Uncertainty assessment of soya bean yield gaps using DSSAT‐CSM‐CROPGRO‐Soybean calibrated by cultivar maturity groups

Soya bean yield gap can be caused by different factors resulting in uncertainties when the objective is to use such information for farm decision‐making and reference yield determination. Thus, this study aimed to quantify the soya bean yield gap for four sites, located in Southern and Midwestern Brazil, as well as the uncertainties of that related to cultivars, sowing dates, soil types and reference yields. The crop simulation model DSSAT‐CSM‐CROPGRO‐Soybean was calibrated for cultivars with similar maturity groups, based on the data obtained from the best farmers at the county level. The yield gap by water deficit (YG_WD) was obtained through the difference between potential and attainable yields, and that one caused by sub‐optimum crop management (YG_CM) by subtracting actual yield of each county, obtained from official statistics between 1989/90 and 2014/15 growing seasons, from the estimated attainable yield. The yield was simulated using four sowing dates, three soil types and two soya bean maturity groups by county. The reference yield uncertainty was quantified using yield reference from crop model and regional winners of the soya bean yield context, conducted by CESB (Brazilian Soybean Strategic Committee), for the growing seasons from 2013/14 to 2015/16. The crop model showed a good agreement between measured and simulated crop development and growth using calibration by maturity group, with low root mean square error (347 kg/ha). Southern sites had a mean YG_WD of 1,047 kg/ha, while in the Midwest, it was lower than 100 kg/ha. The YG_CM was 1,067, 528, 984 and 848 kg/ha, respectively, for Castro, PR, Mamborê, PR, Montividiu, GO and Primavera do Leste, MT, representing the opportunity for yield gain when having the best farmers as reference. The maturity groups, sowing dates and soil types showed to be an important source of uncertainty for yield gap determination, being recommended to investigate the farms in detail for an appropriate quantification. The reference yield showed expressive uncertainties, with some farmers presenting conditions to increase their soya bean yields by more than 3,000 kg/ha, when considering as reference the yields obtained by the winners’ farmers. These results show that uncertainties must be reduced when assessing farm yield gaps, in order to ensure that expected rate of soya bean yield growth could be reached by adopting the same technologies from CESB winners and best farmers in the county as a reference.     

氰戊菊酯对照品的质量检测及赋值

为研制兽用氰戊菊酯国家对照品。取氰戊菊酯原油精制得氰戊菊酯原料,经质量检查,最大紫外吸收波长为277 nm、熔点为53-54℃、水分为0.02%,用正相和反相两种高效液相色谱法测得纯度为99.8%,按质量平衡法进行含量赋值为99.8%,不确定度为±0.1%。     

乙酸龙脑酯标准样品的制备和定值研究

研究了乙酸龙脑酯标准样品的制备、均匀性和稳定性及其定值方法。乙酸龙脑酯标准样品的制备采用高纯度天然龙脑的乙酰化法,乙酸龙脑酯标准样品的含量测定采用气相色谱面积归一化法,制备得到的乙酸龙脑酯标准样品通过了均匀性检验,且至少在24个月内是稳定的。乙酸龙脑酯标准样品的多实验室联合定值结果表示为:乙酸龙脑酯含量的标准值99.93%;标准不确定度0.08%;扩展不确定度(95%置信率)0.16%。     

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。     

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.     

基于气温预报和神经网络的参考作物腾发量预报

采用反向传播人工神经网络(BP-ANN)逼近气象因子-参考作物腾发量ET0函数关系,以天气预报中的最高和最低气温为输入进行短期ET0预报。收集了南京站实测的2010年7月1日至2013年7月7日逐日气象数据和2012年7月1日至2013年6月30日逐日对未来7d的气象预报数据,以最高、最低气温及相应的日序数为3个输入因子,ET0为输出建立一个包含一个隐含层的3层BP网络,以2010年7月1日至2012年6月30日实测气象数据及通过FAO-56PM公式计算的ET0进行网络,以2012年7月1日至2013年6月30日实测气象数据及通过FAO-56PM公式计算的ET0进行网络验证。将2012年7月1日至2013年6月30日逐日对未来7d的气象预报中的最高、最低气温输入训练及验证后的网络,得到2012年7月1日至2013年6月30日逐日对未来7d的ET0预报值,并与FAO-56PM公式计算的ET0值进行比较以验证预报精度。结果表明,预见期1~7d内,预报的ET0和计算的ET0变化趋势基本一致,预报精度随着预见期的增加而降低;平均准确率(±1.5mm/d以内)达88.08%,相关系数为0.77,均方根误差为1.28mm/d,显示出了较高的预报精度。在局部时间段内出现的ET0,PM和预报ET0的较大差别的原因是该时段内的ET0更多地受到除了日最高和最低气温之外的其他因素的影响。提出的方法 ET0预报,随着气象预报准确度的提高,可实现较为精确的ET0预报。     

基于HHT变换的PSO-LSSVM耦合模型估算气象资料短缺地区ET_0

为准确估算气象资料短缺地区参考作物腾发量,构建了一种基于HHT变换的PSO-LSSVM耦合模型,并利用新疆和田气象站2000—2009年单日数据做训练、双日数据做验证。结果表明,该模型估算ET0方法明显优于常规的PSO-LSSVM和GRNN,预测精度较二者分别提高了15.7%~85.6%和15.8%~93.7%;该方法预测ET0的气象要素重要性为RsTmaxTminRHWn,利用该方法对气象要素组合为Tmax/Tmin/RH/Wn、Tmax/RH/Wn、Tmin/Wn、Wn条件下的ET0预测,MSE分别为0.407、0.185、0.149、0.135,说明该方法可以很好地估算资料缺失地区ET0。     

基于Z比分数的参考作物腾发量计算方法优选

参考作物腾发量(ET0)是计算作物需水量的关键,是进行农田水分管理和灌溉预报的主要参数。但不同ET0计算方法的结果存在明显差异。用能力统计量Z比分数,对FAO56Penman-Monteith、Hargreaves-Samani、Irmark-Allen拟合和Priestley-Taylor四种常用ET0计算方法在不同天气条件下的计算结果精度进行了对比分析。结果表明,Priestley-Taylor与FAO56Penman-Monteith方法的计算结果在精度上具有较高的一致性,与有关文献结果相吻合,其中前者精度略佳。且Z比分数参数受极端值的影响较小,计算简便、适用性强,克服了常规方法公式繁杂、编程实现困难的缺点,说明Z比分数法能够更好地适用于ET0计算方法的优选。研究结果可为农业水土工程领域有关参数计算与测定方法的优选提供借鉴。     

Enhancing the Simplified Surface Energy Balance (SSEB) approach for estimating landscape ET: Validation with the METRIC model

Evapotranspiration (ET) can be derived from satellite data using surface energy balance principles. METRIC (Mapping EvapoTranspiration at high Resolution with Internalized Calibration) is one of the most widely used models available in the literature to estimate ET from satellite imagery. The Simplified Surface Energy Balance (SSEB) model is much easier and less expensive to implement. The main purpose of this research was to present an enhanced version of the Simplified Surface Energy Balance (SSEB) model and to evaluate its performance using the established METRIC model. In this study, SSEB and METRIC ET fractions were compared using 7 Landsat images acquired for south central Idaho during the 2003 growing season. The enhanced SSEB model compared well with the METRIC model output exhibiting an r² improvement from 0.83 to 0.90 in less complex topography (elevation less than 2000 m) and with an improvement of r² from 0.27 to 0.38 in more complex (mountain) areas with elevation greater than 2000 m. Independent evaluation showed that both models exhibited higher variation in complex topographic regions, although more with SSEB than with METRIC. The higher ET fraction variation in the complex mountainous regions highlighted the difficulty of capturing the radiation and heat transfer physics on steep slopes having variable aspect with the simple index model, and the need to conduct more research. However, the temporal consistency of the results suggests that the SSEB model can be used on a wide range of elevation (more successfully up 2000 m) to detect anomalies in space and time for water resources management and monitoring such as for drought early warning systems in data scarce regions. SSEB has a potential for operational agro-hydrologic applications to estimate ET with inputs of surface temperature, NDVI, DEM and reference ET.     

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.