荒漠植物红砂(Reaumuria soongorica)叶片元素和水分含量与土壤因子的关系

通过测定中国境内荒漠植物红砂(Reaumuria soongorica)主要分布区21个自然种群407个植株叶片的氮(N)、磷(P)、钾(K)含量、有机质和叶片含水量,以及不同种群内土壤含水量、可溶性盐分含量、有机质、全氮、全磷含量等土壤理化性状指标,分析不同自然种群红砂叶片元素含量与土壤环境因子之间的关系.研究结果表明,随着不同土壤层含水量的增加,红砂叶片N含量和叶片含水量显著增加,而叶片K含量显著降低.土壤养分含量、可溶性盐分含量与红砂叶片P含量显著正相关,与叶片含水量显著负相关.随着土壤pH值的增加,红砂叶片N含量显著下降,叶片含水量显著增加.说明不同自然种群中红砂叶片养分含量受土壤状况的影响显著,不同土壤理化性状指标对红砂叶片元素含量的贡献显著不同.土壤水分含量是生境中影响红砂叶片特征的最关键因子,而红砂叶片含水量则最易受各种土壤理化性状的影响.生境中土壤含水量对红砂各种元素含量的影响和红砂叶片含水量对不同土壤条件的这种响应模式支持了红砂是一种以提高水分利用效率而适应于极端干旱生境的典型超旱生植物.     

Relationship between soil solution aluminium and low molecular weight organic acids in a conservation cropping system

Soil solution and solid phase analyses were compared for stubble standing and stubble burnt systems on an acid, acidified and limed Alfisol in north-eastern Victoria. Exchangeable (1 M KCl) aluminium (Al), soil solution total and monomeric Al, pH (water) and soil solution pH were measured to identify any differences in soil acidification between the stubble burnt and the stubble standing treatments. All measures of Al increased with soil depth down to 10 cm in all stubble treatments and decreased in the 10–20 cm soil depth with the exception of lime treatments. Concentrations of low molecular weight organic acids in the soil solution were determined by high pressure liquid chromatography (HPLC). Aromatic and aliphatic acids were distributed throughout the soil depth (0–20 cm) for the stubble standing treatments but were confined to the 0–5 cm soil depth for the stubble burnt treatment. In this short term field trial (2 years for stubble management), the data suggest that the conventional practice of stubble burning was more acidifying than the soil conservation practice of stubble standing, over the 0–20 cm soil depth for the lime (6 t ha^-1) treatments.     

松嫩平原微地形下土壤水盐与植物群落分布的关系

以微域尺度不同盐渍化程度的盐渍土复区为研究区,利用典范对应分析方法(CCA)分析了不同水文年(丰水年、枯水年)土壤盐碱化指标、地表积水、不同土壤层含水率和相对高程与植物群落之间的关系。结果表明,在枯水年由于水分的减少和盐碱化的加重,稗草向虎尾草群落演替,虎尾草向碱蓬群落演替。而芦苇和碱茅群落相对稳定,只是由湿生向旱生转化,群落间演替较慢。在植物群落演替过程中,Na⁺(991 mg/kg)、CO₃^2-(396 mg/kg)、EC(680 μs/cm),pH值(10)是稗草、芦苇向虎尾草和碱茅群落演替的驱动值。Na⁺(1570 mg/kg)、CO₃^2-(576 mg/kg)、EC(879 μs/cm)是虎尾草、碱茅向碱蓬群落演替的驱动值。地表水的积水时间和积水深度是区分稗草和芦苇、虎尾草和碱茅生长分布的重要水文特征值。研究对苏打盐渍土区植被恢复和重建具有重要的意义。     

Histochemical observations on the salmonids Salmo salar L. and Salmo trutta L. and the ephemeropterans Baetis rhodani (Pict.) and Ecdyonurus venosus (Fabr.) following a simulated episode of acidity in an upland stream

Salmonids (Salmo salar, Salmo trutta) and mayflies (Baetis rhodani, Ecdyonurus venosus) which had been exposed to simulated episodes of low pH, and low pH with elevated aluminium, were examined histochemically for the presence of aluminium and mucus. The control fish and mayflies and those exposed to low pH did not stain for aluminium, although increased mucus production was demonstrated in fish gills. Trout and salmon exposed to aluminium at low pH exhibited extensive aluminium and mucus coating of the secondary gill lamellae. No mucus was produced by mayflies but aluminium was apparent on all parts of the body. Mean aluminium concentrations of digested fish gills were 2950 and 3050 g g^–1 dry wt. for trout and salmon respectively, whilst for whole specimens of B. rhodani and E. venosus values were 1 200 and 3 175 g g^–1 dry wt.     

Effects of nitrogen fertilizers on the aluminium contents of mature tea leaf and extractable aluminium in the soil

Increasing rates of nitrogenous fertilizer decreased the aluminium contents in mature leaf of tea but increased the extractable soil aluminium in the 0–30 cm soil depth. Use of NPKS 25:5:5:5 or NPK 20:10:10 did not affect the order of responses. Different rates of potash had no effect on leaf aluminium levels. The concentrations of aluminium in the mature leaf were well above the minimum required for tea nutrition. The increase in extractable soil aluminium due to higher nitrogen rates in part explains the generally low potassium and calcium contents in the leaf and soil.     

Predawn disequilibrium between plant and soil water potentials in two cold-desert shrubs

Classical water relations theory predicts that predawn plant water potential should be in equilibrium with soil water potential (soil Ψ_w) around roots, and many interpretations of plant water status in natural populations are based on this expectation. We examined this expectation for two salt-tolerant, cold-desert shrub species in glasshouse experiments where frequent watering assured homogeneity in soil Ψ_w and soil-root hydraulic continuity and where NaCl controlled soil Ψ_w. Plant water potentials were measured with a pressure chamber (xylem Ψ_p) and thermocouple psychrometers (leaf Ψ_w). Soil Ψ_w was measured with in situ thermocouple psychrometers. Predawn leaf Ψ_w and xylem Ψ_p were significantly more negative than soil Ψ_w, for many treatments, indicating large predawn soil-plant Ψ_w disequilibria: up to 1.2 MPa for Chrysothamnus nauseosus (0 and 100 mm NaCl) and 1.8 MPa for Sarcobatus vermiculatus (0, 100, 300, and 600 mm NaCl). Significant nighttime canopy water loss was one mechanism contributing to predawn disequilibrium, assessed by comparison of xylem Ψ_p for bagged (to minimize transpiration) and unbagged canopies, and by gas exchange measurements. However, nighttime transpiration accounted for only part of the predawn disequilibrium. Other mechanisms that could act with nighttime transpiration to generate large predawn disequilibria are described and include a model of how leaf apoplastic solutes could contribute to the phenomenon. This study is among the first to conclusively document such large departures from the expectation of predawn soil-plant equilibrium for C₃ shrubs, and provides a general framework for considering relative contributions of nighttime transpiration and other plant-related mechanisms to predawn disequilibrium. Received: 12 November 1998 / Accepted: 5 May 1999     

Positive correlation between soil bacterial metabolic and plant species diversity and bacterial and fungal diversity in a vegetation succession on Karst

The hypothesis that positive links exist among plant taxonomic diversity, belowground microbial taxonomic and metabolic diversities was tested for four secondary vegetation successional stages (tussock (T), shrub (S), secondary forest (SF) and primary forest (PF)) in Huanjiang county, SW China. Soil bacterial communities were characterized by DNA fingerprinting and metabolic profiling. Along the succession, Shannon diversity indices followed the order SF>PF>S>T for plant taxonomic diversity, T>SF>PF>S for bacterial operational taxonomic diversity, SF>T>S>PF for fungal operational taxonomic diversity, and SF>PF>S>T for bacterial metabolic diversity. Significant positive correlations were found between bacterial and fungal taxonomic diversities. However, there was no significant correlation between soil microbial taxonomic diversity and bacterial metabolic diversity. Two-way ANOVA revealed that vegetation and season, as well as their interaction, had significant effects on soil microbial (fungal and bacterial) taxonomic diversities, but that there were no seasonal effects on metabolic diversity. However, PCA and MANOVA revealed highly significant differences among the bacterial community-level physiological profiles, reflecting the successional sequence. The findings from this survey support the notion that there are strong interactions between aboveground and belowground communities and suggest that bacterial metabolic and plant taxonomic diversities, but not microbial taxonomic and metabolic diversities, can be correlated.     

Effect of soil acidity, soil strength and macropores on root growth and morphology of perennial grass species differing in acid-soil resistance

It is unclear whether roots of acid-soil resistant plants have significant advantages, compared with acid-soil sensitive genotypes, when growing in high-strength, acid soils or in acid soils where macropores may allow the effects of soil acidity and strength to be avoided. The responses of root growth and morphology to soil acidity, soil strength and macropores by seedlings of five perennial grass genotypes differing in acid-soil resistance were determined, and the interaction of soil acidity and strength for growth and morphology of roots was investigated. Soil acidity and strength altered root length and architecture, root hair development, and deformed the root tip, especially in acid-soil sensitive genotypes. Root length was restricted to some extent by soil acidity in all genotypes, but the adverse impact of soil acidity on root growth by acid-soil resistant genotypes was greater at high levels of soil strength. Roots reacted to soil acidity when growing in macropores, but elongation through high-strength soil was improved. Soil strength can confound the effect of acidity on root growth, with the sensitivity of acid-resistant genotypes being greater in high-strength soils. This highlights the need to select for genotypes that resist both acidity and high soil strength.     

烤烟巨豆三烯酮含量与土壤理化性状的典型相关分析

采用典型相关分析方法研究了烤烟巨豆三烯酮4种同分异构体含量与土壤理化性状之间的关系.结果表明:随着土壤pH值的提高(5.15～8.30),巨豆三烯酮2和巨豆三烯酮4含量呈现降低趋势;随着土壤有机质含量(0.54%～3.61%)的提高,巨豆三烯酮1呈现增加趋势,而巨豆三烯酮2含量呈现降低趋势;随着土壤粒径介于0.05mm和0.001mm之间的土壤颗粒百分含量(8.08%～92.93%)的提高,巨豆三烯酮2和巨豆三烯酮4含量呈现增加趋势;在一定范围内,随着土壤钙、镁、铁、铝含量的提高和钠含量的降低,巨豆三烯酮2和巨豆三烯酮4含量呈现降低趋势.     

水盐变化对荒漠植物功能多样性与物种多样性关系的影响

研究植物功能多样性与物种多样性关系对土壤水盐环境的响应规律,有助于掌握胁迫环境下植物多样性的维持机理.本研究分析了艾比湖高、低土壤水盐环境下荒漠植物功能多样性、物种多样性差异及二者间关系在不同水盐环境下的变化规律.结果表明:(1)高水盐环境下植物功能离散度显著低于低水盐环境(P<0.05),物种多样性指数Fish-α显著高于低水盐环境;(2)一元与多元回归分析均表明,高水盐环境下物种多样性对功能多样性RaoQ与FRic指数有显著促进作用,低水盐环境下物种多样性对功能多样性和均匀度有显著促进作用,但对功能离散度具有显著抑制作用(P<0.05);(3)物种多样性对功能多样性的影响在低水盐环境下更显著,预测力更强;(4)功能丰富度、离散度与均匀度能较敏感地反映出荒漠植物功能多样性对水盐变化的响应.本研究有助于理解荒漠植物群落构建机制,并为荒漠植物恢复与管理提供理论参考.     

氮添加对草地生态系统土壤pH、磷含量和磷酸酶活性的影响

磷是植物必需的大量营养元素之一,也是草地生态系统功能的重要限制因子。近年来,随着全球氮沉降的迅速增加,草地生态系统土壤磷及磷酸酶活性受到不同程度的影响。本研究采用整合分析方法,分析了草地的氮添加量、氮源种类、持续时间和土层深度等对土壤pH、全磷(TP)含量、有效磷(AP)含量、碱性磷酸酶(AlP)和酸性磷酸酶(AcP)活性的影响,以及土壤pH与磷酸酶活性的相关性。结果表明: 氮添加降低了土壤pH、TP含量和AlP活性,提高了土壤AcP活性,但对土壤AP含量无显著影响。从氮添加量来看,土壤pH、AlP显著降低在氮添加>5 g·m^-2·a^-1条件下即可发生;高水平氮添加(>10 g·m^-2·a^-1)导致AcP活性显著提高;土壤TP、AP含量显著降低仅发生在氮添加量为5～10 g·m^-2·a^-1条件下。硝酸铵处理显著降低了土壤TP含量,提高了AcP活性;尿素处理显著降低了土壤pH和AlP活性。在所有添加量下,当试验持续时间为3～10年时,土壤TP含量、AlP活性显著降低;持续时间大于3年时,土壤pH显著降低;>10年时,AcP活性显著提高。0～10 cm土层的AP含量显著升高,TP含量和AlP活性显著降低;大于10 cm土层中AP含量显著降低。土壤pH与土壤AcP活性呈显著负相关,表明氮添加引起的土壤pH改变可能是土壤磷酸酶活性变化的重要原因。     

Effect of different water salinity levels and organic matter application on the composition of water soluble and exchangeable bases in a brackishwater fish pond soil

Behaviour of different water soluble and exchangeable bases in a brackishwater fish pond soil was studied under four levels of water salinity, in combination with and without organic matter application. The results showed average content of water soluble bases to increase with increase in water salinity. The bases were dominated by Na⁺ followed by Mg⁺⁺, Ca⁺⁺ and K⁺ in decreasing order. SAR values of water increased with increase in water salinity and decreased slightly on organic matter treatment.Total content of exchangeable bases in soils was fairly high and was dominated by Ca⁺⁺ and Mg⁺⁺, followed by Na⁺ and K⁺ respectively. Amount of exchangeable Ca⁺⁺ + Mg⁺⁺ decreased while that of Na⁺ increased with increase in water salinity levels. Amount of exchangeable K⁺ did not show any appreciable change. Application of organic matter tended to increase the exchangeable Ca⁺⁺ + Mg⁺⁺ content and decrease the amount of exchangeable Na⁺ in the soil, while exchangeable K⁺ content remained practically unaffected due to organic matter treatment.Formed part of a Ph.D. thesis submitted to Bidhan Chandra Agricultural University, India in 1978Formed part of a Ph.D. thesis submitted to Bidhan Chandra Agricultural University, India in 1978     

Interactive effects between plant functional types and soil factors on tundra species diversity and community composition

Plant communities are coupled with abiotic factors, as species diversity and community composition both respond to and influence climate and soil characteristics. Interactions between vegetation and abiotic factors depend on plant functional types (PFT) as different growth forms will have differential responses to and effects on site characteristics. However, despite the importance of different PFT for community assembly and ecosystem functioning, research has mainly focused on vascular plants. Here, we established a set of observational plots in two contrasting habitats in northeastern Siberia in order to assess the relationship between species diversity and community composition with soil variables, as well as the relationship between vegetation cover and species diversity for two PFT (nonvascular and vascular). We found that nonvascular species diversity decreased with soil acidity and moisture and, to a lesser extent, with soil temperature and active layer thickness. In contrast, no such correlation was found for vascular species diversity. Differences in community composition were found mainly along soil acidity and moisture gradients. However, the proportion of variation in composition explained by the measured soil variables was much lower for nonvascular than for vascular species when considering the PFT separately. We also found different relationships between vegetation cover and species diversity according the PFT and habitat. In support of niche differentiation theory, species diversity and community composition were related to edaphic factors. The distinct relationships found for nonvascular and vascular species suggest the importance of considering multiple PFT when assessing species diversity and composition and their interaction with edaphic factors. Synthesis: Identifying vegetation responses to edaphic factors is a first step toward a better understanding of vegetation–soil feedbacks under climate change. Our results suggest that incorporating differential responses of PFT is important for predicting vegetation shifts, primary productivity, and in turn, ecosystem functioning in a changing climate.     

Relationships between plant and soil water status in vine (Vitis vinifera L.)

Soil water status and its effect on plant water status are commonly evaluated for water stress diagnosis in annual crops. We investigated the application of this method to vineyards, using the fraction of transpirable soil water (FTSW) to characterise the soil water deficit experienced by the plant. The stability of the relationship between FTSW and predawn leaf water potential (Ψp) was analysed over two years (2000–2001), in two contrasted soils in vineyards in south eastern France, both planted with the cultivar Syrah, but grafted on different rootstocks (SO4 and 140Ru). FTSW was determined from soil moisture measurements performed with a neutron probe down to 2.5 m, under the rows and between the rows (3 replicates in each case). Vertical and horizontal variations in soil water content were analysed and the upper and lower limits of total vine’s transpirable soil water (TTSW) were calculated for each soil. The lower limit was also compared with the value of soil moisture content determined at −1.5 MPa in the laboratory. FTSW could be calculated for the soil depth analysed, without distinguishing horizontal position (row or inter-row). The lower limit of TTSW for vine was higher than the soil water content at −1.5 MPa, except in the upper horizons (0–0.2 m) which are prone to soil evaporation. A single relationship between Ψp and FTSW was obtained for the two vineyards and for the two years of measurement. This relationship was similar to that established by Lebon et al. (2003) on Gewürztraminer/SO4 in a vineyard in northern France. FTSW can therefore be used as an indicator of the water deficit experienced in vineyards, provided that TTSW is correctly estimated.     

Field calibration of liming responses of four crops using soil pH,Al and Mn

Liming trials were conducted at 28 sites in the western Great Plains of Canada for barley, rape, red clover and alfalfa. Yield increases from liming correlated with soil pH and Al but not with Mn. When all sites were included, yield increases from liming correlated closely (r=0.86 to 0.94) with exchangeable Al, percent Al saturation and 0.02M CaCl₂-Al for barley, rape and red clover, these responses having correlated less well (R=0.56 to 0.72) with soil pH. Alfalfa yield responses gave low correlations with both pH and the Al measurements. When only the sites with soil pH≥5 were used, the yield responses to lime of barley and rape still correlated better with the Al measurements than with pH even though the correlations, in general, were much lower than when all sites were included. For the sites with soil pH>-5, the correlations were highest for yield responses of barley and rape with 0.02M CaCl₂-Al. It is suggested that the use of toxic Al and Mn for routinely diagnosing the limiting factor by soil acidity could improve on the economy of liming. Contribution Number 653.     

Models for relating pH measurements in water and calcium chloride for a wide range of pH,soil types and depths

Soil pH is commonly measured in water (pHw) or 0.01 M CaCl₂ (pH_Ca). The need to convert between these methods has led to the publication of linear, quadratic and cubic polynomial relationships for limited suites of soils. Concerns over the applicability of such relationships when mapping a wide range of soils and pH led to the establishment of a database of pH_W and pH_Ca values on each of 7894 samples from soil survey and field experimental sites in Queensland. The relationship between pH_W and pH_Ca across all soils was investigated and preliminary results examining the effect of soil depth and soil type on the relationship are presented.For all soils and depths, a linear regression accounted for 93.2% of the variation but did not predict pH_Ca well at very high or low pH_W values. The inclusion of second and third powers of pH_W accounted for significantly more of the variation (R²=0.94) in pH_Ca and the resultant curve matched the data better at high and low pH.Analysis of surface, sub-surface and subsoil groupings did not reveal any appreciable differences in the relationship between pH_W and pH_Ca attributable to depth. In contrast, differences in the relationship were evident between soil types. Generally, the mildly leached soils had linear relationships, while the weathered soils were distinctly curvilinear at low pH.     

Aluminium-induced changes in the surface and micropore properties of wheat roots: a study using the water vapor adsorption-desorption technique

The geometric and energetic characteristics of root surfaces of two wheat (Triticum L.) varieties, Al tolerant (Inia 66/16) and Al sensitive (Henika), were estimated from experimental water vapor adsorption–desorption data. Roots stressed for around 1 week at pH 4 without and with a toxic aluminium level (0.741 mol m^–3) were studied at the tillering and shooting stages. Roots grown continuously at pH 7 were taken as control. The surface properties of the pH 4 stressed roots were apparently the same as those of the control roots whatever the root age. For the roots of both varieties, the surface area and total micropore volume increased markedly after aluminium treatment. The average micropore radius increased significantly for the sensitive wheat, whereas it increased only slightly for the resistant one. Under Al treatment the number of large pores increased while small pores were fewer for both plants, indicating a possible alteration of the build-up of root tissue. The root surface pores were fractal. The fractal dimension of the sensitive wheat roots decreased under Al treatment, whereas for the resistant wheat this remained apparently unchanged. The adsorption energy distribution functions had different shapes for the sensitive and the resistant wheat varieties: the sensitive variety had greater number of high energy adsorption centers, which implies that the root tolerance on Al stress may be connected with lower polarity of the surface.     

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.     

额济纳绿洲胡杨（Populus euphratica）酚类物质含量和分布及其与土壤水分的关系

采用分光光度法测定了额济纳绿洲胡杨(Populus euphratica)的披针形叶、卵圆形叶、嫩枝、枝(D《5 mm)、枝(5～10 mm)、主干树皮、根(D《2 mm)、根(2～5 mm)和根(5～10 mm)9类器官中的总酚、黄酮和缩合单宁含量.结果表明,总酚含量较高的器官为皮(27.93 mg/s),叶、根、枝中总酚含量分别为17.64 mg/g(两类叶均值)、16.72mg/g(三类根均值)、12.19 mg/g(三类枝均值);黄酮含量较高的器官为皮(51.30 mg/g),叶、根、枝中黄酮含量分别为28.45 mg/g(两类叶均值)、39.99 mg/g(三类根均值)、23.67 mg/g(三类枝均值);根中缩合单宁含量较高,三类根均值为22.10 mg/g,皮、叶、枝中缩合单宁含量分别为8.41 mg/g、4.03 mg/g(两类叶均值)、4.47 mg/g(三类枝均值).披针形叶和卵圆形叶中酚类物质含量没有显著性差异(P》0.05);随着枝不断成熟,嫩枝、枝(D《5mm)、枝(5～10mm)中酚类物质逐渐减少;随着根直径减少,根中缩合单宁逐渐增加,细根(D《2mm)中的缩合单宁含量最高(25.95 mg/g).分析胡杨各器官中酚类物质含量与土壤水分的关系,结果表明卵圆形叶中酚类物质含量与土壤水分含量成显著负相关关系(P《0.05,总酚:r=-0.949;黄酮:r=-0.923;缩合单宁:r=-0.944).研究揭示了极端干旱地区胡杨各器官中酚类物质的变化规律,及其与环境因子的相互作用关系.