不同温度条件下土壤水分对羊草幼苗生长特性的影响

采用生长箱控制方法,研究了羊草幼苗生长对5个温度和5个水分梯度的响应。结果表明,不同温度改变了羊草生物量对土壤水分变化的响应类型。在20～26℃下羊草植株生物量对土壤水分的响应曲线呈三次多项式或抛物线变化规律,而在29～32℃下为指数方程。在温度较低或适度时,轻度乃至中度干旱有促进生长的作用,但在温度较高时轻度干旱及比其程度更高的干旱显著地影响羊草的生长,表明羊草在较高温度下对水分更加敏感。在适当的温度下(26℃),羊草根的贡献率或根冠比与土壤水分呈直线关系。高温加强了干旱对羊草幼苗生长的抑制作用,表明高温降低了羊草对干旱的适应能力。     

Internal water balance of barley under soil moisture stress

Leaf water potential, leaf relative water content, and relative transpiration of barley were determined daily under greenhouse conditions at 3 growth stages: tillering to boot, boot to heading, and heading to maturity. The leaf moisture characteristic curve (relative water content versus leaf water potential) was the same for leaves of the same age growing in the same environment for the first 2 stages of growth, but shifted at the heading to maturity stage to higher leaf relative water content for a given leaf water potential. Growth chamber experiments showed that the leaf moisture characteristic curve was not the same for plants growing in different environments.

Relative transpiration data indicated that barley stomates closed at a water potential of about −22 bars at the 3 stages studied.

The water potential was measured for all the leaves on barley to determine the variation of water potential with leaf position. Leaf water potential increased basipetally with plant leaf position. In soil with a moisture content near field capacity a difference of about 16.5 bars was observed between the top and bottom leaves on the same plant, while in soil with a moisture content near the permanent wilting point the difference was only 5.6 bars between the same leaf positions.

     

Effect of soil strength on root growth under different water conditions

The objective of this study was to determine the effects of soil water and soil strength on root growth in situations where the individual effects of both of these factors were important. Three grain legumes were grown from pre-germinated seeds for five days on 50-mm compacted columns of two major soils of Sri Lanka. Four or five levels of bulk density (1.1 to 1.8 Mg.m^–3) and five or six levels of matric potential (–0.02 to–2.0 MPa) were used.Soil strength and matric potential effects on root growth were independently significant for most crop and soil combinations. Under high (wet) matric potential (>–0.77 MPa) soil conditions, the effect of soil water on root growth was evident only in its effect on soil strength. Bulk density had a significant effect on root growth independent of soil strength and matric potential in three cases.For all crops and soils, root penetration was 80% of the maximum or greater when the average soil strength (soil water not limiting) was 0.75 MPa or less, and when the average matric potential (soil strength not limiting) was –0.77 MPa or greater (wetter). Root penetration was 20% of the maximum or less when the soil strength was greater than 3.30 MPa (soil water not limiting), and when matric potential (soil strength not limiting) was less than –3.57 MPa. The use of pre-germinated seeds, which contained imbibed water, combined with a lack of water loss from the closed chambers containing the plants is the probable cause for the very low (–3.57 MPa) matric potential that allowed root growth at 20% of the maximum.     

Effect of air and soil temperature on water balance of jojoba growing under controlled conditions

Jojoba [ Simmondsia chinensis (Link) Schneider] cuttings were grown in pots under constant light intensity and vapour pressure deficit at wir temperatures of 18 and 27°C in climate-controlled cabinets. Leaf conductance and transpiration rate decreased exponentially as the xylen water potential (Ψ_x) decreased concurrently with the drying out of the soil. At high Ψ_x'leaf conductance and transpiration rate were much higher at the higher air temperature, and as Ψ_x declined both parameters decreased more rapidly at 27°C than at 18°C. When soil temperatures were decreased from 27 to 13°C, leaf water potential was not affected at either air temperatures, but transpiration rate was reduced. A linear negative correlation was found between transpiration rates and soil temperatures. It is suggested that the low soil temperature may restrict reducion of water flux in turn reduces stomatal conductance and transpiration without affecting the water potential in the shoot. The releavance of the response to changes in soil or air temperature to the performance of the plant in its semi-arid habitat is discussed.     

Effect of soil moisture at different temperatures on Rhizoctonia root rot of wheat seedlings

The effect of soil moisture at different temperatures on root rot of wheat seedlings caused by Rhizoctonia solani AG-8 was studied in temperature controlled water tanks under glasshouse conditions. Four moisture levels (15, 30, 50 and 75% of soil water holding capacity at saturation which were equal to –10, –7, –5 and –3 kPa, respectively) were tested in tanks maintained 10, 15, 20 or 25 °C. The role of microbial activity in the effect of soil moisture and temperature on disease severity was also studied by including treatments of steam treated soil. Results showed that at soil moisture levels optimum for plant growth (50 and 75% WHC) disease was more severe at a lower temperature (10 °C), but under relatively dry conditions (15% WHC) disease levels were similar at all temperatures tested. In warm soils (20 and 25 °C) at high soil moisture levels (50 and 75% WHC), disease was more severe in steam treated soil than in non-steam treated soil, indicating that the suppression of disease in natural soil under these conditions was associated with high soil microbial activity.     

Impact of Douglas-fir and Scots pine seedlings on plagioclase weathering under acidic conditions

The weathering of soil minerals in forest ecosystems increases nutrient availability for the trees. The rate of such weathering and its relative contribution to forest tree nutrition, is a major issue when evaluating present and potential forest stand productivity and sustainability. The current paper examines the weathering rate of plagioclase with and without Douglas-fir or Scots pine seedlings, in a laboratory experiment at pH 3–4 and 25 °C. All nutrients, with the exception of Ca, were supplied in sufficient amounts in a nutrient solution. The objective of the experiment was to evaluate the potential of trees to mobilise Ca from the mineral plagioclase that contained 12% of Ca. Amounts of nutrients supplied in the nutrient solution, amounts accumulated in the living tissue of the seedlings and amounts leached from the experimental vessels, were measured. A weathering balance, accounting for leached + accumulated − supplied amounts, was established. Bio-induced weathering, defined as the weathering increase in the presence of trees, relative to the weathering rate without trees (geochemical weathering; control vessels), under the present experimental conditions, explained on average, 40% of total weathering (biological + geochemical). These conditions appeared more beneficial to Scots pine (higher relative growth rate, higher Ca incorporation) than to Douglas-fir.     

Longleaf and loblolly pine seedlings respond differently to soil compaction,water content,and fertilization

Aims

Longleaf pine (Pinus palustris Mill.) is being restored across the U.S. South for a multitude of ecological and economic reasons, but our understanding of longleaf pine’s response to soil physical conditions is poor. On the contrary, our understanding of loblolly pine (Pinus taeda L.) root and shoot growth response to soil conditions is well established.

Methods

We performed a comparative greenhouse study which modeled root length density, total seedling biomass, and the ratio of aboveground:belowground mass as functions of volumetric water content, bulk density and soil fertility (fertilized or not).

Results

Root length density was about 35 % greater in longleaf pine seedlings compared to loblolly pine seedlings, and was reasonably well modeled (R ²?=?0.54) for longleaf pine by bulk density (linear), volumetric water content (quadratic), soil fertility, and the interactions of bulk density, volumetric water content, species, and soil fertility. The aboveground:belowground mass ratio (ABR) increased at both extremes of water content.

Conclusions

This research indicates that young longleaf pine seedling root systems respond more negatively to extremes of soil physical conditions than loblolly pine, and compacted or dry loamy soils should be ameliorated in addition to normal competition control, especially on soils degraded by past management.     

Effect of soil moisture depletion on stem shrinkage and photosynthesis of tree seedlings

Effects of soil moisture depletion on stem contraction and photosynthesis of potted 3-year-old white ash (Fraxinus americana L.) and 4-year-old red pine (Pinus resinosa Ait.) seedlings were investigated in greenhouse experiments. White-ash seedlings transpired faster and consequently depleted soil moisture more rapidly than red-pine seedlings. Cumulative stem shrinkage occurred in both species as soils dried and appreciable stem expansion occurred only after soil was reirrigated. Following irrigation, seedlings rehydrated and their stems expanded to about their original diameters within 24 hours in white ash, and in up to 6 days in red pine seedlings. Photosynthesis was decreased in both species as soil dried, but it declined much faster in white ash than in red pine seedlings. Net emission of CO₂ by red pine seedlings occurred after 13 days of soil drying. In contrast, white-ash seedlings did not show net CO₂ release during severe drought. Several days after droughted white-ash and red-pine seedlings were reirrigated, photosynthesis recovered to pre-drought levels. Publication approved by Director of the Wisconsin Agricultural Experiment Station.     

Effect of soil temperature on nutrient allocation and mycorrhizas in Scots pine seedlings

We studied the effect of soil temperature on nutrient allocation and mycorrhizal development in seedlings of Scots pine (Pinus sylvestris L.) during the first 9 weeks of the growing season. One-year-old seedlings were grown in Carex-peat from a drained and forested peatland at soil temperatures of 5, 9, 13 and 17 °C under controlled environmental conditions. Fourteen seedlings from each temperature treatment were harvested at intervals of three weeks and the current and previous year's parts of the roots, stems and needles were separated. Mineral nutrient and Al contents in all plant parts were determined and the tips and mycorrhizas of the new roots were counted. Microbial biomass C and N in the growth medium were determined at the end of the experiment. None of the elements studied, except Fe, were taken up from the soil by the seedlings during the first three weeks. Thereafter, the contents of all the elements increased at all soil temperatures except 5 °C. Element concentrations in needles, stems and roots increased with soil temperature. Higher soil temperature greatly increased the number of root tips and mycorrhizas, and the numbers of mycorrhizas increased more than did the length of new roots. Cenococcum geophilum was relatively more abundant at lower soil temperatures (5 and 9 °C) than at higher ones (13 and 17 °C). A trend was observed for decreased microbial biomass C and N in the peat soil at higher soil temperatures at the end of the experiment.     

Survival of Bemisia tabaci adults under different climatic conditions

The ability of the sweet potato whitefly, Bemisia tabaci Gennad., to survive a range of environmental conditions was investigated in the laboratory. The range of temperature and humidity investigated corresponds to the normal climatic range during B. tabaci's summer migration in Israel. Adult whiteflies confined to small test cages were exposed to combinations of temperature (25, 30, 35, and 41 °C) and relative humidity (20, 50, 80, and 100%) for periods of 2, 4, or 6 h.A logistic regression model describing the four-dimensional surface defining percent survival as a function of time, temperature, and humidity was developed. Using stepwise regression to exclude non-significant terms, the linear predictor included temperature, and the products of temperature and time, and humidity and time. The model accounted for 75% of the variance. A reparameterization of the fitted regression model suggests that survival potential is conditioned by temperature conditions prevailing during the previous 10 h.Whitefly survival after 2 h exposure ranged from 90% survival at 20°C and 100% RH, to <2% survival at 41°C and 20% r.h.. No whiteflies survived more than 2 h exposure at these latter extremes of temperature and humidity. Survival rates decreased slightly after experimental whiteflies were kept in a cage with food a further 20 h at 25±2°C, 55±5% r.h. Investigations of the effects of hunger and virus infection, showed that both increased mortality.     

Variation in soil respiration under the tree canopy in a temperate mixed forest,central China,under different soil water conditions

The forest canopy cover can directly and indirectly affect soil conditions and hence soil carbon emission through soil respiration. Little is known, however, on the effects of canopy cover on soil respiration under the canopy of different tree species and soil water conditions. We have examined the variation in soil respiration at different soil water conditions (dry <10 %, wet >20 %, v/v) under different tree canopy covers in comparison with the canopy interspace in a temperate coniferous (Pinus armandii Franch) and broadleaved (Quercus aliena var. acuteserrata) mixed forest in central China. The results show that soil respiration measured under tree canopy cover varied with canopy size and soil water content. Soil respiration under small-sized canopies of P. armandii (PS) was higher than that under large-sized (PL) canopies, but the difference was only significant under the dry soil condition. However, soil respiration under large-sized canopies of Q. aliena (QL) was significantly greater than that under small-sized (QS) canopies under both dry and wet soil conditions. The difference in soil respiration between differently sized canopies of Q. aliena (33.5–35.8 %) was significantly greater than that between differently sized canopies of P. armandii (2.4–8.1 %). Differences in soil respiration between inter-plant gaps and under QS canopies in both the dry and wet soil conditions were significant. Significant increases in soil respiration (9.7–32.2 %) during the transition from dry to wet conditions were found regardless of canopy size, but the increase of soil respiration was significantly lower under P. armandii canopies (9.7–17.7 %) than under Q. aliena canopies (25.9–31.5 %). Our findings that the canopy cover of different tree species influences soil respiration under different soil moisture conditions could provide useful information for parameterizing and/or calibrating carbon flux models, especially for spatially explicit carbon models.     

不同水分处理对甘蒙柽柳幼苗根系生长特性的影响

以1年生甘蒙柽柳幼苗为对象,采用人工壕沟挖掘法,对柽柳幼苗在不同水分处理条件下(干旱处理、适度灌溉、充分灌溉)根系生态学特征的季节变化进行了研究.结果表明,不同水分处理对柽柳幼苗根系生长影响显著,垂直根扎根深度和生长速率随着灌溉量的减小而增加.地面灌溉量的增加会导致根系分布的浅表化和根系消弱系数的减小,根系生物量与土壤深度呈显著负对数关系.不同水分处理条件下,7-10月的根/冠比平均值分别为0.43、0.60、0.90、1.12,其根、冠间存在典型的异速生长关系.根/冠比随土壤水分的减小而增加,且生长季后期大于初期.     

Evaluation of factors controlling net photosynthetic rate in Scots pine seedlings under field conditions without water stress

Summary The ecological importance of different factors generating variation in the photosynthetic rate of a pine seedling (Pinus sylvestris) under nonstressing conditions are evaluated. The data consists of 1,300 observations of the photosynthetic rate and environmental factors possibly affecting photosynthesis. Statistical analysis of the data gave the following results: 1. light solely explained about 90% of the variance of photosynthetic rate during a day, 2. light and temperature together explained about 94% of it and 3. the other factors studied (leakage from the cuvette, different spectral sensitivity of photosynthesis and the monitoring apparatus, high transpiration rate, circadian rhythm and inhibition of photosynthesis by carbohydrates) were not found to be significant from the ecological point of view, since they explain less than 0.5% of the variance.     

不同土壤水分下山杏光合作用CO2响应过程及其模拟

在半干旱黄土丘陵区,以2年生盆栽山杏为材料,应用CIRAS-2型光合作用系统,测定了8个土壤水分梯度下山杏光合作用的CO2响应过程,并采用直角双曲线模型、指数方程和直角双曲线修正模型对其CO2响应数据进行拟合,分析了山杏光合作用与土壤水分的定量关系.结果表明:山杏CO2响应过程对土壤水分有明显的阈值响应特征.维持山杏叶片较高的光合速率(Pn)和羧化效率(CE)的土壤相对含水量(RWC)在46.3％～81.9％,在此水分范围内,光合作用没有发生明显的CO2饱和抑制现象;当RWC超出此范围,土壤水分升高或降低均明显降低山杏叶片的光合能力(Pnmax)、CE和CO2饱和点(CSP).在不同土壤水分条件下,3个模型对山杏CO2响应数据的模拟效果有明显差别.在46.3％～81.9％土壤水分范围内,3个模型均能较好地拟合山杏CO2响应过程及其特征参数CE、CO2补偿点(Γ)和光呼吸速率(Rp),其拟合精度均表现为直角双曲线修正模型＞指数方程＞直角双曲线模型;当土壤水分含量过高(RWC＞81.9％)或过低(RWC＜46.3％)时,只有直角双曲线修正模型能较好地拟合山杏CO2响应过程及其特征参数.RWC在46.3％ ～81.9％范围内,山杏具有较高的光合作用效率;与传统直角双曲线模型和指数方程相比,直角双曲线修正模型具有更好的适用性.     

Photosynthesis and transpiration of monterey pine seedlings as a function of soil water suction and soil temperature

Rates of photosynthesis, respiration, and transpiration of Monterey pine (Pinus radiata D. Don) were measured under controlled conditions of soil water suction and soil temperature. Air temperature, relative humidity, light intensity, and air movement were maintained constant. Rates of net photosynthesis, respiration, and transpiration decreased with increasing soil water suction. The decrease in the rates of net photosynthesis and transpiration as a function of the soil temperature at low soil water suctions may be attributed to changes in the viscosity of water. At soil water suctions larger than 0.70 bars rates of transpiration and net photosynthesis may be affected in the same proportion by changes in stomatal apertures.     

不同土壤水分下刺槐和油松的生理特征

在适宜土壤水分(70%θf)、中度干旱(55%θf)和严重干旱(40%θf)3种土壤水分条件下研究了黄土高原常见造林树种刺槐(Robinia pseudoacacia L.)和油松(Pinus tabulaeformis Carr.)的生长及水分利用特性.结果表明:干旱胁迫使2树种的成活率、干物质累积和光合速率均显著下降.在适宜水分下刺槐的单叶水分利用率(WUE)最高,严重干旱下最低.刺槐和油松的枝条快速生长期主要集中在3-6月,在中度干旱条件,2个树种均可良好生长;在严重干旱下2个树种的生长均受到显著抑制,但刺槐受影响较大,油松受影响较小.在3种土壤水分条件下刺槐耗水量、生物量及水分利用率均显著高于油松.2树种在中度干旱下的总WUE最高,严重干旱下最低.刺槐属于高耗水树种,油松属于低耗水树种,油松的耐旱性强于刺槐.研究结果表明,刺槐在黄土高原缺水地区不适宜大面积栽植,只能用于水分条件较好的立地条件下造林.油松应尽可能在含水量较高的阴坡或沟坡地带造林.     

Shoot hydraulic characteristics, plant water status and stomatal response in olive trees under different soil water conditions

Aims

To evaluate the impact of the amount and distribution of soil water on xylem anatomy and xylem hydraulics of current-year shoots, plant water status and stomatal conductance of mature ‘Manzanilla’ olive trees.

Methods

Measurements of water potential, stomatal conductance, hydraulic conductivity, vulnerability to embolism, vessel diameter distribution and vessel density were made in trees under full irrigation with non-limiting soil water conditions, localized irrigation, and rain-fed conditions.

Results

All trees showed lower stomatal conductance values in the afternoon than in the morning. The irrigated trees showed water potential values around ?1.4 and ?1.6 MPa whereas the rain-fed trees reached lower values. All trees showed similar specific hydraulic conductivity (K _s) and loss of conductivity values during the morning. In the afternoon, K _s of rain-fed trees tended to be lower than of irrigated trees. No differences in vulnerability to embolism, vessel-diameter distribution and vessel density were observed between treatments.

Conclusions

A tight control of stomatal conductance was observed in olive which allowed irrigated trees to avoid critical water potential values and keep them in a safe range to avoid embolism. The applied water treatments did not influence the xylem anatomy and vulnerability to embolism of current-year shoots of mature olive trees.     

Distribution of spring barley roots in Danish soils,of different texture and under different climatic conditions

Summary Spring barley root profiles have been investigated in three years with different climatological conditions during the growing season. In total, 50 root profiles were determined by measuring cm root/ml soil in different 10 cm sections of the profile. The investigations, show that the root density was nearly identical for all soil types within the upper part of the plough layer. The decrease in root density with depth is most pronounced for the sandy soils and less for the loamy soils. The mean max. root depth in the sandy soils was roughly 70 cm, while it was roughly 140 cm for the loamy soils. A comparison between the clay and silt content in the subsoil and the thickness of soil layers with more than given root densities shows that there is no correlation between texture and thickness of soil layers with more than 1.0 cm root/ml soil, while there was a clear, positive correlation between thickness of soil layers with lower root densities and the clay and silt content in the subsoil. The different climatological conditions during the growing season give rise to differences in the root development. Very wet springs seem to impede root development in loamy soils with slowly permeable subsoils, while this is not the case in the sandy soils.