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蒸渗仪测定滴灌枣树不同时间尺度下腾发强度特征

本站小编 Free考研考试/2022-01-01

郭丹丹,
马英杰,
马亮,
新疆农业大学水利与土木工程学院 乌鲁木齐 830052
基金项目: 国家自然科学基金项目51369029
水利工程重点学科基金项目SLXK2018-01
干旱区枣树节水调质技术及智能决策系统研发创新团队XJEDU2017T004
新疆水利科技项目2017G04

详细信息
作者简介:郭丹丹, 主要从事节水灌溉理论研究。E-mail:623046780@qq.com
通讯作者:马亮, 主要从事节水灌溉理论研究。E-mail:42409584@qq.com
中图分类号:S271

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出版历程

收稿日期:2018-06-04
录用日期:2018-11-29
刊出日期:2019-03-01

Prediction of the evapotranspiration rate of jujube using lysimeters for drip irrigation

GUO Dandan,
MA Yingjie,
MA Liang,
School of Water Conservancy and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, China
Funds: the National Natural Science Foundation of China51369029
the Key Discipline Fund Project of Water Conservancy EngineeringSLXK2018-01
the Innovation Team of Jujube Water Saving and Quality Control TechnologyXJEDU2017T004
the Xinjiang Water Conservancy Science and Technology Project2017G04

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Corresponding author:MA Liang, E-mail: 42409584@qq.com


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摘要
摘要:为精确测定、准确模拟阿克苏地区滴灌枣树腾发过程,基于大型称重式蒸渗仪测定枣树全生育期逐时及逐日腾发强度(ET),利用水量平衡方程、PM公式及经典统计原理,分析不同时间尺度下叶面积指数(LAI)、气象因素[温度(I)、风速(V)、净辐射(Rn)]、表层土壤含水率(W)与枣树腾发强度的相关关系并建立预测模型。结果表明:枣树日内腾发强度呈单峰型变化趋势,夜间变化幅度较小且腾发贡献率低。枣树全生育期逐日腾发强度变化呈先增大后减小的趋势,花期的腾发强度最大,为4.42 mm·d-1;全生育期腾发总量为640.83 mm,其中花期和果实生长发育期耗水量占比较大,分别为38.61%和32.72%。在小时和日时间尺度上,影响腾发强度的主要因素不完全相同,且影响程度有所差异。综合考虑各影响因素,以萌芽期、花期、果实发育期为基础,分别建立以小时、日尺度下估算腾发强度的经验模型ET1(h)=0.153+0.004T+0.012V+0.176Rn+0.002W+0.067LAI、ET2(d)=-3.325+0.081T+0.163Rn+0.069W+2.089LAI,拟合度R2均在0.7以上,以果实发育期与成熟期数据对模型进行检验,纳什效率系数分别达0.63、0.80。经偏相关检验,冠层净辐射(Rn)对两种尺度的腾发强度均影响最显著,因此以枣树全生育期数据量为基础,仅建立冠层净辐射(Rn)与腾发强度的回归模型ET1(h)=-0.063 3Rn2+0.361 2Rn—0.003 7、ET2(d)=-0.018 3Rn2+0.684 7Rn–1.642 1,R2分别为0.704 7与0.743 6,可满足缺少数据支撑情况下的腾发过程估算。这些模型明确了阿克苏地区滴灌枣树腾发机制及影响程度,可为水分管理精准化提供计算基础。
关键词:腾发强度/
气象因子/
时间尺度/
枣树/
滴灌
Abstract:Measuring field evapotranspiration can provide important information needed for estimating soil moisture and crop water stress and premature drying out, and such information is essential for irrigation formulation. Evapotranspiration can be measured using large lysimeters that have the advantage of confining soil boundaries, flexible measuring intervals, and high precision. Most of studies of evapotranspiration have been done for annual crops such as wheat and maize, and the present study was conducted to measure evapotranspiration of jujubes. Jujube trees of four years were transplanted into lysimeters and evapotranspiration was measured at 30-min intervals for complete growth season. The correlation between evapotranspiration rate and leaf area index, meteorological factors, and surface soil moisture content was analyzed based on water balance and the PM formula. The daily evapotranspiration of jujube was unimodal, taking place mainly in the daytime; the contribution of was small and stable. Evapotranspiration peaked at flowering stage, reaching 4.42 mm·d-1, and then declined gradually. The total evapotranspiration during growth season was 640.83 mm, a large proportion of which occurred during flowering and fruit development stages that accounted for 38.61% and 32.72%, respectively. The observation suggested that there is a need for flowering and fruit stages to be emphasized in irrigation of jujube trees. Hourly and daily evapotranspiration rates of jujube were different in their affecting factors. The wind speed (V) affected hourly evapotranspiration only. The most sensitive factor for evapotranspiration was canopy net radiation (Rn), followed by air temperature (T), wind speed (V), leaf area index (LAI), and surface soil moisture content (W), as summarized in the following empirical equations for hourly and daily evapotranspiration, respectively:ET1(h)=0.153 + 0.004T+ 0.012V+0.176Rn+0.002W+ 0.067LAI, and ET2(d)=-3.325 + 0.081T+0.163Rn + 0.069W+2.089LAI. Because canopy net radiation had the largest and most significant impact (the partial correlation coefficient was 0.562** and 0.468** for the hourly and daily equation, respectively), the regression was simplified as ET1(h)=0.232 6Rn + 0.018, R2=0.719 6, and ET2(d)=0.321 2Rn-0.141 8, R2=0.719 6. These equations were tested to be accurate and could be used to estimate the evapotranspiration rate of jujube for developing drip irrigation in arid areas when input data were complete or partially complete.
Key words:Evapotranspiration rate/
Meteorological factors/
Time scale/
Jujube/
Drip irrigation

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图1枣树果实发育期典型天气腾发强度变化
ET1表示小时尺度下蒸渗仪实测腾发强度; ET0表示参考作物腾发强度。
Figure1.Hourly evapotranspiration rate of jujube under different weather conditions at fruit development stage
ET1 is the measured evapotranspiration rate at hour scale by lysimeter; ET0 is the reference crop evapotranspiration rare.


下载: 全尺寸图片幻灯片


图2枣树各生育期逐日腾发强度(ET)动态变化
P:降水量; I:灌水量; ET0:作物参考腾发量。
Figure2.Daily variation of evapotranspiration rate (ET) of jujube at different growth stages
P: precipitation; I: irrigation; ET0: crop reference evapotranspiration.


下载: 全尺寸图片幻灯片


图3枣树小时尺度(a)和日尺度(b)腾发强度(ET)模拟值和实测值的比较
Figure3.Comparison of simulated and measured evapotranspiration rate (ET) of jujube at hourly scale (a) and daily scale (b)


下载: 全尺寸图片幻灯片


图4小时尺度(a)和日尺度(b)下枣树冠层净辐射(Rn)与腾发强度(ET)的关系
Figure4.Relationship between net radiation (Rn) and jujube evapotranspiration rate (ET) at hourly scale (a) and daily scale (b)


下载: 全尺寸图片幻灯片

表1枣树各生育阶段腾发及相关因素特征
Table1.Characteristics of evapotranspiration and relative factors at different growth stages of jujube
生育阶段
Growing stage
萌芽期
Germination
stage
花期
Florescence
stage
幼果期
Young fruit
stage
果实发育期
Fruit development
stage
成熟期
Mature stage
日期(月-日) Date (month-day) 04-23—05-15 05-16—07-10 07-11—07-27 07-28—09-20 09-21—10-27
天数Number of days (d) 23 56 17 55 37
灌水量Irrigation amount (mm) 56.7 223 44.6 90 0
降雨量Precipitation (mm) 15.2 27.5 13.3 37.4 5.8
实际腾发量Evapotranspiration (ET) (mm) 62.20 247.41 69.55 209.69 51.97
阶段腾发强度
Stage evapotranspiration rate (mm·d-1)
2.70 4.42 4.09 3.81 1.40
阶段腾发模数Stage water modulus (%) 9.71 38.61 10.85 32.72 8.11
参考作物腾发量
Reference crop evapotranspiration (ET0)
(mm)
85.84 256.18 69.25 186.53 57.63
作物系数Crop coefficient 0.74 0.97 1.01 1.13 0.87


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表2不同时间尺度下腾发强度(ET)与各影响因子的回归关系检验
Table2.Regression test of jujube evapotranspiration rate (ET) and influencing factors under different time scales
因变量
Dependent
variable
自变量
Independent
variable
回归系数
Coefficient
偏相关值
Partial correlation
t R α R2 均方误差
Mean square
error
小时尺度
ET
Hourly ET
(ET1)
温度Temperature (T) 0.004 0.309** 21.533 0.853 < 0.001 0.721 0.002 7
风速Wind speed (V) 0.012 0.137** 9.182
冠层净辐射Net radiation (Rn) 0.176 0.562** 45.031
土壤含水率Soil water content (W) 0.002 0.114** 7.621
叶面积指数Leaf area index (LAI) 0.067 0.125** 8.332
日尺度ET
Daily ET
(ET2)
温度Temperature (T) 0.081 0.317** 3.641 0.758 < 0.001 0.775 0.209
冠层净辐射Net radiation (Rn) 0.163 0.468** 5.776
土壤含水率Soil water content (W) 0.069 0.261* 2.954
叶面积指数Leaf area index (LAI) 2.089 0.304** 3.477
**为极显著相关, *为显著相关。** and * indicate extremely significant (P < 0.01) and significant (P < 0.05) correlations, respectively.


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表3枣树不同生育期估算不同时间尺度腾发强度(ET)误差分析
Table3.Error analysis of evapotranspiration rate (ET) estimation at different time scales at different growth stages of jujube
时间尺度
Time scale
生育阶段
Growth stage
实测值
Measured value
(mm·d-1)
模拟值
Simulation value
(mm·d-1)
R RMSE NSE
小时尺度
Hourly scale
果实发育期Fruit development stage 0.158 0.149 0.755** 0.025 0.63
成熟期Mature stage 0.060 0.062 0.796** 0.013 0.66
全生育期Whole growth season 0.119 0.114 0.784** 0.020 0.64
日尺度
Daily scale
果实发育期Fruit development stage 3.798 3.871 0.867** 0.462 0.73
成熟期Mature stage 1.434 1.370 0.937** 0.266 0.87
全生育期Whole growth season 2.847 2.865 0.912** 0.362 0.81
R为复相关系数; RMSE为均方根误差; NSE为纳什效率系数。**为极显著相关(P < 0.01)。R is complex correlation coefficient; RMSE is the root mean square error; NSE is the Nash efficiency coefficient. ** indicates extremely significant (P < 0.01).


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