土壤水分变化对长白山主要树种蒙古栎幼树生长的影响

选择长白山红松阔叶林主要优势树种蒙古栎为研究对象,人工控制3种施水量研究蒙古栎幼树形态、生物量效应和光合生理特征对土壤含水量变化的响应．结果表明,不同土壤含水量变化显著影响蒙古栎叶片、枝、根的生物量及其分配格局和叶片光合气体交换特征．水分胁迫改变幼树树冠结构,抑制幼树树高、地径、叶片大小、地上和地下生物量;同时,蒙古栎幼树根冠生物量比随着土壤水分含量的减少显著提高;供水量减少对幼树净光合速率、CO2利用率和碳利用率等特征有显著的负向影响;而叶片气孔导度、蒸腾速率和水分利用率对不同土壤含水量反应较复杂,只在土壤含水量较低时,幼树气孔导度、蒸腾速率明显降低,叶片水分利用率升高,表现出蒙古栎树种是干旱可变植物,长期水分胁迫可提高树种的耐旱能力．     

养分对旱地小麦水分腔迫的生理补偿效应

利用不同深度渗漏池供水差异所造成的水分胁迫,分期测定冬小麦叶片的净光合速率、气孔阻力、叶肉胞间ＣＯ２浓度、蒸腾强度、叶绿素含量和叶片吸光强度。研究养分对小麦水分胁迫的生理补偿效应。结果表明,水分腔迫后,气孔阻力增加,叶绿素含量和净光合速率显著下降。但在水分胁迫时施用氮肥,蒸腾速率减弱,叶绿素含量,叶片吸光强度和净光合速率增加,因而,短时水分利用效率显著提高。这表明,因水分胁迫导致净光合速率和短时水     

NaC1胁迫对4种豆科树种幼苗生长和K+、Na+含量的影响

以合欢、刺槐、国槐和皂英4种豆科树种盆栽实生幼苗为试验材料,研究了NaC1胁迫下4个树种幼苗的生长、耐盐临界浓度和Na+、K+含量的变化,并对其耐盐性进行了比较.结果表明:NaC1胁迫抑制了4个树种幼苗的生长,苗木的干物质积累量减小、根冠比增大,尤其对合欢和皂荚的影响较大;以相对干质量降至对照组50%时的NaC1浓度作为生长临界NaC1浓度(C50)指标,4个树种的耐盐强弱顺序为:刺槐(5.0‰)＞国槐(4.5‰)＞皂荚(3.9‰)＞合欢(3.0‰);随NaC1浓度的增加,各树种幼苗根、茎、叶中Na+含量逐渐增加,K+含量先增加后减小(合欢根除外),而K+/Na+差异较大.相同浓度NaC1胁迫下,幼苗器官的Na+分布为根＞茎＞叶,K+因树种和NaC1浓度不同而各异,以叶片中较多,K+/Na+为叶＞茎＞根.NaC1胁迫下,刺槐的K+含量和K+/Na+较高,地上部分Na+含量较低,幼苗干物质量大,耐盐性较强;而合欢的K+/Na+较小,高浓度NaC1胁迫下地上部分的Na+含量较高,幼苗干物质量小,耐盐性较差.苗木地上部分对K+的积累和根部对Na+的滞留是影响豆科树种耐盐性能的主要因素.     

土壤干旱条件下玉米叶片内源激素含量及光合作用的变化

利用ＨＰＬＣ和ＥＬＩＳＡ技术研究了土壤干旱条件下玉米叶片内源ＩＡＡ、ＡＢＡ、ＺＲ、ＤＨＺＲ、ｉＰＡ含量的变化情况,以及叶片光合作用过程中,光合速率（Ｐｎ）,气孔导度（Ｇｓ）,ＰＳⅡ光化学效率（Ｆｖ／Ｆｍ）的变化情况,结果发现：叶片中ＩＡＡ浓度,在整个干旱过程中变化不大,与对照相比下降不明显;ＩＡＡ的浓度对干旱的反应不敏感;叶片中ＡＢＡ浓度在干旱最初３ｄ里急剧升高,直至最大值,之后有所下降;ＡＢＡ的     

水杉异砧嫁接植株体内激素的分布和含量变化

同一生期育不同器官或同一器官不同生育的水杉异砧嫁接植株砧穗各器官中均含有ＧＡ３,ＩＡＡ,ＺＴ和ＡＢＡ,以ＧＡ３含量最高,１０、１１月休眠前期,接穗水杉叶片中ＧＡ３,ＺＴ和ＡＢＡ含量显著高于砧木叶片,砧木叶片中ＩＡＡ含量分别是接穗叶片的１．５和１．９倍。砧木根和接穗叶芽,花芽中４种激素含量均高于砧穗的茎,而接穗的雌球花芽则高于雄球花芽。     

土壤干旱期间墨兰的水分生理变化

研究了盆栽墨兰〔Ｃｙｍｂｉｄｉｕｍｓｉｎｅｎｓｅ（Ａｎｄｒ．）Ｗｉｌｌｄ．］在不同土壤含水量情况下的水分生理变化。不同叶龄的叶片对于干旱反应不同,一年生叶比二年生叶敏感。在叶片含水量、叶片水势、叶绿素含量、蒸腾速率和气孔阻力等生理参数中,后两者对干旱反应最灵敏。所以,一年生幼叶的蒸滕速率和气孔阻力可作为指标去判断墨兰植株水分供应情况。墨兰在土壤持水力４４．２％时,相对透性较小,生长正常,一年生动叶的蒸腾速率和气孔阻力分别是３．３６μｇ·ｃｍ￣（－２）·ｓ￣（－１）和７．０８ｓ·ｃｍ￣（－１）;当土壤干旱,持水力降至２２．５％时,相对透性增大３９％,说明细胞已经受旱害,该时的蒸腾速率降至０．９５μｇ、ｃｍ￣（－２）·ｓ￣（－１）,气孔阻力升为２２．２５ｓ·ｃｍ￣（－１）。可以认为,墨兰的土壤临界水分是在土壤持水力４４％—２２％之间。     

4种针叶幼树光合速率,蒸腾速率与土壤含水量的关系及其抗旱性研究

对半干旱区４种针叶幼树的光合速率、蒸腾速率与土壤含水量关系的分析表明,二者均有随土壤含水量下降而减小的趋势,其关系可用回归方程ｙ＝Ａ＋Ｂｅ（－ｋｘ）表示．依此式计算出的净光合速率（Ｙ）等于零时的土壤含水量（Ｘ）值,各树种间有明显的差别,该值小的树种具有较强的抗旱性．其抗旱性顺序为侧柏＞樟子松＞油松＞白扦．     

NaCl胁迫对4种豆科树种幼苗生长和K+、Na+含量的影响

以合欢、刺槐、国槐和皂荚4种豆科树种盆栽实生幼苗为试验材料,研究了NaCl胁迫下4个树种幼苗的生长、耐盐临界浓度和Na⁺、K⁺含量的变化,并对其耐盐性进行了比较.结果表明：NaCl胁迫抑制了4个树种幼苗的生长,苗木的干物质积累量减小、根冠比增大,尤其对合欢和皂荚的影响较大;以相对干质量降至对照组50%时的NaCl浓度作为生长临界NaCl浓度(C₅₀)指标,4个树种的耐盐强弱顺序为：刺槐(5.0‰)＞国槐(4.5‰)＞皂荚(3.9‰)＞合欢(3.0‰);随NaCl浓度的增加,各树种幼苗根、茎、叶中Na⁺含量逐渐增加,K⁺含量先增加后减小（合欢根除外）,而K⁺/Na⁺差异较大.相同浓度NaCl胁迫下,幼苗器官的Na⁺分布为根＞茎＞叶,K⁺因树种和NaCl浓度不同而各异,以叶片中较多,K⁺/Na⁺为叶＞茎＞根.NaCl胁迫下,刺槐的K⁺含量和K⁺/Na⁺较高,地上部分Na⁺含量较低,幼苗干物质量大,耐盐性较强;而合欢的K⁺/Na⁺较小,高浓度NaCl胁迫下地上部分的Na⁺含量较高,幼苗干物质量小,耐盐性较差.苗木地上部分对K⁺的积累和根部对Na⁺的滞留是影响豆科树种耐盐性能的主要因素.     

浙东常绿阔叶林植物功能性状对土壤含水量变化的响应

研究群落演替过程中植物功能性状与土壤含水量的关系, 揭示植物对水分供给变化的响应策略, 具有重要的生态学意义。该研究以浙江东部天童山、南山和双峰山的3个常绿阔叶林演替系列为对象, 旨在探索不同演替阶段常见植物的功能性状与森林群落土壤含水量的相互关系。研究结果显示: 森林演替中后期的树木高度、树冠面积、叶片干物质含量显著大于演替前期植物; 相反, 叶片净光合速率和蒸腾速率随演替进程而降低。随森林演替, 表层土壤(0-20 cm)的含水量显著增加, 深层土壤(20-40 cm)含水量随演替进程增加但不显著。表层土壤含水量与树木高度、树冠面积和叶片干物质含量显著正相关, 与叶片净光合速率和蒸腾速率显著负相关; 深层土壤含水量与树冠面积显著正相关, 与叶片净光合速率、气孔导度和蒸腾速率显著负相关。树木高度、树冠面积、叶片干物质含量、叶片净光合速率、气孔导度和蒸腾速率均可解释土壤含水量随演替进程的变化趋势, 而冠长比对土壤水分变化的响应最为敏感。     

欧洲3种常见乔木幼苗在两种光环境下叶片的气体交换、叶绿素含量和氮素含量

在室内测定了分别栽培于全光照和20％光照条件下的垂枝桦Betulapendula,欧洲水青冈Fagussylvatica和欧洲白栎Quercusrobur幼苗叶片的光合作用－光响应曲线、叶片气孔导度、胞间二氧化碳浓度、水分利用效率,叶绿素含量和氮素含量,并分析叶片叶绿素含量和净光合速率的回归关系．20％光照条件引起净光合速率的光饱和点下降,叶片气孔导度和水分利用效率以及单位叶面积叶绿素含量降低,叶片的光合物质积累减少,但氮素含量上升．回归分析结果表明,叶片叶绿素含量与净光合速率成正相关．3种植物的幼苗对荫蔽条件有一定的适应性,其中B．pendula和Q．robur的耐荫能力比Fsylvatica强.     

黄土区树种抗旱性指数的研究

根据ＰＶ曲线主要水分参数测定数据,进行了黄土区６个乔,灌木树种抗旱性季节变化趋势和树种间抗旱性指数排序分析,结果表明,树种抗旱性指数在生长季（５－１０月）呈具有阶段降低的持续增大趋势,仅在雨季中后期（即树木年第２４生长高峰期）略有减小,在年生长季土壤严重干旱阶段,树种的抗旱性指数大小排序为：海红〉河北杨〉柠条〉小叶杨〉北京杨〉刺槐。     

Impact of flooding on soil bacterial communities associated with poplar (Populus sp.) trees

Soil bacterial communities were analyzed in different habitats (bulk soil, rhizosphere, rhizoplane) of poplar tree microcosms (Populus tremulaxP. alba) using cultivation-independent methods. The roots of poplar trees regularly experience flooded and anoxic conditions. Therefore, we also determined the effect of flooding on microbial communities in microcosm experiments. Total community DNA was extracted and bacterial 16S rRNA genes were amplified by PCR and analyzed by terminal restriction fragment length polymorphism (T-RFLP) analysis, cloning and sequencing. Clone libraries were created from all three habitats under both unflooded and flooded conditions resulting in a total of 281 sequences. Numbers of different sequences (<97% similarity) in the different habitats represented 16-55% of total bacterial species richness determined from the nonparametric richness estimator Chao1. According to the number of different terminal restriction fragments (T-RFs), all of the different habitats contained approximately 20 different operational taxonomic units (OTUs), except the flooded rhizoplane habitat whose community contained less OTUs. Results of cloning and T-RFLP analysis generally supported each other. Correspondence analysis of T-RFLP patterns showed that the bacterial communities were different in bulk soil, rhizosphere and rhizoplane and changed upon flooding. For example OTUs representing Bacillus sp. were highest in the unflooded bulk soil and rhizosphere. Sequences related to Aquaspirillum, in contrast, were predominant on the poplar roots and in the rhizosphere of flooded microcosms but were rarely found in the other habitats.     

采煤沉陷区不同造林树种恢复土壤酚酸物质对土壤微生物的影响

酚酸物质是影响微生物群落和结构的最重要因子之一,研究酚酸物质在不同造林树种土壤中的变化规律及其与微生物群落结构的关系,有助于更好地了解和揭示采煤沉陷区恢复造林条件下微生物群落变化的机制.本研究在双鸭山宝山采煤沉陷区的撂荒地基础上营造三针一阔(红松、落叶松、樟子松和杨树)人工林,测定这4种造林地土壤酚类物质、11种酚酸物质和微生物群落结构.结果表明: 复合态酚含量总体表现为人工林显著高于撂荒地,其中,落叶松人工林和杨树人工林的复合态酚含量较高,落叶松人工林和红松人工林的总酚含量显著高于撂荒地,红松人工林的水溶性酚含量显著高于撂荒地;在11种酚酸物质中,阿魏酸、松香酸、β-谷甾醇、齐墩果酸、莽草酸、亚油酸和硬脂酸的含量在人工林土壤中较高.土壤酚类物质与土壤微生物生物量不存在显著的相关关系,个别的酚酸物质与土壤微生物的相关关系显著,其中,阿魏酸、松香酸和β-谷甾醇对土壤微生物生物量有明显的促进作用,与真菌和真菌/细菌存在显著的正相关关系.杨树人工林的酚酸物质含量较高,说明营造杨树人工林对采煤沉陷区的土壤恢复有益.     

Microbial community biomass and structure in saline and non-saline soils associated with salt- and boron-tolerant poplar clones grown for the phytoremediation of selenium

Poplar trees (Populus spp.) are often used in bioremediation strategies because of their ability to phytoextract potential toxic ions, e.g., selenium (Se) from poor quality soils. Soil microorganisms may play a vital role in sustaining health of soil and/or tolerance of these trees grown in poor quality soils by contributing to nutrient cycling, soil structure, overall soil quality, and plant survival. The effect of naturally occurring salts boron (B) and Se on soil microbial community composition associated with poplar trees is not known for bioremediation strategies. In this study, three Populus clones 13–366, 345–1, and 347–14 were grown in spring 2006 under highly saline, B, and Se clay-like soils in the west side of the San Joaquin Valley (SJV) of CA, as well as in non-saline sandy loam soils located in the east side of the SJV. After 7 years of growing in the respective soils of different qualities, soil samples were collected from poplar clones grown in saline and non-saline soils to examine and compare soil quality effects on soil microbial community biomass and composition. The phospholipid fatty acid (PLFA) analysis was used to characterize microbial community composition in soils from trees grown at both locations. This study showed that microbial biomass and the amount and proportion of arbuscular mycorrhizal fungal (AMF) community were lower in all three poplar clones grown in saline soil compared to non-saline soil. Amounts of Gram + bacterial and actinomycetes PLFAs were significantly lower in poplar clone 13–366 grown in saline soil compared to non-saline soil; however, they did not differ significantly in poplar clones 347–14 and 345–1. Additionally, amounts of saprophytic fungal, Gram ? bacterial and eukaryotic PLFA remained similar at saline and non-saline sites under poplar clones 347–14, 345–1, and 13–366. Therefore, this study suggested that salinity and B do have an impact on microbial biomass and AMF; however, these poplar clones still recycled sufficient amount of nutrients to support and protect saprophytic fungal and bacterial communities from the effects of poor quality soils.     

A generic 3D finite element model of tree anchorage integrating soil mechanics and real root system architecture

Understanding the mechanism of tree anchorage in a forest is a priority because of the increase in wind storms in recent years and their projected recurrence as a consequence of global warming. To characterize anchorage mechanisms during tree uprooting, we developed a generic finite element model where real three-dimensional (3D) root system architectures were represented in a 3D soil. The model was used to simulate tree overturning during wind loading, and results compared with real data from two poplar species (Populus trichocarpa and P. deltoides). These trees were winched sideways until failure, and uprooting force and root architecture measured. The uprooting force was higher for P. deltoides than P. trichocarpa, probably due to its higher root volume and thicker lateral roots. Results from the model showed that soil type influences failure modes. In frictional soils, e.g., sandy soils, plastic failure of the soil occurred mainly on the windward side of the tree. In cohesive soils, e.g., clay soils, a more symmetrical slip surface was formed. Root systems were more resistant to uprooting in cohesive soil than in frictional soil. Applications of this generic model include virtual uprooting experiments, where each component of anchorage can be tested individually.     

黄土区4个树种水势特征的研究

采用压力室法对晋西北黄土区柠条(Caragana korshinskii)、河北杨(Populus hopeiensis)、北京杨(Populus beijingensis)和小叶杨(Populus simonii)4 个树种的小枝水势、叶含水率及其环境因子的日变化进行了定期测定。分析了4 个树种水势日变化与光照(L)、气温(T)、相对湿度(RH)日变化及叶含水率(LWC)日变化的关系以及其水势的季节变化与土壤水分季节变化的关系。主要结果如下:整个生长期所测4 个树种小枝水势的日变化为呈抛物线型。生长期小枝水势的平均值分别为柠条(-1.569 MPa)、河北杨(-1.030 MPa)、北京杨(-0.993 MPa)和小叶杨(-0.971MPa)。小枝水势与环境单因子的相关性大小依次为:光照、气温、相对湿度。水势与光温复合因子(L*T)、光湿复合因子(L/RH)的相关性大于它与单因子的相关性。小枝水势与叶含水率的相关性较差。生长期清晨水势(Wp)季变化与土壤水分(X)季节变化的最佳关系模型为Wp=Ae^-BX型。但生长期午间水势的季节变化与土壤水分季节变化的关系均不显著。土壤水分含量对水势有较大影响。     

有机物料对滨海盐渍土重金属根际效应的影响 Ⅰ.土壤内源Zn形态分布

研究了排水条件下施用腐熟有机物料、种稻改良滨海盐渍土内源Zn形态分布。结果表明,单淹水使土中各形态Zn一定程度上向生物有效性较低的Zn形态转化,有效态Zn降低。土壤盐分量不同,明显影响无定形氧化铁结合态、紧结有机态以及硅酸盐矿物态Zn变化。种稻不施有机物料,根际交换态和硅酸盐矿物态Zn亏缺;碳酸盐结合态、氧化锰结合态和无定形氧化铁结合态Zn富集。根际Zn形态转化强度大于非根际,其有效态Zn量接近临界值并高于非根际。有机物料利于根际内外土壤中硅酸盐矿物态Zn的转化,低盐土壤根际更强烈。随有机物料用量增加,促使根际硅酸盐矿物态、碳酸盐结合态及氧化锰结合态Zn向交换态、紧结有机态和无定形氧化铁结合态Zn转化,低盐土壤较明显。     

Non-significance of rhizosphere degradation during phytoremediation of MTBE

Methyl tertiary butyl ether (MTBE) is a gasoline additive associated with groundwater pollution at gas station sites. Previous research on poplar trees in hydroponic systems suggests that phytovolatilization is an effective mechanism for phytoremediation of MTBE (Rubin and Ramaswami, 2001), but the potential for microbial degradation of MTBE in the rhizosphere of trees had not been assessed. MTBE had largely been considered recalcitrant to microbial processes, but recent fieldwork suggests rapid biodegradation may occur in certain cases. This paper investigates the potential for rhizosphere degradation of MTBE at time frames relevant for phytoremediation. Three experiments were conducted at different levels of aggregation to examine possible degradation of MTBE by rhizosphere microorganisms that had been acclimated to low levels of MTBE for 6 weeks. MTBE soil die-away studies, conducted with both poplar trees and fescue grass, found no significant differences between MTBE concentration in vegetated and unvegetated soils over a two-week attenuation period. Closed chamber tests comparing hydroponic and rhizospheric poplar tree systems also showed essentially complete recovery of MTBE mass in both systems, suggesting an absence of degradation. Finally, rhizosphere microbes tested in aerated bioreactors were found to be thriving and metabolizing root materials, but did not show measurable degradation of MTBE. In all tests, the MTBE degradation product, Tert Butyl Alcohol (TBA), was not detected. The insignificance of MTBE degradation by rhizosphere microorganisms suggests that plant processes be the primary focus of further research on MTBE phytoremediation.     

Autumnal changes in total nitrogen, salt-extractable proteins and amino acids in leaves and adjacent bark of black alder, eastern cottonwood and white basswood

Autumnal changes in total nitrogen, salt-extractable protein and amino acid concentrations in leaves and adjacent bark of black alder [ Ainus glutinosa (L.) Gaertn.], eastern cottonwood ( Populus deltoides Bartr. ex Marsh.) and white basswood ( Tilia heterophylla Vent.) were determined for trees growing on minespoils and a prairiederived loamy soil in central Illinois. The composition of free amino acids in foliage was also determined at peak concentration for each tree species during late senescence. Total nitrogen concentration in the leaves decreased slowly throughout most of the fall for all species. In the final stages of senescence, total leaf nitrogen concentrations were about halved in eastern cottonwood and white basswood but continued to decrease slowly in black alder. The concentration of salt-extractable proteins in leaves of all species peaked early in the fall and then declined prior to leaf abscission. This decline coincided with an increase in the concentration of free amino acids in the leaves. The increase stabilized in both eastern poplar and white basswood but continued in black alder. Glutamine in black alder and eastern cottonwood, and asparagine in white basswood were the most abundant free amino acids at the time of peak concentration of total free amino acids in senescent leaves. Bark of trees of all species had higher nitrogen concentrations and higher proportions of salt-extractable proteins to estimated total proteins after leaf senescence than during the preceding summer. Results indicate that autumnal fluxes in leaf and bark nitrogen fractions of alder can differ substantially from fluxes in other broadleaved winter-deciduous trees in a way which suggests that alder does not effectively conserve leaf nitrogen through retranslocation to bark tissue.     

有机物料对滨海盐渍土重金属根际效应的影响Ⅰ.土壤内源Zn形态分布

研究了排水条件下施用腐熟有机物料、种稻改良滨海盐渍土内源Ｚｎ形态分布．结果表明,单淹水使土中各形态Ｚｎ一定程度上向生物有效性较低的Ｚｎ形态转化,有效态Ｚｎ降低．土壤盐分量不同,明显影响无定形氧化铁结合态、紧结有机态以及硅酸盐矿物态Ｚｎ变化．种稻不施有机物料,根际交换态和硅酸盐矿物态Ｚｎ亏缺;碳酸盐结合态、氧化锰结合态和无定形氧化铁结合态Ｚｎ富集．根际Ｚｎ形态转化强度大于非根际,其有效态Ｚｎ量接近临界值并高于非根际．有机物料利于根际内外土壤中硅酸盐矿物态Ｚｎ的转化,低盐土壤根际更强烈．随有机物料用量增加,促使根际硅酸盐矿物态、碳酸盐结合态及氧化锰结合态Ｚｎ向交换态、紧结有机态和无定形氧化铁结合态Ｚｎ转化,低盐土壤较明显．