水肥互作对滴灌玉米氮素吸收、水氮利用效率及产量的影响

优化水、氮供应是实现作物高产与水肥资源高效利用的有效途径.本文研究了田间试验条件下,水(4500、6750、9000 m³·hm^-2)、氮(0、225、330、435、540 kg·hm^-2)互作对高密度(≥105000 株·hm^-2)滴灌玉米干物质积累、氮素吸收及产量的影响.结果表明: 玉米干物质积累与吸氮量均随灌溉和施氮水平的增加明显升高,当施氮量大于435 kg·hm^-2和灌溉量大于9000 m³·hm^-2时则呈减少趋势.完熟期玉米干物质积累对灌水的响应表现为W₆₇₅₀(36359 kg·hm^-2)>W₉₀₀₀(35077 kg·hm^-2)>W₄₅₀₀(33451 kg·hm^-2),施氮对玉米吸氮量的变化表现为N₄₃₅(459.9 kg·hm^-2)>N₅₄₀(458.1 kg·hm^-2)>N₃₃₀(416.3 kg·hm^-2)>N₂₂₅(351.3 kg·hm^-2),N₄₃₅比N₃₃₀、N₂₂₀分别升高9.1%、32.7%,N₅₄₀比N₄₃₅降低0.6%.在施氮量0～435 kg·hm^-2范围内,玉米最大氮素吸收速率随施氮量增加而升高,在施氮量为435 kg·hm^-2时达最大(6.57 kg·hm^-2·d^-1).灌水与施氮均可显著增加玉米产量、穗粒数和穗粒质量,二者有明显的正交互作用,且以氮为主效应.在施氮0～435 kg·hm^-2范围内,氮肥利用率随施氮量的增加而升高,此后反而降低;灌溉水分生产率随施氮量升高而增加,随灌水量增加而明显下降,灌溉定额为4500～6750 m³·hm^-2时,灌溉水分生产率可达2.57～3.80 kg·m^-3.玉米最高产量18072 kg·hm^-2的施氮量为567.0 kg·hm^-2.最佳经济施氮量为427.9～467.7 kg N·hm^-2时,玉米产量在17109～17138 kg·hm^-2,氮素偏生产力和氮肥利用率分别达122 kg N·hm^-2和45.0%.水氮一体化施肥可实现滴灌玉米高产协同水、氮利用效率的共同提高.     

调亏灌溉对菘蓝水分利用及产量的影响

通过探究水分调亏对河西地区膜下滴灌菘蓝(Isatis indigotica)各项生理指标、产量和水分利用的影响, 为菘蓝高效节水种植提供理论指导。于2016年在河西走廊中部张掖市民乐县益民灌溉试验站进行菘蓝水分调亏研究, 在保持苗期和肉质根成熟期充分灌溉的情况下, 在菘蓝营养生长期和肉质根生长期分别进行轻度、中度和重度的水分亏缺处理, 并测定各项光合生理指标、产量和水分利用率。结果表明, 营养生长期和肉质根生长期的中度与重度水分亏缺显著降低了菘蓝叶片净光合速率、叶面积指数、株高及主根长, 并且随水分亏缺程度加重降幅增大; 而轻度水分亏缺与对照组的差异不显著。营养生长期和肉质根生长期轻度水分亏缺处理的菘蓝产量与水分利用效率最高, 分别达到8 239.56 kg·hm^-2和24.11 kg·hm^-2·mm^-1; 其它水分亏缺处理组产量和水分利用效率均有所降低, 与对照组之间差异显著(P<0.05), 重度水分亏缺处理各项指标均最低。因此, 最优的菘蓝水分调控处理为营养生长期和肉质根生长期的轻度水分调亏, 能够降低菘蓝耗水量, 提高水分利用效率且其产量不会降低。     

覆膜与滴灌对河套灌区玉米花粒期叶片光合特征的影响

光合作用是作物生长发育和产量形成的基础,栽培方式和土壤含水量变化显著影响作物的光合作用.灌浆期和乳熟期是玉米花粒期2个重要阶段,是玉米籽粒形成和干物质积累的关键时期.通过大田试验研究了河套灌区不同覆膜方式与滴灌水平对不同生育时期玉米光合特征及产量的影响.结果表明: 灌浆期玉米叶片光合特征在不同处理下无显著差异,乳熟期净光合速率和蒸腾速率在半覆膜(B₂)和全覆膜(Q₂)滴灌水平2(350 mm)处理下均显著高于半覆膜(B₁)和全覆膜(Q₁)滴灌水平1(200 mm),并且B₁和Q₁处理下灌浆期叶片的净光合速率、蒸腾速率、水分利用效率及气孔导度等显著高于乳熟期.不同处理下灌浆期和乳熟期叶片的净光合速率、蒸腾速率,灌浆期的气孔导度以及乳熟期的水分利用效率等在日变化上存在着同步关系,均呈现出倒“U”型的日变化特征,而胞间CO₂浓度则呈现相反的变化趋势.逐步回归分析显示,光合有效辐射、大气温度和空气相对湿度等气象因子是影响玉米叶片光合特征的主要环境因子.此外,B₂和Q₂处理下玉米产量显著高于B₁和Q₁处理(分别增加了29.3%和50.9%),但B₁和Q₁处理间并无显著差异.这表明与覆膜方式相比,滴灌水平对干旱地区玉米产量的影响更大.     

Development of a concentration method for detection of tobacco mosaic virus in irrigation water

Tobacco mosaic virus (TMV) causes significant yield loss in susceptible crops irrigated with contaminated water. However, detection of TMV in water is difficult owing to extremely low concentrations of the virus. Here, we developed a simple method for the detection and quantification of TMV in irrigation water. TMV was reliably detected at concentrations as low as 10 viral copies/μL with real-time PCR. The sensitivity of detection was further improved using polyethylene glycol 6000 (PEG6000, MW 6000) to concentrate TMV from water samples. Among the 28 samples from Shaanxi Province examined with our method, 17 were tested positive after virus concentration. Infectivity of TMV in the original water sample as well as after concentration was confirmed using PCR. The limiting concentration of TMV in water to re-infect plants was determined as 10² viral copies/mL. The method developed in this study offers a novel approach to detect TMV in irrigation water, and may provide an effective tool to control crop infection.     

棉花苞叶光呼吸和PSII热耗散对土壤水分的响应

在新疆气候生态条件下, 采用膜下滴灌植棉技术, 设置不同滴灌水分处理, 研究了不同滴灌量条件下棉花(Gossypium hirsutum)苞叶和叶片碳同化、光呼吸作用、光系统II (PSII)热耗散作用及其光破坏防御机制的差异, 以揭示滴灌节水条件下棉花苞叶缓解光抑制的机理及与棉花抗旱特性的关系。结果表明: 棉花开花后苞叶及叶片在高温强光下实际光化学效率(Φ_PSII)显著降低, 发生明显的光抑制现象, 但苞叶的光抑制程度较叶片轻; 与正常滴灌量处理相比, 节水滴灌条件下棉花水分亏缺, 叶片净光合速率(P_n)、Φ_PSII、光呼吸(P_r)、光化学猝灭系数(q_P)降低, 非光化学猝灭系数(NPQ)升高, 叶片光抑制程度加重, 而苞叶P_n、Φ_PSII、P_r、q_P、NPQ变化不大, 与正常滴灌量处理相比, 光抑制程度无显著差异。苞叶光呼吸速率与光合速率的比值(P_r/P_n)显著高于叶片; 滴灌节水条件下棉花适度水分亏缺对苞叶光呼吸及P_r/P_n无显著影响。高温强光下, 棉花节水滴灌对叶片PSII量子产量的转化与分配影响显著, 但对苞叶的影响不显著; 苞叶非调节性能量耗散的量子产量(Y(NPQ))高于叶片, 因此能有效地将PSII的过剩光能以热的形式耗散。综上所述, 与叶片相比, 苞叶对轻度水分亏缺不敏感, 是棉花适应干旱逆境较强的器官, 苞叶光呼吸和热耗散作用对光破坏防御具有重要意义。     

Roles of Aquaporins in Root Responses to Irrigation

Due to current environmental issues concerning the use of water for irrigation, the improvement of crop water-use efficiency and a reduction in water consumption has become a priority. New irrigation methods that reduce water use, while still maintaining production have been developed. To optimise these techniques knowledge of above- and below-ground plant physiological responses is necessary. During growth, plant roots are exposed to cycles of wetting and drying in normal rain-fed and irrigation situations. This review concentrates on the below-ground aspects, in particular the water permeability of roots. Significant research has been conducted on the root anatomy and hydraulic conductivity of desert plants subjected to wetting and drying. Major intrinsic proteins (MIPs), most of which show aquaporin (water-channel) activity are likely to be involved in balancing the water relations of the plants during water deficit. However, many MIPs seem to allow permeation of other small neutral solutes and some may allow permeation of ions under certain conditions. The ability of the plant to rapidly respond to rewetting may be important in maintaining productivity. It has been suggested that aquaporins may be involved in this rapid response. The down-regulation of the aquaporins during dry conditions can also limit water loss to the soil, and intrinsic sensitivity of aquaporins to water potential is shown here to be very strong in some cases (NOD26). However, the response of aquaporins in various plant species to water deficits has been quite varied. Another component of aquaporin regulation in response to various stresses (hypoxia/anoxia, salinity and chilling) may be related to redistribution of flow to more favourable regions of the soil. Some irrigation techniques may be triggering these responses. Diurnal fluctuations of root hydraulic conductance that is related to aquaporin expression seem to match the expected transpirational demands of the shoot, and it remains to be seen if shoot-to-root signalling may be important in regulation of root aquaporins. If so, canopy management typical of horticultural crops may impact on root hydraulic conductance. An understanding of the regulation of aquaporins may assist in the development of improved resistance to water stress and greater efficiency of water use by taking into account where and when roots best absorb water.     

The air-borne distribution of zoonotic agents from livestock waste spreading and microbiological risk to fresh produce from contaminated irrigation sources

Aims:  To assess the risks of zoonotic agents in dissemination of livestock wastes into the environment by airborne distribution. To subsequently assess the survival time of zoonotic agents, introduced in irrigation water, on the phylloplane of produce.
Methods and Results:  An Escherichia coli marker was introduced into pig slurry which was spread using a rain gun sprayer. Air sampling was undertaken to determine the distance reached by the marker. No recoveries were observed at a distance of 250 m. Borehole water, contaminated with zoonotic agents, was used to irrigate field plots sown with lettuce and spinach. Decline in bacterial numbers on the phylloplane was observed with time. After initial rapid decreases, we were unable to detect any pathogen from the phylloplane, 1 month after contamination.
Conclusions:  These preliminary results suggest that the risks to public health from the aerosolized spread of bacteria during slurry spreading by rain gun are low. Although, zoonotic agents on crop phylloplanes perish quickly, the risks of overhead irrigation of fresh produce 3 weeks before harvest should still be considered.
Significance and Impact of the Study:  These preliminary results improve our understanding on the fate of zoonotic agents in the environment. Spreading liquid livestock wastes by an airborne mechanism may not pose a significant public health risk. Detection of zoonotic agents 3 weeks after contamination of lettuce and spinach means that consideration should be given by the farmers until the time of harvest, when irrigating fresh produce with water that may have been directly or indirectly contaminated by livestock wastes.     

Effects of elevated CO2 concentration, supplemental irrigation and nitrogenous fertilizer application on rain-fed spring wheat yield

It is expected that the CO₂ concentration of the Earth’s atmosphere will reach 600–1000 ppm by the end of the 21st century. Therefore, in this study, we evaluated the effects of elevated CO₂ concentrations on the development of rain-fed spring wheat in an attempt to identify a practical pathway to increase crop production. To accomplish this, a field experiment was conducted at Guyuan Experimental Station in a semiarid region of China during 2005–2007. During this experiment, the CO₂ concentration was increased to 40.0 ppm and supplemental irrigation and nitrogenous fertilizer (N fertilizer) were applied. The experimental results showed that the elevated CO₂ concentration significantly improved the thousand-grain weight and the grain number per spike. Furthermore, supplemental irrigation and N fertilizer application during the elongation and booting stage of rain-fed spring wheat in conjunction with an elevated CO₂ concentration improved the water use efficiency (WUE), nitrogen use efficiency (NUE), thousand-grain weight, and the yield by 14.6%, 39.6%, 9.3%, and 14.7%, respectively, when compared to groups subjected to the same treatment but not grown under elevated CO₂ concentrations. Furthermore, the spring wheat yield was improved by 81.8% in response to an elevated CO₂ concentration, 60 mm of supplemental irrigation and applied N fertilizer (37.5 g m^?2 NH₄NO₃). However, the presence of an elevated CO₂ concentration without supplemental irrigation and N fertilizer only resulted in an increase in the wheat yield of 7.8%. Consequently, the combination of elevated CO₂ concentration, supplemental irrigation and N fertilizer application played an important role in the improvement of WUE, NUE, thousand-grain weight, and grain yield of rain-fed spring wheat in this region.