Flux and sources of nutrients in the Mississippi-Atchafalaya River Basin: Topic 3 Report for the Integrated Assessment on Hypoxia in the Gulf of Mexico.

Ths report addresses the following two questions: 1) What are the loads (flux) of nutrients transported from the Mississippi-Atchafalaya River Basin to the Gulf of Mexico, and where do they come from within the basin? 2) What is the relative importance of specific human activities, such as agriculture, point-source discharges, and atmospheric deposition in contributing to these loads? These questions were addressed by first estimating the flux of nutrients from the Mississippi-Atchafalaya River Basin and about 50 interior basins in the Mississippi River system using measured historical streamflow and water quality data. Annual nutrient inputs and outputs to each basin were estimated using data from the National Agricultural Statistics Service, National Atmospheric Deposition Program, and point-source data provided by the USEPA. Next, a nitrogen mass balance was developed using agricultural statistics, estimates of nutrient cycling in agricultural systems, and a geographic information system. Finally, multiple regression models were developed to estimate the relative contributions of the major input sources to the flux of nitrogen and phosphorus to the Gulf of Mexico.

Accelerating loss of seagrasses across the globe threatens coastal ecosystems

Coastal ecosystems and the services they provide are adversely affected by a wide variety of human activities. In particular, seagrass meadows are negatively affected by impacts accruing from the billion or more people who live within 50 km of them. Seagrass meadows provide important ecosystem services, including an estimated $1.9 trillion per year in the form of nutrient cycling; an order of magnitude enhancement of coral reef fish productivity; a habitat for thousands of fish, bird, and invertebrate species; and a major food source for endangered dugong, manatee, and green turtle. Although individual impacts from coastal development, degraded water quality, and climate change have been documented, there has been no quantitative global assessment of seagrass loss until now. Our comprehensive global assessment of 215 studies found that seagrasses have been disappearing at a rate of 110 square kilometers per year since 1980 and that 29% of the known areal extent has disappeared since seagrass areas were initially recorded in 1879. Furthermore, rates of decline have accelerated from a median of 0.9% per year before 1940 to 7% per year since 1990. Seagrass loss rates are comparable to those reported for mangroves, coral reefs, and tropical rainforests and place seagrass meadows among the most threatened ecosystems on earth.

温带灌木生态系统的动态特征--生物量和元素循环

本文通过对北京郊区的一个经皆伐以后，自然发育二十多年的次生灌木生态系统的定量研究，结果如下： 1）该生态系统年中最高生物量可达20.30 t/ha，但没有明显的年净增加，从而推出该系统可能进入一种比较稳定的平衡状态，生物量最高出现于秋季（生长季末）;最低为春季（生长季始），这主要是由于从秋季到春季经历了凋落和休眠的过程。另外，灌木的地下部分生物量与地上之比接近1，这也是对灌木生长发育特征的反映。 2）植物各个部位--侧根，主根，主枝，侧枝，叶---有不同的烧失量，但三种植物几乎有相似的顺序，即：主枝>侧枝><主根>侧根>叶（荆条的叶与侧根有相反的顺序）。烧失量反映了有机物质在植物各个部位的含量。 3）十种元素（N，K，Ca，Mg，Na，Cu，Zn，Fe，Al，Mn）在同一种植物，同种元素在不同植物，植物的不同部位，都有不同的含量，并且随着季节的变化而变化。 4）降水中所含的元素是生态系统营养的重要来源，尤其是一些大量元素如K, Na, Ca, Mg等。一般地冠流中的元素含量要高于降水中的，冠流中元素浓度与降水中的比值，不同的元素是不相同的，其中K为2-7倍，Na为1-3倍，Ca, Mg为1-2倍，对同一元素，比值的大小降水的时间有一定的关系，也即有时间性的变化。 5）土壤的水分含量不仅由于雨季和旱季而发生变化，还随土壤的不同的而异，而这种变化又随着季节性而不同。 6）营养元素输入--输出预算表明，各个元素基本上没有明显的存留，甚至有微量的亏损，但仍可以判断，该生态系统基本上处于一种较稳定的平衡状态。

森林生态系统的养分循环-一个温带落叶阔叶林生态系统的研究

l、有机质和全N在草甸土壤的不同层次之间呈现明显的差异，表现力随着土壤深度的增加，含量逐渐降低。无机N包括NH4+-N和No3--N在土层之闻的差异并没有象全N和有机质那么显著。NH4+-在表面30Cm的土壤中明显高于NO3--N的。全P在各层土壤中的含量差异并不显著，但有效p在三层土壤中表现出明显的差异，表现为随土壤深度的增加而降低。 K、Na、Ca、Mg、Fe和AI等6种金属元素的可交换成分在革甸土壤中的含量除K表现出明显的土层间的差异外，在表层30cm的土壤中并没有明显的随土壤深度变化的趋势。 有机质和全N在东灵山地区主要森林土壤中的含量以0~lOcm土层中的显著高于10~20cm的土层中的。20cm的土层中无机N中也以NH4+-为主，这与草甸土壤中的一致。全p和有效P在两个土层之间的差异并不十分显著，而以0^lOcm土层略高于10～20Cm土层的。 K、Na、Ca、Mg、Fe和AI等6种金属元素的可交换成分在不同土层间的差异以K和Ca较为明显，K和Ca在O—1Ocm的土层中要高于lO-20cm的。 森林土壤中的有机质、全N（包括NH4+-N）、全p（包括有效P)都表现为低于亚高山草甸土壤中的，主要原因是亚高山革甸分布于海拔1800cm至2300m，而主要森林类型则基本分布在海拔120m至1500m，亚高山草甸较为恶劣的气候条件明显不利于有机质的矿化，因而分解速率较低，积聚了较多的有机质．而森林土壤中较低的NH4+-N和有效P则可能是由于森林中旺盛的生命活动，尤其是微生物的活动，而大量被植物和微生物固持，因而，即使在森林土壤中有较高的矿化速率，但仍具有较低的NH4+-N和有效p的含量． 不同类型的森林土壤之间各化学成分并没有发现有明显的变化趋势，即使森林类型差异较大的落叶阔叶林和针叶林之间也并没有发现十分显著的差异，这说明各森林类型土壤之间养分特征的一致性。两种针叶林均为人工林，林龄不超过30，而在这之前推测也是以落叶阔叶林为主，森林土壤在这30年间并没有发生十分明显的变化。 在l100m至I500m之间的各种森林类型的土壤也没有表现出十分明显的与海拔高度的相关性。同一森林土壤在不同时间的采样之间，各化学成分也没有表现出明显的差异。 2、降水引起的树干茎流水分中全N的含量在降水季节的初期的含量略高于大量降水期间的。而在降水季节后期，随着每次降雨量的减少，降水间隔时间的增加，树干茎流中N的含量明显地有很大幅度的升高。NO3-N在树干茎流中的含量也同样受到了降水量的影响，表现在后期也发生显著的升高，但升高的幅度没有全N的大。受到降水量影响的元素还有S。 全p在树干茎流水分中含量随降水时间的变化，在各个树种之间有很大的差异。 其它几种元素的可交换态在茎流水分中的含量以K的含量为最高;其次是S、ca、Mg，AI在所有分析的元素中含量最低。不过，AI在降水初期(6月22日)的取样中，含量在几个树种的茎流水分样品中普遍较高，Ca和Mg也被发现有类似的情形。 穿透雨中全N的含量在降水初期略高于降水中期的，而至降水末期时又略有升高，这种格局与树干茎流水分中的具有一致性。全P、K、Ca、Mg、S．ＡＩ等包括全N及其无视成分与树干茎流中的含量的差异并不显著． 地表径流中的全N含量在去除枯枝落叶层的径流场的变化格局与树干茎流和穿透雨中的较为一致．表明这三者之间存在一定的相关性．但与未去除枯枝落叶层的径流场的径流水分中全N和NO３－Ｎ的含量并不十分一致，全N和NO３－N的含量有时较高． 取自马牙石沟流水堰口的集水区水样中全N和NO３-N的含量均变化在l～3ｍｇ／L之间;而取自南沟流水堰口的集水区水样中的全N和N03-N的含量均在l～2mg／L之间，但在这两者之间并没有十分显著的差异，说明取自两个集水区溪流水分中的全N和N03-N的含量基本一致。 3、通过对三个森林立地乔木层生物量的两次调查（相隔6年），发现尽管以辽东栎为主要优势树种的暖温带落叶阔叶混交林（91- 03）第一次调查的生物量低于辽东栋林（91 - 02）和桦木林（91 - 04)的，但在生长6年后，该立地的乔木层生物量已明显超过桦木林的，其增长速率在三个样地中为最高。 根据两次调查的结果，三个样地中出现的11种乔木树种胸径的增加可以分成两组，第一组包括北京花楸、糠椴、白桦和辽东栎，另一组则由山杨、五角枫、棘皮桦、大叶白蜡、蒙椴、黄花柳和沙涞组成。6年中，第一组树种的胸径增加量在1.O～l.4em之间，而第二组的增量在0.2~O.9cm之间，两者之间具有显著的差异。 常用的生物量预测模型包括两个因子，即胸径(D)和树高(H)。D通常可以实测得到，但H大部分只能估计得到。本研究通过比较6年前后两次树高的实际估测结果，证明用D和H共同建立的模型预测结果可能会产生较大的人为误差，建议改用D的单因子预测模型。 无论是实测结果还是树木年轮分析结果，都表明处于目前径级水平的暖温带地区分布的这几个树种还处在不断生长的过程中，随着年龄的增加，表现为胸径还有很大程度的增加，因为这些树种目前的大径级个体的年平均增加速率大于小径级的． 树木年龄与胸径的相互关系的分析结果表明，树木年龄和胸径可以很好地用饱和模型Y=a-be－ｃｘ来拟合． 4、通过近5年对辽东栎枝条( D<0.5cm)和叶片凋落物分解的观察和分析，发现辽东栎枝条的总失重率达到了43%，分解速率常数k为2.713x10－3／周，而叶的总失重率则可以达到70%，分解速率常数k为6.234xl0-3/周. 枝条分解过程中的有机质含量变化可以分为三种类型，一种是单调上升型的，如蛋白质，其含量从3.5%增加到约6%;-种是单调下降型的，如半纤维素，约从15%降低至7%;另一种则是相对变化不大，如粗纤维（包括纤维素和木质素），粗纤维的含量变化在58％±3%，木质素变化在56%±2.5%，纤维素则变化在1%～3%之间。 用Olson指数方程拟合，结果表明粗纤维、木质素和半纤维素三者的分解以半纤维素为最快，分解速率常数为5.693xl0-3／周，其次是木质素和粗纤维，分别为2.461x10-3/周和2.352xl0-3／周．而蛋白质和纤维素的拟合结果较差或根本无法拟合． 用Olsoｎ指数方程拟合的结果表明，有些元素在凋落物分解过程中可以很好地用该方程拟合，如K，Na、Mn和C，p和N，Mg，Zn，而一些元素如Ca和Cu没有取得很好的拟合效果。 几种元素在叶片凋落物分解过程过程的丢失速率也以K为最快，其它元素的顺序为，e，N，p，Na，Mn，Mg和Ca（Ca的拟合效果较差），而Cu、Zn也不能很好地用Olson指数方程拟合。 5、根据对东灵山地区6年(199l~1997)的气象观测结果，可得到该地区的年平均降水量和总降水量，用1994年分析的降水中养分含量的数据可以近似计算得东灵山地区每年通过降水进入该暖温带落叶阔叶林生态系统的几种养分输入量。同理可以计算降水输入养分在树干茎流和穿透雨中的分配，还可以计算养分从地表径流中的输出。通过对这几个水分循环的主要环节中养分输入或输出量的计算，发现每年通过降水而进入系统的养分，大部分将积累在系统中，而输出份额只占很小的一部分。 K和Mg两种养分元素在降水通过林冠和树干表面时，将产生大量的淋溶，而Ca的淋溶较小．N、P和AI则产生少量的吸附或吸收。对于S来说，淋溶和吸收或吸附作用相当，或两者都很小。 通过生物量的年平均增量和生物量中的养分含量可以计算得到每年积累在生物量中的养分量即存留量，同理可以计算年凋落物中的养分量、归还量及生物系统从土壤中吸收的养分量，每年养分的存留率．通过以上计算，发现该落叶阔叶林对养分的存留率较低，这可能是由于该落叶阔叶林森林生态系统每年具有较高的养分归还量，对于一些元素来说，还具有较高的淋溶量，尤其是K和Mg．

森林生态系统中养分循环特征的比较研究

　通过研究都江堰地区三个不同林型下（般若寺亚热带常绿阔叶林、龙池杉木林、月亮湾楠木林）土壤氮素分布的异质性及其矿化动态、凋落物的分解，得出以下结论： 　　1. 在野外用顶盖埋管法培养土壤，测定土壤中的速效氮含量变化，我们发现，尽管铵态氮含量在三种林型下都大于硝态氮含量，但只有在龙池杉木纯林下净氨化速率和净硝化速率基本持平，其它两种林型下，净硝化速率都远远大于净氨化速率。净硝化速率的增强，暗示着土壤的退化程度的加剧。 　　2. 净氨化速率和净氮矿化速率在三种林型下均和土壤温度呈现一定程度的负相关，其中净氨化速率在龙池杉木纯林下和土壤温度达到了显著的负相关。而硝化速率在三种林型下均和土壤温度呈一定程度的正相关。这说明，虽然温度是影响净硝化速率、净氨化速率和净氮矿化速率的最重要的环境因子之一，但温度是通过影响土壤微生物的种群、数量和活力等来影响上述过程的，而由于生长环境的巨大差异性，温度的影响效果会出现很大的差异。另外，土壤含水量对三种林型下的净硝化速率、净氨化速率和净氮矿化速率也有很大的影响，但均没有达到显著的相关。 　　3. 不同的林型下具有不同物种多样性，而物种多样性会通过凋落物的质量和数量，土壤微生物类群的组成和性质以及植被盖度等角度对森林生态系统的土壤氮素循环产生深刻的影响。生物多样性的丧失会导致土壤无机氮（特别是硝态氮）流失的潜力增加，导致无机氮库的逐渐缩小。速效氮含量迅速降低。 　　4.铵态氮和硝态氮共同组成了土壤无机氮的绝大部分。但由于硝态氮易于淋溶, 从地表径流中流失，易被植物吸收，也可能通过反硝化损失掉，因此硝态氮的含量常常表现出较大的波动性，而且硝态氮的含量要远低于铵态氮的含量。但硝态氮占总速效氮的比例在不同的研究地点和时间上有很大的差别。 　　5 通过地统计学的变异函数和时间序列分析，我们发现，全氮和铵态氮在整个研究区域的异质性很大，并且异质性随着时间的推移发生了很大的变化，其中全氮和铵态氮的自相关尺度变化不大，但空间自相关度随着时间的推移变化明显，这说明，随着时间的推进，全氮和铵态氮的空间格局在大尺度上的变化很小，在小尺度的却发生了很大的变化。本研究还发现，对于全氮和铵态氮的空间异质性格局进行地统计学分析时，最小取样间隔应小于5米，并且铵态氮由于其自身的不稳定性，其在小尺度的空间异质性格局更明显，而其取样间隔应小于全氮的取样间隔。 　　6. 应用网袋法进行凋落物分解的实验，发现混合凋落物的分解速率在第一年就比按各组分混合比例计算的理论值更低。说明在本实验中几种凋落物——黄牛奶树、青冈栎、栲树和润楠的混合对分解没有促进作用。 　　7. 土壤湿度和凋落物干物质分解密切相关，而不同林地的温度差异对干物质分解影响不大。但对于具体元素（本文中的C和N）的分解而言，分解受更复杂的机制调节，其中可能包括不同林型土壤中的分解微生物群落以及土壤理化性质的差异，相比之下，土壤湿度影响就不重要了。 　　8. 初始凋落物中的C/N浓度的比值显著影响分解速率，和腐解率呈显著负相关。因此可以用它来预测分解。在N的分解中，初始凋落物中的N浓度也会影响分解，具体反映在初始N浓度和实验截止时的N浓度成正比。 　　9. 亚热带气候下，凋落物的分解比在暖温带分解要快，并且初始凋落物中N元素的含量普遍较高，因而在分解中没有出现大量富集。 　　10.凋落物质量本身分解较快的树种，有机质的分解并没有相应快，说明在凋落物干物质降解过程中占主要地位的不是有机质。

落叶松人工林养分循环与养分利用效率研究

通过对抚顺市温道林场20、53和69年生长白落叶松（Larix olgensis）人工林生物量和营养元素的积累与分配、养分利用效率和养分再吸收效率、养分生物循环的研究，探讨了长白落叶松生长发育不同阶段的养分生态学特征；对东北林业大学帽儿山实验林场17年生兴安落叶松（Larix gmelinii）人工林进行5年的施肥（NH4NO3，15 g•m-2•a-1），研究了施肥对人工林养分生物循环的影响。结果表明： （1）20、53和69年生单株落叶松生物量分别为33.14 kg•tree-1、311.42 kg•tree-1和408.46 kg•tree-1，随林龄的增长而增加。各器官生物量的分配格局为：树干>根>树枝>树皮>针叶。树干生物量的分配比例为50.16%~69.20%，随林龄的增长比例增大，而其他器官生物量的分配比例则逐渐减小。20、53和69年生单株落叶松净生产力分别为3.04 kg•tree-1•a-1、9.68 kg•tree-1•a-1和10.21 kg•tree-1•a-1，随林龄的增长而增大。针叶和树干的净生产力最大，分别占整株林木净生产力的40.07%~47.93%和27.32%~40.97%，并且随林龄的增长而增大。树枝、树皮和根的净生产力则表现出随林龄的增长呈抛物线状。 （2）20、53和69年生单株落叶松N、P、K、Ca、Mg等5种营养元素的总贮量分别为308.14 g•tree-1、2021.01 g•tree-1和2485.24 g•tree-1，随林龄的增长而增加。5种营养元素的贮量大小为：Ca>N>K>Mg>P。树干养分贮量的分配比例为19.74%~34.23%，随林龄的增长呈抛物线状。针叶、树枝和树皮的养分贮量占整株林木养分贮量的比例为35.16%~45.59%，建议在采伐木材时实施去皮、打枝等措施，留下针叶、树枝和树皮在林地中，让其自然分解以使营养元素重新归还利用，对于维持林地的养分平衡和长期生产力具有积极作用。 （3）20、53和69年生单株落叶松年吸收养分量分别为35.31 g•tree-1•a-1、97.83 g•tree-1•a-1和100.08 g•tree-1•a-1，随林龄的增长而增加。5种营养元素的年吸收量大小为：Ca>N>K>Mg>P。落叶松的养分利用效率随林龄的增长而增大，但生长到一定年龄阶段后，其养分利用效率逐渐趋于稳定。落叶松的最佳采伐年龄应为养分利用效率保持稳定时的年龄，此时采伐单位干材所带走的林地养分量较少。不同营养元素的利用效率不同，P的利用效率最高，Mg、K次之，N、Ca最低。不同器官的养分利用效率不同，树干的养分利用效率最高，其次是根、树枝、树皮，针叶最低。随着林龄的增长，树干和根的养分利用效率增大，而树枝和树皮的养分利用效率减小。 （4）落叶松叶片的N再吸收效率为50.76%~55.11%，随林龄的增长表现出增大的趋势；P和K再吸收效率分别为64.38%~68.85%和87.85%~90.62%，随林龄的增长表现出减小的趋势。从养分利用效率和养分再吸收效率综合判断，本研究区落叶松生长可能受土壤N、P、K供应的限制，3种营养元素的限制作用大小为：K>P>N。 （5）落叶松人工林养分的年吸收量、年存留量和年归还量分别为51.94~78.35 kg•hm-2•a-1、17.77~29.43 kg•hm-2•a-1和34.18~48.92 kg•hm-2•a-1，均随林龄的增长而减少，这与林分密度逐渐减小有关。5种营养元素的年吸收量和年存留量大小均为：Ca>N>K>Mg>P，年归还量大小为：Ca>N>Mg>K>P。落叶松人工林的养分循环速率为0.624~0.658，随林龄的增长而增大。5种营养元素的循环速率以Mg、N最快，Ca、P次之，K最慢。K的循环速率较低，可能与研究区土壤K含量较低而表现出的K再吸收效率较高有关。 （6）施肥导致落叶松叶片N再吸收效率显著降低，而凋落叶片的N浓度显著增加，从而使凋落叶片的C/N比由80.29降低到60.29。施肥林地凋落叶片C/N比的降低使其分解速率加快，有利于其养分归还土壤，从而加快了系统的养分循环速率，提高了系统的养分利用率。因此，在人工林经营中，施肥不仅能提高林地生产力，而且对于维持林地养分循环具有积极作用。

花椒主效化感物质分离鉴定及化感作用研究

近年来，随着对作物重茬障碍原因的深入研究，植物的化感作用越来越受到国内外众多学者的重视。花椒（Zanthoxy piperitum.）为芸香科植物，是一种收益早、用途广、价值高的经济树种，是川西干旱河谷地区的重要经济作物，其连作障碍也倍受关注，系统研究花椒化感作用将有助于理解和最终解决花椒连作障碍问题。本文首先通过萃取、层析等方法分离花椒主效化感成分；通过外加不同浓度的花椒叶水浸液研究了对土壤氮素养分循环的影响；研究了花椒叶水浸液对苜蓿生理生化、光合作用、氮素养分吸收的影响，并对外施氮肥对这种化感影响的缓解作用做了研究；研究了花椒化感潜力对全球变化——UV-B增强辐射的响应。主要研究结果如下： 1．用不同极性的有机溶剂对花椒叶水浸液浓缩浸膏萃取、柱层析，结合生物活性检测，分离得到主效化感作用组分的一种化感物质——对甲氧基苯酚。采用该物质纯品进行生物活性检测，证明其具有化感作用。 2．花椒叶水浸液处理土壤30天后，土壤硝态氮、铵态氮、无机氮（硝态氮＋铵态氮）与对照相比，随着花椒叶水浸液浓度的增加呈现降低的趋势，其中土壤铵态氮含量显著降低，而硝态氮含量的变化则不显著，无机氮含量也显著降低。土壤脲酶和蛋白酶的活性与无机氮含量的变化趋势相同。随着花椒叶水浸液浓度的增加，氨化细菌数量显著降低，固氮菌的数量变化不显著，硝化细菌和反硝化细菌数量有减少的趋势。60天后，硝态氮含量、铵态氮含量、无机氮随水浸液浓度增加的变化趋势与30天时相似；随着花椒叶水浸液浓度的增加，氨化细菌、固氮菌的数量显著减少，硝化细菌数量、反硝化细菌数量仍呈减少趋势；土壤脲酶、蛋白酶活性与第30天的变化趋势相同。第60天与第30天的结果相比，相同水浸液浓度处理的硝态氮、铵态氮、无机氮均有下降的趋势，但除了25g.L－1水浸液处理的外，其它相同浓度的处理间差异均不显著；除了12.5 g.L的处理外土壤脲酶活性均呈增强的趋势；蛋白酶活性都有不同程度的增加；花椒叶水浸液处理的土壤硝化细菌和反硝化细菌数量呈增加趋势。 3．随着花椒叶水浸液浓度的增加，显著抑制了苜蓿根长、地上地下生物量、叶绿素含量、叶片中可溶性蛋白的含量，净光合速率。苜蓿体内四种抗氧化酶（POD、SOD、CAT、APX） 活性随着水浸液浓度的增加而降低，而丙二醛含量则增加。苜蓿氮初级同化相关酶硝酸还原酶（NR）、谷氨酰合成酶(GS)、谷氨酸脱氢酶（GDH）的活性随着水浸液浓度的增加受到不同程度的影响。总的来说，苜蓿硝酸还原酶、谷氨酰合成酶的活性受到抑制，而谷氨酸脱氢酶活性的变化则比较复杂，根呈先降低后增加的趋势，叶片则无显著变化。外施两种不同浓度的硝酸铵氮肥后，对12.5、25 g.L－1花椒叶水浸液处理的苜蓿化感作用有显著的缓解作用，表现在株高、生物量、光合作用等方面，大多达到与对照（0 g.L－1）未施氮肥无显著差异的水平，而对50 g.L－1水浸液处理的苜蓿幼苗，虽有一定的缓解作用，但这种作用均未达到与对照（0 g.L－1）未施氮肥时无显著差异的水平。 4． UV-B增强辐射处理花椒后，花椒的化感潜力显著增强。花椒叶片内UV-B吸收物质的含量和总酚含量均显著增加。 In recent years, with profound research on the reasons of continuous cropping obstacles, allelopathy received increasing attention to many scholars at home and abroad. Zanthoxy bungeanum as a Rutaceae plant is a high economic value species which gains early and uses widely. Zanthoxylum is an important economic crop in the arid valley of western Sichuan region, and its not even has received much concern for the continuous cropping obstacles. The systematic study of allelopathy of Zanthoxylum will contribute to the understanding and final settlement of this issue. The major allelopathic composition was separated through the extraction, chromatography combined with other methods. The impact on soil nutrient cycling was also studied through the addition of different concentrations of water extracts of Zanthoxylum. Furthermore, the effects of water extracts of Zanthoxylum leaves on alfalfa leaf physiological and biochemical indexes, photosynthesis, soil enzymes and nutrient uptake of nitrogen and the mitigation of allelopathy through using external fertilizer were studied to put forward scientific resolvent for Zanthoxylum continuous cropping obstacles .The response of allelopathic potential of Zanthoxylum to global change - UV-B enhanced radiation was studied . The main findings are as follows: 1. Through extraction with different polar organic solvents on concentrated water extract of Zanthoxylum leaf and then using column chromatography combined with detection of biological activity, one of the main allelopathic components- methoxy-phenol was isolated. The biological activity testing of the pure material of methoxy-phenol proved that it does have allelopathic potential. 2. Thirty days after treating soil with water extract of Zanthoxylum leaf, as compared with the control, the contents of soil nitrate, ammonium, nitrate plus ammonium nitrogen showed a trend of decrease with the increase of the concentration of water extract whereas the content of ammonium nitrogen showed a significant reduction, and the content of nitrate did not change significantly, the content of nitrate plus ammonium nitrogen also showed a significant (P <0.05) redction. The activity of soil urease and protease showed the same trend as the content of nitrate nitrogen plus ammonium nitrogen. With the increase in the concentration of water extract, the number of ammonification bacteria significantly reduced but nitrogen-fixing bacteria did not change significantly and there was a decreasing trend in the number of nitrifying bacteria and denitrifying bacteria. Sixty days after the treatment, with the increase in solution concentration of water extract of Zanthoxylum leaf, the content of nitrate、 ammonium nitrogen, nitrate plus ammonium nitrogen showed a similar change trend to 30 days’; the number of ammonification bacteria, nitrogen-fixing bacteria significantly reduced ; the number of nitrifying bacteria, denitrifying bacteria was still an downward trend; the activity of soil urease and protease showed the same trend as the 30th days’. Compared to the results of the 30th days’, the content of nitrate, ammonium, nitrate plus ammonium nitrogen showed a decrease trend between the treatment of same concentration, but there was no significant difference except the treatment of 25g.L-1 between the same concentration; the activity of soil urease showed enhanced trend except the treatment of 12.5 g.L-1; the activity of protease increased to varying degrees; the number of ammonification bacteria、 nitrifying bacteria and denitrifying bacteria were growing while nitrogen-fixing bacteria reduced.. 3. With the increase of the concentration of water extract of Zanthoxylum leaf, the water extract significantly inhibited the root length, aboveground biomass, content of chlorophyll and soluble protein in leaf and net photosynthetic rate. The activity of four antioxidant enzymes (POD, SOD, CAT, APX) reduced with the increase in concentration of the water extract but the content of MDA increased. The activity of enzymes related to primary nitrogen assimilation such nitrate reductase (NR), glutamyl synthetase (GS), glutamate dehydrogenase (GDH) were subject to different degrees with an increase in the concentration of water extracts. In general, the activity of nitrate reductase, glutamyl synthetase were inhibited, while change in the activity of glutamate dehydrogenase was more complex. The activity of glutamate dehydrogenase in leaf was first reduced and then increase,but did not change significantly in root. After using two external different concentrations of nitrogen fertilizer, there was a significant mitigation in inhibiton in plant height, biomass, photosynthesis, etc. in the treatment of 12.5,25 gL-1 of water extract of Zanthoxylum leaf, and most of these indexes showed no significant difference with the control (0 g.L-1, no external fertilizer was added) .Although there showed a certain degree of ease in the treatment of 50 g.L-1 , there was still a significant difference compared with the control (0 gL-1) in which no external fertilizer was used. 4.The allelopathic potential of Zanthoxylum positively responded to enhanced UV-B significantly. The content of UV-B absorbing compounds and the total phenol also significant increased.

氮肥对黄瓜根际土壤线虫群落组成、结构及其多样性的影响

土壤线虫是土壤动物的主要功能类群之一，在土壤养分分解和循环中起到重要的作用。本研究通过施用两种形态氮肥，硝态氮(NO-3–N)和铵态氮(NH+4–N)，对黄瓜整个生长期内根际土壤线虫的群落组成、结构及其多样性等的影响进行了比较研究。为增进土壤健康，提高土壤质量以及合理施用氮肥提供科学的理论依据。研究结果如下： 1. 氮肥处理后，不同浓度NO-3–N处理提高了根际土壤线虫数量，而NH+4–N处理（202.5 kg N/ hm2）抑制了线虫数量的增加。线虫群落结构相对较稳定，营养类群变化不大。且少量优势科/属会对土壤线虫群落特征起着至关重要的作用。 2. 在整个生长季节内，非寄生线虫的群体动态变化与寄生线虫的群体的动态变化具有相反的变化趋势。其中，NO-3–N处理和NH+4–N处理后植物寄生线虫出现频率的变化趋势相近，都是由高到低；非植物寄生线虫出现频率的变化趋势则都是由低到高。这说明非植物寄生线虫数量增长和空间占位对植物寄生线虫群体有一定的抑制作用。另外，也反映了适量氮肥在一定程度上能够减轻植物寄生线虫对黄瓜的危害。 3. 由多样性指数变化可知，NO-3–N和NH+4–N在低肥（67.5 kg N/hm2）和高肥（202.5 kg N/hm2）处理较中肥（135.0 kg N/hm2）处理，更不利于提高土壤线虫多样性地提高和线虫群落的稳定性。中肥不同形态氮肥处理与对照相比，H´指数在初花期和结果期显著增加了土壤线虫的H´指数，说明施入两种形态的氮肥能够提高线虫生物多样性程度。NH+4–N处理在初花期和结果期显著降低了土壤线虫种类的丰富性。土壤线虫生物多样性变化中，H´和SR指数在一定程度上能够反映施用无机氮肥对土壤线虫的多样性的影响，而J指数和λ指数效果不明显。NO-3–N和NH+4–N处理相比较，NO-3–N处理对黄瓜土壤线虫的多样性指数影响更大，促进了土壤线虫群体的多样化和种类的丰富度，更有利于提高土壤线虫的多样性，增加其稳定性。这些结果表明适量无机氮肥特别是NO-3–N的施用对黄瓜土壤线虫的生物多样性有一定的维护和提高作用。 4. 线虫数量与土壤质量指标的相关分析表明：线虫数量与有关土壤理化生指标，如土壤NO-3–N、NH+4–N、有机质含量等的正相关程度高，与总酚含量等显著负相关；与根际土壤微生物，细菌、真菌、放线菌数量等呈显著正相关。另外，线虫数量与土壤含水量未表现出显著相关关系。 Nematodes play a major role in decomposition and nutrient cycling in soil. Nematode community analyses are useful in assessing soil ecosystem status and function. The effects of two forms of mineral nitrogenous fertilizers (NO-3–N and NH+4–N) on nematode community composition, structure and diversity in rhizosphere of cucumber were investigated during different growing seasons of cucumber. Systematically research of effects of nitrogenous fertilizers could help to obtain better undstanding of a healthy soil and using nitrogenous fertilizers in reason. The main results are as follows: 1. The total numbers of nematode were more abundant in NH+4–N treatments than other teatments. However, NH+4–N teatment（202.5 kg N/hm2）dramatically inhibited it. All the tropic groups in the soil nematode communities were stable, and the dominant family or genus had an important function in the nematode community structure. 2. There was similar trend of the frequency of plant parasitic nematodes between NO-3–N and NH+4–N treatment, the similar trend of the frequency of non-plant parasitic nematodes was also found. But the frequency of plant parasitic nematodes exhibited a contrary trend to that of plant parasitic nematodes after different nitrogenous fertilizer treatments. The results showed that the increasing trend of the frequency and the niche of non-plant parasitic nematodes inhibited the plant parasitic nematodes, and indicated that right chemical fertilizers dosage could abate plant parasitic nematodes harm to cucumber. 3. The changes of the biodiversity index showed that the nitrogen treatment（135.0 kg N/hm2）promoted the stabilization of soil nematode diversity than other nitrogen treatments(67.5 kg N/hm2 and 202.5 kg N/hm2). In the treatment（135.0 kg N/hm2）,The changes in nematode diversity between the control plots and treated plots were compared by the biodiversity index (H´, J, SR, λ). Among these tested index, H´ and SR were effective in reflecting the effects of different nitrogenous fertilizers on the diversity of soil nematodes. In comparison with the NH+4–N treatment, the NO-3–N treatment promoted the stabilization of soil nematode diversity. 4. Correlation coefficients between nematode abundance and soil quality indices indicated that the total numbers of nematode were affected positively by NO-3–N, NH+4–N and the organic matter, and negatively by total phenolic acids; the total num- bers of nematode had positive correlation with bacteria, fungi and actinomycetes nu- mbers. Soil water contents had only a weak negative influence on it.

岷江上游人工针叶、阔叶林土壤可溶性有机物质特征及其对凋落物分解的响应

土壤可溶性有机物质（Dissolved organic matter，DOM）作为土壤有机质的活性组分，在陆地生态系统物质循环中扮演非常重要的角色。土壤DOM的主要成分可溶性有机碳（Dissolved organic carbon，DOC）和氮（Dissolved organic nitrogen，DON）参与C、N循环过程。为深入揭示全球C、N循环过程机制，在未开展DOC和DON的地区进行相关研究是有必要的。森林土壤（包括枯枝落叶层）DOC、DON动态及调控机理的研究是目前国际上森林生态系统C、N循环研究热点之一。本研究立足于暖温带岷江上游茂县地区人工林植被，对土壤DOC和DON的库容量，季节动态及其与其它养分之间的关系进行了系统研究，旨在了解DOC和DON在该区生态系统中的重要作用，并探讨作为DOM主要来源的叶凋落物对DOC和DON的动态影响，研究有助于更加详细地了解该区生态系统C和N循环过程。本论文主要研究结论如下： 1研究了岷江上游地区两大主要土壤类型（棕壤和褐土）不同植物群落下土壤的DOC和DON含量及特征，结果表明：DOC和DON在两种土壤类型中均有库容量存在，DOC在0-10cm和10-20cm土层的含量幅度分别111.96~159.95 mg kg-1和69.02~100.84 mg kg-1。DON在0-10cm和10-20cm土层的含量幅度分别11.88~23.08 mg kg-1和4.70~10.77 mg kg-1。游离氨基酸在0-10cm和10-20cm土层的含量幅度分别0.84~1.66 mg kg-1和0.39~0.73 mg kg-1。DOC、DON与土壤中的一些养分因子表现出了显著的相关关系，共同反映了土壤的状况和质量，在该区开展DOC和DON的系统研究是有必要的。 2 对油松与连香树林地土壤DOC、DON以及其它化学指标的季节动态进行了研究，结果表明：油松与连香树林地土壤DOC和DON的季节动态变化表现了类似的规律，DOC和DON的含量均以秋季最高。DOC和DON的季节动态变化主要受凋落物生物因素的影响，但其微生物活力的生物因素以及降雨、温度等非生物因素也是控制土壤DOC和DON含量的重要因素。土壤DON在土壤中的行为不同于矿质氮，其季节动态不同于NO3--N和NH4+-N的季节动态，在研究N循环过程中，应考虑DON的变化情况。 3 对油松与连香树林地分解层和表层土壤（0-10cm）氨基酸周转动态进行了研究，结果表明：油松林地和连香树林地均以分解层的氨基酸含量高于矿质表层土壤的含量。每个取样时期，油松林地内各层次的氨基酸含量高于连香树林地内相应层次的含量。两林地各层次无机氮含量均超过了氨基酸的含量，并且室内培养30天后无机N的含量仍然高于氨基酸的含量，所以可以认为该区立地条件下无论是在有机分解层还是矿质土层植物吸收利用的氮素仍是以无机N为主。 4 松林下松针凋落物易于累积，这与松针凋落物分解缓慢有关，从而导致松林内养分周转缓慢。通过用不同性质凋落物和灌丛地土壤构建微生态系统，比较油松、辐射松、连香树、灌丛虎榛子凋落物分解对C、N循环过程的影响，结果显示油松和辐射松针叶凋落物比连香树、虎榛子凋落物分解更慢，减缓了养分循环过程。然而将针叶凋落物与阔叶凋落物混合后，油松和辐射松针叶凋落物的分解加快，C、N元素的循环过程也加速。此结果表明在松林内维持具有高质量凋落物的灌丛植被或在松林内栽植一些阔叶树种如连香树对维持和增进松树人工林的土壤肥力有重大的作用。室内培养的结果还显示添加凋落物后土壤DOC和DON的含量显著增加，表明凋落物是土壤DOM的直接来源。然而不同物种凋落物处理下土壤DOC和DON的含量有所不同，并随时间发生改变。混合凋落物处理下土壤DOC和DON的含量均高于松针凋落物单独处理下土壤DOC和DON的含量。DON是一个主要的水溶性N库，随时间的变化趋势与无机N的变化趋势不同，在土壤N循环过程中起到了中间N库的作用。 As a labile fraction of soil organic matter, dissolved organic matter (DOM) plays a very important role in material cycling of terrestrial ecosystem. The turnover of DOM is now being considered as main components in nutrient cycling. DOM mainly includes dissolved organic carbon (DOC), -nitrogen (DON), -phosphorous (DOP) and –sulfur (DOS). Among these constituents, DOC and DON directly participate in C and N cycling. It is essential to study DOC and DON dynamics and their controlling factors in the areas where no related study has ever been carried out. Study about them can provide data supports on understanding the mechanism of the global C and N cycling. DOC and DON dynamics and their controlling factors have been focused on in the research of C and N cycling of forest ecosystems. Based on forest plantations of Maoxian, Minjiang River in warm temperate zone, soil DOC and DON pool size, their seasonal dynamics, and the correlation between DOC, DON and other nutrients were studied in order to understand the importance of DOC and DON in the study area. Soil DOC and DON dynamics induced by leaf litter decomposition were also studied. The study contributed to comprehensively understanding C and N cycling processes and providing baseline data for including DOC and DON into the indices system of evaluating nutrient conditions. The results were as follows: 1 Several different plant communities under brown soil and Cinnamon soil were chosen as sampling plots. The contents and features of soil DOC and DON were evaluated. The results showed that DOC and DON were present under the two soil types. DOC contents in the top soil (0-10 cm) and the subsoil (10-20 cm) respectively varied from 111.96 mg kg-1to 159.95 mg kg-1, and 69.02 mg kg-1 to 100.84 mg kg-1. DON contents in the top soil (0-10 cm) and the subsoil (10-20 cm) respectively varied from 11.88 mg kg-1to 23.08 mg kg-1, and 4.70 mg kg-1 to 10.77 mg kg-1. Free amino acid contents in the top soil (0-10 cm) and the subsoil (10-20 cm) respectively varied from 0.84 mg kg-1to 1.66 mg kg-1, and 0.39 mg kg-1 to 0.73 mg kg-1. Significant correlations were found between DOC, DON and some nutrient indices, which together reflected soil condition and quality. It was hence essential to study DOC and DON in the study area. 2 Seasonal dynamics of DOC, DON, inorganic N, microbial biomass C and N were studied under Pinus tabulaeformis and Cercidiphyllum japonicum plantation. The results indicated that seasonal dynamics of soil DOC and DON under the two plantations performed similar change pattern, with the highest values in autumn. The seasonal dynamics of soil DOC and DON were mainly influenced by the litterfall. However, biotic factors such as soil microbial activities and abiotic factors such as precipitation and temperature also controlled the dynamics of soil DOC and DON. The seasonal dynamic of DON was different from that of NO3--N and NH4+-N, which showed that the behavioral differences between DON and inorganic nitrogen. And hence, it was proposed to include DON into soil N cycling in the study area. 3 Amino acid dynamics in Oa and topsoil (0-10 cm) under P. tabulaeformis and C. japonicum plantation were studied. The results showed that amino acid content in Oa was significantly higher than that in mineral soil. At each sampling time, significantly higher amino acid contents were found in P. tabulaeformis plantation than in C. japonicum plantation. The content of inorganic nitrogen was much higher than the content of amino acid in each sampling layer at each sampling time. After a 30-days laboratory incubation the content of amino acid was still lower than the content of inorganic nitrogen. The results implicated that the form of N absorbed by plants in these study sites were mainly inorganic nitrogen. 4 Usually needle litter is more resistant to decomposition, which leads to needle litter accumulation in pure coniferous stands and slows down the rate of nutrient circulation. By constructing microcosms with local shrubland soil and containing the four single-species (P. tabulaeformis, P. radiata, C. japonicum, Ostryopsis davidiana) litters, the decomposition rates and related C and N dynamics of needle litters and broadleaved litters during the early stage were compared. The results showed that the decomposition rates of pine needles were lower than those of broadleaved litters, which descended C and N cycling processes. However, the presence of C. japonicum or O. davidiana litter into pine needles increased the decomposition rates of pine needles and also dramatically promoted C and N cycling processes. It should be appropriate for plantation managers to consider C. japonicum as an ameliorative species or remain O. davidiana in pine plantations to improve soil conditions and help maintain soil fertility. The laboratory incubation still showed that DOC and DON contents in all litter-amended treatments were significantly higher than no litter-amended treatment, which proved that litter could be a direct source of DOM in soils. Different species litters induced different soil DOC and DON contents, which correspondingly changed over time. DOC and DON contents in mixed litter treatments were higher than those in pine needle litter treatments. As a major soluble N pool, DON developed a different changing pattern over time compared with inorganic N and played a role of interim N pool in soil N cycling.

A Global Crisis for Seagrass Ecosystems

Seagrasses, marine flowering plants, have a long evolutionary history but are now challenged with rapid environmental changes as a result of coastal human population pressures. Seagrasses provide key ecological services, including organic carbon production and export, nutrient cycling, sediment stabilization, enhanced biodiversity, and trophic transfers to adjacent habitats in tropical and temperate regions. They also serve as “coastal canaries,” global biological sentinels of increasing anthropogenic influences in coastal ecosystems, with large-scale losses reported worldwide. Multiple stressors, including sediment and nutrient runoff, physical disturbance, invasive species, disease, commercial fishing practices, aquaculture, overgrazing, algal blooms, and global warming, cause seagrass declines at scales of square meters to hundreds of square kilometers. Reported seagrass losses have led to increased awareness of the need for seagrass protection, monitoring, management, and restoration. However, seagrass science, which has rapidly grown, is disconnected from public awareness of seagrasses, which has lagged behind awareness of other coastal ecosystems. There is a critical need for a targeted global conservation effort that includes a reduction of watershed nutrient and sediment inputs to seagrass habitats and a targeted educational program informing regulators and the public of the value of seagrass meadows.

黄土丘陵区梯田谷子养分循环特征与生产力关系的研究

以新修梯田7年长期肥料定位试验为依据,研究了不同施肥条件下谷子各部位生物量、养分携出量、养分平衡以及耕层土壤养分时空变化。结果表明,有机肥与N、P肥配合施用可提高谷子的籽粒产量和生物产量。养分携出量的大小顺序为籽粒>叶>糠秕>茎,为同类地区农业生产及生态环境建设提供科学依据。