武夷山甜槠林生态系统的养分平衡研究(英文)

本文通过比较大气降水的养分输入与由地表径流与地下渗流的养分输出,对武夷册甜槠林生态系统的养分平衡进行了研究。结果表明,在１９９３年４月至１９９４年４月期间,通过大气降水进入甜槠林的养分元素以Ｎ最高,为３４．２０７ｋｇ．ｍ＾２,其余依次为Ｃａ,Ｓ,Ｎａ,Ｋ和Ｍｇ,以Ｐ的输入最低,仅１．７７９ｋｇ．ｈｍ２;由地表径流和地下渗流的养分输出总量Ｎ,Ｐ,Ｋ,Ｃａ,Ｍｇ,Ｓ,Ｎａ分别为５．６８,１０１６,７．     

长白松人工林生态系统营养元素的分配格局和积累规律

对长白松人工林生态系统营养元素的分配格局和积累规律研究表明,乔木层不同器官营养元素含量为叶＞枝＞根＞干皮＞干材;同化器官──针叶中养分含量为Ｎ＞Ｋ＞Ｃａ＞Ｐ＞Ｍｇ;吸收器官──根中养分含量为Ｃａ＞Ｎ＞Ｋ＞Ｐ＞Ｍｇ;人工林生态系统中的养分含量为土壤＞凋落层＞草本层＞灌木层＞乔木层,乔木层养分贮量和积累率分别为８８．７９％和７６．４３％;长白松林生态系统中植物对Ｎ、Ｐ的吸收较强烈．     

香港桃金娘群落植物的养分分配、季节动态和生物循环

研究香港桃金娘灌木林中植物Ｎ,Ｐ,Ｋ养分,结果表明：（１）生物量和养分贮量的分配格局明显不同。桃金娘茎和枝的生物量占地上部生物量的６６．３％,其Ｎ,Ｐ,Ｋ贮量分别只占地上部Ｎ,Ｐ,Ｋ贮量的３８．０％,３７．６％和５１．６％,叶子的生物量占地上部生物量的１８．９％,其Ｎ,Ｐ,Ｋ贮量却分别占３９．９％,３５．４％和２８．０％。（２）常绿的桃金娘叶子终年保持相对高的养分贮量,花和果的养分贮量则存在的有规     

植被砍伐对土壤养分的影响

研究了不同砍伐频率下,香港、深圳和鹤山研究样地山坡地Ｎ、Ｐ、Ｋ含量的差异．不同采样地之间,养分全量和有效量差异显著．在尚未砍伐的山坡地,土壤养分含量显著高于经常砍伐的山坡地．未伐土壤的Ｎ含量顺序为香港样地＞深圳样地＞鹤山样地．下层土壤Ｐ的含量高于上层土壤．深圳样地常代土壤养分含量高于鹤山．结果建议采用最适砍伐频率和在最适季节砍伐,以便减少砍伐产生的不利影响．     

Nitrogen and phosphorus translocation of forest floor mosses as affected by a pulse of these nutrients

藓类是亚高山森林、北方针叶林和极地苔原等原始生态系统的重要组成部分。养分沉降是这些生态系统的主要养分来源。然而,对 藓类如何利用大气沉降这一时间上异质性较高的养分来源的认识缺乏,限制了我们对藓类在生态系统养分循环中作用的认识,也制约了模 拟和预测生态系统服务功能动态变化的有效性。本研究中,我们重点关注如下问题：(1)藓类新生部分的氮、磷含量随氮或磷沉降量的变化; (2)氮或磷养分沉降如何影响藓类的氮磷转运;(3)氮磷转运与藓类新生部分养分含量的关联性？为此,我们在位于青藏高原东部的亚高山 冷杉林中开展了设置有不同氮、磷施加量水平的突发养分沉降实验。以林下优势度最高的塔藓和锦丝藓为对象,我们在施加实验处理8天和1年后,分别测定了不同年龄藓类茎段中的氮、磷含量。研究结果发现,养分处理8天后,锦丝藓和塔藓的所有茎段的氮或磷含量均随处理中氮或磷施加量的增加而增加,表明它们能够高效率地吸收施加的氮或磷。养分处理1年后,形成于养分处理后的新生茎段中的氮、磷含量以及氮磷比与处理后8天的藓类茎段中氮、磷含量以及氮磷比呈正相关关系,表明藓类将吸收的养分转运至新生部分,转运过程受源—库关系的调控。磷转运效率解释了新生茎段21%–23%的氮磷比变化,而氮转运与新生茎段氮磷比没有显著关系,结果暗示磷转运对藓类生长的重要性。上述结果表明,养分转运是藓类植物利用间断的沉降养分的关键机制,也使藓类成为生态系统中重要的养分库。     

北方稻田生态系统水量平衡及水分效率研究

１９９３～１９９５年研究了５种不同模式水稻田生态系统水量平衡及水分效率结果表明,不同水稻田模式其总耗水量之间有明显差异,其中节水模式和节水节肥模式较常规模式节省灌溉水达１５～２３％,水分生产效率增加３０％以上．各模式蒸发蒸腾耗水量在同一生长季内基本相同．田间结构及调控管理对其无明显影响实测水稻生育期田间蒸发蒸腾量与计算的可能蒸发蒸腾量相差不过５％。     

施肥对水稻产量和稻田土壤理化性质的影响

稻田土壤中养分的平衡主要取决于养分的输入与输出,其又主要受肥料的输入与植物所带走的养分所制约。不同的肥料品种、不同的施肥时期都影响养分在土壤中的吸收、转化与淋失,从而影响养分的输入与输出。稻田土壤生态系统中养分循环的研究已有很多报道。主要是不同耕作制度、不同施肥水平下,各输入输出因子的研究以及对土壤肥     

植物养分利用效率研究综述

养分利用效率的概念是理解生态系统功能的中心。本文从植物养分利用效率的概念出发,对养分利用效率的表示与计算方法、影响因素以及养分再吸收的生物化学基础等进行综述,分析目前研究中存在的问题,最后指出今后应加强研究的方面。     

杉木人工林生态系统水文学过程的养分特性

根据5a定位观测的数据,对湖南会同24～28a生的杉木人工林生态系统各水文学过程中的养分特性进行了研究。结果表明：林冠降水是杉木人工林生态系统养分输入的重要来源,其中Ca的养分含量最高,P的含量最低。林内穿透水各养分元素的含量明显高于林冠降水中养分的含量。除Ca外,树干茎流中其它养分元素的含量为林冠降水的6倍以上。可见,林内穿透水和树干茎流是杉木林生态系统内养分循环的重要组成部分,有利于提高系统的养分利用率。地表径流中除硝态氮外,各元素的含量与穿透水的含量接近,其中P、Na和K三种元素的含量较低,但未超过林冠降水中养分元素含量。地下径流中N和K的含量较低,而Ca的含量与林冠降水相比没有差异。因而地表径流和地下径流不可避免的造成生态系统的养分损失,但24～28a生杉木林生态系统的调控能力较强,地表径流和地下径流量较小,生态系统的养分损失也相对较小,养分为净积累。不同季节之间水文学过程中养分元素含量存在一定程度的差异。降水形态、雷电和地形等要素影响养分元素含量。硝态氮在冰雹中未检出,而在雨水中的含量是雪水的2倍。铵态氮、K和Mg等元素在雨水中的含量最高。P和Ca以雪水的含量最高,与雨水和冰雹相比不存在数量级差异。雷电明显增加降水中养分的含量,特别是林冠上层的低空放电使降水中N的含量增加3～5倍。由于山谷和山麓的立地条件较好,其穿透水中养分含量比山坡的高,山谷与山麓的大致相等。在采集水样进行养分分析时,应考虑降水时间、降水形态和地形等因子的影响。     

红壤旱坡地农田生态系统养分循环和平衡

通过田间定位试验从生态系统的角度比较研究了中亚热带红壤低丘岗地几种主要旱坡地农田生态系统的水土流失、养分循环和平衡特征、土壤养分消长动态及空间分异,结果表明：水土流失是红壤旱坡地生态系统养分损失的重要途径之一,固体径流具有养分富集现象,速效养分损失以地表径流为主,水土流失养分损失量大小顺序为：有机碳＞全钾＞速效钾＞全氮＞全磷＞水解氮＞速效磷;免耕覆盖和垄作能显著减少水土流失及养分损失量;红壤旱地淋溶也是养分,尤其是氮素损失的重要途径;在养分平衡有盈余状况下,土壤养分水平是可以逐步提高的,其中,土壤速效磷、速效钾提高的速度较快,土壤全氮、有机质和全磷也有所提高,但仍处于较低水平;复合农林系统中,土壤养分存在明显的空间分异,农作物区域由于养分投入较高,土壤养分水平明显高于林木区域。     

Element loss on rain forest conversion in East Amazonia: comparison of balances of stores and fluxes

Nutrient loss from forest ecosystems by burning and leaching can be estimated by comparing nutrient stores before and after the disturbance, and by measuring the nutrient fluxes during disturbance. We applied both methods to a clear cutting experiment near Belem, Eastern Amazon, in a correct time series of 15 months duration. Nutrient flux measurements include wood export, loss to the atmosphere by burning, and leaching. The latter was based on water flux simulation with a soil water model, and on element analysis of soil water extracts (ceramic cup lysimeter). Two plots with 33 and 92tha^–1 of residual biomass (left after export of wood >7cm diameter) were compared with a forest control plot. Store and flux balances agreed well in case of Na, K, Mg, and S, and partially also for Ca and total P. Deviations seem to be caused by erratic but statistically not significant variations of the soil stores (mainly C and total N). Spacial variability of soil parameters demand very high sample replication, especially after disturbance. Flux measurements are better but more costly.     

Merging aquatic and terrestrial perspectives of nutrient biogeochemistry

Although biogeochemistry is an integrative discipline, terrestrial and aquatic subdisciplines have developed somewhat independently of each other. Physical and biological differences between aquatic and terrestrial ecosystems explain this history. In both aquatic and terrestrial biogeochemistry, key questions and concepts arise from a focus on nutrient limitation, ecosystem nutrient retention, and controls of nutrient transformations. Current understanding is captured in conceptual models for different ecosystem types, which share some features and diverge in other ways. Distinctiveness of subdisciplines has been appropriate in some respects and has fostered important advances in theory. On the other hand, lack of integration between aquatic and terrestrial biogeochemistry limits our ability to deal with biogeochemical phenomena across large landscapes in which connections between terrestrial and aquatic elements are important. Separation of the two approaches also has not served attempts to scale up or to estimate fluxes from large areas based on plot measurements. Understanding connectivity between the two system types and scaling up biogeochemical information will rely on coupled hydrologic and ecological models, and may be critical for addressing environmental problems associated with locally, regionally, and globally altered biogeochemical cycles.We dedicate this paper to the memory of Catherine Lisa Dent, a member of our working group who contributed much to the ideas presented herein, and to the joy of developing them together.Due to an error in the citation line, this revised PDF (published in December 2003) deviates from the printed version, and is the correct and authoritative version of the paper.     

华南人工林凋落物养分及其转移

对华南 5种人工林凋落物量、凋落物养分及绿叶养分含量的测定结果表明 ,各种人工林凋落物量大小依次为 :马占相思 (11.1t·hm-2 ) >湿地松 (7.3t·hm-2 ) >荷木 (6 .5t·hm-2 ) >大叶相思 (4.8t·hm-2 ) >柠檬桉(2 .6t·hm-2 ) .马占相思通过落叶回归土壤的养分量高于其它类型 .5种人工林均通过养分转移机制 ,大量从枯老叶中转移N、P、K养分 ,其中马占相思转移的养分量最大 ,营养转移的季节性差别较大 .各种人工林对其它元素的转移现象不确定 .     

Leaf phosphorus fractionation and growth responses to phosphorus of the forage legumes Trifolium repens, T. dubium and Lotus pedunculatus

'Grasslands Huia' white clover ( Trifolium repens L.), 'Grasslands Maku' lotus ( Lotus pedunculatus Cav.) and suckling clover ( T. dubium Sibth) were grown in a controlled environment at various levels of P supply. Dry weights and the concentration of inorganic-, lipid-, ester- and residual-P in trifoliate leaves were measured. Lotus grew better than white or suckling clover at low P. White clover and lotus responded steeply to increased P and had similar shoot dry weights at high P. Suckling clover had lower shoot weights than the other species at all P levels. The superior growth of lotus at low levels of p was probably due to better root growth and P uptake. Lotus had higher shoot P concentrations at low levels of P but lower concentrations than the others at high levels. White clover and suckling clover had similar shoot P concentrations at all levels of supply. In white and suckling clover total leaf P concentration rose with P supply. Of the P fractions, inorganic-and residual-P showed the largest rises in concentration. The increases in lipid- and ester-P were smaller. Increases in lotus leaf P were small, primarily because of the relatively small rises in inorganic- and residual-P. White clover is a vigorous species but requires high levels of P for best growth. Suckling clover has a relatively small response to improvements in P availability. The behaviour of the various P fractions is similar to that in white clover. Lotus grows well at low P but also shows rapid growth at high P supply. Whether efficiency is defined as the ability to extract P from the environment or to maintain low internal P concentration, lotus makes efficient use of P over the whole range of P supply.     

灵长类营养生态学的研究进展

营养生态学是现代生态学领域研究动物食物数量和质量、营养适应以及营养对种群特征作用规律的分支学科.目前从营养生态学研究灵长类食性需求主要分为五种假说,1)能量最大化假说;2)氮(蛋白质)最大化假说;3)植物次级代谢产物调节假说;4)膳食纤维调节假说;5)食物营养均衡假说.本文从研究方法和研究内容分别介绍了这些假说在灵长类...     

若干北方落叶树木叶片养分的内外迁移：Ⅰ.浓度和含量的变化

研究了北方 1 2个落叶树种单位面积叶干重、叶片灰分、有机物质和 7个元素的浓度和含量在落叶前后的变化 ,同一元素不同树种间及同一树种不同元素间有着不同的变化模式 .单位面积叶干重、叶片有机物质浓度和含量在落叶后均表现下降的趋势 ;所有树种叶片灰分浓度和大部分树种的灰分含量 (除刺槐、胡颓子、核桃楸外 )均有增加 ;落叶时 N、P、K的单位叶面积含量均可减少约 1 / 3～ 2 / 3;Mg含量的减少在胡颓子、核桃楸、春榆、蒙古栎、日本落叶松等 5个树种中发生 ,其余树种表现增加 ;落叶中 Fe含量除胡颓子下降外 ,其余均表现升高 ;落叶中 Ca、Si浓度和含量在所有分析树种中均表现增加趋势     

Changes in ecosystem functioning after replacement of forest by Lantana shrubland in Kumaun Himalaya

Abstract. Lantana camara shrubland is compared with the adjacent Quercus leucotrichophora and Pinus roxburghii forests to understand changes occurring in net primary productivity and nutrient cycling, as a consequence of degradation of these forests. The total net primary productivity of Lantana camara shrubland was 17 t ha^-1 yr^-1, which is similar to the values reported for forests: 16 - 21 t ha^-1 yr^-1. Total nutrient content (N, P) in the soil in the L. camara shrubland: 2932 kg ha^-1 N and 111 kg ha^-1 P, was lower than that of the forest soils.     

Nutrient resources for crop production in the tropics

For the foreseeable future a majority of the population, and almost all the mal- and under-nourished, will continue to be found in the tropics and subtropics. Food security in these parts of the world will have to be met largely from local resources. The productivity of the land is to a large extent determined by the fertlity of the soil, which in turn is mostly determined by its organic matter content and stored nutrients. Soil organic matter is readily lost when organic matter inputs are reduced upon cultivation and more so upon intensification. The concomitant loss of topsoil and possible exposure of subsoil acidity may cause further soil degradation.<br>Plant nutrients to replenish what is yearly taken from the soil to meet the demands for food and fibre amount to 230 million tonnes (Mt). Current fertilizer consumption stands at about 130 Mt of N, P₂O₅,and K₂O, supplemented by an estimated 90 Mt of N from biological nitrogen fixation worldwide. Although 80 per cent of the population lives in the developing world, only half the world''s fertilizer is consumed there. Yet, as much as 50% of the increase in agricultural productivity in the developing world is due to the adoption of fertilizers. World population growth will cause a doubling in these nutrients requirements for the developing world by 2020, which, in the likely case of inadequate production, will need to be met from soil reserves. Because expansion of the cultivable land area is reaching its limits, the reliance on nutrient inputs and their efficient use is bound to grow.<br>With current urban expansion, nutrients in harvested products are increasingly lost from the rural environment as a whole. Estimates of soil nutrient depletion rates for sub-Saharan Africa (SSA) are alarmingly high. The situation may be more favourable in Latin America and Asia where fertilizer inputs are tenfold those of SSA. Closing the nutrient cycle at a community level in rural areas may be tedious; on an inter-regional level it is associated with considerable costs of collection, detoxification and transportation to the farms. Yet, at the rate at which some of the non-renewable resources such as phosphorus and potassium are being exploited, recycling of these nutrients will soon be required. <br>