1. 西安理工大学水利水电学院,西安,710048
2. 中国农业科学院农田灌溉研究所,河南,新乡,453002
3. 南昌工程学院,南昌,330099
[ "樊向阳(1974-),男,博士研究生,研究员,主要从事农业水资源安全高效利用及水环境研究。E-mail:fxy0504@126.com" ]
纸质出版:2019
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樊向阳, 费良军, 代智光, 等. 基于Hydrus-3D模型的再生水涌泉根灌模拟及布置参数预测[J]. 水土保持学报, 2019,33(4):133-139.
FAN Xiangyang, FEI Liangjun, DAI Zhiguang, et al. Simulation of Surge-root Irrigation with Reclaimed Water and Prediction of Emitters Layout Parameters Based on Hydrus-3D[J]. 2019, 33(4): 133-139.
樊向阳, 费良军, 代智光, 等. 基于Hydrus-3D模型的再生水涌泉根灌模拟及布置参数预测[J]. 水土保持学报, 2019,33(4):133-139. DOI: 10.13870/j.cnki.stbcxb.2019.04.019.
FAN Xiangyang, FEI Liangjun, DAI Zhiguang, et al. Simulation of Surge-root Irrigation with Reclaimed Water and Prediction of Emitters Layout Parameters Based on Hydrus-3D[J]. 2019, 33(4): 133-139. DOI: 10.13870/j.cnki.stbcxb.2019.04.019.
为了探寻再生水果树涌泉根灌条件下灌水器的最优布设埋深和间距,以饱和―非饱和土壤水分运动理论为依据,选取了典型研究区一年和多年生桃树,利用Hydrus-3D模型对再生水涌泉根灌土壤水分入渗过程进行数值模拟,并将模拟结果与田间试验实测结果进行对比验证,同时预测了双源涌泉根灌灌水器的最优布置参数。结果表明,Hydrus-3D模型对再生水涌泉根灌湿润锋运移距离以及灌水结束后不同时刻含水量分布的模拟值和实测值之间决定系数R2均大于临界决定系数,均方根误差RMSE分别小于1.5和0.05,且F检验P值均在0.05以上。说明Hydrus-3D模型可以用于再生水双源涌泉根灌土壤水分运移的模拟;利用Hydrus-3D模型预测结果表明,1,5,10年生桃树再生水双源涌泉根灌灌水器最优布设埋深分别为35,35,45 cm,最优布设间距分别为40,50,40 cm。
Soil water infiltration movement is an important part of the evaluation of surge-root irrigation efficiency. Based on the theory of saturated-unsaturated soil water movement
we simulated the soil water infiltration under surge-root irrigation with a double-point source by Hydrus-3D and compared the simulated results with the field measured data. At the same time
the typical peach trees were selected and the optimal arrangement parameters of the surge-root irrigation were predicated. The study results showed that all the correlation coefficients between the simulated and the measured values of the soil wetting front of the surge-root irrigation and soil water content after irrigation were always greater than the critical correlation coefficient
RMSE was less than 1.5 and 0.05
respectively
and the P values of T-test were greater than 0.05. It indicated that Hydrus-3D could be used for soil moisture migration simulation of surge-root irrigation with reclaimed water. Using the Hydrus-3D model
the results showed that the optimal depth was 35
35
and 45 cm respectively for peach tree with 1-year
5-year and 10-year old
and the corresponding spacing was 40
50
and 40 cm respectively.
刘智超.从河湖管理与保护角度看新时代兴水治水"系统治理"的必然:关于"系统治理"的学习心得[J].水利发展研究,2018,18(7):22-23.
夏军,石卫,雒新萍,等.气候变化下水资源脆弱性的适应性管理新认识[J].水科学进展,2015,26(2):279-286.
中华人民共和国国家质量监督检验检疫总局,中国国家标准化管理委员会.GB/T 25499-2010城市污水再生利用绿地灌溉水质[S].北京:中国标准出版社,2010.
刘静,陈莹,赵辉,等.关于促进我国再生水利用的思考[J].中国水利,2017(15):6-8.
张陆军.山地枣树涌泉根灌适宜灌水器布置方式与灌水量研究[D].陕西杨凌:西北农林科技大学,2010.
费良军,曹俊,聂卫波.涌泉根灌土壤湿润体特性试验[J].排灌机械工程学报,2011,29(3):260-265.
樊晓康.涌泉根灌土壤湿润体影响因素的试验研究[D].陕西杨凌:西北农林科技大学,2012.
黎朋红,汪有科,马理辉,等.涌泉根灌湿润体特征值变化规律研究[J].水土保持学报,2009,23(6):190-194.
车银伟.枣树涌泉根灌的灌水效果及其灌水技术研究[D].陕西杨凌:西北农林科技大学,2012.
汪有科,黎朋红,马理辉,等.涌泉根灌在黄土坡地的水分运移规律试验[J].排灌机械工程学报,2010,28(5):549-554.
吴恒卿,黄强,魏群.涌泉根灌双点源交汇入渗湿润体试验研究[J].西北农林科技大学学报(自然科学版),2015,43(5):201-207.
Crevoisier D, Popoca Z, Mailhol J C, et al. Assessment and simulation of water and nitrogen transfer under furrow irrigation[J]. Agricultural Water Management,2010,95(4):354-366.
CoteC M, BristowK L, Charlesworth P B, et al. Analysis of soil wetting and solute transport in subsurface trickle irrigation[J]. Irrigation Science,2003,22(3/4):143-156.
Bristow K L, Cote C M, Thorbum P J, et al. Soil wetting and solute transport in trickle irrigation systems[R].Cape Town, South Africa:6th International Micro-irrigation Conference,22-27 October 2000.
Bhatnagar P R, Chauhan H S. Soil water movement under a single surface trickle source[J].Agricultural Water Management,2008,95(7):799-808.
Beggs R A, Tchobanoglous G, Hills D, et al. Modeling subsurface drip application of onsite wastewater treatment system effluent//On-Site Wastewater Treatment X, Proceedings of the Tenth National Symposium on Individual and Small Community Sewage Systems,2004:92-103.
Patel N, Rajput T B S. Dynamics and modeling of soil water under subsurface drip irrigated onion[J].Agricultural Water Management,2008,95(12):1335-1349.
Skaggs T H, Trout T J, Rothfuss Y. Drip irrigation water distribution pattern:Effects of emitter rate, pulsing and antecedent water[J].Soil Science Society of America Journal,2012,74(6):1886-1896.
李耀刚,王文娥,胡笑涛.基于HYDRUS-3D的涌泉根灌土壤入渗数值模拟[J].排灌机械工程学报,2013,31(6):546-552.
李久生,张建君,饶敏杰.滴灌施肥灌溉的水氮运移数学模拟及试验验证[J].水利学报,2005,36(8):931-936.
余根坚,黄介生,高占义.基于Hydrus模型不同灌水模式下的土壤水盐运移模型[J].水利学报,2013,44(7):826-834.
周广林,王全九,李云,等.Hydrus-3D模型模拟田间点源入渗与水分再分布准确性价[J].干旱地区农业研究,2015,33(2):113-121.
张亚飞,罗静静,彭福田,等.肥料袋控缓释对桃树根系生长、氮素吸收利用及产量品质的影响[J].中国农业科学,2017,50(24):4769-4778.
王晨冰,赵秀梅,常毅,等.垄膜保墒集雨栽培对旱地桃树根系分布的影响[J].甘肃农业科技,2013(6):9-11.
徐艳如.桃根系分布特点及其对不同施肥处理的反应[D].山东泰安:山东农业大学,2011.
白岗栓,邹超煜,于健,等.激光平地对灌水均匀度及春小麦生长的影响[J].水土保持学报,2014,28(4):85-90.
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