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1.
The clogging of drippers caused by crop root intrusion has been a great concern of subsurface drip irrigation (SDI) systems. To attempt to solve the problem of root clogging of drippers, a series of field experiments were conducted in the growing seasons of 2006-2008. The goal was to investigate the effects of Treflan injection on dripper clogging by roots, and on root distribution, yield, and the quality of winter wheat (Triticum aestivum L.) under SDI. For each growing season, two Treflan injection dates (March 6 and April 15 for the 2006-2007 growing season, and March 6 and April 15 for the 2007-2008 growing season) and three injection concentrations of 0, 3, and 7 mg/l were arranged in a randomized block experimental design. During harvest, root length density (RLD) and Treflan concentration at different soil layers were measured using the auger-sampling method. Thirty-five drippers from each treatment were randomly chosen to observe evidence of root intrusion into the dripper flow passage in order to estimate root clogging. The experimental results showed that Treflan injection could effectively reduce root density in areas adjacent to drippers, thereby significantly decreasing the potential of root clogging. In 2007, 4 out of the 35 drippers were found with root intrusion problems in the control (without Treflan injection), while no root clogging existed any dripper in Treflan application treatments. In 2008, 6 drippers from the control but only 1 dripper from those treated with Treflan application showed root clogging. In addition, within the range of concentration used by the current experiment, Treflan concentrations had no significant effects on winter wheat root distribution, yield, and quality. Injection date, however, influenced the vertical root distribution significantly. Injection of Treflan late in the growing season influenced the root distribution only in the areas close to the drippers; the influenced areas increased if Treflan was injected early in the growing season.  相似文献   

2.
线源滴灌土壤湿润均匀性的影响因素试验研究   总被引：2，自引：1，他引：2  
线源滴灌设计中,滴灌管出流均匀性与土壤湿润均匀性有本质不同,前者仅仅是后者必要的基础,但是要保证线源滴灌土壤湿润均匀性,还需要考虑滴头间距、滴头流量、滴水量和土壤质地的差别。对影响线源滴灌土壤湿润均匀性的主要因素进行了试验研究。试验中所用土壤为沙土和沙壤土;滴头间距为30 cm和50 cm;滴头流量为0.3~4 L/h;滴水量为10~25 L不等。试验表明,沿滴灌管方向的土壤湿润均匀度取决于湿润区的交汇程度,而湿润区的交汇程度又取决于土壤湿润区水平运移宽度和滴头间距。沙土沿滴灌管方向的土壤湿润均匀度随滴水量的增大而显著增大,沙壤土的相应指标则随滴头流量的增大而增大。土壤湿润均匀度随滴头间距的增大而减小。线源滴灌设计时,粘粒含量较少的土壤应该有一定的设计湿润深度和较小的滴头间距才能保证其湿润均匀度满足设计要求。研究结论对完善滴灌技术设计理论有帮助。  相似文献   

3.
This study was carried out at the experimental field station of the Atomic Energy Authority in Anshas, Egypt, by the aim of assessing the soil moisture status under surface and subsurface drip irrigation systems, as a function of the variation in the distance between drippers along and between laterals. Moisture measurements were carried out using neutron moisture meter technique, and water distribution uniformity was assessed by applying Surfer Model. The presented data indicated that the soil moisture distribution and its uniformity within the soil profile under surface drip was to great extent affected by the distance between drippers rather than that between laterals. Generally, the soil moisture distribution under using 30-cm dripper spacing was better than of that under 50 cm. Under subsurface drip irrigation, the allocation of the irrigation system was the factor that dominantly affected the moisture trend under the studied variables. Installing the system at 30 cm from the soil surface is the one to be recommended as it represents the active root zone for most vegetable crops, beside it leads to a better water saving in sandy soils than that allocated at 15 cm depth.  相似文献   

4.
The uniform and precise application of microbial particles close to the target organism and to the plant to be protected can increase the success of a biological control treatment. The use of systems or technologies which are usually available in agriculture could influence the acceptability of biocontrol agents by farmers, and enlarge the market. A pilot system was realized using dripper lines, drippers, filters and other tools commonly used in irrigation and precision agriculture in the greenhouse to evaluate their suitability for applying and distributing microbial biocontrol agents. Conidial suspensions of marketed or marketable agents were used, i.e. Fusarium oxysporum, F. solani, Trichoderma harzianum and Paecilomyces lilacinus. The experiments carried out demonstrated that conidial suspensions (106 conidia ml−1) can pass through the drippers without causing clogging, regardless of their size, and remained viable. The term ‘microbigation’ is here proposed for this kind of microbial application technique.  相似文献   

5.
葡萄分层地下滴灌滴头布设深度优化   总被引：1，自引：0，他引：1  
为解决不同树龄葡萄根系的差异使得地下滴灌系统在布设应用中存在的困难,采用室内试验和HYDRUS-2D数值模拟相结合的方法,以宁夏和关中葡萄产区为例,研究了2种土质条件下分层地下滴灌土壤水分运动规律,提出了分层地下滴灌带最佳布设深度.研究结果表明,HYDRUS-2D模拟值与试验实测值具有良好的吻合度.地下滴灌带的埋深直接影响土壤水分的分布,2种土质下湿润体内部处于最佳含水率区间的土壤体积随滴头间距的增加而增大.通过适当增大浅层滴头埋深并减小深层滴头埋深可减小表层水分无效损耗.从避免水分无效消耗以及提高湿润体与根系匹配效果等角度出发,建议关中地区葡萄单滴头灌溉且适宜滴灌带布设深度为20 cm;宁夏贺兰山地区滴灌带布设深度以15 cm和45 cm为宜.  相似文献   

6.
The increased use of marginal quality water with drip irrigation requires sound fertigation practices that reconcile environmental concerns with viable crop production objectives. We conducted experiments to characterize dynamics and patterns of soil solution within wet bulb formed by drip irrigation. Time-domain reflectometry probes were used to monitor the distribution of potassium nitrate (KNO3) and water distribution from drippers discharging at constant flow rates of 2, 4 and 8 L h−1 in soil-filled containers. Considering results from different profiles, we observed greater solute storage near the dripper decreasing gradually towards the wetting front. About half of the applied KNO3 solution (48%) was stored in the first layer (0–0.10 m) for all experiments, 29% was stored in the next layer (0.10–0.20 m). Comparing different dripper flow rates, we observed higher solution storage for 4 L h−1, with 45, 53 and 47% of applied KNO3 solution accumulating in the first layer (0–0.10 m) for dripper flow rates of 2, 4 and 8 L h−1, respectively. The results suggest that based on the volume and frequency used in this experiment, it would be advantageous to apply small amounts of solution at more frequent intervals to reduce deep percolation losses of applied water and solutes.  相似文献   

7.
Dripper clogging is a major drawback of microirrigation systems that must be addressed to improve their efficiency and durability. Particle-induced clogging is first studied in situ. The experiments consist in observing in real conditions the behavior of a series of drippers fitted on an agricultural plot in the south of France. The plot is supplied from a canal with Durance River water. The latter is loaded with sediments that gradually clog drippers and filters. Water analysis reveal that physicochemical clogging prevails over biological clogging. This characterization helps in setting in-lab experiment protocol. Indeed, besides field observation of clogging, laboratory analyses of both the irrigation water and the clogging material are performed with reactive and inert clay: smectite and an illite–calcite mix. A surprising tendency is observed: Salt concentration in smectite seeded water decreases the clogging, whereas it increases agglomerate size. Computational fluid dynamic simulations are carried out to investigate the impact of particles on flow behavior. Results demonstrate that clay particles interacting with the flow govern the complex structure of the fluid velocity fields inside the dripper labyrinth channel.  相似文献   

8.
为探明加气滴灌下滴头堵塞规律及影响因素,选用4种不同特征参数(流量Q、最小断面尺寸min(W,D)和入水栅格面积M)的内镶贴片式滴头E1,E2,E3和E4,分别在加气(AI)和未加气(CK)条件下进行了滴头堵塞测试,并通过泥沙絮凝沉降试验对其结果进行了验证.结果表明:加气和滴头结构对滴头堵塞性能具有显著影响(P<0.05).加气加剧水中泥沙颗粒的絮凝沉降、加速絮凝颗粒在毛管内和流道入口的黏附、增大滴头入口发生突然堵塞风险是造成加气加剧滴头堵塞的主要原因;当选择入口尺寸较大的E4滴头时,其流道入口堵塞风险降低、流道内泥沙絮凝沉降速率减缓而表现出加气减缓滴头堵塞,而选择入口尺寸较小的E1—E3滴头时,其毛管内泥沙絮凝沉降速率增大、滴头入口堵塞风险增高而表现出加气加剧滴头堵塞.  相似文献   

9.
通过小麦盆栽试验,研究向地下滴灌系统施加氟乐灵的排根效应。结果表明,地下滴灌不施药时滴头所在的竖直方向根密度较大,而施加少量氟乐灵后,滴头所在位置处根密度有不同程度降低,说明氟乐灵有抑制小麦根系向滴头附近生长的趋势。施药时间、施药浓度和施药量均对药物排根效应显著影响,其中施药时间为极显著。施药时间越晚,排根范围越小,出苗后50d施药的平均排根范围仅为3.03cm2;施药浓度越小,排根范围越小,浓度为1.5g/L及1.2g/L的排根范围接近,而浓度为0.9g/L的平均排根范围最小,为6.0cm2;施药量越小排根范围越小,施药量为0.023g/滴头的平均排根范围为8.37cm2。  相似文献   

10.
Wetting plant foliage with saline irrigation increases the uptake of toxic ions Na+ and Cl−. Over three consecutive seasons, Colombard vines grafted on Ramsey rootstock were irrigated with saline water (EC 3.5 dS/m) by over-canopy sprinklers during any one of the first three of the four annual growth stages: bud burst to full bloom (treatment BB-FB), full bloom to veraison (treatment FB-V), and veraison to harvest (treatment V-H). At other times, vines received non-saline water (EC 0.5 dS/m) as did the control. Seasonal average soil salinities remained relatively constant over the trial. In contrast, the concentrations of Na+ and Cl− in one-year old wood and grape juice more than doubled. In treatments FB-V and V-H the average yield over the three seasons was reduced by up to 15%. Results were compared with those obtained in an earlier study which was undertaken in the same vineyard with the same treatments applied via dripper. With drippers, the maximum reduction in the average yield over three seasons was 2%. Saline sprinkling caused rises in Na+ and Cl− concentrations of fruit, leaf lamina and one-year-old wood that were at least 7-fold, 5-fold and 2-fold greater, respectively, than the rises caused by application of the same treatments with drip. Progressive seasonal rises in the concentrations of Na+ and Cl− in these tissues were due in part to carryover of salt added in previous seasons; with saline sprinkling the magnitude of these carryovers was 4-fold greater than those with saline drip irrigation. With saline water, vignerons can reduce losses by using irrigation systems which do not wet the foliage.  相似文献   

11.
Intercropping, drip irrigation, and the use of plastic mulch are important management practices, which can, when utilized simultaneously, increase crop production and save irrigation water. Investigating soil water dynamics in the root zone of the intercropping field under such conditions is essential in order to understand the combined effects of these practices and to promote their wider use. However, not much work has been done to investigate soil water dynamics in the root zone of drip-irrigated, strip intercropping fields under plastic mulch. Three field experiments with different irrigation treatments (high T1, moderate T2, and low T3) were conducted to evaluate soil water contents (SWC) at different locations, for different irrigation treatments, and with respect to dripper lines and plants (corn and tomatoes). Experimental data were then used to calibrate the HYDRUS (2D/3D) model. Comparison between experimental data and model simulations showed that HYDRUS (2D/3D) described different irrigation events and SWC in the root zone well, with average relative errors of 10.8, 9.5, and 11.6 % for irrigation treatments T1, T2, and T3, respectively, and with corresponding root mean square errors of 0.043, 0.035, and 0.040 cm3 cm?3, respectively. The results showed that the SWC in the shallow root zone (0–40 cm) was lower under non-mulched locations than under mulched locations, irrespective of the irrigation treatment, while no significant differences in the SWC were observed in the deeper root zone (40–100 cm). The SWC in the shallow root zone was significantly higher for the high irrigation treatment (T1) than for the low irrigation treatment, while, again, no differences were observed in the deeper root zone. Simulations of two-dimensional SWC distributions revealed that the low irrigation treatment (T3) produced serious severe water stress (with SWCs near the wilting point) in the 30–40 cm part of the root zone, and that using separate drip emitter lines for each crop is well suited for producing the optimal soil water distribution pattern in the root zone of the intercropping field. The results of this study can be very useful in designing an optimal irrigation plan for intercropped fields.  相似文献   

12.
通过室内滴灌入渗的三维水盐运移试验,分析了斥水和亲水土壤在相同滴头流量下的湿润锋变化规律,研究了轻微斥水土壤的湿润锋随时间变化规律、含水率的三维空间分布特征以及不同斥水度土壤中含盐量和Cl-浓度分布特点。结果表明,在相同的滴头流量(0.07mL/min)下,亲水土壤与轻微斥水土壤的水平、垂直湿润锋与入渗时间具有良好的幂函数关系;亲水土壤与轻微斥水的土壤含盐量与距滴头距离符合良好的二阶多项式关系;虽然定量结果不同,但总体上轻微斥水的土壤在入渗中仍与亲水土壤具有相似的水分、盐分分布特征。在轻微斥水的农田中,滴灌灌水技术仍可为作物创造有利的水盐环境。  相似文献   

13.
  The size of the free-water ponds under drippers is an important field characteristic of trickle irrigation. Here we review four existing analytical theories that purport to describe 3-D infiltration. We show how they can be used to predict the extent of the pond from basic soil parameters, and the dripper discharge rate. Via a numerical example it is shown that the different theories give significantly different free-water pond radii, especially for high drip discharge rates when the flow is dominated by gravity. We then describe field experiments that were carried out to permit a comparison of the measured and predicted values using independently-measured soil parameters. This test of the different theories was conducted on a loamy soil. Raats' (1971) solution gave the best estimates of the free-water pond radius, across the range of discharge rates. The free-water pond radius, a determinant of the lateral spread away from the dripper, was found to vary only weakly with drip discharge in the range of practical applications. Consequences for management are discussed. Received: 24 September 1995  相似文献   

14.
黄土高原重力式地下滴灌水分运动模型与分区参数研究   总被引：6，自引：6，他引：0  
建立了重力式地下滴灌条件下的土壤水分运动模型,分析地下滴灌土壤水分入渗规律.对黄土高原不同分区的4种典型土壤、不同灌水技术要素条件下的地下滴灌土壤湿润体形态、滴孔处出流量及土壤土水势进行数值模拟得出:榆林紧砂土土壤导水率较大,向下渗漏过多,不适宜地下滴灌;安塞砂壤土、洛川中壤土、武功重壤土在相同灌水量下,供水压力与滴孔孔径对地下滴灌湿润体形态影响微弱,但对滴孔出流量有较大影响,因此在地下滴灌工程设计时,只需根据田块长度和渗水管损失设计孔径和供水压力,并采用较小供水压力,降低供水水池高度,减小工程量;对武功重壤土,孔径和供水压力较大时地下滴灌滴孔处土壤易饱和板结,宜采用较小的孔径和供水压力.  相似文献   

15.
A field study was conducted at North Platte, Nebraska in 2007–2009, imposing eight irrigation treatments, ranging from dryland to fully irrigated. Four of the eight treatments allowed for various degrees of water stress only after tasseling and silking. In 2007, corn yield ranged from 8.9 Mg ha?1 with a season total of 41 mm of irrigation water to 11.5 Mg ha?1 for the fully irrigated treatment (264 mm of irrigation water). The treatment with the greatest reduction in irrigation water after tasseling and silking (158 mm) had a mean yield of 10.9 Mg ha?1, only 0.6 Mg ha?1 less than the fully irrigated treatment. In 2009, yields ranged from 12.6 to 13.5 Mg ha?1. There were no significant yield differences between the irrigation treatments for several possible reasons: more in-season precipitation and cooler weather required less irrigation water; much of the irrigation water was applied after the most water-stress sensitive stages of tasseling and silking; and lower atmospheric demand allowed for soil water contents well below 50 % management allowed depletion (MAD) not to cause any yield losses.  相似文献   

16.
A 2-year experiment was carried out to investigate the effects of different drip irrigation regimes on distribution and dynamics of soil water and salt in north Xinjiang, China. Five treatments—F7 (0.24 dS m?1 + Once every 7 days), B7 (4.68 dS m?1 + Once every 7 days), S7 (7.42 dS m?1 + Once every 7 days), F10 (0.24 dS m?1 + Once every 10 days) and F3 (0.24 dS m?1 + Once every 3 days)—were designed. For all treatments, additional 150-mm fresh water was applied on 10th November in 2009 (winter irrigation) to leach the accumulated salt. The results revealed that irrigation frequency and water quality had significant effects on the spatial distribution and change of soil water content, soil salt and the crop water consumption rate, but had a limited impact on the seasonal accumulative water consumption, and the cotton yield decreased with the decrease in irrigation frequency and water quality on the whole. During the cotton growing season, results showed that the salt mainly accumulated in the 0- to 60-cm soil layer, while the soil salt in 60- to 100-cm layer changed slightly, indicating that the drip irrigation could not leach the soil salt out of the root zone under the irrigation regimes. Therefore, salt leaching was necessary to maintain the soil water–salt balance and to prevent excessive salt accumulation in the root zone. After the 150-mm winter irrigation and subsequent thawing, soil salts were leached into the deeper layers (below 60 cm), and the soil salt content (SSC) (EC1:5) in root zone in the next year was about 0.2 dS m?1. Moreover, compared to 2009 season, the SSC within the root zone did not increase even the EC of the irrigation water was up to 7.42 dS m?1. Additionally, it is important to note that the results were concluded based on the data of the 2-year experiment; further studies are need to optimize winter irrigation amount and assess the sustainability of saline water irrigation since long-term utilization of saline water may lead to soil degradation.  相似文献   

17.
Emitter discharge of subsurface drip irrigation (SDI) decreases as a result of the overpressure in the soil water at the discharge orifice. In this paper, the variation in dripper discharge in SDI laterals is studied. First, the emitter coefficient of flow variation CV q was measured in laboratory experiments with drippers of 2 and 4 L/h that were laid both on the soil and beneath it. Additionally, the soil pressure coefficient of variation CV hs was measured in buried emitters. Then, the irrigation uniformity was simulated in SDI and surface irrigation laterals under the same operating conditions and uniform soils; sandy and loamy. CV q was similar for the compensating models of both the surface and subsurface emitters. However, CV q decreased for the 2-L/h non-compensating model in the loamy soil. This shows a possible self-regulation of non-compensating emitter discharge in SDI, due to the interaction between effects of emitter discharge and soil pressure. This resulted in the irrigation uniformity of SDI non-compensating emitters to be greater than surface drip irrigation. The uniformity with pressure-compensating emitters would be similar in both cases, provided the overpressures in SDI are less than or equal to the compensation range lower limit.  相似文献   

18.
A field experiment was conducted for 3 years to evaluate the effect of deficit irrigation under different soil management practices on biomass production, grain yield, yield components and water productivity of spring wheat (Triticum estivum L.). Soil management practices consisted of tillage (conventional and deep tillage) and Farmyard manure (0 and 10 t ha?1 FYM). Line source sprinkler laterals were used to generate one full- (ETm) and four deficit irrigation treatments that were 88, 75, 62 and 46 % of ETm, and designated as ETd1, ETd2, ETd3, and ETd4. Deep tillage significantly enhanced grain yield (14–18 %) and water productivity (1.27–1.34 kg m?3) over conventional tillage. Similarly, application of FYM at 10 t ha?1 significantly improved grain yield (10–13 %) and water productivity (1.25–1.31 kg m?3) in comparison with no FYM. Grain yield response to irrigation varied significantly (5,281–2,704 kg ha?1) due to differences in soil water contents. Water productivity varied from 1.05 to 1.34 kg m?3, among the treatments in 3 years. The interactive effect of irrigation × tillage practices and irrigation × FYM on grain yield was significant. Yield performance proved that deficit irrigation (ETd2) subjected to 75 % soil water deficit had the smallest yield decline with significant water saving would be the most appropriate irrigation level for wheat production in arid regions.  相似文献   

19.
Laboratory experiments were carried out to investigate bioclogging on three types of online emitters using synthetic wastewater filtered at 10 μm (COD = 200 mg L?1). The three types of emitters were as follows: non-pressure-compensating emitters delivering 2 L h?1 (NPC2), non-pressure-compensating emitters delivering 4 L h?1 (NPC4) and pressure-compensating emitters delivering 2.2 L h?1 (PC). They were plugged on two parallel pipe diameters (16 and 20 mm). Emitter performance was followed by flow rate measurements. The results showed that PC emitters seemed to be more sensitive to clogging than NPC emitters. Biofilm was observed mainly on NPC flow paths and PC membranes; its presence was also confirmed by the assessment of different water quality parameters such as total organic carbon and pH. Experimental results compared with a model designed with computational fluid dynamics Software (ANSYS Fluent®) showed relations between biofilm development and velocity distribution on NPC flow paths. Finally, pipe diameter also appeared to be a parameter inducing emitter clogging.  相似文献   

20.
A laboratory experiment was carried out to study the emitter performance of three commonly used emitter types with the application of freshwater and treated sewage effluent (TSE). The three emitter types are the inline-labyrinth types of emitters with a turbulent flow (E1) and a laminar flow (E2) and the online pressure-compensation type of emitters (E3). The qualities of freshwater and TSE were measured, and the emitter performance was evaluated, using the relative emitter discharge, the reduction of emitter discharge (qreduction), the coefficient of variation of emitter discharge (CV), the emission uniformity (EU), Christiansen uniformity coefficient (CU), and the percentage of emitter clogging (Pclog). Results showed that all indices were affected by water quality, emitter type and time of operation. The values of qreduction, CV and Pclog for the TSE treatments were greater than those for the freshwater treatments. The values of EU and CU for the TSE treatment were lower than those for the freshwater treatments. The qreduction, CV and Pclog increased and the EU and CU decreased as operational time increasing for the TSE treatment. For both freshwater and TSE treatments, the emitter clogging was more severe, the CV was greater, and the EU and CU were smaller for emitter type E2 than those for emitter types E1 and E3. Thus a more severe clogging was found for emitter type E2 due to its smaller flow-path dimension and higher manufacturing coefficient of variation in addition to the high pH values and relatively high total dissolved solids (TDS) values of the used water. Analyses of water quality and the precipitation components inside and at the outlet of emitters revealed that chemical precipitation was the main reason for emitter clogging due to high pH and ions’ concentration, especially in the TSE. Flushing emitters and drip pipes did not efficiently alleviate emitter clogging caused by chemical precipitation. In a conclusion, emitter type E3 showed a better anti-clogging function than emitter types E1 and E2 and was recommended for irrigation with TSE in the Beijing area of China.  相似文献   

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