Time series analysis of irrigation return flow in a semi-arid agricultural region,Iran

The irrigation return-flow coefficient (IRFC) is based on rule of thumb estimations in most aquifers in Iran. The errors may be significant, and thus misleading for water resources management. We used lysimeters to more accurately predict IRFC. Five wheat and barley farms of different soil textures, which were irrigated using a border system, plus one with a sprinkler system, were selected for the installation of lysimeters. The practices at each farm were applied to the lysimeters. Irrigation return flows (IRF) were measured every other day over two growing seasons. The IRF time series displayed sharp peaks at the initial stages of the growing season and decreasing towards the end. IRFCs were classified into early and late stages. The average IRFC during the early stage was 29.9%, decreasing to 6.5% in the late stage. High IRFC values are due to the limitations of border irrigation to provide a small uniform amount of water, and over-irrigation due to low water demand during the early stage of growth. Variations in annual IRFCs of 0.4 to 38.7% are functions of total applied water, border length, management and soil texture. The early stage IRFC for the sprinkler system was small. Therefore, high early stage IRFCs can be reduced by changing from border irrigation to a sprinkler system.     

Estimation of reference evapotranspiration and crop coefficient in wheat under semi-arid environment in India

Abstract

The comparison of six standard reference evapotranspiration (ETo) estimate models was carried out with measured lysimeter evapotranspiration (ETc) in wheat crop in a semi-arid environment at Rahuri, India. The globally accepted reference evapotranspiration model of FAO 56 Penman Monteith underestimated the references ETo by 19.2% (420.5 mm) over lysimeter ET (520.7 mm). Out of the remaining five models, the Hargreaves model ranked first and was overestimated by 6.5% followed by the Blaney Criddle model (underestimated by ?5.6%). The references ETo by pan evaporation model underestimated the reference ETo to the extent of ?28.8%. The influence of statistical indicators like RMSE, MBE which was computed by considering Lysimeter ETc as standard, was quite low in the Hargreaves model compared to the rest of the models and hence, the Hargreaves method is quite acceptable for ETo estimates as this method requires much less climatic parameters (temperature and extraterrestrial radiation) than Penman Monteith (FAO56) and Modified Penman of FAO 24 as these models require aerodynamic and radiation terms, besides additional physical terms in former models of ETo estimates. The seasonal crop coefficients were 1.24, 1.13, 0.94, 0.85, 1.06 and 1.40 in Penman Monteith, Modified Penman, Hargreaves, Radiation balance, Blaney Criddle and Pan Evaporation models, respectively.     

应用层次分析法计算分插机构优化目标的权重

分插机构优化是一个多目标、多参数优化问题。该文在分插机构可视化辅助分析优化平台上得到多组可行优化结果之后,为进一步评价出最优解,对评判方法中权值的求解方法进行了应用分析。将分插机构的12个优化目标中的10个作为评判方法的评价指标,分别应用层次分析法中的0～2三标度法和1～9标度法确定各评价指标的权值,即通过建立初始评判矩阵和比较矩阵,并通过一致性检验得到最终判断矩阵,继而得到所有目标的权重集,其结果分别为(0.6216,0.2450,0.0881,0.0302,0.0101,0.0033,0.0011,0.0004,0.0001,0.0001)和(0.6892,0.2233,0.0620,0.0175,0.0052,0.0017,0.0006,0.0003,0.0001,0.0001)。2组结果均与实际相符,1～9标度法结果精度更高。试验结果表明,应用AHP求解分插机构的优化目标权值是合理、客观、有效的。此方法可为一般农机多目标优化问题的权值求解起到一定的借鉴作用。     

基于称量反馈的设施番茄灌溉系统的构建与应用

为提高设施番茄灌溉的精准性,该研究设计了一种基于称量反馈的灌溉系统,该系统包括称量反馈模块、多源信息采集传输模块、灌溉决策模块与水肥执行模块。称量反馈灌溉决策首先利用卫星定位模组获取灌溉地经纬度信息自动计算当天的日出时刻、日落时刻、日中时刻,结合椰糠条吸水特性与番茄植株日需水量变化规律,把1 d自动划分为4个不同的动态灌溉阶段;根据温室内温湿度信息及排液电导率（electrical conductivity,EC）值反馈的番茄植株根部信息,制定了一般模式灌溉肥液或洗盐模式灌溉清水（或低浓度营养液）。设计试验以基于辐射累积控制灌溉、定时灌溉作为对照,分别从栽培效果、灌溉效果、应用效益方面验证该灌溉系统的应用效果。结果显示使用该称量反馈灌溉系统比基于辐射累积控制灌溉系统灌溉量增加1.8%,用肥量减少7.3%,排液比降低7.9%,排液EC值降低9.3%;与定时灌溉方式相比灌溉量减少11.3%,用肥量减少20.0%,排液比降低17.9%,排液EC值降低4.9%。栽培效果显示,使用该称量反馈灌溉系统的椰糠条栽培番茄在茎粗、叶片叶绿素相对含量、糖度值、单穗质量和基于辐射累积的控制灌溉相比无显著性差异（P>0.05）,但株高增加4.8%;与定时灌溉相比在株高、茎粗、叶片叶绿素相对含量、糖度值、单穗质量均无显著性差异（P>0.05）。预计使用该称量反馈灌溉系统,园区15栋日光温室（1.22 hm²）相比基于辐射累积控制灌溉,应用效益月节约0.276万元,与定时灌溉方式相比,园区月节约2.247万元。该系统简化了番茄植株需水量的计算过程,实现了番茄栽培水分的精准感知与按需精量灌溉。     

河北坝上地区雨养裸燕麦田间蒸散规律

依托大型称重式蒸渗仪在2018年和2019年裸燕麦生育期内进行田间蒸散量的测定,利用根区水质模型(RZWQM2)对田间蒸散量变化的动态过程进行了模拟,并分析了不同时间尺度下田间蒸散特征及其环境影响因素.结果表明:RZWQM2模型对裸燕麦生育期内田间蒸散量模拟结果较好,2018年和2019年绝对平均误差(MAE)分别为1...     

Seasonal trends in hydraulic conductance of field-grown ‘Valencia’ organge trees

Leaf water potential (ψ₁), whole tree transpiration (F) and leaf surface conductance (g), together with a number of environmental parameters, were measured from early summer until late winter in a well-watered mature ‘Valencia’ orange (Citrus sinensis (L.) Osb.) orchard during the growing season of 1977/78. F and g showed a seasonal trend, with maximum values reached during the late summer. Tree conductance (C_tree), calculated as the ratio between transpiration and the water potential difference between the wet soil and the sunlit leaves, was found to vary seasonally and showed maximum values during late summer. The soil temperature (T_s) showed a seasonal trend similar to C_tree. Analysis of this and other data from the literature confirmed that the sensitivity of tree conductance to soil temperature is related to the climatic origin of the plant species.The linear regression fitted to the relationship between C_tree and T_s was used to calculate soil temperature at apparent zero C_tree. This datum can be used as an index of plant sensitivity to root medium temperature.     

Glyphosate application in forest—ecological aspects

The vegetation of four different forest soils in lysimeters was killed with glyphosate. New vegetation became established in some of the treated lysimeters the year after application. During this year, leachates from lysimeters without vegetation had nitrate concentrations up to 4.5 mM NO₃ ^? in the fall. A corresponding increase in leached cations was evident. The settlement of one raspberry or one willow herb in treated lysimeters effectively hindered nitrate leaching as soon as the plants were sufficiently large (in mid‐summer). As plants became established in treated lysimeters, the chemistry of these leachates approached those of untreated lysimeters. The absolute effect of even small plants in controlling water regime and water chemistry was evident.     

Determining fertilizer phosphorus requirement of upland rice

Abstract

Assessing the fertilizer phosphorus requirement (FPR) of crops is an important component of research for efficient and rational use of fertilizers. Soil and plant tests are used to determine the FPR of crops. Two methods were evaluated for determining the FPR of upland rice grown on an Ultisol in the humid forest zone of Cote d'Ivoire. The first method used a simple model based on P uptake using the equation: FPR=(Up‐U0)/PRF, where Up is P uptake at a given yield, Uo is P uptake from unfertilized soil, and PRF is the P recovery fraction of applied P. The parameters, U0, Up, and FPR were determined in field experiments for the rice cultivars grown on an Ultisol under rainfed upland conditions. The second method was based on the P applied, P uptake, and grain yield relationships for upland rice. First, P uptake at a given rice yield was determined from the relationship between total P uptake and grain yield. The amount of fertilizer P applied for the given P uptake and grain yield was then, determined from the relationship between P applied and P uptake. There was a good agreement between the observed values of FPR and the predicted values of FPR determined by the two methods. The results suggest that the simple model based on P uptake can be utilized for determining the fertilizer P requirements of crops.     

Interpretation of lysimeter weighing data affected by wind

Weighing lysimeters are valuable devices for measuring water‐balance components with high temporal resolution and high accuracy. However, some older lysimeter facilities still operate with lever‐arm‐counterbalance weighing systems that are sensitive to disturbances, e.g., forces exerted by wind. Filtering and averaging are commonly used for processing noisy raw data. We studied some data of a lever‐arm weighing system and performed additional experiments in order to (1) determine the measurement accuracy of the current weighing scheme (facility, and measuring and averaging procedure) regarding wind effects, (2) describe the oscillation behavior, (3) test the mechanical performance of the system, and (4) adapt the averaging procedure with respect to improved interpretation of the weighing data. The measurement accuracy for a wind velocity < 5 m s^–1, measured in 10 m height, was ≈ ± 0.4 kg (equivalent to ± 0.14 mm); at a higher wind velocity, the accuracy was three times lower, but there was no linear relationship. Additional experiments showed that the weighing system is oscillating with more or less irregular amplitudes. A loading–unloading experiment delivered proper results of the measured loads. The mechanical system reacted immediately, and no directional effects were found. However, small changes of < 1 kg could hardly be determined due to the oscillations. A time series of raw data measured every 2 s served as basis for improving the averaging method. A moving average from 64 values was computed representing the currently used method, and serving as reference. With this procedure an accuracy of ± 0.38 kg could be reached. Averaging 150 values led to an accuracy of ± 0.28 kg (0.1 mm) for a wind velocity < 5 m s^–1.