土壤水分对温室春黄瓜苗期生长与生理特性的影响

以津优1号黄瓜为试验材料．研究了土壤不同水分含量对温室春黄瓜苗期生长与生理特性的影响。结果表明,在土壤水分为田间持水量90％时．黄瓜幼苗长势健壮,茎粗大,根系活力强,叶绿素含量和光合速率高．与其它处理差异显著,说明土壤含水量过高或过低均不利于培育黄瓜壮苗。株高和叶面积随土壤含水量的升高而增加;细胞汁液浓度随土壤含水量的升高而降低．且对植株水分状况反应十分敏感,可以用来作为判断植株水分盈亏状况的生理指标。     

土壤含水量对极小种群毛枝五针松幼苗抗氧化活性的影响

为探究水分对毛枝五针松(Pinus wangii)幼苗生理特性的影响,对不同土壤含水量下幼苗松针的抗氧化活性进行了研究。结果表明,土壤含水量为田间持水量的40%~80%时,其POD、SOD和CAT活性较强;随着处理时间的延长,细胞质膜渗透性减弱,抗逆性变弱;脯氨酸、可溶性糖和蛋白质含量均以20%~40%的田间持水量较高;处理30 d后丙二醛含量随着土壤含水量的增加而提高,在土壤含水量为田间持水量的40%时,丙二醛含量最低,抗逆性最强。因此,人工培育幼苗时,土壤水分过多的时间尽量不要超过30 d,控制土壤水分为田间最大持水量的30%~50%,这样能提高幼苗存活率。     

金矮生苹果叶片气体交换参数对土壤水分的响应

 在黄土高原半干旱地区,通过测定10年生金矮生苹果（Malus pumila cv. Goldspur）叶片气体交换参数与土壤水分的定量关系,探讨了土壤水分胁迫对光合作用的影响规律,以确定苹果园节水灌溉适宜的土壤水分调控标准。结果表明：叶片的净光合速率（Pn）、蒸腾速率（Tr）、水分利用效率（WUE）、气孔导度（Gs）、细胞间隙CO2浓度（Ci）和气孔限制值（Ls）对土壤水分的变化具有明显不同的阈值反应。土壤含水量（SWC）大约在田间持水量的60%～86%范围内,Pn和Tr均保持较高的水平,小于田间持水量的60%～86%后,两者均随土壤湿度的减少而明显下降。维持较高叶片水分利用效率（WUE）的SWC约在田间持水量的50%～71%左右。当SWC小于田间持水量的48%以后,Gs和Ls明显降低,而Ci急剧增加,水分胁迫条件开始直接作用于叶肉细胞,导致光合速率下降,由气孔限制因素转变为非气孔因素。据此我们认为：在半干旱黄土高原地区,金矮生苹果园节水灌溉适宜的SWC范围大约在田间持水量的50%～71%左右,所允许的土壤水分亏缺程度为田间持水量的48%左右。     

不同土壤水分条件下硅对紫花苜蓿水分利用效率及产量构成要素的影响

硅是地壳中含量仅次于氧的元素,植物不可能在无硅的环境中生长.通过盆栽试验研究了不同土壤水分条件下硅对紫花苜蓿(Medicago sativa)水分利用效率及产量构成要素的影响.结果表明,在土壤含水量为田间最大持水量的35%和80%的条件下,硅对紫花苜蓿水分利用效率和生物量没有显著影响,而在土壤含水量为田间最大持水量的50%和65%的条件下,硅显著提高了紫花苜蓿水分利用效率和生物量(p<0.05),紫花苜蓿水分利用效率的增幅分别为35%和20%,主要途径为降低叶片蒸腾速率;紫花苜蓿生物量增幅分别为41%和14%,主要通过促进分枝和株高生长,而不受单枝生物量的影响.因此硅对紫花苜蓿水分利用效率和生物量的有益作用与其生长环境中的土壤水分条件密切相关.     

温室滴灌条件下土壤水分亏缺对番茄产量及其形成过程的影响

采用小区试验,在温室滴灌条件下研究了不同生育阶段土壤水分状况对番茄果实大小、坐果数、畸形果及产量形成过程的影响,分析了温室滴灌条件下番茄总产量与灌水量的关系.结果表明：番茄苗期适度水分亏缺（田间持水量的50%～55%）可提高坐果率,畸形果形成减少,但果实总体偏小,果实成熟主要集中在采摘后期;开花坐果期过度水分亏缺（田间持水量的65%以下）虽可促进果实成熟,但降低了坐果数,易形成小果和畸形果;采摘期水分过高（田间持水量的80%以上）或过低（田间持水量的65%以下）均可降低番茄产量,水分亏缺（田间持水量的65%以下）则使坐果数降低、畸形果增加.各水分处理对果实成熟时间无明显影响;温室番茄总产量、灌溉水利用效率与全生育期灌水总量之间均呈二次抛物线关系;当番茄土壤水分（占田间持水量的百分比）下限控制在苗期60%～65%、开花坐果期70%～75%、成熟采摘期70%～75%时,番茄畸形果形成量减少,产量及坐果率较高,可作为滴灌条件下温室番茄适宜的土壤水分控制指标.     

黄土塬区3种豆科牧草对土壤水分的消耗利用研究

在田间完全旱作条件下采用3个密度和2种播种方式观察了3种多年生豆科牧草生长第2年对土壤水分的消耗利用情况。结果表明:苜蓿主要耗水深度在2~3 m,最深可达5 m,其中、高密度处理3 m以上土壤水分含量都在稳定田间持水量之下,已经开始形成土壤下伏干层;沙打旺耗水深度在0~2 m,最低含水量(11.61%)处于80~100 cm,在雨季可以恢复到稳定田间持水量之上;达乌里胡枝子主要耗水深度在1 m以上,最低含水量也在稳定田间持水量之上。单播沙打旺、苜蓿和达乌里胡枝子全生长期内对土壤水分的消耗分别为249.9、180.2和136.6 mm,水分利用效率分别是29.39、26.04和8.91 kg.mm-1.hm-2。混播、加大播种密度都会增加3种牧草土壤水分消耗,降低土壤储水量,提高干草产量和水分利用效率,但影响程度因牧草种类、播种方式以及不同的生长时段而异。     

土壤水分亏缺对春小麦根系干物质累积和分配的影响

在人工气候室中进行实验,实施光、温自动控制,研究了土壤水分对春小麦根系干物质积累和分配的影响,３个处理是春小科整个生长发育期内土壤水分分别控制在田间持水量的３０％,６０％,９０％,实验结果表明,在四叶一心－抽穗开花期间,３个处理气孔阻力逐渐降低,光合速率蒸腾速度逐渐上升,其中,中等水分条件下蒸腾速率明显低于充分供水,而光合速率则接近或显著高于是。抽一开花期,下层以根长,根竽中等水分处理显著高于其余     

土壤水分胁迫对不同茬次紫花苜蓿丙二醛及抗氧化酶含量的影响

为研究土壤水分胁迫对不同茬次紫花苜蓿丙二醛含量及抗氧化酶活性的影响，文章以新疆大叶苜蓿为研究对象，采用盆栽称重法控制土壤含水量（TA为充分供水，85%田间持水量；TB为轻度胁迫，65%田间持水量；TC为重胁迫，45%田间持水量），来研究不同土壤水分胁迫对不同茬次过氧化物酶（POD）、超氧物歧化酶（SOD）、过氧化氢酶（CAT）在分枝期、返青期、现蕾期、开花期的活性，同时也研究不同水分胁迫下新疆大叶苜蓿各时期丙二醛（MDA）含量。实验结果表明，随着植物器官生育期的发展和土壤水分胁迫的加剧，MDA含量呈逐渐增长趋势；同时也表明，3种抗氧化酶在分枝期达最大值，且在轻度水分胁迫（TB）下达到最大值，最大值分别为POD=6.543 6,SOD=226.388 1,CAT=38.106 6。该结论为干旱、半干旱地区植物的抗旱机制研究提供了科学依据。     

水分胁迫效应对冬小麦生长发育影响的试验研究

利用大型水分试验场遮雨棚遮档自然降水,采用人工定量补水进水进行冬小麦土壤占田间持量40％－50％、45％－50％、50％－55％、50％－60％、55％－60％、60％－70％持续时间分别为5、10、15d水分胁迫处理的控制试验。试验结果表明：控制结束复水后,50％－60％、55％－70％水分胁迫处理诱发冬小麦根、茎、叶、总生物量显著增长或明显减缓其衰老速率。土壤含水量占田间持水量50％－60％处理,具有明显的增产、节水效率,确定土壤含水量占田间持水量55％为冬小麦拔期水分胁迫应增产节水的水分临界指标。     

不同膜下滴灌方式对设施黄瓜生理特性及水分利用效率的影响

为了探明黄瓜膜下分根交替滴灌的节水效果,为设施黄瓜节水灌溉提供理论依据和技术参数,以‘津优3号’黄瓜为试材,采用随机区组设计,以土壤田间持水量的65%为灌水下限,田间持水量的90%为灌水上限,研究了分根交替滴灌(APDI)、固定1/2根区滴灌(FPDI)和传统滴灌(CDI)3种灌溉模式对黄瓜生长、生理特性、产量与品质及水分利用效率的影响,结果表明:(1)随灌溉处理时间的延长,3种灌溉模式的单株叶面积和株高的差异越来越显著,而茎粗和叶片数差异不显著;(2)与传统滴灌相比,分根交替滴灌模式下黄瓜叶片净光合速率略有下降而蒸腾速率显著降低,水分利用效率显著提高;(3)分根交替滴灌处理下黄瓜可溶性蛋白、可溶性糖含量与传统滴灌相比差异不显著,Vc含量却显著增加;(4)分根交替滴灌模式下黄瓜产量比传统滴灌下降1.5%,而灌水量减少17%,水分利用效率提高18.6%,节水效果显著。综上所述,分根交替滴灌可以在保证设施黄瓜产量没有显著下降的前提下,改善品质和显著提高水分利用效率,可作为设施节水提质增效的一种灌溉模式,推广应用前景广阔。     

Role of water transport in origin of water stress

Intensity of transpiration, intensity of water absorption, water saturation deficit (w.s.d.) in different parts of samples and rate of water transport was investigated in samples from leaf tissue of fodder cabbage and banana-tree. In all experiments (at initial w.s.d. 0% and 20%, in samples from upper, middle and lower leaves of fodder cabbage and from leaves of banana-tree) a distinct gradient of w.s.d. in the direction of transport of water was determined, therefore the limiting factor in the water balance was rate of water transport and not rate of water absorption. The lowest amount of water was always transported within transpiring part of sample. When the initial w.s.d. was 0% not only the water transported by tissue from the environment, but also the water of the leaf tissue itself took part in water lost by transpiration and therefore water stress originated in the whole sample. At an initial w.s.d. of 20%, the rate of water absorption was higher than the rate of water transport and therefore the increase of w.s.d. in the transpiring part of the sample was accompanied by a simultaneous decrease of w.s.d. in the transporting part. An increase in the value of w.s.d. in leaf tissue proportionally increased the resistance of water transport in the liquid phase (on the average from 1·7 . 10³ to 6·7 . 10³ atm min cm² g^?1) and also in the gaseous phase (on the average from 2·7 . 10^?2 to 14·0 . 10^?2 min cm^?1). It was proved that insufficient rate of water transport can be responsible for the origin of water stress. At the same time the rate of water transport was influenced by the value of the w.s.d. since every change of w.s.d. in leaf tissue not only the gradient of water potential changed but also the resistance to water transport.     

Decomposition of young water hyacinth leaves in lake water

Rates of weight loss and release of nutrients during different phases of decomposition in young water hyacinth leaves were determined under laboratory conditions. The leaves decomposed solely by physical leaching during the initial 4-day phase and later by microbial processes. The largest part of weight loss and nutrient release by physical leaching took place within the first 4 h of incubation and thereafter the decomposition rate declined. Microbial processes decayed leaves at a significantly higher rate than that by physical leaching. The overall decay rate constants were related inversely and the release of nutrients directly to the levels of leaf additions in the lake water. The dissolved inorganic and organic nutrients were released chiefly by abiotic processes during the initial as well as later phases of decay. The release was significantly higher during the initial phase in comparison with that during the later phase. Microbes utilized only a small amount of nutrients that were released during decomposition of water hyacinth leaves. The % release of various elements from the decaying leaves was in the order of K > P > C > Na > N.     

Decomposition of water hyacinth detritus in eutrophic lake water

A study was conducted to determine the seasonal production of detritus by water hyacinths [Eichhornia crassipes (Mart.) Sohns] cultured in eutrophic Lake Apopka water, and the decomposition of detritus in situ and under laboratory conditions. Annual averages for C, N and P deposited through detritus production at the sediment-water interface were 2870, 176 and 19 kg ha^-1 yr^-1, respectively.Decomposition rates were faster in the root zone of hyacinth mats than at the sediment-water interface. Approximately 92% of the detritus C deposited at the sediment-water interface was decomposed in one year, while only 11% of the detrital organic N was mineralized. Detrital tissue gained P during decomposition, suggesting P limitation for the system. Dry-weight loss of detrital tissue was significantly correlated with the mass of C lost (r ² = 0.947^**), C/N ratio (r ² = 0.644^**) and C/P ratio (r ² = 0.428^**).Florida Agricultural Experiment Stations Journal Series No. R-00348.     

水的饱和辛醇溶液水分标准物质的研制

生物燃料的国家标准规定了产品的技术指标和相应的检测方法。水的饱和辛醇溶液的水分标准物质,用于生物燃料水分测量时仪器的校准和方法的验证,能够保障测量结果的准确可靠和等效一致。该标准物质采用卡尔·费休库仑法、卡尔·费休容量法和定量核磁共振等三种不同原理的方法定值。通过方法研究和改进,实现了库仑法和容量法的一致;通过引入新的核磁共振方法,提高了结果的准确性。最终标准物质的水分量值为4.76％,扩展不确定度为0.09％。     

Relative water content and water potential of tissue 1

Relative water content (RWC) and water potential as measuredwith the pressure chamber were evaluated as indicators of waterstatus of tissue-cultured apple shoots and plantlets (shootswith roots). During the hydration required for RWC measurement,both water content and water potential exhibited the same hydrationkinetics, indicating that 10 h were required for full hydration.Once full hydration was reached, shoot mass remained relativelyconstant. Moisture release characteristics were also constructedand the associated shoot and plantlet water relations parameterswere estimated. Underin vitroconditions, both shoot and plantletwater potential were similar to the water potential of the culturemedium in which they were grown. The moisture release characteristicof shoots and plantlets was consistent with that expected fortypical plant tissues, and gave estimates of maximum modulusof elasticity (6.201.14 MPa), osmotic potential at saturation(–0.85 0.10 MPa), osmotic potential at zero turgor (–1.16 0.14 MPa) and RWC at zero turgor (78 2%) which were similarto values in the literature. Higher values of leaf conductanceand RWC were found in shoots and plantlets placed at 95% RH(21 C) compared to those at 90% RH. Plantlets had higher valuesof both conductance and RWC compared to shoots, suggesting thatinvitroroots are functional in water uptake. Relative water contentwas related to measures of physiological activity such as leafconductance, and it was also easier to measure than water potential.Relative water content is suggested as a sound index of waterstatus in tissue culture plants. Key words: Conductance, microculture, water status, water stress.     

Inferring foliar water uptake using stable isotopes of water

A growing number of studies have described the direct absorption of water into leaves, a phenomenon known as foliar water uptake. The resultant increase in the amount of water in the leaf can be important for plant function. Exposing leaves to isotopically enriched or depleted water sources has become a common method for establishing whether or not a plant is capable of carrying out foliar water uptake. However, a careful inspection of our understanding of the fluxes of water isotopes between leaves and the atmosphere under high humidity conditions shows that there can clearly be isotopic exchange between the two pools even in the absence of a change in the mass of water in the leaf. We provide experimental evidence that while leaf water isotope ratios may change following exposure to a fog event using water with a depleted oxygen isotope ratio, leaf mass only changes when leaves are experiencing a water deficit that creates a driving gradient for the uptake of water by the leaf. Studies that rely on stable isotopes of water as a means of studying plant water use, particularly with respect to foliar water uptake, must consider the effects of these isotopic exchange processes.     

Global monthly water scarcity: blue water footprints versus blue water availability

Freshwater scarcity is a growing concern, placing considerable importance on the accuracy of indicators used to characterize and map water scarcity worldwide. We improve upon past efforts by using estimates of blue water footprints (consumptive use of ground- and surface water flows) rather than water withdrawals, accounting for the flows needed to sustain critical ecological functions and by considering monthly rather than annual values. We analyzed 405 river basins for the period 1996-2005. In 201 basins with 2.67 billion inhabitants there was severe water scarcity during at least one month of the year. The ecological and economic consequences of increasing degrees of water scarcity--as evidenced by the Rio Grande (Rio Bravo), Indus, and Murray-Darling River Basins--can include complete desiccation during dry seasons, decimation of aquatic biodiversity, and substantial economic disruption.