欢迎来到园艺星球(共享文库)! | 帮助中心 分享价值,成长自我!
园艺星球(共享文库)
换一换
首页 园艺星球(共享文库) > 资源分类 > PDF文档下载
 

滴灌灌水均匀系数与灌水量对土壤水分分布及温室番茄产量的影响.pdf

  • 资源ID:8080       资源大小:712.57KB        全文页数:10页
  • 资源格式: PDF        下载权限:游客/注册会员/VIP会员    下载费用:0金币 【人民币0元】
快捷注册下载 游客一键下载
会员登录下载
微信登录
下载资源需要0金币 【人民币0元】
邮箱/手机:
温馨提示:
系统会自动生成账号(用户名和密码都是您填写的邮箱或者手机号),方便下次登录下载和查询订单;
验证码:   换一换

加入VIP,免费下载
 
友情提示
2、PDF文件下载后,可能会被浏览器默认打开,此种情况可以点击浏览器菜单,保存网页到桌面,既可以正常下载了。
3、本站不支持迅雷下载,请使用电脑自带的IE浏览器,或者360浏览器、谷歌浏览器下载即可。
4、本站资源下载后的文档和图纸-无水印,预览文档经过压缩,下载后原文更清晰   

滴灌灌水均匀系数与灌水量对土壤水分分布及温室番茄产量的影响.pdf

2020 2 28 2 Chinese Journal of Eco Agriculture Feb 2020 28 2 286 295 E mail nwq E mail liangbh229 2019 07 18 2019 10 28 The study was supported by the Talent Reward Fund of Ningxia Dry Farming and Water Saving and High Efficiency Agricultural Engineering Technology Research Center Corresponding author E mail nwq Received Jul 18 2019 accepted Oct 28 2019 DOI 10 13930 ki cjea 190543 J 2020 28 2 286 295 LIANG B H NIU W Q GUO L L WANG Y L WANG J W Effects of drip irrigation uniity and amount on soil moisture and tomato yield in solar greenhouse J Chinese Journal of Eco Agriculture 2020 28 2 286 295 梁博惠 1 2 牛文全 2 3 郭丽丽 2 王愉乐 4 王京伟 5 1 750021 2 712100 3 712100 4 430072 5 030000 为探索灌水均匀系数与灌水量对温室番茄产量和土壤水分变化的影响 确定合理的滴灌灌水均匀系 数 本研究设置 65 75 和 85 3 个灌水均匀度水平 190 mm 220 mm 和 250 mm 3 个灌水量水平 测量番茄 生育期内土壤含水率及番茄产量 计算土壤含水率均匀系数和番茄灌溉水利用效率 结果表明 当灌水均匀系数 为 65 85 时 土壤水分均匀系数均值 82 57 93 76 接近或高于设置的滴灌灌水均匀系数的最大值 85 滴灌灌水均匀系数对土壤含水率均匀系数影响权重最大 灌水量 灌水均匀系数 土壤初始含水率均值 3 个影 响因素与土壤含水率均匀系数均值之间呈线性关系 P 0 05 决定系数为 0 918 当土壤初始含水率占田间持水 量比重 60 灌水量低于 15 mm 时 灌水均匀系数与灌水量二者的交互作用与土壤含水率均匀系数为显著线性 关系 P 0 05 其他情况下均无显著性关系 灌水量对产量为显著影响 P 0 05 灌水均匀系数及二者的交互作用 对番茄产量无显著影响 考虑产量及灌溉水分利用效率 灌水量 220 mm 灌水均匀系数 75 组合为最优组合 因此在西北地区 综合考虑经济性和系统的可靠性 建议下调现行滴灌灌水均匀系数标准 滴灌 灌水均匀系数 灌水量 土壤含水率均匀系数 番茄 S275 6 OSID Effects of drip irrigation uniity and amount on soil moisture and tomato yield in solar greenhouse LIANG Bohui 1 2 NIU Wenquan 2 3 GUO Lili 2 WANG Yule 4 WANG Jingwei 5 1 Ningxia Institute of Water Resources Research Yinchuan 750021 China 2 College of Water Resources and Architectural Engineering Northwest A 3 Institute of Soil and Water Conservation Chinese Academy of Sciences and Ministry of Water Resources of the People s Republic of China Yangling 712100 China 4 School of Water Resource and Hydropower Engineering Wuhan University Wuhan 430072 China 5 College of Resources and Environment Shanxi University of Finance and Economics Taiyuan 030000 China Abstract Drip irrigation is an important factor associated with the water and fertilizer integration technology The uniity 2 287 of drip irrigation is an important perance index to measure its quality Therefore choosing the appropriate drip uniity can achieve the dual targets of cost effectiveness as well as high crop yield A field experiment was carried out from October 2016 to April 2017 in the Yangling Agricultural Hi tech Industries Demonstration Zone Shaanxi Province China Experimen tal treatments applied in the split plot design included three irrigation quantities in Zone A 190 mm 220 mm and 250 mm and three drip irrigation uniities in Zone B 65 75 and 85 In the early stages of planting test no crop experiment was set up in the same area with only the drip irrigation belt laid and the experimental treatments were also applied in a split plot divided into main treatment Zone 1 and sub treatment Zone 2 The Zone 1 was treated with three irrigation quantities 5 mm 10 mm and 15 mm and in Zone 2 the same there drip irrigation uniities to Zone B were set The results showed that when the irrigation uniity was between 65 and 85 the mean soil moisture uniity during entire growth period was higher than the highest drip irrigation uniity 85 approximately The influence of drip irrigation uniity on the uniity coefficient of soil moisture was enormous There was a significantly linear relationship P 0 05 with de termination coefficient of 0 918 between the mean soil moisture uniity and the three factors i e irrigation quantity irrigation uniity and initial soil water content When the initial soil moisture was approximately 60 of the field capacity and the irrigation amount was less than 15 mm the interaction between the drip irrigation uniity and the irrigation amount was linear P 0 05 and significantly related to the soil moisture uniity In other cases there was no significant associa tion The irrigation amount had significant effect on tomoto the irrigation uniity and their interaction had no significant effect on tomato yield Taking into account the yield and use efficiency of irrigation the combination of irrigation amount of 220 mm and drip irrigation uniity of 75 was the optimal one Considering the economics and reliability of the system the involving small amount of multiple irrigation should be chosen This was also suggested for the reduction in the standard of drip irrigation uniity in the Northwest China Keywords Drip irrigation Drip uniity coefficient Irrigation amount Soil moisture uniity coefficient Tomato 1 GB T50485 2009 C u 80 2 E u 70 95 3 80 90 30 4 5 Wu 6 Warrick 7 8 Montazar 9 66 78 Medicago sativa Wilde 10 Gossypium spp 11 12 Zea mays 80 Bordovsky 13 14 15 Guan 16 17 Solanum lycopersicum 65 85 190 250 mm 1 材料与方法 1 1 2016 10 5 2017 4 2 288 2020 28 108 02 E 34 02 N 190 m 5 5 m 510 m 16 2 614 h 210 d 6 10 550 650 mm 1 400 mm 塿 0 02 mm 25 4 0 02 0 002 mm 44 1 0 002 mm 30 5 1 39 g cm 3 49 38 32 96 1 2 2016 10 1 2017 3 1 5 82 7 m 5 5 m 3 3 A 190 mm I1 220 mm I2 250 mm I3 3 1 B 65 C1 75 C2 85 C3 3 9 3 27 3 3 1 m SBS 2 4 m 5 5 m 39 cm 80 cm 39 5 10 m 1 7 L h 1 2 0 L h 1 2 2 L h 1 3 0 L h 1 5 3 L h 1 0 1 MPa 30 cm Monte Carlo 18 表 1 不同灌水量处理下番茄不同生育阶段的灌水量 Table 1 Irrigation amounts of tomato at different growth stages under different irrigation amount treatments mm Treatment Seeding stage Blooming and setting stage Fruiting period Last fruit ing period Total irrigation amount Irrigation date month day 10 25 11 10 12 05 12 16 12 22 01 01 01 12 01 27 02 14 10 01 03 01 I1 15 20 50 30 50 35 25 15 15 190 I2 15 20 40 30 40 25 20 15 15 220 I3 15 20 30 30 30 20 15 15 15 250 C u 19 C u 1 u 1 100 1 n i i qq n C q 1 q i i L h 1 q L h 1 n 3 61 78 87 5 1 2 1 5 mm Ia 10 mm Ib 15 mm Ic 2 B 65 C1 75 C2 85 C3 3 9 3 27 1 3 Burt 20 Kang 21 Field TDR 200 1 Trime 10 cm 3 TDR 15 1 2 289 1 Trime 10 cm 0 20 cm 20 30 cm 30 40 cm 40 50 cm 50 60 cm Field TDR 2 4 9 5 1 d 2 d 15 d Field TDR 2 80 cm 5 30 cm 10 cm 20 cm 30 cm 22 33 2 d 5 2 d 图 1 试验小区滴灌带和采样点布置图 Fig 1 Experiment plots arrangement plans of the drip irrigation tape and sampling plots C uw 19 1 uw 1 100 1 n i i N C 2 C uw i i N 3 4 5 I WUE WUE 100 Y I I 3 I WUE kg m 3 Y kg hm 2 I m 3 hm 2 1 4 Microsoft Excel 2007 SPSS 22 0 Duncan T Origin 9 0 Excel 3 2 结果与分析 2 1 2 1 1 2 0 20 cm 20 30 cm 30 40 cm 40 50 cm 50 60 cm 2 65 C1 290 2020 28 C1I3 C1I2 C1I1 C1 C2 C3 2 2 2 82 57 93 76 85 C3 20 30 cm 50 60 cm P 0 05 P 0 01 20 30 cm P0 05 P 0 05 P 0 01 C1 C2 and C3 indicate irrigation uniity coefficients of 65 75 and 85 I1 I2 and I3 indicate irrigation amounts of 190 mm 220 mm and 250 mm NS means no significant difference at 0 05 level among different treatments and mean significant differences at 0 05 and 0 01 levels respectively among different treatments 2 291 2 1 2 2 I X 1 C u X 2 0 X 3 C uw 4 R 0 918 F 18 613 2 1 e 0 286 R 2 0 918 3 3 i r iy r y C u C uw I 0 C uw 0 167C u 0 001I 0 002 0 R 2 0 918 4 表 3 番茄生育期内土壤含水率均匀系数均值与影响因素的通径分析结果 Table 3 Path analysis result of mean soil moisture uniity coefficient and influencing factors during tomato growth period Indirect path coefficient Variable Correlation coefficient r i Effect weight i Direct path coefficient p i r 1 p 1 r 2 p 2 r 3 p 3 Total Irrigation amount I X 1 0 614 0 641 0 642 0 438 0 015 0 453 Irrigation uniity coefficient C u X 2 0 712 0 727 0 713 0 457 0 017 0 472 Initial soil water content 0 X 3 0 037 0 039 0 024 0 024 0 001 0 025 P 0 05 means significant effect at 0 05 level 2 2 5 15 mm 0 20 cm 58 65 20 30 cm 60 44 2 d 4 0 30 cm P 0 05 P 0 01 表 4 灌水均匀系数和灌水量对不同深度土壤含水率均匀系数影响的方差分析结果 Table 4 ANOVA of soil moisture uniity coefficients at different soil depths for irrigation uniity coefficient and irrigation amount Soil depth cm Irrigation amount I Irrigation uniity coefficient C u I C u 0 20 NS NS 20 30 NS NS NS P 0 05 P 0 01 NS means no significant effect at 0 05 level and mean significant effects at 0 05 and 0 01 levels respectively I C u C uw 5 R 0 518 F 2 377 2 1 C uw 0 105C u 0 003 1I 0 773 R 0 518 5 2016 12 22 30 mm 40 mm 50 mm 2 d 1 d 3 50 93 65 59 5 5 20 50 cm 50 60 cm 0 60 cm 292 2020 28 5 30 50 cm 58 65 60 44 表 5 不同土壤初始含水率下灌水均匀系数和灌水量对土壤含水率均匀系数影响的方差分析结果 Table 5 ANOVA of soil moisture uniity coefficients at differents soil depths for irrigation uniity coefficient and irrigation amount under different initial soil water moistures Soil depth cm Initial soil moisture FC Resources of variance Christiansen Irrigation amount I NS Irrigation uniity coefficient C u NS 0 20 50 93 I C u NS Irrigation amount I Irrigation uniity coefficient C u NS 20 30 55 07 I C u NS Irrigation amount I Irrigation uniity coefficient C u NS 30 40 58 60 I C u NS Irrigation amount I Irrigation uniity coefficient C u NS 40 50 60 52 I C u NS Irrigation amount I Irrigation uniity coefficient C u NS 50 60 65 59 I C u NS FC NS P 0 05 P 0 05 P 0 01 FC is the proportion of field moisture capacity NS means no significant effect at 0 05 level and mean significant effects at 0 05 and 0 01 levels respectively 60 15 mm 2 3 6 74 63 87 39 t hm 2 12 76 t hm 2 8 62 kg m 3 I1 I2 C2 C1 3 52 12 08 t hm 2 250 mm C1 C1 C3 220 mm 75 3 讨论 65 85 190 250 mm 23 14 Brassica pekinensis 24 2 293 表 6 灌水均匀系数和灌水量对番茄产量及灌溉水分利用效率的影响 Table 6 Effects of irrigation uniity coefficient and irrigation amount on yield and irrigation water use efficiency of tomato Treatment Total water irrigation mm Total yield t hm 2 Irrigation water use efficiency kg m 3 C1I1 190 74 63 3 96b 39 28 2 08abc C2I1 190 78 15 6 88ab 41 13 3 62a C3I1 190 76 83 1 50ab 40 44 0 79ab C1I2 220 74 82 3 15b 34 01 1 43d C2I2 220 86 90 8 31a 39 50 3 78abc C3I2 220 77 80 7 44ab 35 36 3 38bcd C1I3 250 87 39 11 69a 34 96 4 67cd C2I3 250 81 28 0 95ab 32 51 0 38d C3I3 250 86 60 2 64ab 34 64 1 06cd F F value I 4 378 11 735 C u 0 590 NS 0 785 NS I C u 0 814 NS 1 725 NS C1 C2 C3 65 75 85 I1 I2 I3 190 mm 220 mm 250 mm NS P 0 05 P 0 05 P 0 01 C1 C2 and C3 indicate irrigation uniity coefficients of 65 75 and 85 I1 I2 and I3 indicate irrigation amounts of 190 mm 220 mm and 250 mm NS means no significant difference at 0 05 level among different treatments and mean significant differences at 0 05 and 0 01 levels respectively among different treatments 25 26 Hawke 27 Liu 28 29 1 9 5 5 0 64 0 72 0 039 29 60 15 mm 29 30 17 75 65 4 结论 1 65 85 82 57 294 2020 28 93 76 85 3 P 0 05 0 918 2 60 15 mm P 0 05 3 220 mm 75 参考文献 References 1 G 2003 LI J S ZHANG J J XUE K Z Principles and Applications of Fertigation through Drip Irrigation Systems G Beijing China Agricultural Science and Technology Press 2003 2 GB T 50485 2009 S 2009 Ministry of Housing and Urban Rural Development of the People s Republic of China General Administration of Qual ity Supervision Inspection and Quarantine of the People s Republic of China GB T 50485 2009 Technical Code for Microirrigation Engineering S Beijing China Planning Press 2009 3 ASAE Standards EP405 1 Design and Installation of Mi croirrigation Systems S St Joseph Mich ASAE 2003 4 J 2011 2 175 179 ZHU D L WU P T WANG J Effect of emitters manufactur ing variation of micro irrigation on uniity and lateral cost J Journal of Drainage and Irrigation Machinery Engi neering 2011 2 175 179 5 J 1995 11 2 128 132 CHEN Q C ZHENG Y Q Optimizing determination of irri gation uniity in the design of micro irrigation system J Transactions of the CSAE 1995 11 2 128 132 6 WU I P BARRAGAN J Design criteria for Microirrigation systems J Transactions of the ASAE 2000 43 5 1145 1154 7 WARRICK A W GARDNER W R Crop yield as affected by spatial variations of soil and irrigation J Water Resources Research 1983 19 1 181 186 8 J 2009 25 12 51 57 ZAI S M WU F WEN J et al uation of soil wa ter distribution uniity under conditions of field subsur face drip irrigation J Transactions of the CSAE 2009 25 12 51 57 9 MONTAZAR A SADEGHI M Effects of applied water and sprinkler irrigation uniity on alfalfa growth and hay yield J Agricultural Water Management 2008 95 11 1279 1287 10 WILDE C JOHNSON J BORDOVSKY J P Economic analysis of subsurface drip irrigation system uniity J Applied Engineering in Agriculture 2009 25 3 357 361 11 J 2011 27 1 36 43 LI J S YIN J F ZHANG H et al Effects of drip fertigation uniity and nitrogen application level on growth yield and quality of Chinese cabbage J Transactions of the CSAE 2011 27 1 36 43 12 D 2012 ZHANG H The distributions of water and nitrogen in soil and the growth of spring maize as affected by drip irrigation uni ity in North China Plain D Beijing China Institute of Water Resources and Hydropower Research 2012 13 BORDOVSKY J P PORTER D O Effect of subsurface drip irrigation system uniity on cotton production in the Texas High Plains J Applied Engineering in Agriculture 2008 24 4 465 472 14 J 2010 26 12 27 33 LI J S YIN J F ZHANG H et al Field uation of drip fer tigation uniity effects on distributions of water and ni trogen in soil J Transactions of the CSAE 2010 26 12 27 33 15 J 1993 1 1 4 LI J S Study on the relationship of water application uni ity and deep percolation J Irrigation and Drainage and Small Hydro power Station 1993 1 1 4 16 GUAN H J LI J S LI Y F Effects of drip system uniity and irrigation amount on cotton yield and quality under arid conditions J Agricultural Water Management 2013 124 37 51 17 D 2016 WANG J Optimal value of drip irrigation uniity and sys tem design D Yangling Northwest A F University 2016 18 D 2006 JIN C Study on random number generator and random sam pling in Monte Carlo D Dalian Dalian University of Technology 2006 19 CHRISTIAN J E Hydraulics of sprinkling systems of irriga 2 295 tion J Transaction of the ASCE 1942 107 221 239 20 BURT C M Rapid field uation of drip and microspray distribution uniity J Irrigation and Drainage Systems 2004 18 4 275 297 21 KANG S Z SHI P PAN Y H et al Soil water distribution uniity and water use efficiency under alternate furrow ir rigation in arid areas J Irrigation Science 2000 19 4 181 190 22 J 2017 33 3 113 120 ZHANG R C NIU W Q DUAN X H et al Optimization of drip irrigation uniity model considering location of clogged emitters J Transactions of the CSAE 2017 33 3 113 120 23 J 1999 10 3 311 318 Lei Z D Hu H P Yang S X A review of soil water research J Advances in Water Science 1999 10 3 311 318 24 J 2014 32 1 72 79 ZHANG J NIU W Q ZHANG L L et al Effects of soil initial water content on line source infiltration characteristic in moistube irrigation J Journal of Drainage and Irrigation Machinery Engineering 2014 32 1 72 79 25 J 2010 26 3 9 13 ZHANG B W SHAO M A Effect of initial soil water content on crude oil infiltration into soils J Transactions of the CSAE 2010 26 3 9 13 26 J 2010 41 9 36 43 WU Z D WANG Q J Effect of saline water continuous irri gation on winter wheat yield and soil physicochemical prop erty J Transactions of the Chinese Society for Agricultural Machinery 2010 41 9 36 43 27 HAWKE R M PRICE A G BRYAN R B The

注意事项

本文(滴灌灌水均匀系数与灌水量对土壤水分分布及温室番茄产量的影响.pdf)为本站会员(wdh@RS)主动上传,园艺星球(共享文库)仅提供信息存储空间,仅对用户上传内容的表现方式做保护处理,对上载内容本身不做任何修改或编辑。 若此文所含内容侵犯了您的版权或隐私,请立即通知园艺星球(共享文库)(发送邮件至admin@cngreenhouse.com或直接QQ联系客服),我们立即给予删除!

温馨提示:如果因为网速或其他原因下载失败请重新下载,重复下载不扣分。




固源瑞禾
关于我们 - 网站声明 - 网站地图 - 资源地图 - 友情链接 - 网站客服 - 联系我们

copyright@ 2018-2020 华科资源|Richland Sources版权所有
经营许可证编号:京ICP备09050149号-1

     京公网安备 11010502048994号


 

 

 

收起
展开