927 resultados para Blade of irrigation
Resumo:
Irrigation in the eleven River Basin Authorities and in particular in the South Chad Irrigation Project and the Baga Polder Project is increasing and demands high yearly investments for aquatic weed control in canals and drains. If the weeds are biologically controlled by the grass carp (Ctenopharyngodon idella Val.), the costs will be turned into profit, particularly when the fish production (resident fish plus grass carp) is harvested and sold for food. The use of irrigation canals and drains for aquaculture in the form of fish polyculture may be a wise step towards increased fish production. This paper highlights the concept of fish production from aquatic weed control and concludes that it is a proven profitable venture in several countries
Resumo:
[ES]estudio del comportamiento de un rodamiento de vuelco situado en la unión buje-pala de un aerogenerador mediante diferentes técnicas de modelización por elementos finitos y su comparación. Los análisis realizados son: estático con contacto Rough, estático con contacto Bonded y mediante técnicas de subestructuras. En el estudio se ha utilizado ANSYS Mechanical APDL.
Resumo:
As inundações são fenômenos naturais que ocorrem devido às chuvas de grande magnitude, agravadas nas áreas urbanas pela impermeabilização do solo e ineficiência dos sistemas de drenagem. Os telhados verdes surgem como uma medida compensatória estrutural que pode reter parte da água precipitada, adiando o pico de escoamento. O objetivo deste trabalho foi de desenvolver uma combinação de solo e condicionadores para telhado verde, promovam um aumento relevante na capacidade de retenção hídrica e um maior adiamento do pico de escoamento das águas pluviais. Este estudo foi dividido em duas etapas. Na Etapa 1, foram analisadas, em colunas de percolação, três condicionadores nas seguintes concentrações: Gel retentor Stockosorb (2; 4; 6 g/dm3), Fertilizante de liberação lenta Osmocote (4,7; 7,1; 9,0 g/dm3) e Zeólita (30; 50; 70 g/dm3), em três eventos (regas) consecutivos de chuva simulada na intensidade de 57 mm/h. A avaliação das concentrações mais adequadas dentre as testadas para cada condicionante foi baseada nas análises referentes à retenção hídrica (altura do meio após a rega; tempo de adiamento do escoamento; mm retidos; intensidade da água percolada em mm/min) e à qualidade da água percolada (pH, oxigênio dissolvido, turbidez e sólidos). Na Etapa 2, foi avaliada, em vasos, a influência da presença de três espécies de plantas (Arachis pintoi; Raphanus sativus; Lavandula angustifolia) em dois tipos de meio: solo sem condicionadores; solo com condicionadores nas melhores concentrações indicadas na Etapa 1, sendo simulada apenas um evento de chuva de 57 mm/h. Foram analisados parâmetros biológicos (germinação; plantas sobreviventes; comprimento do caule e da raiz; pesos da biomassa do caule e da raiz); retenção hídrica (altura do meio após a rega; tempo de adiamento do escoamento; mm retidos; intensidade da água percolada em mm/min); qualidade da água percolada (pH; oxigênio dissolvido; turbidez; sólidos; nitrato; amônia; fósforo total). Os resultados da Etapa 1 indicaram que o gel promoveu de forma significativa um aumento na retenção hídrica, e adiou o início da percolação de água, além de promover ligeira elevação do pH na água percolada. A adição de zeólita resultou em um aumento significativo da retenção hídrica, porém tal aumento não é vantajoso visto que este representa um custo adicional que poderia ser reduzido com o aumento da proporção do gel na coluna. A adição de fertilizantes não promoveu mudanças na qualidade da água percolada. Na Etapa 2, somente o efeito da presença de A. pintoi (maior produção de biomassa de raiz e caule) e R. sativus foram avaliadas. A presença dos condicionantes no solo proporcionou um desempenho significativamente superior em relação a retenção hídrica (altura do substrato e adiamento do pico de chuva) e qualidade da água percolada (pH e turbidez) quando comparados aos testes realizados na presença somente de solo. O fertilizante influenciou nas altas concentrações dos nutrientes (nitrogênio e fósforo) na água percolado nos resultados. A presença do gel no substrato, resultou numa capacidade superior de retenção de hídrica, e consequentemente no adiamento do pico de intensidade de chuva. Sendo assim, recomenda-se a aplicação do gel em telhados verdes para futuros estudos em ambientes externos.
Resumo:
利用室内控制试验研究了根据不同深度土壤水分传感器灌溉处理对冬小麦生物学性状及水分利用率等的影响。结果显示,以10 cm探头控制灌溉最为省水,同时冬小麦生物学性状及水分利用率等最佳。由于试验冬小麦处于生育前期,随着小麦生育期延伸,当根系超过30 cm深度时,根系吸水的深度增加,探头的埋设深度需要田间试验进行更详细的研究。
Resumo:
研究灌溉方式对樱桃番茄产量和品质的影响,为番茄栽培过程中合理用水提供理论依据。【方法】采用棚室内小区试验,研究6种灌溉方式(Ⅰ.常规沟灌;Ⅱ.交替沟灌;Ⅲ.固定灌溉种植行;Ⅳ.固定灌溉操作行;Ⅴ.前期采用常规沟灌,结果期采用交替沟灌;Ⅵ.前期采用交替沟灌,结果期采用常规沟灌)对樱桃番茄产量与品质的影响。【结果】不同灌溉方式之间樱桃番茄产量与品质特征值达到极显著差异水平,其中处理Ⅰ和Ⅵ的果形指数、单果质量及产量均极显著高于其他4种处理,果形指数分别为1.22和1.21,平均单果质量高达14.28和14.05g;但处理Ⅱ~Ⅳ的果实糖酸比、VC含量、可溶性固形物含量及干物质含量均极显著高于处理Ⅰ、Ⅵ和Ⅴ,只是造成硝酸盐含量轻度积累。【结论】前期采用交替沟灌,而结果期采用常规沟灌,不仅提高了樱桃番茄的产量与品质,而且还有节水的效果,这种灌溉方式可以在番茄生产中加以推广应用。
Resumo:
利用野外试验方法,在滴灌条件下研究了保水剂在坡地枣林中的使用效果。试验结果证明:施用保水剂的土壤含水量较对照提高了15.3%~39.2%,使10~70 cm土层有较高贮存水量,在年生育期平均降雨量为395 mm情况下,确定红枣整个生育期(为210 d)共灌水4次,按大约每55 d灌溉一次计算,可减少灌溉2次,节约用水264 m3/hm2;0~60 cm土壤平均容重降低0.05~0.16 g/cm3,改善了土壤的通气透水的土壤物理性质,促进了枣树的生长发育,与对照株产5.6 kg相比,四年生红枣单株最高可增产2.85 kg/株;就不同保水剂综合来说,Hs和Hm表现出良好的适宜性。
Resumo:
采用小区试验研究了不同灌溉方式对津春4号黄瓜根系特性与产量的影响。结果表明,不同灌水方式之间黄瓜根系的特征值差异达到显著水平,前期交替沟灌结果期常规沟灌处理单株根条数、根长、根体积、根冠比均高于其余五种处理,根系伤流量为19.86 mg/min,根系活力高达0.55 mg/(g.h)。灌水方式对黄瓜单果重的影响不大,前期交替沟灌结果期常规沟灌处理的单株产量显著高于常规沟灌。因此,前期交替沟灌结果期常规沟灌有利于黄瓜根系的发育与产量的提高。
Resumo:
以长俊木瓜为材料,研究了其体细胞胚胎诱导过程中各个环节的影响因素。结果表明:愈伤组织诱导的适宜外植体是叶片,培养基为MS+6-BA1.0 mg.L-1+2,4-D0.2 mg.L-1,黑暗培养;非胚性愈伤组织向胚性愈伤组织转化的适宜培养基是MS+6-BA1.0 mg.L-1+NAA1.0 mg.L-1;胚性愈伤组织的保持与增殖应在黑暗条件下进行,培养基为MS+6-BA1.0 mg.L-1+2,4-D0.2 mg.L-1;长俊木瓜叶片体胚的发生以加入ABA2.0 mg.L-1的MS培养基最为有利。
Resumo:
文冠果(Xanthoceras sorbifolia Bunge)是我国北方特有的木本油料树种,已被列为生物质能源树种之一。现阶段产量低是限制其发展的重要因素。本文以内蒙古赤峰市翁牛特旗文冠果经济林场内50年生文冠果树为研究对象,对文冠果生物学、生态学特性进行定位观测和试验,分析了文冠果发育节律与积温的关系。野外布置水肥措施试验,测定了文冠果产量和叶片、果实养分元素(N、P、K、Mg、Ca、Fe、Zn、Cu、Mn)的含量,分析了水肥措施对叶片、果实养分分配的影响。 主要结论: 1.文冠果物候期与积温呈显著的直线函数关系。能够用来预测文冠果年生长发育期有效积温的理论值,为经营管理提供依据。 2.文冠果叶片中主要元素含量随物候期的变化呈下降趋势,但微量元素呈增加趋势。养分重吸收水平由大到小的顺序是:Mg>N>K>P,一定的水肥措施提高了文冠果养分再吸收水平,并降低了功能叶中的N/P、C/N。 3.文冠果果实中Ca和Fe随物候期的变化呈下降趋势,其他元素呈先减后增趋势。水肥措施降低了果实对养分元素的分配和收获系数;提高了养分利用效率。 4.合理的水肥措施能显著提高种子产量,增加含油率。最佳水肥措施为:5月初灌水50mm,施肥量为N 63 g•株-1、P2O5 83.3 g•株-1,于5、7月初分2次等量施入。 5.水分、P是文冠果生长的主要限制性因子,限制性因子具有阶段性。水分对肥效有“激发效应”。
Resumo:
现代化的灌溉用水管理是实现农业高效用水的重要措施之一,它可实现灌溉水资源的合理配置和灌溉系统的优化调度,达到节水增产目的,使有限的水资源获得最大的效益。采用手工方式进行灌溉用水管理,难以及时提供水资源利用最优化方案,因此急需研制出具有网络通信功能的可视化操作界面的灌溉信息管理系统,为灌区水资源评价和利用、规划等工作奠定良好的数据基础。GIS不仅具有强大的空间数据管理功能,还具有丰富的多元地学数据分析处理能力和直观的图形显示效果,因此利用GIS进行灌区的管理与建设将会有效提高灌区的工作效率和经济效益。笔者在实践调研的基础上,根据灌溉信息管理系统的功能规划及结构设计,利用MapX组件工具开发了陕西省冯家山灌区灌溉信息系统,对提高灌溉用水的管理效率进行了实例尝试,并着重对下列关键技术的运用进行了实践与思考:(1)阐述了利用可视化编程工具结合数据库管理技术、地理信息系统组件技术、网络通信技术等进行系统开发的过程;(2)着重介绍了基于MapX组件的空间数据库的建立与关联技术、灌溉管理信息的网络通信实现技术;(3)最后对在灌溉管理工作中运用GIS技术进行科学管理等相关问题进行了有益的探讨。
Resumo:
利用田间小区试验研究了不同灌水对冬小麦旗叶光合功能衰退的影响。研究表明 :小麦旗叶光合衰退初期引起光合下降的原因主要是气孔限制 ,后期则为非气孔限制。灌水可提高旗叶光合速率 ,并使由气孔限制向非气孔转变的时间推后 ,同时 ,还可增加叶绿素含量 ,增强根活力 ,使小麦旗叶光合功能持续期延长。过量灌水改善旗叶光合衰退的效果主要表现在后期 ,对产量提高的意义并不大。
Resumo:
Based on field survey, laboratory testing and numerical modeling, engineering characteristics of undisturbed loess and the mechanism of long-runout loess landslides caused by underground water level rise, as well as the formation conditions and spatial distribution of landslides, are systematically studied and analyzed. Loess landslides at south Plateau of Jingyang County are mainly classified as flowslide, slide and fall. Flowslide is the main type characteristic of high velocity, long runout and multi-stages. The steep relief composed of loose structured loess-old aged soil serials and the rise of groundwater table are the predominant conditions for landslides in the study area. To study loess mechanic poperties and loess landslides mechanisims, isotropically and anisotropically consolidated undrained compression(ICU and ACU) tests and constant-deviator-drained compression (CQD) tests were carried out on undisturbed samples. The results of undrained compression tests performed at the in-situ stress level show that the soils are of consistently strain-softening in the stress-strain relations and cause high excess pore pressure. The steady-state line and the potential region of instability are obtained from ICU and ACU test results. A necessary condition for liquefaction is that the soil state initially lies in or is brought into the potential instability region. In addition, a strong strain-softening model is also formed. CQD tests demonstrate that the mobilized friction angle is far less than the steady-state angle and that the soil experiences undrained contractive failure suddenly at very small strains when its stress path during drained loading tries to cross the potential instability region,thus validates the proposed instability region. Based on the location of the region of potential instability and the stress state of slope soil, a method of static liquefaction analysis is proposed for loess landslides caused by rise in groundwater table. Compared with other liquefaction analysis methods, this method overcomes the limitations inherent in conventional slope stability method and undrained brittleness index method. Triaxial tests composed of constant water content (CW) and wetting tests at constant deviator stress are performed on undisturbed unsaturated samples. The stress-strain relation of CW tests takes on strain-hardening behavior; The results of wetting tests at constant deviator stress designed to study the mechanics of failure of unsaturated loess caused by an increase in the degree of saturation (wetting) shows that a contractive failure occurs in the undisturbed samples. On the basis of the above triaxial test results, the initiation of static liquefaction is presented for long-runout loess landslides caused by rise in groundwater table, that is, the loess slope soil gradually transfer from unsaturated to saturated state under the infiltration of irrigation. A contractive failure occurs in the local region at very small strain by increasing the pore-water pressure at constant deviator stresses under drained conditons. It is the contractive failrue resulting from rise of pore pressure that leads to high excess pore pressure in the neighbour soil which reduces shear resistance of soil. The neighbour soils also fail due to the rapid increase in pore-water pressure. Thus a connected failure surface is developed quickly and a flowslide occurs. Based on the saturated-unsaturated seepage theory, transient seepage is computed using the finite element method on loess slope under groundwater table rise. Pore-water pressure distribution for every time step after irrigation are obtained. The phreatic surface in the slope increases with the groundwater table. Pore-water pressure distribution within 8m above the phreatic surface changes very quickly,but the water content and pore water pressure in the region ranging from 8m above the phreatic surface up to ground surface is almost not affected and the matric suction usually is kept at 100~120 kPa. Based on the results of laboratory tests and seepage flow analysis, the development process of loess landslide is modeled considering groundwater table rise. The shearing plastic zone first occurs at the slope toe where the soil is soaked for long term during rise in groundwater table. As irrigation continues, the shearing plastic zone gradually extends to the interior soils, with the results that the tensile plastic zone occurs at the slope crown. As time goes on, both the shearing plastic zone and tensile plastic zone continue to extend. Then a connected plastic zone is formed and fowslide occurs. In comparision to laboratory test results, the results of numerical simulation quite well verify the presented mechanism of static liquefaction of long-runout loess landslides caused by rise in groundwater table.
Resumo:
Projeto de Pós-Graduação/Dissertação apresentado à Universidade Fernando Pessoa como parte dos requisitos para obtenção do grau de Mestre em Medicina Dentária
Resumo:
Projeto de Pós-Graduação/Dissertação apresentado à Universidade Fernando Pessoa como parte dos requisitos para obtenção do grau de Mestre em Medicina Dentária