豫北地区基于天气预报的ET_0预测模型

运用茆智提出的ET0预测方法,并结合其他学者对方法的改进,利用日常的天气预报信息,分别对豫北地区的冬小麦和夏玉米生育期内的ET0进行了预测。结果表明,在冬小麦生育期的ET0预测值,返青前绝对误差不超过0.8mm/d,返青以后93%的预测结果相对误差小于20%,53%的预测结果小于10%;在夏玉米生育时期内的预测值,95...     

参考作物腾发量计算方法在玛纳斯河流域的应用比较

基于玛纳斯河流城4个气象站莫索湾、炮台、石河子、乌兰乌苏1961-2005年的日观测气象数据,采用SWAT2000模型里引入的Penman- Monteith, Hargreaves, Priestley-Taylor方法计算每日参考作物腾发量(ETo),比较计算结果之间的差异性.结果表明,莫索湾站与炮台站Hargre...     

气象因子的变化对参考作物蒸发蒸腾量的影响

根据东江流域1961—2005年的气象资料,利用平均影响量和气象因子缺失数值试验,分析气象因子变化对参考作物蒸发蒸腾量的影响。结果表明,日照时数的平均影响量最大,温度、相对湿度其次,二者相近,风速最小;夏季日照时数的平均影响量比其他因子大得多,冬、春季日照时数的平均影响量依然最大,但与温度、相对湿度的平均影响量差距减小...     

车辆防抱制动系统滑移率自适应控制策略

分析了车辆制动过程的数学模型,为了克服模型非线性、变参数对系统的影响,采用了参考模型自适应控制.为了适应各种路况条件,使车辆以比较理想的滑移率制动,缩短制动时间,提出了滑移率自适应调节方法.通过仿真证明,该方法简单可行,控制效果好.     

Inverse Modeling to Quantify Irrigation System Characteristics and Operational Management

Remotely sensed (RS) data is a major source to obtain spatialdata required for hydrological models. The challenge for thefuture is to obtain besides the more direct observable data(landcover, leaf area index, digital elevation model andevapotranspiration), non-visible data such as soilcharacteristics, groundwater depth and irrigation practices.In this study we have explore the option of using inversemodeling to obtain these non-RS-visible data. For a commandarea in Haryana, India, we applied for the 2000–2001 rabiseason a RS-GIS-combined inverse modeling approach to derivenon-RS-visible data required in the regional application ofhydrological models. A Genetic Algorithm loaded stochasticphysically based soil-water-atmosphere-plant model (SWAP) wasdeveloped for the inverse problem and used in the study. Theresults showed good agreement with the inventoried data suchas soil hydraulic properties, sowing dates, groundwaterdepths, irrigation practices and water quality. The deriveddata could be used to predict the state of the system at anytime in the cropping season, which can be used to evaluateoperational management strategies.     

作物节水灌溉需水规律研究

基于节水灌溉条件下作物需水量试验资料,分析了控制灌溉和覆膜旱作节水灌溉的水稻需水规律以及节水高效灌溉模式下冬小麦、夏玉米和棉花作物的需水规律。结果表明,节水灌溉模式通过对水稻、冬小麦、夏玉米和棉花等作物产生的生长调控作用与补偿生长效应,使植株蒸腾量和棵间蒸发量较大幅度减少,各阶段需水量、需水强度和需水模系数均发生显著变化,形成了节水灌溉模式的主要农作物新的需水规律。可为节水灌溉制度的制定、节水型灌区动态配水及灌溉预报等提供科学依据。     

日光温室作物蒸发蒸腾量的计算方法研究及其评价

对FAO推荐计算参考作物蒸发蒸腾量的Penman-Monteith(缩写为P-M)公式,在日光温室微气候的条件应用作了详细的分析。将P-M公式分为2个部分,即辐射项(ETrad)和空气动力学项(ETaero),推导出了计算温室内参考作物蒸发蒸腾量的P-M修正公式,解决了P-M公式假定温室内风速为“0”所引起的一系列问题。并根据2004年和2005年温室内实测气象数据和水面蒸发对其进行了验证,通过相关分析得出用修正后的P-M公式计算作物蒸发蒸腾量比FAO推荐的P-M公式计算值误差小、精度高。建议在日光温室里使用修正后的P-M公式计算参考作物的蒸发蒸腾量。     

Remote sensing of biotic and abiotic stress for irrigation management of cotton

The applicability of commercially available remote sensing instrumentation was evaluated for site-specific management of abiotic and biotic stress on cotton (Gossypium hirsutum L.) grown under a center pivot low energy precision application (LEPA) irrigation system. This study was conducted in a field where three irrigation regimes (100%, 75%, and 50% ET_c) were imposed on areas of Phymatotrichum (root rot) with the specific objectives to (1) examine commercial remote sensing instrumentation for locating areas showing biotic and abiotic stress symptomology in a cotton field, (2) compare data obtained from commercial aerial infrared photography to that collected by infrared transducers (IRTs) mounted on a center pivot, (3) evaluate canopy temperature changes between irrigation regimes and their relationship to lint yield with IRTs and/or IR photography, and (4) explore the use of deficit irrigation and the use of crop coefficients for irrigation scheduling. Pivot-mounted IRTs and an IR camera were able to differentiate water stress among irrigation regimes. The IR camera distinguished between biotic (root rot) and abiotic (drought) stress with the assistance of groundtruthing. The 50% ET_c regime had significantly higher canopy temperatures than the other two regimes, which was reflected in significantly lower lint yields when compared to the 75% and 100% ET_c regimes. Deficit irrigation down to 75% ET_c had no impact on lint yield, indicating that water savings were possible without reducing yield.     

Measuring versus estimating net radiation and soil heat flux: Impact on Penman–Monteith reference ET estimates in semiarid regions

The standardized ASCE Penman–Monteith and FAO-56 equations were used to estimate reference evapotranspiration (ET₀) using estimated and measured net radiation (R_n) and soil heat flux (G), based on hourly and daily meteorological data. The estimates were evaluated against lysimeter measurements. The results indicate that using measured or estimated values of R_n and G can have significant effect on the accuracy of the ET₀ estimations, especially when calculations were made on an hourly basis. The FAO-56 version performed very well during the irrigation season on a daily basis. The use of measured R_n and G did not improve ET₀ estimation on a daily basis, therefore, the use of estimated R_n and G appears to be dependable when calculations are based on 24-h weather data. When daily ET₀ was calculated from hourly estimations, the results were different depending on the version used. The ASCE version was more accurate, especially when R_n and G were measured. Therefore, measurement of R_n and G may have potential to improve estimation only when daily ET₀ is calculated from hourly estimations. The PM FAO-56 version was always a little less accurate than the ASCE version. For hourly calculations, using a constant surface resistance (as in FAO-56 version), the PM method underpredicted for high evaporative demand and vice versa. The ASCE version performed better than PM FAO-56 version when R_n and G were measured and estimated. Therefore, ASCE version tended to provide quite accurate values of hourly ET₀, even using estimated values of R_n and G. As conclusion, the methods proposed by FAO-56 for estimating R_n and G tended to produce accurate estimates for daily and hourly ET₀ under semiarid conditions and can be used with some degree of confidence for estimating ET₀. In addition, results suggest that the ASCE standardized equation on an hourly basis improved the accuracy of ET₀ estimation with respect to the FAO-56 version.     

参考作物蒸发蒸腾量的气象因子响应模型

基于江苏省南通市2000～2004年的旬气象资料,用FAO推荐的Penman-Monteith公式计算了参考作物蒸发蒸腾量,研究了参考作物蒸发蒸腾量与最高气温、最低气温、平均气温、相对湿度、日照时数、风速和气压等气象因素间的关系,建立了参考作物蒸发蒸腾量的响应模型.结果表明,参考作物蒸发蒸腾量与"温度因子"的关系最强,其次为"湿度和日照因子","风速因子"也有一定的影响,"气压因子"影响作用则稍弱;建立的气象因子响应模型模拟精度较高,可以简化参考作物蒸发蒸腾量计算.