西双版纳热带雨林土壤与叶片生态化学计量特征的干湿度效应

基于地理格局对西双版纳热带雨林的干湿度梯度效应和生态化学计量学的研究思路,结合野外试验监测和室内分析,对西双版纳热带雨林土壤-植物系统元素化学计量特征对海拔和干湿度效应响应进行了研究探讨,结果发现:西双版纳热带雨林土壤和叶片碳氮磷化学计量特征均不同程度的受到海拔和干湿季影响。季雨林与山地雨林的水热梯度受海拔梯度重要影响,随海拔梯度升高,土壤含水率变化显著,且含水率在干湿季均对土壤有机碳(SOC)存在显著影响(P0.01),雨季其对土壤全氮(STN)和土壤全磷(STP)的影响要显著于干季;叶片全磷(TP)随含水率的增大而升高,而叶片全氮(TN)在干季会随含水率的升高而增大,雨季含水率升高到一定程度时会抑制TN含量的增加并出现单峰现象;而土壤C/P与海拔和干季土壤含水率的极显著相关性(P0.01)及干季叶片C/N与叶片含水率的显著相关关系(P0.05)说明,干季水分匮乏条件下,土壤含水率影响土壤P的矿化度和植物对P的吸收利用水平,而且叶片C/N对反馈植物水分含量具有明显指示作用。因此,水热梯度是土壤-叶片系统碳氮磷生态化学计量特征变化的重要驱动因素。此外,全球变化区域响应方面,多雨高温可能会削弱季雨林叶片C的同化能力,且叶N含量降低,但受氮沉降的影响,对C/N的影响尚无法确定;由于P循环对其他元素的耦合作用,雨林土壤-叶片系统的元素循环周期将会被缩短,但干季山地雨林植物生态系统P的限制作用有可能会减弱。     

西双版纳望天树林土壤养分含量及其季节变化

 对西双版纳望天树(Shorea chinensis)林地0～10 cm和10～25㎝土层的有机质,全氮、磷、钾,速效氮、磷、钾等几种营养元素的含量状态及雨季前后的变化进行了研究。结果表明：土壤的养分含量变化为旱季结束＞雨季结束,沟谷地带雨林＞低山地带雨林,并且差异显著;表土0～10 cm是养分富集区,10 cm以下土层的养分含量锐减,两层养分含量对比,除钾元素以外均差异显著,表明望天树热带雨林生存的环境与植被的生活习性,对土壤养分的含量都有一定的影响。雨季对林地土壤的全钾和速效磷含量影响很大,对有机质、全磷和速效钾的含量影响较小,对氮素的影响是低山雨林＞沟谷雨林。雨季期间土壤中的磷素消耗到严重缺乏的水平。     

丛林式橡胶林内植物水分利用效率与叶片养分含量

选取西双版纳地区丛林式橡胶林为研究对象,以纯橡胶林为对照,分别在2016年干季(3月)和雨季(5、6、7月)进行取样,测定两个样地内植物叶片δ13C值,比较植物水分利用效率,测定叶片C、N、P含量,计算叶片N/P值,分析植物对养分的利用与竞争关系,并综合分析植物水分利用效率与养分之间的相关性。结果表明,干季橡胶树受到干旱胁迫,其水分利用效率显著高于雨季,此时叶片N、P含量也显著高于雨季;丛林式橡胶林内橡胶树水分利用效率低于纯橡胶林内橡胶树,叶片N、P含量和N/P值均高于纯橡胶林中橡胶树;两个样地内不同植物与不同时间的水分利用效率,叶片C、N、P含量和N/P值均存在显著差异;相关性分析表明,水分利用效率与叶片N、P含量呈正相关,与叶片C含量、N/P值呈负相关。因此,丛林式橡胶林内橡胶树能更好地应对干旱,具有较强的养分获取能力。该研究揭示了丛林式橡胶林内植物水分利用效率以及养分利用特征,表明丛林式橡胶林是一种值得推广的农林复合生态系统。     

典型岩溶洼地土壤水分的空间分布及影响因素

在桂西北典型岩溶洼地的旱季和雨季,用地统计学结合GIS方法研究了洼地表层(0—16cm)土壤水分的空间分布特征及其影响因素。结果表明:土壤含水量受前期降雨量的影响,且旱季土壤水分对降雨量的反应较雨季敏感。土壤水分均呈中等变异且变异系数随着平均含水量的增加而减少。土壤水分的半方差参数显示土壤水分空间变异及其主导因素随旱、雨季而不同。此外,不同取样区域及取样时段内土壤含水量高低差别明显,分布格局及空间变异程度各异,这主要与当地环境和人为因素的综合影响有关。旱、雨季土壤水分均与前期降雨导致的土壤平均含水量变化呈相反趋势,且不同土地利用方式下的土壤含水量不同。土壤含水量还与土壤有机碳含量呈显著正相关,此外,地势及裸岩率也是造成洼地土壤水分变异及其分布差异的重要因素。下一步应根据旱季和雨季土壤水分分布及影响因素的差异,在岩溶洼地采取有针对性地土壤水资源利用及其水分管理策略。     

The effects of varying culture nitrogen and phosphorus levels on nutrient uptake and storage by the waterhyacinth Eichhornia crassipes (Mart) Solms

The uptake of nitrogen (N) by waterhyacinth (Eichhornia crassipes) was maximal when the culture solution contained a combination of 36 ppm N and 6,53 ppm phosphorus (P). N uptake was inhibited by increasing P or decreasing N in the culture medium. Uptake of P was stimulated by the elevation of either N or P or both. An increase of P above O ppm inhibited the accumulation of N. Similarly, the accumulation of P was enhanced by increasing levels of P but was reduced with increasing levels of N. Both N and P levels were always greatest in leaves; next highest in floats and lowest in roots. High tissue levels of these two nutrients and the capacity for nutrient removal from water by waterhyacinth indicates a possible role for this plant in the reduction of eutrophication in nutrient polluted waters as well as the use of harvested, dried tissue for fertilizer.     

滇南喀斯特地区不同季节土壤和灌木叶片化学计量特征及对水分添加的响应

干旱是影响南方喀斯特地区植物生长的重要限制因子, 气候变化会影响该地区的降水量和分布格局。研究该地区土壤和植物化学计量特征及其水分响应格局, 具有重要意义。自2017年4月开始, 在云南建水喀斯特植物群落进行加水试验, 2018年4月(旱季)和8月(雨季)分别采集土壤和优势灌木鞍叶羊蹄甲(Bauhinia brachycarpa)和假虎刺(Carissa spinarum)叶片样品, 测定碳、氢、氮、磷、硫、钾、钙、镁、铝、钠、铁、锰、锌、铜14种元素含量。结果表明, 水分添加影响了表层土壤中碳、氮、钠的含量, 相比于旱季, 雨季土壤中钠和硫含量明显减少, 其余土壤元素在水分添加和季节变化下并未表现出明显差异。土壤水分含量的增加使得鞍叶羊蹄甲和假虎刺叶片中钾含量下降, 钙含量上升。在水分条件变化下, 两种植物叶元素含量的稳定性与植物中元素的含量有关, 含量越接近极大值(基本元素碳、氢、氮等)或极小值(微量元素铜、锌等)的元素其变异系数越小(越稳定), 两种植物中含量接近于1 mg·g^-1的元素磷、硫、镁的变异系数最高。在土壤水分条件变化下, 假虎刺中碳、氮、磷等大量元素含量的稳定性显著高于鞍叶羊蹄甲。降水变化和水分添加导致的土壤水分变化, 对滇南喀斯特地区土壤和植物中不同元素含量的影响不同, 这些结果将为该地区的土壤、植被修复和管理提供科学参考。     

云南南涧干热退化山地人工植被恢复初期生物量及土壤环境动态

 研究了云南南涧干热河谷退化山地人工恢复植被初期阶段(3～5年)主要植物群落的地上生物量和恢复植被后土壤水分及养分的相关动态。结果表明,几种外来植物的适应性强,早期生长迅速并能很快郁闭。人工群落生物量都高于当地次生的坡柳灌草丛。引进种的地上生物量和总平均生长量分别是坡柳的3～16倍和5～20倍,其生长速度也高于乡土树种云南松。雨季人工植被下土壤含水量比光坡地增加约100％,表土层则增加2倍以上。但在旱季,林地土壤含水量与光坡地相近甚至低于光坡地。植被的恢复使土壤养分朝着良性循环转变。土壤有机质、速效钾含量提高,全氮含量稍有降低但不明显,速效磷含量降低,pH值有所下降。这些变化主要发生在土壤表层,人工植被及其土壤生态系统的恢复仍处于不稳定状态。     

三峡库区消落带立柳(Salix matsudana)生长及营养元素分配特征

立柳因良好的耐淹性常被用于三峡库区消落带的植被重建。为探讨立柳如何通过营养元素的积累和分配来适应库区消落带冬季水淹,于2015年5月对三峡库区消落带植被修复示范基地内3个采样带(175 m,170 m和165 m)中立柳的生长状况以及叶、枝条和根的营养元素含量特征进行分析。结果表明:(1)经过3个水淹周期后,随着水淹强度的增加,立柳的株高、基径和冠幅均受到一定的抑制;但与种植初期相比,3个采样带中立柳的株高、基径和冠幅均显著增加,且生长状态良好。(2)立柳各器官中营养元素含量均处于正常水平,但水淹抑制了根中N、P的积累,促进了Fe和Mn的积累;水淹显著降低了海拔165 m处立柳叶和枝条中Ca含量、枝条和根中Cu和Zn的含量。(3)水淹胁迫导致N、P、K、Mg元素更多地在叶中积累,而Cu和Zn在枝条中大量积累,这有利于退水后植株的光合合成以及恢复生长;Fe、Mn元素在根中大量积累,其对根系正常生理可能造成的干扰值得进一步关注。研究表明,在不同的水淹胁迫梯度下,立柳可针对性地调整其营养元素积累和分配方式,保持植株正常的生长状态,对维护三峡库区消落带生态系统的正常结构和功能具有重要作用。但在库区消落带植被恢复和重建工作中,需加强170 m以下海拔区域立柳生长的监测和研究。     

Effect of different constant soil moisture levels on net assimilation rate,relative transpiration,osmotic pressure of cell sap and water saturation deficit of the leaves

A study was made of the effect of different constant soil moisture (90, 60 and 30 or 40% maximum capillary capacity) on the net assimilation rate (N.A.R.) in maize in relation to changes in relative transpiration (R.T.), water saturation deficit of the leaves (W.S.D.) and osmotic pressure of the cell sap (O.P.). The soil moisture was maintained constant either from the planting of the germinating grain, or from the phase of 4–6 leaves. An attempt was made to interpret the mechanism of action of water deficit on photosynthesis and at a rough differentiation between the indirect effect through changes in internal diffusive resistance to carbon dioxide and the direct effect on the hydration of the photosynthetizing tissue. In plants exposed to different constant soil moisture levels from the phase of 4–6 leaves, the initial difference in N.A.R. corresponding to the degree of lowering of soil moisture gradually evened out during the vegetation season. On applying different constant soil moisture levels from the time of planting no marked differences in N.A.R. were found between plants cultivated at high values of soil moisture (60% and 90%). In plants cultivated from planting at 40% soil moisture, the course of changes in N.A.R. was qualitatively different from that of the above two variants and corresponded more or less to changes characteristic for the process of adaptation to unfavourable conditions. From the analogous course of N.A.R. and R.T. it can be assumed that in all cases the intensity of photosynthesis was very markedly influenced by changes in diffusive resistance to carbon dioxide. On the basis of an analysis of changes in O.P. of the cell sap and W.S.D. of the leaf tissue, the assumption was made that in plants cultivated from planting at 40% and to some extent at 60% soil moisture, irreversible adaptation changes occurred in the structural conditions of photosynthesis as a result of continuous dehydration. In plants cultivated at similar soil moisture levels from the phase of 4–6 leaves, the changes in the intensity of photosynthesis were more likely caused by actual dehydration of the photosynthetizing tissue.     

Sclerophylly in Qualea Parviflora (Vochysiaceae): Influence of Herbivory, Mineral Nutrients, and Water Status

Qualea parviflora Mart. (Vochysiaceae) is a deciduous tree, commonly observed in campo sujo, cerrado sensu stricto and cerradão vegetation types in Brazilian cerrado (savannas). In this study we investigated herbivory, nutritional, and water status effects on leaf sclerophylly of Q. parviflora. Twenty fully expanded leaves were taken from 10 plants in each vegetation type four times a year. Mean leaf concentration of N, P, K, Ca, C, Al, Si, and percentage of total phenols, herbivory and tannins were measured on a plant basis. Leaf specific mass (LSM) (g m^?2), a sclerophylly index, and pre-dawn leaf water potential (MPa) were also recorded. Soil samples below each tree were collected to quantify N–NO₃, N–NH₄, P, K, Mn, soil moisture, organic matter, Si, and Al. Qualea parviflora showed a LSM from 69 to 202 g m^?2 and leaves were younger and less sclerophyllous in November (beginning of rainy season). Q. parviflora inhabiting the cerradão had leaves with higher concentration of nutrients and lower sclerophylly while trees in campo sujo and cerrado sensu stricto did not show significant differences in leaf sclerophylly. The concentrations of N, P, K and tannins had an inverse relationship with leaf age. Concentration of phenols, Al, C, Ca, Si, C/N and Ca/K increased with leaf age. The concentrations of P and Ca/K ratio in leaves explained 60% of variation observed in leaf sclerophylly. We did not find any significant relationship between the level of sclerophylly and water potential or herbivory. Our results corroborate the hypothesis that predicts lower concentrations of essential macronutrients would be the main factors influencing higher sclerophylly in leaves of Q. parviflora plants in Cerrado.     

Drought and warming induced changes in P and K concentration and accumulation in plant biomass and soil in a Mediterranean shrubland

A field experiment involving drought and warming manipulation was conducted over a 6-year period in a Mediterranean shrubland to simulate the climate conditions projected by IPCC models for the coming decades (20% decreased soil moisture and 1°C warming). We investigated P and K concentration and accumulation in the leaves and stems of the dominant species, and in soil. Drought decreased P concentration in Globularia alypum leaves (21%) and in Erica multiflora stems (30%) and decreased K concentration in the leaves of both species (20% and 29%, respectively). The general decrease of P and K concentration in drought plots was due to the reduction of soil water content, soil and root phosphatase activity and photosynthetic capacity that decreased plant uptake capacity. Warming increased P concentration in Erica multiflora leaves (42%), but decreased it in the stems and leaf litter of Erica multiflora and the leaf litter (33%) of Globularia alypum, thereby demonstrating that warming improved the P retranslocation and allocation from stem to leaves. These results correlate with the increase in photosynthetic capacity and growth of these two dominant shrub species in warming plots. Drought and warming had no significant effects on biomass P accumulation in the period 1999–2005, but drought increased K accumulation in aboveground biomass (10 kg ha⁻¹) in Globularia alypum due to the increase in K concentration in stems. The stoichiometric changes produced by the different responses of the nutrients led to changes in the P/K concentration ratio in Erica multiflora leaves, stems and litter, and in Globularia alypum stems and litter. This may have implications for the nutritional value of these plant species and plant–herbivore relationships. The effects of climate change on P and K concentrations and contents in Mediterranean ecosystems will differ depending on whether the main component of change is drought or warming.     

Experimental manipulation of water levels in two French riverine grassland soils

In this experimental study, we simulated the effects of different river flooding regimes on soil nutrient availability, decomposition and plant production in floodplain grasslands. This was done to investigate the influences of soil water contents on nutrient cycling. Water levels were manipulated in mesocosms with intact soil turfs from two French floodplain grasslands. Three water levels were established: a `wet' (water level at the soil surface), an `intermediate' (water level at –20 cm) and a `dry' treatment (water level at –120 cm). With increasing soil moisture, soil pH became more neutral, while redox-potential and oxygen concentration decreased. The `dry' treatment showed much lower values for process rates in soil and vegetation than the `intermediate' and `wet' treatments. Regressions showed that soil C-evolution and N-mineralization were positively related to soil moisture content. Not all mineralized N was available for plant uptake in the wet treatment, as a considerable part was denitrified here. Denitrification was especially high as soil water contents increased to levels above field capacity, where redox-potentials sharply dropped. Further, soil P availability was higher under wet conditions. In the `dry' treatment, soil water content was close to the wilting point and plant production was low. In the `intermediate' treatment, plant production was most likely limited by nitrogen. The `wet' treatment did not result in a further increase in plant production. Dam construction and river bed degradation can result in lower river levels and summer drought on floodplains. This experimental study suggests that summer drought on floodplain soils reduces decomposition of soil organic matter, nutrient availability, denitrification, plant production and nutrient uptake. This can affect the capacity of floodplains to remove or retain nutrients from river water in a negative way.     

Influence of gap size and soil properties on microbial biomass in a subtropical humid forest of north-east India

We examined the effects of treefall gap size and soil properties on microbial biomass dynamics in an undisturbed mature-phase humid subtropical broadleaved forest in north-east India. Canopy gaps had low soil moisture and low microbial biomass suggesting that belowground dynamics accompanied changes in light resources after canopy opening. High rainfall in the region causes excessive erosion/leaching of top soil and eventually soil fertility declines in treefall gaps compared to understorey. Soil microbial population was less during periods when temperature and moisture conditions are low, while it peaked during rainy season when the litter decomposition rate is at its peak on the forest floor. Greater demand for nutrients by plants during rainy season (the peak vegetative growth period) limited the availability of nutrients to soil microbes and, therefore, low microbial C, N and P. Weak correlations were also obtained for the relationships between microbial C, N and P and soil physico–chemical properties. Gap size did influence the microbial nutrients and their contribution to soil organic carbon, total Kjeldhal nitrogen and available-P. Contribution of microbial C to soil organic carbon, microbial N to total nitrogen were similar in both treefall gaps and understorey plots, while the contribution of microbial P to soil available-P was lower in gap compared to the understorey. These results indicate that any fluctuation in microbial biomass related nutrient cycling processes in conjunction with the associated microclimate variation may affect the pattern of regeneration of tree seedlings in the gaps and hence be related with their size. This revised version was published online in June 2006 with corrections to the Cover Date.     

水分对敦煌阳关湿地芦苇叶片与土壤C、N、P生态化学计量特征的影响

土壤水分是影响干旱区植物养分吸收和利用策略的关键因子之一。研究不同水分梯度叶片与土壤生态化学计量特征,有助于揭示植物对环境变化的响应特征及生态适应性。通过野外调查与实验分析,对敦煌阳关不同水分梯度芦苇叶片与土壤碳(C)、氮(N)、磷(P)生态化学计量特征及其关系进行了研究。结果表明:(1)随土壤含水率升高,叶片C、N、P含量降低,叶片C/N、C/P、N/P升高。(2)随土壤含水率升高,土壤有机碳(OC)、总氮(TN)、总磷(TP)含量及土壤N/P升高,土壤C/N降低,土壤C/P先升后降。(3)低水分梯度叶片N、C/N与土壤N、C/N显著负相关(P0.05),叶片C、P、C/P、N/P与土壤C、P、C/P、N/P无显著相关性(P0.05);高、中水分梯度叶片C、N、P与土壤C、N、P化学计量特征相关性均不显著(P0.05)。低水分梯度叶片受干旱胁迫和土壤养分制约,且能够保持较高的叶养分含量,体现了干旱区湿地植物异质生境下独特的养分调节机制。     

Soil nutrient dynamics in response to irrigation of a Panamanian tropical moist forest

We measured concentrations of soil nutrients (0–15 and 30–35 cm depths) before and after the dry season in control and dry-season irrigated plots of mature tropical moist forest on Barro Colorado Island (BCI) in central Panama to determine how soil moisture affects availability of plant nutrients. Dry-season irrigation (January through April in 1986, 1987, and 1988) enhanced gravimetric soil water contents to wet-season levels (ca. 400 g kg^–1 but did not cause leaching beyond 0.8 m depth in the soil. Irrigation increased concentrations of exchangeable base cations (Ca²⁺, Mg²⁺, K⁺, Na⁺), but it had little effect on concentrations of inorganic N (NH₄ ^+C, NO₃ ^– and S (SO₄ ^2–). These BCI soils had particularly low concentrations of extractable P especially at the end of the dry season in April, and concentrations increased in response to irrigation and the onset of the rainy season. We also measured the response of soil processes (nitrification and S mineralization) to irrigation and found that they responded positively to increased soil moisture in laboratory incubations, but irrigation had little effect on rates in the field. Other processes (plant uptake, soil organic matter dynamics) must compensate in the field and keep soil nutrient concentrations at relatively low levels.     

控制性分根交替灌溉下氮形态对番茄生长、果实产量及品质的影响

以高产大果型西红柿品种中研988为材料,采用分根培养的方法,研究了控制性分根交替灌溉(APRI)条件下,不同氮素形态(硝态氮、铵态氮)对番茄生长、产量及果实品质的影响.结果表明: 同一灌溉方式或下限处理下,铵态氮对番茄植株前期生长有利,而硝态氮促进番茄植株后期生长,并促进果实产量增加.在APRI同一灌水下限下,硝态氮处理可提高果实维生素C含量及糖酸比,提高营养品质.同一氮素形态供应下,APRI番茄的株高和叶面积均小于正常灌溉(CK),但灌水下限为60%田间持水量(θ_f)的APRI处理番茄茎粗在生长后期有所增加.在同一氮素形态下,与CK相比,APRI各处理的产量均下降,其中灌水下限在40%θ_f的APRI处理产量下降了22.4%～26.3%;而灌水下限在60% θ_f的APRI处理仅下降了5.3%～5.4%,下降幅度相对较小,而品质显著提高,并具有明显的节水效果.因此,控制灌水下限在60%θ_f、供应硝态氮的APRI处理为番茄高产、优质、节水的最佳处理.
     

Foliar demand and resource economy of nutrients in dry tropical forest species

Important phenological activities in seasonally dry tropical forest species occur within the hot‐dry period when soil water is limiting, while the subsequent wet period is utilized for carbon accumulation. Leaf emergence and leaf area expansion in most of these tree species precedes the rainy season when the weather is very dry and hot and the soil cannot support nutrient uptake by the plants. The nutrient requirement for leaf expansion during the dry summer period, however, is substantial in these species. We tested the hypothesis that the nutrients withdrawn from the senescing leaves support the emergence and expansion of leaves in dry tropical woody species to a significant extent. We examined the leaf traits (with parameters such as leaf life span, leaf nutrient content and retranslocation of nutrients during senescence) in eight selected tree species in northern India. The concentrations of N, P and K declined in the senescing foliage while those of Na and Ca increased. Time series observations on foliar nutrients indicated a substantial amount of nutrient resorption before senescence and a ‘tight nutrient budgeting’. The resorbed N‐mass could potentially support 50 to 100% and 46 to 80% of the leaf growth in terms of area and weight, respectively, across the eight species studied. Corresponding values for P were 29 to 100% and 20 to 91%, for K 29 to 100% and 20 to 57%, for Na 3 to 100% and 1 to 54%, and for Ca 0 to 32% and 0 to 30%. The species differed significantly with respect to their efficiency in nutrient resorption. Such interspecific differences in leaf nutrient economy enhance the conservative utilization of soil nutrients by the dry forest community. This reflects an adaptational strategy of the species growing on seasonally dry, nutrient‐poor soils as they tend to depend more or less on efficient internal cycling and, thus, utilize the retranslocated nutrients for the production of new foliage biomass in summer when the availability of soil moisture and nutrients is severely limited.     

持续淹水对河竹器官养分元素分配格局的影响

为探明持续淹水对河竹器官养分元素分布格局的影响,揭示竹子耐受水淹胁迫的养分适应机制,以2年生河竹(Phylllostachys rivalis)盆栽苗为试材,设置不同深度的淹水处理(水位高出栽培基质5 cm(Ⅰ)、10 cm(Ⅱ)和正常供水(CK)),测定了持续淹水90、180 d和360 d河竹叶、枝、秆、鞭和根中养分元素C、N、P、K、Ca、Fe和Mg的含量,分析了淹水条件下河竹器官营养元素分布格局的变化。结果表明:1)淹水深度和时间显著影响河竹器官C含量,与对照比较,淹水90 d时,叶、枝和根C均显著增加(P0.05),随着淹水时间的延长(180 d),C含量维持稳定状态,至淹水360 d,植株C含量降低,尤其淹水Ⅱ显著降低。2)淹水显著影响河竹器官的N、P、K、Ca、Fe和Mg含量(P0.05),且处理时间、处理水平和器官间存在显著交互作用(P0.001),处理90 d时,河竹叶片N、P、Ca、Fe和Mg含量均显著升高,而根的N、P含量则显著降低,淹水180 d和360 d时,除根部的K、Fe和Mg含量升高外,其它器官中各元素均显著降低。3)水位深度对元素之间的关系产生明显影响,在淹水Ⅰ叶片的CK、N-K、P-K、Fe-Ca和Fe-Mg的相关系数升高,元素间协同性增强,而在淹水Ⅱ中这些相关系数则降低,说明元素间的协同性减弱。4)淹水Ⅱ河竹叶片C/N、C/P较对照显著增加(P0.05),而N/P变化不显著(P0.05),说明河竹在淹水条件下具有较高内稳定性。综上,淹水影响河竹根系矿质元素吸收能力,促进其向顶运输,以维持碳同化能力和元素内稳性,这可能是河竹适应持续水淹胁迫的重要机制。     

Ecology of deepwater rice-fields in Bangladesh 5. Mineral composition of the rice plant and other aquatic macrophytes

The mineral composition of deepwater rice (cultivar Kartik Sail) was studied during 1986 in a field near Sonargaon, Bangladesh, which is flooded by water from R. Meghna. Samples were taken four times, once prior to flooding and three times during the flood season. On two of the latter days (10 August = end of first flood peak, 23 September = second flood peak) the study was extended to other components of the ecosystem (sediments + soil, water, other aquatic macrophytes). On 23 September, 32% of the mass of the plant was out of water, 65% in water and 3% in sediment/soil. There were marked differences between elements in their pattern of accumulation by deepwater rice through the season. In comparison with the final totals for each element, about 48% of N, but only 11% of P and 10% of Na had been accumulated by the time the floodwater had arrived. The aquatic roots doubled in mass between the times of the two flood peaks and it is suggested that much of the P taken up by the plant may reach the plant via its aquatic roots after having becoming mobilized and released to the water when sediments become anaerobic. In comparison with other parts of the plant, Na was always much higher in the stem and Zn in the basal roots.Other aquatic macrophytes (weeds) increased from 0.40% of the mass (dry weight) of deepwater rice on 10 August to 4.0% on 23 September. However their content of each element (% dry weight) was considerably higher than that in deepwater rice, so they may at times compete effectively with the rice for nutrients. During the flood period (to 23 September) weeds accumulated 16% of the N accumulated by rice during the same period.     

供磷水平对米老排苗木生长及养分状况的影响

为探讨供磷(P)对米老排(Mytilaria laosensis)生长和养分状况的影响,采用土培的方法,研究了不同供磷水平下米老排苗木的生长、养分含量、养分累积量和P吸收效率。结果表明,随着供P水平的提高,米老排苗木的苗高、生物量和养分累积量均呈先上升后下降的趋势;地径呈先增加后稳定的趋势;叶片和全株中的养分含量变化一致,氮(N)含量变化不明显,钾(K)含量呈先降低后升高的趋势,而P含量明显提高;P吸收效率呈现降低-升高-降低的趋势。在单株供P为30 mg时,米老排苗木的叶生物量、根生物量、叶片中N累积量及P吸收效率最大。当供P水平达到45 mg时,米老排苗木的苗高、茎生物量、总生物量、叶片中的P、K累积量和全株中的N、P、K累积量均达到最大值。而供P水平达60 mg时,米老排苗木苗高、生物量、养分累积量和P吸收效率均明显下降。这说明适合米老排苗木生长的供P水平为每株30~45 mg。