SWAT模型在天山林区林冠截留过程中的改进应用

林冠截留是森林生态水文的重要环节,SWAT （Soil and Water Assessment Tool）模型对其模拟过程还较为粗糙,为了在流域水文模拟中更精细的刻画林冠截留过程从而得到更佳的模拟结果,以SWAT模型为基础,使用半理论林冠截留模型（Gash模型）与SWAT模型进行耦合,以天山林区为研究区对SWAT模型林冠截留模块进行优化改进。通过对改进前后的模拟结果进行对比分析,结果表明：1） SWAT模型和SWAT-Gash模型的R²分别为0.59-0.83和0.65-0.86,NSE值分别为0.58-0.82和0.63-0.85,两种模型PBIAS为7.2%-17.1%,证明SWAT-Gash模型具有更好的适用性;2）相较于出山口径流数据,SWAT模型和SWAT-Gash模型的RMSD值分别为3.49-7.80 m³/s和3.22-4.68 m³/s,SWAT-Gash模型在校准期和验证期的皮尔逊相关系数分别为0.93和0.81,高于SWAT模型的0.91和0.77;3）基于分位数回归（QR）的不确定性分析表明,SWAT模型和SWAT-Gash模型验证期的P因子分别为0.93和0.96,R因子为1.26和1.19,95%不确定性置信区间平均宽度分别为13.50 m³/s和12.86 m³/s;4） SWAT模型与SWAT-Gash模型在验证期的月平均地表径流量分别为6.55 m³/s和8.50 m³/s,表明在该流域内原始SWAT模型会高估林冠截留量。以天山北坡中段林区为例对云杉森林的林冠截留进行精细化模拟,虽然对模型输入数据要求提高,林冠截留数据的收集增加了模型模拟的不确定性,但对本研究区基于物理过程的水文模拟精度提升明显,改进后模型与出山口实测径流数据一致性更强,可以为天山林区小流域水资源管理提供更可靠的依据。     

川西云杉天然种群表型多样性

为了揭示川西云杉(Picea balfouriana)天然种群表型变异程度和变异规律, 以四川甘孜藏族自治州天然分布的川西云杉为研究对象, 调查了12个种群360个单株的种实和针叶表型性状, 采用变异系数、巢式方差分析、相关分析和聚类分析等方法, 分析了种群间和种群内表型多样性。结果表明: 川西云杉表型性状在种群间和种群内存在极其丰富的多样性, 种群间表型分化系数均值为36.53%, 小于种群内变异(63.47%); 球果、针叶、种鳞和种翅的表型分化系数均值分别为47.15%、31.93%、21.89%和45.14%, 球果、针叶、种鳞和种翅4类表型性状的变异系数分别为12.56%、22.16%、12.61%和16.53%, 种鳞的变异系数和表型分化系数最小, 表明其性状最为稳定; 12个表型性状间多数呈显著或极显著正相关, 球果长、球果径、针叶长和种鳞长为川西云杉重要的表型性状。川西云杉表型变异在空间分布上呈现以经度(球果和针叶)和纬度(种鳞和种翅)并存的单向变异模式; 利用种群间欧氏距离进行聚类分析, 可以把川西云杉12个种群划分为3类。     

温度对党参害虫烟草甲实验种群生长发育的影响

以中药材党参(Codonopsis pilosula)为寄主食料,在人工气候箱内,研究了温度对烟草甲(Lasioderma serricorne)卵、幼虫和蛹的生长和发育的影响;计算了烟草甲各虫态的发育起点温度和有效积温;通过Logistic模型及"王-兰-丁"模型对温度与烟草甲各虫态之间的关系进行拟合,优化拟合温度与烟草卵和幼虫发育关系的Logistic方程6个,温度与烟草甲幼虫发育关系的"王-兰-丁"方程5个。结果表明,烟草甲卵、幼虫、蛹及卵-蛹期的发育起点温度分别为16.51℃、11.07℃、11.78℃和12.20℃,其卵、幼虫、蛹及卵-蛹期的发育有效积温分别为89.59、669.53、137.12和912.72日度;温度的升高有利于烟草甲的各虫态的生长和发育;"王-兰-丁"模型拟合对研究较宽温度幅度的昆虫发育与温度之间的关系拟合效果优于Logistic模型。本研究结果可为危害储藏期中药材的烟草甲种群数量控制技术提供技术支撑。     

Ethylene effects on peroxidases and cell growth patterns in Picea abies hypocotyl cuttings

The effect of 2-chloroethylphosphonic acid (ethrel) on cell growth patterns and per-oxidase activity (EC 1.11.1.7) and location in young Norway spruce cuttings ( Picea abies [L.] Karst.) was investigated. The peroxidase activity in a fraction containing soluble and membrane bound enzymes show a diurnal variation, with decreased activity during the light period and a corresponding increase during the following dark period. The decrease during the day could to some extent be counteracted by treatment with ethrel. It appears that ethrel affects only peroxidases in the isolated membrane fraction, since peroxidases bound to the cell wall were not affected by ethrel. In vitro experiments indicated that the hydrophobicity of soluble peroxidases was increased by treatment with ethylene. Cytochemical localization of peroxidase activity in differentiating tracheids revealed a clear ethrel-induced increase in the tonoplast. It appears that ethylene affects soluble peroxidases in vivo in such a way that they are directed to a more hydrophobic environment, like the tonoplast. Treatment with ethrel also changed the appearance of the rough endoplasmic reticulum (ER) and Golgi apparatus. Dilated ER cisternae were observed on electron micrographs, as a result of treatment with ethrel. The number of vesicles produced by the Golgi apparatus and also the amount of vesicles fusing with the plasma membrane in secondary-wall-forming tracheids increased considerably. The results clearly indicate that the stimulatory effect of ethylene in spruce seedlings on lignification and cell wall formation, is due to a general stimulation on both synthesis, transport and secretion of cell wall material and not on a stimulation of peroxidase activity as reported for other species.     

Growth and shoot: root ratio of seedlings in relation to nutrient availability

The influence of mineral nutrient availability, light intensity and CO₂ on growth and shoot:root ratio in young plants is reviewed. Special emphasis in this evaluation is given to data from laboratory experiments with small Betula pendula plants, in which the concept of steady-state nutrition has been applied.Three distinctly different dry matter allocation patterns were observed when growth was limited by the availability of mineral nutrients: 1, Root growth was favoured when N, P or S were the major growth constraints. 2, The opposite pattern obtained when K, Mg and Mn restricted growth. 3, Shortage of Ca, Fe and Zn had almost no effect on the shoot:root ratio. The light regime had no effect on dry matter allocation except at very low photon flux densities (< 6.5 mol m^-2 day^-1), in which a small decrease in the root fraction was observed. Shortage of CO₂, on the other hand, strongly decreased root development, while an increase of the atmospheric CO₂ concentration had no influence on dry matter partitioning. An increased allocation of dry matter to below-ground parts was associated with an increased amount of starch in the tissues. Depletion of the carbohydrate stores occurred under all conditions in which root development was inhibited. It is concluded that the internal balance between labile nitrogen and carbon in the root and the shoot system determines how dry matter is being partitioned in the plant. The consistency of this statement with literature data and existing models for shoot:root regulation is examined.     

Effects of Mg(OH)2-fertilization on nutrient cycling in a heavily damaged Norway spruce ecosystem (NE Bavaria/FRG)

Main objective of this study was to test the effects of Mg(OH)₂-fertilization in a Norway spruce ecosystem showing severe symptoms of Mg-deficiency.The site is characterized by high atmospheric inputs with deposition rates of 1.25 kg H, 42 kg S, and 32 kg N per ha and year. The typic Dystrochrept derived from granite is acidified down to greater depths. The pH-values in soil solution of the organic surface layer and the upper mineral soil are around 3.5. Concentrations of Al, SO₄ ^2-, and especially NO₃ ^- and DOC are very high. The element balance indicates a significant influence of N-inputs and processes of N-turnover on the chemical status of the soil and probably on tree nutrition. Nitrification in the upper mineral soil leads to a transformation of a major part of NH₄ ⁺ into NO₃ ^-, which is quantitatively leached, resulting in an ecosystem-internal H⁺-production of 1.8 keq ha^-1yr^-1. NO₃ ^- and SO₄ ^2- govern the seepage output from the ecosystem.Mg(OH)₂ fertilization resulted in manifold increased Mg²⁺ concentrations in soil solution down to 70 cm soil depth and to a significant increase of pH down to 25 cm mineral soil depth. Nitrate concentrations were elevated after fertilization, but decreased within 15 months below the level of the control plot. As a mean over the whole experimental period, N-output was not increased by fertilization. Despite an elevated internal proton production due to nitrification, acid buffering in the soil was clearly increased, but enhanced Al-mobilization was not observed. Mg/Al- and Ca/H-ratios in soil solution indicate much more favourable conditions for fine root growth. Fertilization also increased the amount of exchangeable Mg down to 40cm mineral soil depth. Mg contents in current-year needles increased after three vegetation periods. Thirty months after application, only 10% and 4% of the fertilized Mg had left the organic surface layer and the mineral soil with seepage water output, respectively.     

Dependence of the Q10 values on the depth of the soil temperature measuring point

The parameter Q₁₀ is commonly used to express the relationship between soil CO₂ efflux and soil temperature. One advantage of this parameter is its application in a model expression of respiration losses of different ecosystems. Correct specification of Q₁₀ in these models is indispensable. Soil surface CO₂ efflux and soil temperature at different depths were measured in a 21-year-old Norway spruce stand and a mountain grassland site located at the Experimental Ecological Study Site Bily Kriz, Beskydy Mts. (NE Czech Republic), using automated gasometric systems. A time-delay and goodness-of-fit between soil CO₂ efflux and soil temperature at different measuring depths were determined. Wide ranges of values for the time-delay of CO₂ efflux in response to temperature, Q₁₀ and the determination coefficient (R²) between CO₂ efflux and temperature were obtained at the both sites. The values of Q₁₀ and the CO₂ time-delay increased with depth, while the R² of the CO₂-temperature relationship significantly decreased. Soil temperature records obtained close to the soil surface showed the highest values of R² and the lowest value of the time-delay at both sites. Measurement of soil temperature at very shallow soil layer, preferably at the soil surface, is highly recommended to determine useable values of Q₁₀. We present a new procedure to normalize Q₁₀ values for soil temperatures measured at different depths that would facilitate comparison of different sites.     

Natural revegetation on forest topsoil and subsoil along roadsides in boreal forest

Questions: Does natural revegetation from indigenous soil improve the restoration success of roadside areas? What are the effects of topsoil, subsoil and fertilization on natural revegetation? Location: Akershus county, SE Norway (10°25′ E, 59° 44′ N). Methods: We used a recently constructed road through a boreal coniferous forest for a three year (2000–2002), fully replicated revegetation experiment (six replications). Treatments were soil type (two levels; one topsoil and one subsoil type) and fertilization (two levels; NPK and unfertilized control). Ordination methods, constrained ordination methods as well as univariate statistical methods, such as Wilcoxon's signed‐rank test and correlation analysis, were used to assess the relative importance and significance of treatments on the plant species composition. Results: There was no fertilization effect on species composition. The species composition on both soil types was stabilised by the second year. The species dominating the topsoil were more in accordance with the indigenous vegetation than was the case on the subsoil. The significant difference in species composition among blocks, persisting for the entire study period, indicated that local factors are important determinants of the outcome of revegetation. Conclusions: Unfertilized topsoil provides a revegetation result in better accordance with the indigenous vegetation than does subsoil.     

Occurrence of leeches (Hirudinea, Piscicolidae) on some marine fishes in Norway

Marine fish from several locations along the west coast of Norway were examined for leeches. Seven leech species were detected, Calliobdella nodulifera (Malm, 1863) from codfish, flatfish and a ray, Calliobdella lophii van Beneden & Hesse, 1863 from Lophius piscatorius L., Platybdella anarrhichae (Diesing, 1859) on Anarhichas lupus L., Platybdella quadrioculata Malm, 1863 on Symphodus melops (L.), Oceanobdella sp. on Zeugopterus punctatus (Bloch), Malmiana brunnea (Johansson, 1896) on Myoxocephalus scorpius (L.) and Malmiana bubali Srivastava, 1966 on Taurulus bubalis (Euphrasen). Calliobdella nodulifera infected unrelated hosts (euryxenic); the others appeared to be host specialists (oio- or stenoxenic). Details on the occurrence of Calliobdella nodulifera on Enchelyopus cimbrius (L.) during 1 year are given, which together with other observations suggest that its life cycle exceeds a year. A brief account on the morphology of “Platybdella” quadrioculata is provided, justifying its transfer to the genus Oceanobdella Caballero, 1956 as O. quadrioculata comb. nov. With the new additions, the Norwegian marine piscicolid fauna contain 12 species. At least ten additional species, known from adjoining areas, also probably occur along the Norwegian coast.