迹和耕地面积总体上均呈下降趋势;绿水足迹对各区域作物生产水足迹的构成贡献最大,占比均超过62.0%;和顺县西部地区作物生产水足迹和耕地的空间聚集性不断增强;和顺县作物生产水足迹、蓝水足迹、绿水足迹与耕地之间的空间失配均逐渐加剧,中部和东部地区农业水土资源分别为中度失配和重度失配,是和顺县未来农业水土资源调控的重点地区;可以将县域10个乡镇分别划分为水源涵养调蓄、水土优化调控与引水节水灌溉3个调控区。总的来说,受社会经济、生产要素投入和气候条件的影响,和顺县农业水土资源匹配协调水平处于失衡状态,但在调控区划分的基础上,有针对性地进行人工调控,仍可实现农业水土资源匹配协调水平的较大提升。

宁夏沿黄绿洲参考作物蒸散演变特征及其归因

参考作物蒸散(Reference crop evapotranspiration,ET_(0))是生态水文过程中的关键因子,研究ET_(0)在干旱绿洲区的演变,不仅有助于理解气候变化背景下的绿洲水文过程响应,亦对绿洲水土资源高效配置和生态系统稳定性维持有指导意义。以宁夏沿黄绿洲为例,基于1960—2019年的气象资料和Penman-Monteith模型计算ET_(0),利用Mann-kendall突变检验、相对敏感系数和Morlet小波分析等方法,对宁夏沿黄绿洲近60 a的ET_(0)演变特征及其归因进行研究。结果表明:(1)宁夏沿黄绿洲ET_(0)年内呈单峰形态,ET_(0)在5—7月间较高,累积ET_(0)占年总ET_(0)的43.6%;近60 a的ET_(0)年均值为1226.38 mm,并以1.66 mm/a(P<0.01)幅度上升,但年际波动特征明显,其中在1988年突变之前,ET_(0)无显著变化趋势,而突变之后则以每10 a左右的周期显著增加或降低。(2)年ET_(0)主要以20—40 a和50—60 a周期振荡,且有多重时间尺度的复杂嵌套现象,不同季节的周期振荡差异较大,夏、秋季振荡幅度较强,其周期接近于年ET_(0)规律,而冬、春季振荡幅度较弱。(3)虽然ET_(0)与6种气象因子均存在显著相关性,但ET_(0)对不同气象因子的敏感性存在差异,其中对最高温度和相对湿度的敏感性较高,敏感系数分别为11.58%和8.40%。(4)宁夏沿黄绿洲ET_(0)与区域气候变化特征有较强的耦合性,区域气候的持续升温和相对湿度持续降低、以及由此引发的饱和水汽压亏缺持续增强是推动ET_(0)上升的重要原因,而气候由湿润向干旱的突变和平均风速的异常波动是诱发ET_(0)突变的原因。

基于CCS软件的IIR滤波器实验设计

借助CCS软件完成了IIR滤波器实验设计,主要设计工作包括输入序列x(n)设计、求解系统函数H(z)的程序设计和求解常系数差分方程的程序设计。首先,通过输入序列x(n)设计和系统函数H(z)设计,求出x(n)和常系数差分方程的系数;其次,调用递推方法求解常系数差分方程的子程序,计算IIR滤波器的输出序列y(n)。借助time/frequency选单观察y(n)的时域波形和频谱。

海东市平安区土壤与农作物Se含量分布特征

为探究青海省海东市平安区的土壤及农作物的硒含量及富集特征,系统地采集分析了平安区七个乡镇152份0~50 cm深度土壤样品及1161份植物样品,采用氢化物-原子荧光光谱法测定土壤及作物硒含量。结果表明,平安区表层硒含量平均值为0.27 mg/kg,高于全国及世界土壤硒平均值,有75.36%的地区处于适量硒状态,且三合镇的土壤硒含量最高,古城乡最低,总体上各乡镇采集的0~10 cm、10~20 cm、20~30 cm、30~50 cm土层之间的硒含量差异不显著,但随土壤深度的增加,硒含量逐渐降低。在几种作物中,油菜的平均硒含量最高,达到富硒标准,小麦、玉米、豌豆、燕麦、马铃薯硒含量平均值均达到足硒标准,青稞和蚕豆在土壤硒含量较高的三合镇达到足硒标准以上。综合分析,土壤硒含量与相应的作物籽粒硒含量呈正相关,油菜、小麦、玉米硒的富集系数较高,对硒具有良好的吸收能力,因此适宜在相应的富硒地发展富硒农产品,豌豆、蚕豆、燕麦、青稞属于中等富硒作物,马铃薯的富集系数最小而变异系数最高,适合在硒含量较高的地方种植马铃薯。

修正双作物系数法估算不同计划湿润层深度下春玉米蒸散

为利用修正后的双作物系数法来准确估算不同生育期计划湿润层深度下春玉米蒸散量(ET_(c))。根据不同生育期设定不同计划湿润层深度(T1、T2、T3),试验灌水下限设定为65%田间持水量(θ_(FC)),灌水上限为100%θ_(FC)。利用实测叶面积指数(LAI)修正双作物系数模型中的基础作物系数(K_(cb))和土壤蒸发系数(K_(e)),并结合山西省中心灌溉试验站的气象数据等估算了春玉米ETc,同时用实测数据对估算值进行适应性评价。2023年T1、T2、T3春玉米全生育期ETc分别为438.46 mm、397.68 mm和419.86 mm;估算的全生育期ET_(c)为454.08 mm、431.87 mm和452.47 mm。改正后的双作物系数法的决定系数(R^(2))、均方根误差(RMSE)、模型效率系数(E_(ns))、平均绝对误差(AAE),T1为0.82、0.67 mm/d、0.84和0.57 mm/d,T2为0.81、0.79 mm/d、0.78和0.55 mm/d,T3为0.75、0.90 mm/d、0.71和0.60 mm/d。灌水较多的T1和T2的R2和E_(ns)均高于T3,RMSE和AAE小于T3,T1和T2的参数相差不大,说明灌水量较少时会影响模型的估算精度,T1处理的灌水量最大,蒸散量最大,模型的拟合程度最高,T2和T3次之。因此,修正后的双作物系数法可用于不同湿润层深度下春玉米蒸散量的预测,该模型更适用于水分充足条件下春玉米蒸散量估算。