56 research outputs found

    Distribution of Fine Roots in a Mixed Cunninghamia lanceolata-Tsoongiodendron odorum Plantation

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    对27年生混交比例为2行杉木和1行观光木的混交林和杉木纯林群落细根分布的研究表明,杉木和观光木行间的杉木细根密度虽比杉木与杉木行间的低8.5%,但观光木细根密度则高152.09%,其细根总密度比杉木与杉木行间的大10.43%。混交林中杉木各径级活细根密度呈单峰型分布,均以5-10cm土层最大,而观光木各径级活细根主要分布在0-10cm土层内。纯林杉木各径级活细根密度亦基本呈单峰型分布,但峰值出现在10-20cm或20-30cm土层。不同树种不同径级死细根的分布均与其各自的活细根分布相似。混交林中灌木细根密度在30-40cm的土层最大,而纯林中的灌木细根集中于0-10cm的表土层;混交林和纯林中的草本细根均集中在0-5cm土层。与纯林的相比,混交林中杉木细根主要分布的土层明显上移,表层土壤细根所占比重增大,有利于更好利用土壤养分和提高群落生产力。Fine roots were measured by soil core sampler in a mixed plantation of 27-year-old Cunninghamia lanceolata (C) and Tsoogiodeudron odorum (T) in Fujian Province. Fine root density of C at interrow between C and T was lower by 8.5% than that between C and C, but fine root denstiy of T and total fine root density were higher by 152.09% and 10.43%, respectively. High density of living fine roots with different thickness of C in mixed plantation appeared at 5-10 cm soil depth, whereas that of T at 0-10 cm. Compared to mixed plantation, living fine root density in pure C plantation appeared at 10 -30 cm of soil depth. The distribution of dead fine roots had the same pattern. In mixed plantation, upward trend of soil layer with maximum fine roots of C was obvious, showing that mixed plantation had an advantage over pure plantation in nutrient absorption.中国博士后科研基金项目(1999-10);;福建省科委重大基础研究项目(2000-F-004);; 高等学校骨干教师资助计划项目;;福建省自然科学基金项目(B0110025

    Study on the Model both Cutting Variable-speed of the Log-core Veneer Lathe and Moving Locus Model with Constant-speed Peeling

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    详细分析了无卡轴旋切机的工作原理,推导了旋切过程中刀刃进给速度与圆木直径的数学模型,同时得出旋切时间的近似计算式。从中可知,旋切过程中刀刃进给速度必须按一定规律变化才能保证旋切机正常工作。建立了旋切机恒线速旋切的运动轨迹模型,推导出旋切机恒线速旋切时间的精确计算式,并在此基础上提出了旋切时间简便的近似计算式。这些研究结果均可用于指导设计和进行实际生产。Working principle of log-core veneer lathe had been analyzed in detail,and the mathematical model between the knife-carriage feeding speed and the diameter of the log core was established,in the meantime,the approximation cutting time formula was also derived.The feeding speed must be changed with continuousness and a rule,which can let the lathe work well.Moving locus model of invariable-speed peeling was also founded,precision calculating formula of invariable-speed peeling was deduced.In the same time,the simplification cutting-speed formula was also derived.These results of the research will provide a guide for the designing and the producing practice

    NUTRIENT CYCLING OF N AND P BY A MIXED FOREST OF CUNNINGHAMIA LANCEOLATA AND TSOONGIODENDRON ODORUM IN SUBTROPICAL CHINA

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    通过对福建三明 2 7年生杉木 (Cunninghamialanceolata) 观光木 (Tsoongiodendronodorum)混交林 (混交比例2 :1)及杉木纯林群落N、P养分循环进行为期 2年的研究。结果表明 ,混交林中杉木和观光木地上各组分的N、P含量大小均为叶 >活枝 (或皮 ) >枯枝 >干 ,而根系的则随径级的减小而增大 ,且观光木各组分的N含量均高于杉木的 ;混交林群落的N、P总积累量达 5 85 .2 2 3kg·hm-2 和 12 8.784kg·hm-2 ,分别是纯林群落的 1.5倍和 1.3倍。混交林群落N、P养分年归还量达 75 .740kg·hm-2 和 5 .493kg·hm-2 ,分别是杉木纯林的 113 .0 %和 79.6 %。混交林通过凋落物、降水淋溶和细根枯死 3种途径的N归还量分别占群落总归还量的 6 7.1%、8.4%和 2 4.5 % ,而纯林的则分别为 6 9.3 %、8.1%和 2 2 .6 % ;混交林 3种途径的P归还量分别占群落总归还量的 6 4.0 %、7.5 %和 2 8.5 % ;而纯林则为 74.8%、5 .3%和 19.9%。混交林中林下植被层的N、P归还量分别占群落总归还量的 14.8%和 37.3 % ;而纯林的则为 2 9.5 %和 5 9.4%。混交林群落的N、P富集率和利用系数均低于纯林的 ,而周转期则均大于纯林的。混交林群落的P吸收系数小于纯林的 ,而循环系数则高于纯林的 ,但其两者的N吸收系数和循环系数则相似。A study on the cycling of N and P in a pure forest of Chinese fir ( Cunninghamia lanceolata (Lamb.) Hook. and a Chinese fir_ Tsoongiodendron odorum Chun mixed forest (2 Chinese fir: 1 T. odorum ) over two years was carried out in Sanming, Fujian, China. For both Chinese fir and Tsoongiodendron odorum, the concentrations of N and P in aboveground fractions were in the order of leaves>living branches (or stem bark)>dead branches> stem wood, and those in roots increased with an increase in root diameter. N concentrations in various fractions of T. odorum were higher than their respective values for Chinese fir. The standing crops of N and P in the mixed stand were up to 585.223 kg·hm -2 and 128.784 kg·hm -2 , being 1.5 and 1.3 times as much as that in the pure stand, respectively. The annual return of N and P amounted to 75.740 and 5.493 kg·hm -2 in the mixed forest, respectively, being 113.0% and 79.6% of that in the pure forest. The fractions of annual N return through litterfall, rain leaching and fine root turnover were 67.1%, 8.4% and 24.5% in the mixed forest, respectively, and the corresponding values were 69.3%, 8.1% and 22.6% in the pure forest. These three pathways contributed to 64.0%, 7.5% and 28.5% of total P return in the mixed forest, and 74.8%, 5.3% and 19.9% in the pure forest, respectively. 14.8% of N return and 37.3% of P return in the mixed forest, and 29.5% of N return and 59.4% of P return in the pure forest were derived from the undergrowth vegetation. For both N and P elements, the enrichment ratios and the utilization coefficients were lower, and the recycling periods were higher in mixed forest than in pure stand. For P, the absorption coefficient was lower, and the cycling coefficient was higher, in mixed forest than in pure forest, while there were no significant differences for those of N between the two forests.中国博士后科研基金;; 福建省科委重大基础研究项目 ( 2 0 0 0_F_0 0 4);; 高等学校骨干教师资助计划项

    Zooplanktonic diversity in the western Pacific

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    西太平洋区是全球海洋生物种源中心,许多类群的最高物种多样性都出现于该区域,因此,在该区开展种类多样性的研究不仅重要和必要,而且具有在跨国尺度上进行综合管理和相互合作的迫切性。本文在西太平洋的浮游动物样品鉴定分类、编目、文献资料整理和分析的基础上,记录和编入西太平洋10个浮游动物类群2,658种(含亚种),隶属于206科675属,其中水螅水母类99科251属697种,栉水母类12科22属59种,浮游软体动物14科35属86种,介形类8科89属416种,桡足类51科156属908种,糠虾类4科58属202种,磷虾类2科8属56种,十足类8科22属105种,毛颚类5科8属48种,被囊类5科26属81种。The western Pacific region has been operating as a centre for the origin of marine biodiversity: the richest diversity of many marine taxa was found in these waters.Therefore,biodiversity research and con-servation efforts in this area are necessary in order to promote the integrative and international management of this resource.The present work is a compilation of numbers of all the families,genera and species of ma-jor taxa of zooplankton known in the western Pacific Ocean(106°–150°E,0°–44°N).In all,2,658 zooplank-tonic species(including subspecies) belonging to 206 families and 675 genera have been recorded from taxonomic identifications and literature,99 families,251 genera and 697 species belong to the Medusozoa,12 families,22 genera and 59 species to the Ctenophora,14 families,35 genera and 86 species to the pelagic Molluscs(Pteropoda and Heteropoda),8 families,89 genera and 416 species to the Ostracoda,51 families,156 genera and 908 species to the Copepoda,4 families,58 genera and 202 species to the Mysidcea,2 fami-lies,8 genera and 56 species to the Euphausiacea,8 families,22 genera and 105 species to the Decapoda,5 families,8 genera and 48 species to the Chaetognatha,5 families,26 genera and 81 species to the Tunicata.908专项“中国海洋生物种类名录和图谱”(908-ZC-II-02)和908专项海洋生物样品库;科技部基础工作专项“我国和邻近西北太平洋海洋生物物种编目和分布图集编制”(2006FY220700

    Fine root distribution, seasonal pattern and production in a native forest and monoculture plantations in subtropical China

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    作者简介: 杨玉盛(1964~ ) , 男, 福建仙游人, 博士, 教授, 主要从事亚热带常绿阔叶林C、N 循环研究。E2mail: [email protected] tt. fj. cn 致谢: 福建农林大学蔡丽平、林瑞余、谢锦升, 陈爱玲、陈清山、邹双全、李春林, 硕士研究生郭剑芬、刘艳丽、岳永杰、于占源、江淼华、卢豪良等, 及莘口教学林场郑燕明、刘春华、王巧珍、陈辉等参加了项目研究[中文文摘] 通过对福建三明格氏栲天然林及在其采伐迹地上营造的33年生格氏栲人工林和杉木人工林细根分布、季节动态与净生产力进行的为期3a(1999~2001)的研究,结果表明,格氏栲天然林、格氏栲和杉木人工林活细根生物量分别为4.944t/hm2、3.198t/hm2和1.485t/hm2,死细根生物量分别为3.563t/hm2、2.749t/hm2和1.287t/hm2;死细根生物量占总细根生物量的比例分别为41.9%、46.2%和46.4%;0.05);活细根生物量最大值均出现在3月份,最小值一般出现在5~7月份或11~翌年1月份间。0~10cm表土层格氏栲天然林活细根生物量高达295.65g/m2,分别是格氏栲人工林和杉木人工林的2.4倍和8.1倍;该层格氏栲天然林活细根生物量占全部活细根生物量的59.8%,均高于格氏栲人工林(39.07%)和杉木人工林(24.51%)。格氏栲天然林、格氏栲人工林和杉木人工林细根分解1a后的干重损失率分别为68.34%~80.13%、63.51%~77.95%和47.69%~60.78%;年均分解量分别为8.747、5.143和2.503t/hm2;死亡量分别为8.632、5.148和2.492t/hm2;年均净生产量分别为8.797、5.425和2.513t/hm2,年周转速率分别为1.78、[英文文摘]In the last decades, large scale native forests have been converted to fast growing and high yield commercial forest plantations to meet the demands for timber, fuel material, and other forest products. Some silvicultural measures, such as planting pure stands, clear cutting and slash burning, have been widely applied during this conversion. Yield decline and land deterioration in such disturbed ecosystem has become serious. In this context, the ecological comparisons between native forests and monoculture plantations are necessary in providing the implications for sustainable management. Few studies on fine roots dynamics have been conducted within these ecosystems though the importance of fine roots in carbon and nutrient cycling has been increasingly emphasized due to their rapid turnover rates. Two 33 year old plantations, Chinese fir (Cunninghamia lanceolata, CF) and Castanopsis kawakamii (CK), were chosen to examine fine root (005). An early spring flush of root biomass (March) was found in these three forests, and the minimum value mainly occurred during May July or November January. For the NF, 598% of root biomass was found in the top soil of 0~10 cm, a layer that maximum depth distribution difference among these forests occurred, where root biomass of the NF was 237 times and 812 times as much as that of the CK and the CF, respectively. Percentages of original mass lost during the first year of decomposition ranged from 4379%~5631% for the FH to 6834%~8013% for the NF Mean annual root decomposition, mortality and production ranged from 847 t/(hm 2·a), 8632 t/(hm 2·a) and 95 t/(hm 2·a) in the NF to 2503 t/(hm 2·a), 2492 t/(hm 2·a) and 2513 t/(hm 2·a) in the CF. The mean root turnover rate ranged from 178 times/a in the NF to 169 times/a in the CF.国家自然科学基金资助项目(30170770);福建省自然科学基金资助项目(B0110025);高等学校优秀青年教师教学科研奖励计划资助项目;福建省基础研究重大资助项目(2000-F-004

    中国物理海洋学研究70年:发展历程、学术成就概览

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    本文概略评述新中国成立70年来物理海洋学各分支研究领域的发展历程和若干学术成就。中国物理海洋学研究起步于海浪、潮汐、近海环流与水团,以及以风暴潮为主的海洋气象灾害的研究。随着国力的增强,研究领域不断拓展,涌现了大量具有广泛影响力的研究成果,其中包括:提出了被国际广泛采用的"普遍风浪谱"和"涌浪谱",发展了第三代海浪数值模式;提出了"准调和分析方法"和"潮汐潮流永久预报"等潮汐潮流的分析和预报方法;发现并命名了"棉兰老潜流",揭示了东海黑潮的多核结构及其多尺度变异机理等,系统描述了太平洋西边界流系;提出了印度尼西亚贯穿流的南海分支(或称南海贯穿流);不断完善了中国近海陆架环流系统,在南海环流、黑潮及其分支、台湾暖流、闽浙沿岸流、黄海冷水团环流、黄海暖流、渤海环流,以及陆架波方面均取得了深刻的认识;从大气桥和海洋桥两个方面对太平洋–印度洋–大西洋洋际相互作用进行了系统的总结;发展了浅海水团的研究方法,基本摸清了中国近海水团的分布和消长特征与机制,在大洋和极地水团分布及运动研究方面也做出了重要贡献;阐明了南海中尺度涡的宏观特征和生成机制,揭示了中尺度涡的三维结构,定量评估了其全球物质与能量输运能力;基本摸清了中国近海海洋锋的空间分布和季节变化特征,提出了地形、正压不稳定和斜压不稳定等锋面动力学机制;构建了"南海内波潜标观测网",实现了对内波生成–演变–消亡全过程机理的系统认识;发展了湍流的剪切不稳定理论,提出了海流"边缘不稳定"的概念,开发了海洋湍流模式,提出了湍流混合参数化的新方法等;在海洋内部混合机制和能量来源方面取得了新的认识,并阐述了混合对海洋深层环流、营养物质输运等过程的影响;研发了全球浪–潮–流耦合模式,推出一系列海洋与气候模式;发展了可同化主要海洋观测数据的海洋数据同化系统和用于ENSO预报的耦合同化系统;建立了达到国际水准的非地转(水槽/水池)和地转(旋转平台)物理模型实验平台;发展了ENSO预报的误差分析方法,建立了海洋和气候系统年代际变化的理论体系,揭示了中深层海洋对全球气候变化的响应;初步建成了中国近海海洋观测网;持续开展南北极调查研究;建立了台风、风暴潮、巨浪和海啸的业务化预报系统,为中国气象减灾提供保障;突破了国外的海洋技术封锁,研发了万米水深的深水水听器和海洋光学特性系列测量仪器;建立了溢油、危险化学品漂移扩散等预测模型,为伴随海洋资源开发所带来的风险事故的应急处理和预警预报提供科学支撑。文中引用的大量学术成果文献(每位第一作者优选不超过3篇)显示,经过70年的发展,中国物理海洋学研究培养了一支实力雄厚的科研队伍,这是最宝贵的成果。这支队伍必将成为中国物理海洋学研究攀登新高峰的主力军

    四元硝酸盐与硅酸钙多孔载体复合的新型低温复合相变材料

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    常用的低温相变材料主要有石蜡、高级脂肪烃、和无机水合盐等。本文使用Ca(NO_3)_2、LiNO_3、NaNO_3、KNO_3四元混合硝酸盐制备而成的相变材料,熔点100℃,通过与多孔硅酸钙载体复合,得到了一种新型的低温复合相变材料。通过扫描电镜(SEM)观察到相变材料很好的吸附在载体的孔隙中,X射线图谱(XRD)分析表明相变材料与载体具有良好的化学相容性,示差扫描热法(DSC)实验表明复合材料450℃以内性能稳定未产生分解。经过1000次储(放)热循环测试,本复合相变材料仍能维持其结构形状和储热密度不变。研究表明这种新型材料有望应用于低温相变储热

    柔性飞艇阵风响应数值模拟研究

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    采用松耦合方法形成了定常流固耦合计算方法,流体部分通过求解RANS方程得到飞艇在大尺度绕流条件下对应的表面力;结构部分通过有限元方法求解得到非线性大变形模型的边界位移量,利用流固耦合接口来实现两者之间的数据信息交换。计算了飞艇在15 m/s风场中,横向3m/s,周期2 s的周期性阵风条件下的响应特征
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