基于称重式蒸渗仪的淮北平原冬小麦蒸散估算模型的本地化

为了解不同作物蒸散量估算方法在淮北地区的适用性,利用新马桥实验站称重式蒸渗仪测定了2016-2017年冬小麦全生育期的实际蒸散值,结合Hargreaves-Samani(H-S)、 FAO-56 PM、Turc、Makkind(Mak)、 Priestley-Taylor(P-T)、Mcloud(Mcl)和DeBruin-Keijman(D-K)7个模型,分析了冬小麦田的蒸散特征,将蒸散的估算值(ET_0)和实测值(ET_C)进行了对比。结果表明,相对于ET_C值,7个模型拟合得到的ET_0的RMSE值为0.99～2.29 mm·d~(-1),且H-S FAO-56 PMTurcMakP-TMclD-K; ET_C与ET_0的相关系数为0.74～0.97,其中FAO-56 PM的相关性最高,P-T、 Mak、 D-K、 H-S也表现出较好的相关性。综合来看,H-S法总体表现较好,更适合该地区。对6种主要气象要素与实测蒸散值进行主成分分析发现,温度是影响ET_C的主要因子,湿度、日照时数和平均风速(2 m)对淮北冬小麦田蒸散值的影响不大;H-S模型以温度数据为基础,利用线性订正法和湿度指数项订正法将H-S模型本地化后检验发现,其优化结果良好,RMSE降低(0.68 mm·d~(-1))。     

青藏高原典型高寒荒漠生长季蒸散及水分消耗特征研究

为探究青藏高原典型高寒荒漠下垫面水分消耗规律,以2019年青藏高原典型高寒荒漠地区沱沱河站监测的涡动数据和微气象数据为基础,分析不同时间尺度蒸散值的变化特征和下垫面水分消耗特征,研究结果表明：小时平均蒸散发量最大值出现在14—15时,达0.46 mm·h^-1;日蒸散值最大值出现在7月7日,为8.58 mm·d^-1,最小值出现在4月2日,为0.30 mm·d^-1;整个生长季蒸散值呈先增加后减小趋势,其中7月份最大,为120.68 mm,4月份最小,为64.80 mm;生长季总蒸散发量为581.15 mm,平均每天蒸散4.01 mm。整个生长季累计降水量为235.70 mm,蒸散发量与降水量（Precipitation,Pr）的差值（The difference between ET and Precipitation,IETP）显示,2019年青藏高原典型高寒荒漠植被生长季（4—8月）水汽交换以下垫面水分消耗为主。     

Cover crop evapotranspiration under semi-arid conditions using FAO dual crop coefficient method with water stress compensation

Cover cropping is a common agro-environmental tool for soil and groundwater protection. In water limited environments, knowledge about additional water extraction by cover crop plants compared to a bare soil is required for a sustainable management strategy. Estimates obtained by the FAO dual crop coefficient method, compared to water balance-based data of actual evapotranspiration, were used to assess the risk of soil water depletion by four cover crop species (phacelia, hairy vetch, rye, mustard) compared to a fallow control. A water stress compensation function was developed for this model to account for additional water uptake from deeper soil layers under dry conditions. The average deviation of modelled cumulative evapotranspiration from the measured values was 1.4% under wet conditions in 2004 and 6.7% under dry conditions in 2005. Water stress compensation was suggested for rye and mustard, improving substantially the model estimates. Dry conditions during full cover crop growth resulted in water losses exceeding fallow by a maximum of +15.8% for rye, while no substantially higher water losses to the atmosphere were found in case of evenly distributed rainfall during the plant vegetation period with evaporation and transpiration concentrated in the upper soil layer. Generally the potential of cover crop induced water storage depletion was limited due to the low evaporative demand when plants achieved maximum growth. These results in a transpiration efficiency being highest for phacelia (5.1 g m⁻² mm⁻¹) and vetch (5.4 g m⁻² mm⁻¹) and substantially lower for rye (2.9 g m⁻² mm⁻¹) and mustard (2.8 g m⁻² mm⁻¹). Taking into account total evapotranspiration losses, mustard performed substantially better. The integration of stress compensation into the FAO crop coefficient approach provided reliable estimates of water losses under dry conditions. Cover crop species reducing the high evaporation potential from a bare soil surface in late summer by a fast canopy coverage during early development stages were considered most suitable in a sustainable cover crop management for water limited environments.     

Effects of planting density on the productivity and water use of tea (Camellia sinensis L.) clones: I. Measurement of water use in young tea using sap flow meters with a stem heat balance method

Sap flow meters based on the stem heat balance method were used to measure the mass flow rates or water use in young potted tea (Camellia sinensis L.) plants of clones AHP S15/10 and BBK35. The meters were constructed on site and installed onto the stem or branch sections of field growing plants in an experiment originally designed to study the effects of plant population density and drought on the productivity and water use of young tea clones. The objective of the study was to use the SHB method as a first attempt to use sap flow meters for determining the water use of young tea growing in the field under well watered conditions in Tanzania. The results are reported and recommendation made for further work on using the technique.     

模拟降水量对毛乌素沙柳幼苗蒸发蒸腾的潜在影响

选择毛乌素沙地优势灌木沙柳为对象,研究157.5、315、472.5和630 mm 4种人控年降水量,对沙柳幼苗蒸发蒸腾作用的影响.结果表明,沙柳蒸发蒸腾量随着降水量的增加而逐渐增大,从157.5 mm增至630 mm,日蒸散量分别为1.63、3.11、4.37和5.66 mm,其中沙地蒸发量占主要部分.少量降水时,幼苗蒸腾速率明显呈现"午睡”现象,而充足降水则能消除"午睡”现象.相关分析结果表明,环境因子,如沙地含水率、太阳有效辐射、大气温度和饱和水汽压差,以及植物因素,如叶面积指数、叶片温度和气孔导度等,均能显著影响沙柳的蒸腾作用.     

速效肥和缓释肥对草坪蒸散量的影响

2002年5～11月在田间条件下就速效肥和缓释肥对草坪蒸散量的影响进行了研究.结果表明 施肥后草坪的蒸散量增大,其中,速效肥处理超过对照96.1mm,多耗水17.1%;速效肥+缓释肥和缓释肥处理分别增加了60.7mm和52.0mm,多耗水10.8%和9.2%;速效肥处理草坪蒸散量明显高于速效肥+缓释肥和缓释肥处理(P<0.05).施肥提高蒸散量的原因是增大了草坪草的生长速度及分蘖密度.缓释肥处理生长速度的增加幅度较小,株丛密度较高,且各月份比较稳定,速效肥处理则波动很大;此外,施用缓释肥更有利于地下生物量的积累.综合比较,在草坪管理中应减少速效肥的使用量,适当增加缓释肥的应用比例.     

Effects of water stress at different development stages on yield and water productivity of winter and summer safflower (Carthamus tinctorius L.)

A field study was carried out to determine the effects of water stress imposed at different development stages on grain yield, seasonal evapotranspiration, crop-water relationships, yield response to water and water use efficiency of safflower (Carthamus tinctorius L.) for winter and summer sowing. The field trials were conducted on a loam Entisol soil in Thrace Region in Turkey, using Dincer, the most popular safflower variety in the research area. A randomised complete block design with three replications was used. Three known growth stages of the plant were considered and a total of 8 (including rainfed) irrigation treatments were applied. The effect of irrigation or water stress at any stage of development on grain yield per hectare and 1000 kernel weight, was evaluated. Results of this study showed that safflower was significantly affected by water shortage in the soil profile due to omitted irrigation during the sensitive vegetative stage. The highest yield was observed in the fully irrigated control and was higher for winter sowing than for summer sowing. Evapotranspiration calculated for non-stressed production was 728 and 673 mm for winter and summer sowing, respectively. Safflower grain yield of the fully irrigated treatments was 4.05 and 3.74 t ha⁻¹ for winter and summer season, respectively. The seasonal yield response factor was 0.97 and 0.81 for winter and summer sowing, respectively. The highest total water use efficiency was obtained in the treatment irrigated only at vegetative stage while the lowest value was observed when the crop was irrigated only at yield stage. As conclusions: (i) winter sowing is suggested; (ii) if deficit irrigation is to apply at only one or two stages, Y stage or Y and F stages should be omitted, respectively.     

Water Requirements for Castor Oil Crop (Ricinus communis L.) in a Mediterranean Climate

A field study was conducted to assess the effect of irrigation on castor ( Ricinus communis L.) and to define the water requirements of the crop. Three irrigation regimes, corresponding to 0.0, 0.5 and 1.0 fractions (kd) of the evapotranspiration (ETm) in the area were compared, factorially combined with the varieties Pronto and Negus in 1995. In 1996 and 1997 one more irrigation treatment corresponding to 0.75 of the ETm was included, and Negus was replaced by HD912. Irrigation was found necessary for castor production since seed and oil yields obtained with irrigation were much higher compared to yields of rainfed plants, and also castor could not be competitive to winter cereals in rainfed areas. In 1995 seed yield increased to kd = 1.0, but the response of both varieties was curvilinear. In 1996 kd = 0.50 was enough for the maximum yield by both varieties, while in 1997 higher amounts of water were needed (kd = 1.00 and 0.75 for Pronto and HD912, respectively). The beneficial effect of irrigation was mainly due to the increased number of secondary racemes. Oil yield was mainly determined by seed yield. Thus, the aim of the growers should be to increase the seed yield. The suggested amount of water for the irrigation of castor in the Northern Greece is equal to 75 % of the evapotranspiration of the plant in the area. With this amount the yield is satisfactory and the management of water resources is doing in a rational way.     

Estimation of irrigation return flow from paddy fields considering the soil moisture

The objective of this study was to estimate irrigation return flow in irrigated paddy fields considering the soil moisture. The proposed model was applied to examine its feasibility with regard to the growing period of rice. Simulation results showed a good agreement between the observed and simulated values: root mean square error (RMSE) of 6.05-7.27 mm day⁻¹, coefficient of determination (R²) of 0.72-0.73, and coefficient of efficiency (E) of 0.54-0.55. The estimated average annual irrigation return flow during the period from 1998 to 2001 was 306.2 mm, which was approximately 25.7% of the annual irrigation amounts. Of this annual irrigation return flow, 14.1% was attributable to quick and 11.6% to delayed return flow. These results indicate that considerable amounts of irrigation water in the paddy fields were returned to streams and canals by surface runoff and groundwater discharge. The modeling assessment method proposed in this study can be used to manage agriculture water and estimate irrigation return flow under different hydrological and water management conditions.     

APPROACHES DETERMINING EVAPOTRANSPIRATION OF A NATURAL SECONDARY WHITE BIRCH FOREST

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