Role of canopy interception on water and nutrient cycling in Chinese fir plantation ecosystem

The role of canopy interception on nutrient cycling in Chinese fir plantation ecosystem was studied on the basis of the position data during four years. Results indicate that the average canopy interception amount was 267.0 mm/year. Canopy interception play a significant role in water cycle and nutrient cycle processes in ecosystem, and was an important part of evaporation from the Chinese fir plantation ecosystem, being up to 27.2%. The evaporation from the canopy interception was an important way of water output from ecosystem, up to 19.9%. The flush-eluviation of branches and leaves caused by canopy interception brought nutrient input of 143.629 kg/(hm² · year), which was 117.2% of the input 63.924 kg/(hm² · year) from the atmospheric precipitation. The decreased amount of 80.1 mm precipitation input caused by canopy interception reduced the amount of rainfall into the stand surface and infiltration into the soil, reduced the output with runoff and drainage, and decreased nutrient loss through output water. Therefore, the additional preserve of nutrient by canopy interception was 8.664 kg/(hm² · year). __________ Translated from Scientia Silvae Sinicae, 2006, 42(12): 1–5 [译自: 林业科学]     

Relationship and its ecological significance between plant species diversity and ecosystem function of soil conservation in semi-humid evergreen forests, Yunnan Province, China

In recent years, the relationship between biodiversity and ecosystem stability, productivity, and other ecosystem functions has been extensively studied by using theoretical approaches, experimental investigations, and observations in natural ecosystems; however, results are controversial. For example, simple systems were more stable than complex systems in theoretical studies, and higher productivity was observed in human-made ecosystems with poorer species composition, etc. The role of biodiversity in the ecosystem, such as its influence on sustainability, stability, and productivity, is still not understood. Because accelerated soil-erosion in various ecosystems has caused a decrease of primary productivity, a logical way used in the study of the relationship between biodiversity and ecosystem function can be used to study the relationship between plant species diversity and soil conservation. In addition, biodiversity is a product of evolutionary history, and soil erosion is a key factor controlling the evolution of modern environment on the surface of the Earth. A study on the relationship between biodiversity and soil-erosion processes could help us understand the environmental evolution of Earth. Fifteen 10 m × 40 m standard runoff plots were established to measure surface runoff, soil erosion, and total P loss in different secondary communities of semi-humid evergreen broad-leaved forests that varied in composition, diversity, and level of disturbance and soil erosion. The following five communities were studied: AEI (Ass. Elsholtzia fruticosa + Imperata cylindrical), APMO (Ass. Pinus yunnanensis + Myrsine africana + Oplismenus compsitus), APLO (Ass. Pinus yunnanensis + Lithocarpus confines + Oplismenus compsitus), AEME (Ass. Eucalyptus smith + Myrsine africana + Eupatorium adenophorum), and ACKV (Ass. Cyclobalanopsis glaucoides + Keteleeria evelyniana + Viola duelouxii). Tree density, the diameter of the tree at breast height, and the hygroscopic volume of plant leaves were determined in each plot. Results indicated that surface runoff, soil erosion, and total P loss decreased as a power function with increase in plant species diversity. Their average values for three years were 960.20 m³/(hm² · year), 11.4 t/(hm² · year), and 127.69 kg/(hm² · year) in the plot with the lowest species diversity, and 75.55 m³/(hm² · year), 0.28 t/(hm² · year), and 4.71 kg/(hm² · year) in the plot with the highest species diversity, 12, 50, and 25 times respectively lower compared with the lowest species diversity plots. The coefficients of variation of surface runoff, soil erosion, and total P loss also followed a power function with the increase of plant species diversity, and were 287.6, 534.21, and 315.47 respectively in the lowest species diversity plot and 57.93, 187.94, and 59.2 in the highest species diversity plot. Enhanced soil conservation maintained greater stability with increased plant species diversity. Plant individual density increased linearly and the canopy density and cross section at breast height increased logarithmically with the increase of plant species diversity. The hydrological function enhanced as the plant species diversity increased. There were obviously relationships between plant species diversity and rainfall interception, coverage, and plant individual density, which was related to soil conservation functions in the five forest communities. The complex relationships between plant species diversity and the above-mentioned ecological processes indicated that plant species diversity was an important factor influencing the interception of rainfall, reducing soil erosion and enhancing the stability of soil conservation, but its mechanism is not known. This experiment showed that plant species diversity promoted soil and nutrient conservation and ultimately lead to the increase of the primary productivity of the ecosystem, and was thus a good way to study the relationship between biodiversity and ecosystem stability. Rainfall interception could be assessed easily using the hygroscopic volume of plant leaves. Because there were strong correlations between plant species diversity and soil conservation functions, the patterns of plant species diversity will show a certain level of predictability on the interactions of life systems with surface processes of the Earth. __________ Translated from Journal of Plant Ecology, 2006, 30(3): 392–403 [译自: 植物生态学报     

热带山地雨林生态系统水文化学循环规律的研究

根据５ａ定位观测，对尖峰岭热带山地雨林更新林生态系统的水文化学循环规律的数据分析表明，年均降雨量为２６６８．３ｍｍ，其中总径流量占４６．７％，蒸散量５３．３％，冠层截留量１４．０％。Ｎ、Ｐ、Ｋ、Ｃａ、Ｍｇ的年均降雨输入量为７８．４ｋｇ／（ｈｍ２·ａ），总径流输出５６．７ｋｇ／（ｈｍ２·ａ），净积累２１．６ｋｇ／（ｈｍ２·ａ）；Ｓｉ、有机Ｃ、Ａｌ、Ｍｎ的年均降雨输入量为２５．０ｋｇ／（ｈｍ２·ａ），总径流输出为１１２．３ｋｇ／（ｈｍ２·ａ），净损失８７．３ｋｇ／（ｈｍ２·ａ），更新林系统仅处于更新进展过程中，同时证实了冠层对降水化学的淋溶效应，净淋溶系数达４．１１；提出了降雨、林内净降雨、总径流的各水化学物含量与其相应水量的回归模式     

热带山地雨林生态系统水文化学循环规律的研究

根据５ａ定位观测，对尖峰岭热带山地雨林更新林生态系统的水文化学循环规律数据分析表明，年均降雨量为２６６８．３ｍｍ，其中总径流量占４６．７％，蒸散量５３．３％，冠层留量１４．０％。Ｎ、Ｐ、Ｋ、Ｃａ、Ｍｇ的年均降雨输入量为７８．４ｋｇ（ｈｍ＾２．ａ），总径流输出５６．７ｋｇ／（ｈｍ＾２．ａ），净积累２１．６ｋｇ／（ｈｇｍ＾２．ａ），Ｓｉ，有机Ｃ、Ａｌ、Ｍｎ的年均降雨输入量为２５．０ｋｇ（ｈｍ＾２．ａ）     

Carbon fluxes and their response to environmental variables in a Dahurian larch forest ecosystem in northeast China

The Dahurian larch forest in northeast China is important due to its vastness and location within a transitional zone from boreal to temperate and at the southern distribution edge of the vast Siberian larch forest. The continuous carbon fluxes were measured from May 2004 to April 2005 in the Dahurian larch forest in Northeast China using an eddy covariance method. The results showed that the ecosystem released carbon in the dormant season from mid-October 2004 to April 2005, while it assimilated CO₂ from the atmosphere in the growing season from May to September 2004. The net carbon sequestration reached its peak of 112 g·m⁻²·month⁻¹ in June 2004 (simplified expression of g (carbon)·m⁻²·month⁻¹) and then gradually decreased. Annually, the larch forest was a carbon sink that sequestered carbon of 146 g·m⁻²·a⁻¹ (simplified expression of g (carbon)·m⁻²·a⁻¹) during the measurements. The photosynthetic process of the larch forest ecosystem was largely affected by the vapor pressure deficit (VPD) and temperature. Under humid conditions (VPD < 1.0 kPa), the gross ecosystem production (GEP) increased with increasing temperature. But the net ecosystem production (NEP) showed almost no change with increasing temperature because the increment of GEP was counterbalanced by that of the ecosystem respiration. Under a dry environment (VPD > 1.0 kPa), the GEP decreased with the increasing VPD at a rate of 3.0 μmol·m⁻²·s⁻¹·kPa^-1 and the ecosystem respiration was also enhanced simultaneously due to the increase of air temperature, which was linearly correlated with the VPD. As a result, the net ecosystem carbon sequestration rapidly decreased with the increasing VPD at a rate of 5.2 μmol·m⁻²·s⁻¹·kPa⁻¹. Under humid conditions (VPD < 1.0 kPa), both the GEP and NEP were obviously restricted by the low air temperature but were insensitive to the high temperature because the observed high temperature value comes within the category of the optimum range.     

人工毛竹林水文生态功能的初步研究

在2009年3—10月对浙江庙山坞自然保护区人工毛竹林的水文生态特征进行了定位样地和径流场观测研究,以探讨其林内降水分配规律和水土保持功能。结果表明:(1)观测期内,林外总降水量达1 220.8 mm,穿透雨量、茎流量、林冠截留量分别占总降水量的78.2%、7.3%和14.5%。随着林外降水量的增加,穿透雨量、茎流量呈线性增加,而林冠截留量先是迅速增加,当林外降水量达10 mm后增速减缓,并趋于稳定(5 - 6 mm)。(2)人工毛竹林林地凋落物现存量平均为4.37 t·hm^-2,最     

Growth characteristics of multipurpose tree species,crop productivity and soil properties in agroforestry systems under subtropical humid climate in India

Multipurpose tree species （MPTs） were studied in an agroforestry arboretum under subtropical humid climate in Northeast India. Out of 12 MPTs planted under agroforestry systems, Acacia auriculiformis in spacing of 2 m × 2 m （2500 stems·hm^-2） could have the potentiality to meet the timber/fuelwood requirement due to its high wood production of 635 m^3·hm^-2 with mean annual increment （MAI） of 2.54×10^-2 m^3.treel.a^-1 in a short rotation period of 10 years. Thus, A. auriculiformis is a short rotation forest tree species suitable to grow in subtropical humid climate. On the other hand, at 16 years of age, Eucalyptus hybrid and Michelia champaca in spacing of 3 m × 3 m （1111 stems.hm^2） produced appreciably high timber volume of 315 m^3.hm^-2 and 165 m^3.hm^-2 with MAI of 1.77×10^-2 m^3.tree^-1·a^-1 and 0.92×10.2 m^3.tree^-1.a^-1, respectively. At 16 years of age, Gmelina arborea produced a timber volume of 147 m^3.hm^-2 with MAI of 1.47×10^-2 m^3.tree^-1.a^-1 followed by Samania saman （140 m^3.hm^-2）, Albizziaprocera （113 m^3·hm^-2） and Tectona grandis （79 m3.hm^-2） with MAI of 1.40, 1.13 and 0.78 × 10^-2 m^3 .tree^-1a^-1, respectively in 4 m × 4 m spacing （625 stems.hm^-2）. Gliricidia maculata and Leucaena leucocephala could be used as live fences around the farm boundary to supply their N-rich leaves for mulch as well as manure to crops. In agroforestry arboretum, direct seeded upland rice （Oryza sativa - variety, AR-11）, groundnut （Arachis hypogaea - variety, JL-24） and sesamum （Sesamum indicum - variety, B-67） were grown during the initial period upto 8 years of tree establishment. Under other MPTs, there was a reduction in crop productivity as compared to open space. After 8 years of tree establishment, horti-silvi and silvi-pastoral systems were developed and pineapple （Ananas comosus - variety Queen）, turmeric （Curcuma longa -variety RCT -1） and cowpea （Vigna sinensis - variety Pusa Barsati） as forage crop were raised. The productivity of p     

Effects of light radiation intensity on photosynthetic characteristics and water use efficiency of Platycladus orientalis and Pinus tabulaeformis seedlings

In order to offer a scientific basis for cultivation and management of forests, effects of light radiation intensity on photosynthetic characteristics and water use efficiency of Platycladus orientalis and Pinus tabulaeformis were studied under different soil moisture contents. By adopting artificial control methods to soil moisture, and under simulated photosynthetic radiation (SPR), the net photosynthetic rate (P _N), transpiration rate (T _r), water use efficiency (WUE) and intercellular CO₂ concentration (C _i) of Platycladus orientalis and Pinus tabulaeformis in the semi-arid region of the Loess Plateau, were studied. Results are as follows: within the photon range of 0–2,200 μmol/(m²·s), P _N, T _r and WUE were enhanced with an increase in SPR in both species. P _N and WUE of Platycladus orientalis and Pinus tabulaeformis, however, declined with continued increase in SPR. P _N, T _r, WUE and light saturation point (LSP) of Platycladus orientalis were higher than those of Pinus tabulaeformis, while light compensation point (LCP) of Platycladus orientalis was lower than that of Pinus tabulaeformis at the same soil moisture content. The efficiency of light energy utilization of Platycladus orientalis was higher than that of Pinus tabulaeformis; P _N, T _r and C _i of Platycladus orientalis and Pinus tabulaeformis were enhanced by increasing soil moisture content, whereas WUE declined. At soil moistures of 7.90%, 13.00% and 19.99%, LSP of Platycladus orientalis was 1,275, 1,450 and 1,675 μmol/(m²·s) respectively, and LCP was 42, 25 and 13 μmol/(m²·s) respectively, with corresponding maximal net CO₂ photosynthetic rates (P _max) of 3.04, 4.06 and 5.53 μmol/(m²·s). At soil moistures of 7.83%, 13.04% and 20.15%, the LSP of Pinus tabulaeformis was 1,100, 1,325 and 1,500 μmol/(m²·s) respectively, and LCP was 60, 30 and 23 μmol/(m²·s), with P _max of 1.08, 3.35 and 4.36 μmol/(m²·s) respectively. __________ Translated from Science of Soil and Water Conservation, 2006, 4(3): 108–113 [译自: 中国水土保持科学]     

不同栽培措施对尾巨桉生长的影响及经济效益分析

试验采用列区试验设计,设造林密度和追肥2个因素,每个因素6个水平,4次重复.密度因子作主区,追肥因子作副区,各个因素和各处理按随机区组排列.每个试验小区面积0.04 hm2(20 m×20 m),共计144个小区,连续5 a观测.经过方差分析得出,造林试密度对林分平均高、平均胸径和蓄积量都有极显著的影响.在6种参试密度中,造林密度越大,林分平均高、胸径越小,蓄积量越大;6种配方追肥对林分平均高影响不显著,对胸径和蓄积量生长影响显著;密度与追肥的交互作用不显著.在所有36个列区试验组合中,按经济效益排列前5名的密度和追肥最佳组合分别为:2 222株.hm-2和每公顷施N、P、K分别为200、150、100 kg,1 667株.hm-2和每公顷施N、P、K分别为300、200、200 kg;1 667株.hm-2和每公顷施N、P、K分别为200、150、100 kg;2 222株.hm-2和每公顷施N、P、K分别为100、50、50 kg;1 250株.hm-2和每公顷施N、P、K分别为200、150、100 kg.它们的蓄积量分别为183.94、188.43、169.95、164.33、163.03 m3.hm-2;利润值分别为14 977.44、14 965.09、13 832.83、13 785.80和13 345.18元.hm-2.     

Organic matter contribution to soil fertility improvement and maintenance in red Alder （Alnus rubra） silvopastoral systems

An investigation was conducted to quantify fine roots and roots nodules over the four seasons in forestry and agroforestry alder (Alnus rubra) stands in North Wales. Soil samples collected in each season were excavated at three sampling points (0.30 m, 0.57 m and 1.00 m distance from the base of each tree) from nine trees of the agroforestry and forestry plots. Result showed that the density of live fine root had significant differences in between seasons and treatments (P ＜ 0.001). The mean weight density of live fine root over the four seasons in agroforestry and forestry was 0.27±0.01 kg·m-3 and 0.54±0.03 kg·m-3, respectively. Weight density of dead root in each system remained constant throughout the year. The mean weight density of dead root was also significantly different (P ＜ 0.01) between forestry and agroforestry systems. Weight density of live and dead root nodule was both constant throughout the year and between the different sampling distances. The mean weight densities of live and dead root nodule over the four seasons were 0.09±0.03 kg·m-3 and 0.05±0.03 kg·m-3 in agroforestry and 0.08±0.02 kg·m-3 and 0.03±0.01 kg·m-3 in the forestry plots, respectively.     

麻竹人工林水文生态效应

在福建南靖连续4a对1995年春在杉木采伐迹地上营造的株行距为3m×4m、4m×5m和5m×6m3种密 度的麻竹试验林进行水文生态效应观测。结果分析表明:(1)麻竹林冠截持量与降水量和林分密度均呈正相关,而 秆茎流和林内降水量与降水量呈正相关,与林分密度呈负相关。密度为825丛·hm-2的麻竹林的年林冠平均截持 量和截持率为155.2 mm和14．61％,林内平均降水量和降水率为829．0 mm和78．11％,竹秆茎流量和茎流率为 77.3mm和7.31％。(2)麻竹林地表枯落物具有吸持其自身干质量2．8倍水量的潜在能力。(3)3种密度麻竹林的 0-60 cm土壤层最大潜在蓄水量为315．3-326．3 mm,略低于毛竹林367．9mm。(4)麻竹林地表径流和泥沙流 失量与降水量呈正线性相关,与林分密度呈负相关;竹林密度为825丛·hm-2的麻竹林年地表平均径流量、土壤侵 蚀模数是密度为330丛·hm-2的麻竹林的0．55、0．45倍,其NO3-、NH4 、PO43-、K 等养分年流失量则分别是密 度为330丛·hm-2的麻竹林的0．58、0．49、0．36、0．49倍。     

Root biomass and productivity in dominant plantation populations in the mountainous area in western Sichuan

This study investigated root biomass and productivity in dominant populations in western Sichuan, China. A total of 4 plots (Picea balfouriana plantation for 22 age in Maerkang, 9 trees, mean DBH of population for 10.4 cm and height for 10.5 m; Larix maxteriana plantation for 22 age in Wolong, 9 trees, mean DBH of population for 17.0 cm and height for 13.8 m; Abies fabri plantation for 35 age in Ebian, 18 trees, mean DBH of population for 14.1 cm and height for 11.9 m; Larix kaempferi plantation for 23 age in Miyaluo, 8 trees, mean DBH of population for 17.4 cm and height for 14.5 m; a 20 m×25 m plot located on each of the 4 types in western Sichuan, China) were randomly selected and excavated to a depth of 60 cm for each of the 4 plantation types. To estimate the root biomass of an individual tree using D ² H, an exponential model was selected with the highest coefficient ranging from 0.94 to 0.99. The total root biomass per hm² varied among plantation population types following the order: L. kaempferi (37.832 t/hm²) > A. fabri (24.907 t/hm²) > L. maxteriana (18.320 t/hm²) > P. balfouriana (15.982 t/hm²). The biomass fractions of a given root size class compared to the total root biomass differed among plantation population types. For all 4 studied plantation types, the majority of the roots were distributed in the top 40 cm of soil, e.g., 97.88% for P. balfouriana population, 96.78% for L. maxteriana, 95.65% for A. fabri, and 99.72 for L. kaempferi population. The root biomass fractions distributed in the top 20 cm of soil were 77.13% for P. balfouriana, 77.13% for L. maxteriana, 65.02% for A. fabri and 80.66% for L. kaempferi, respectively. The root allocation in the 0–20, 20–40, and 40–60 cm soil layers gave ratios of 34:12:1 for P. balfouriana, 24:6:1 for L. maxteriana, 15:7:1 for A. fabri, and 64:4:1 for L. kaempferi populations. The root biomass density of dominant plantation population was 10.782 t/(hm²·m) for P. balfouriana, 8.230 t/hm²·m) for L. maxteriana, 24.546 t/(hm²·m) for A. fabri, and 13.211 t/(hm²·m) for L. kaempferi population, respectively. The root biomass productivity was found to be 0.57 t/(hm²·year) for P. balfouriana, 0.83 t/(hm²·year) for L. maxteriana, 0.71 t/(hm²·year) for A. fabri and 1.64 t/(hm²·year) for L. kaempferi population, respectively. __________ Translated from Acta Ecologica Sinica, 2006, 26(2): 542–551 [译自: 生态学报, 2006, 26(2): 542–551]     

分月扇舟蛾颗粒体病毒生物测定

从黑龙江省双城林场采集健康的分月扇舟蛾2龄幼虫,将室内保存一年的分月扇舟蛾虫尸研碎,分离提纯得到纯净的颗粒体病毒。将病毒悬液稀释为1..58×103PIB·mL-1,1.58×104PIB·mL-1,1.58×105PIB·mL-1,1.58×106PIB·mL-1,1.58×107PIB·mL-1,1.58×108PIB·mL-1,1.58×109PIB·mL-17种浓度,采集新鲜的杨树叶分别浸入上述不同浓度的悬液,对采集的健康幼虫进行接毒。9天实验结果表明,浓度为1..58×103PIB·mL-1时校正死亡率最小(7.32%),浓度是1.58×109PIB·mL-1时校正死亡率最大(97.36%),浓度对数和死亡几率值的回归直线方程为y=1.946 0.558x,LC50为2.97×105PIB·mL-1。1.58×105PIB·mL-1,1.58×106PIB·mL-1,1.58×107PIB·mL-1,1.58×108PIB·mL-1,1.58×109PIB·mL-1w所对应的半致死时间(LT50)分别为8.55d,6.89d,5.9d,4.65d,4.08d。随着浓度的增大,LT50逐渐缩短,说明该病毒的毒力较强,作为杀虫剂具有很好的应用潜力。     

A study on the shade tolerance ofMuehlewbeckia complera

Muehlewbeckia complera was introduced to China in 2002 as indoor-hanging ornamental foliage plant. The experiment of the shade tolerance for this species was carried out in different light intensities (0.14–946.00 μmol·m⁻²·s⁻¹). After 40 days in experimental areas, leaf photosynthentic characteristics indexes ofM. complera in different photosynthesis active radiation (PAR) were measured with LI-COR6400 apparatus, such as the light compensation point, light saturation point, and maximum net photosynthesis rate, at the same time, the increments of total leaf area and leaf amount were measured. The results showed that the optimum light intensity range forM. complera was from 9.26 μmol·m⁻²·s⁻¹ to 569.00 μmol·m⁻²·s⁻¹ (463–28150 lx, relative humidity (RH) for 46–60%, temperature at 16–22°C). Under this condition, leaf photosynthetic efficiency was tiptop. AlthoughM. complera belonged to the moderate sun-adaptation plant species, the plant growth was inhibited when PAR increased to the level of 569.000 μmol·m⁻²·s⁻¹ or above.M. complera could sprout new leaves in photosynthesis active radiation of 0.16–19.22 μmol·m⁻²·s⁻¹ (8–961 lx), or 10 μmol·m⁻²·s⁻¹ for above 6 h. Foundation item: This study was supported by the Research Foundation of Northeast Forestry University. Biography: YUE Hua (1962-), female, Associate professor in Northeast Forestry University, Harbin 150040, P. R. China. Responsible editor: Zhu Hong     

德国中部Soiling云杉-山毛榉混交林冠层组成对土壤CO2排放的影响

It was hypothesized that soil respiration can be affected by canopy composition. Hence, admixture of trees as a common forest management practice may cause significant change in the carbon cycling. This study was conducted in a mixed spruce-beech stand at Solling forest in central Germany to investigate the effect of canopy composition on soil respiration. The canopy cover was classified in four major canopy classes (pure beech, pure spruce, mixed and gap), and the area under each canopy class was identified as a sub-plot. Soil respiration in each sub-plot (n=4) was measured monthly from Jun 2005 to July 2006. Results show significant difference in annual soil respiration between the beech (359 g·m⁻²·a⁻¹ C) and gap (211 g·m⁻²·a⁻¹ C) sub-plots. The estimation of the total below-ground carbon allocation (TBCA) based on a model given by Raich and Nadelhoffer revealed considerably higher root CO₂ production in the beech sub-plot (231 g·m⁻²·a⁻¹ C) compare to the gap sub-plot (51 g·m⁻²·a⁻¹ C). The contribution of the root respiration to the total soil respiration was higher in the soil under the beech canopy (59%) compared with the soil in the gap (29%). The findings suggested that the condition under the beech canopy may cause more desirable micro-site for autotrophic respiration and consequently higher CO₂ release into the atmosphere.     

Carbon sink in Phoebe bournei artificial forest ecosystem

Biomass, carbon content, carbon storage and spatial distribution in the 32-year-old Phoebe bournei artificial forest were measured. The mean biomass of the forest stand was 174.33 t/hm², among which the arbor layer was 166.73 t/hm², which accounted for 95.6%. Carbon contents of stems, barks, branches, leaves, root, shrub layer, herb layer, lichen layer and litter layer were 0.5769 g C/g, 0.4654 g C/g, 0.5232 g C/g, 0.4958 g C/g, 0.4931 g C/g, 0.4989 g C/g, 0.4733 g C/g, 0.4143 g C/g, 0.3882 g C/g, respectively. The mean carbon content of soil was 0.0139 g C/g, which reduced gradually along with soil depth. Total carbon storage of the P. bournei stand ecosystem was 227.59 t/hm², among which the arbor layer accounted for 40.13% (91.33 t/hm²), the shrub layer accounted for 0.17% (0.38 t/hm²), the herb layer accounted for 0.76% (1.71 t/hm²), the lichen layer accounted for 0.28% (0.63 t/hm²), and the litter layer accounted for 0.29% (0.66 t/hm²). Carbon content (0–80 cm) of the forest soil was 58.40% (132.88 t/hm²). Spatial distribution ranking of carbon storage was: soil layer (0–80 cm) > arbor layer > herb layer > litter layer > lichen layer > shrub layer. Net production of the forest stand was 8.5706 t/(hm²·a), in which the arbor layer was 6.6691 t/(hm²·a), and it accounted for 77.82%. Net annual carbon sequestration of the P. bournei stand was 4.2536 t/(hm²·a), and the arbor layer was 3.5736 t/(hm²·a), which accounted for 84.01%. __________ Translated from Scientia Silvae Sinicae, 2008, 44(3): 34–39 [译自: 林业科学]     

黄土丘陵区小流域林业土地生产潜力研究

黄土丘陵区小流域林业土地生产潜力研究＊王冬梅孙保平刘敬军关键词黄土丘陵区小流域土地生产潜力气候生产潜力现实生产潜力土地是由土壤、气候、地貌、岩石、植被和水文等因素组成的自然历史综合体,是一切生产和一切生物生存的源泉。长期以来,黄土高原由于人口数量的迅...     

Photosynthetic induction responses of Pinus koraiensis seedlings grown in different light environments

The time processes of photosynthetic induction responses to various irradiances in Korean pine (Pinus koraiensis) seedlings grown in open-light environments and in understory of forest were studied in an area near the Research Station of Changbai Mountain Forest Ecosystems, Jilin Province, China from July 15 to August 5, 1997. The results showed that at 200 μmol·m⁻²·s⁻¹ photosynthetic photon flux density (PPFD) and 500 μmol·m⁻²·s⁻¹ PPFD, the induction time for the photosynthetic rates of understory-grown seedlings to reach 50% and 90% steady-state net photosynthetic rates was longer than that of the open-grown seedlings. The induction responses of open-growth seedlings at 500 μmol·m⁻²·s⁻¹ PPFD were slower than those at 200 μmol·m⁻²·s⁻¹ PPFD, but it was the very reverse for understory-growth seedlings, which indicates that the photosynthetic induction times of Korean pine seedlings grown in the understory depended on the sunfleck intensity. Biograph: ZHOU Yong-bin (1970-), female, associate professor of Shenyang Agricultural University, Shenyang 110161, P.R. China. Responsible editor: Song Funan     

长白山典型阔叶红松林土壤二氧化碳排放通量

随着大气CO2浓度的升高,主要由其引起的温室效应与对生物新陈代谢的影响变得越来越显著。森林生态系统在全球碳循环中扮演着重要的角色。为了评估和理解森林土壤CO2通量及其随空气和土壤温度的季节和昼夜变化规律,我们在长白山北坡典型阔叶红松林内利用静态箱技术进行了原位观测。实验在整个生长季(6月初至9月末)昼夜进行,利用气相色谱进行气体分析。结果表明: 长白山阔叶红松林土壤是大气二氧化碳源,其CO2通量具有明显的季节和昼夜变化规律。通量的变化范围是(0.30-2.42)μmol穖-2穝-1,平均值为0.98μmol穖-2穝-1。土壤CO2排放的季节规律表明,土壤CO2通量的变化与气温和土壤温度的变化有关。CO2平均通量的最大值出现在7月((1.27±23%)μmol穖-2穝-1),最小值出现在9月((0.5±28%)μmol穖-2穝-1)。土壤CO2的昼夜波动与土壤温度变化有关,而在时间上滞后于温度的变化。森林下垫面土壤CO2通量与土壤温度显著相关,与6cm深度土层温度相关系数最大。基于气温和土壤温度计算的Q10值范围为2.09-3.40。图2表3参37。     

Fine roots refilling process in an artificial gap in a Picea mongolica forest

Picea mongolica is an endemic but endangered species in China. The spruce forest is only found in sandy forest-steppe ecotones. In this study, we examined the initial response of the quantity and refilling process of fine roots in an artificial canopy gap with a diameter of 36 m in a P. mongolica forest. Under the canopy, the fine root length densities of trees, shrubs and herbs were 2,622, 864 and 3,086 m·m–2, respectively. The fine root biomass of trees, shrubs and herbs were 148, 62 and 65 g·m–2, respect...