黄河三角洲柽柳植株周围土壤盐分离子的分布

为探讨柽柳的盐分富集效应及其对不同盐分离子分布的影响,以黄河三角洲盐碱地柽柳为研究对象,分析了离植株不同距离不同土层中的盐分离子组成、含量、离子比及不同离子之间的相关性。研究结果表明:各土层阳离子中Na~+含量最高,其次是Ca~(2+)和Mg~(2+),K~(+)最低,Cl~(-)在阴离子中的含量最高,SO_4~(2-)次之,HCO_3~-最低,而未检测到CO_3~(2-)。在柽柳植株周围,尤其是表层土壤中,离植株越近盐分含量越高,显示出柽柳对盐分的富集效应,其中对不同阳离子的富集程度表现为K~+Na~+Mg~(2+)Ca~(2+),而对阴离子的富集程度表现为HCO_3~-Cl~-SO_4~(2-)。冠层下凋落物中盐分的释放和树干径流可能是导致盐分在柽柳植株周围水平方向上存在差异的主要原因。土壤总可溶性盐含量随着土层的加深而升高。阳离子和阴离子向下迁移程度分别表现为Na~+Mg~(2+)Ca~(2+)K+和Cl~-SO_4~(2-)≈HCO_3~-,因而随土层加深而升高的Na~+、Ca~(2+)、Mg~(2+)和Cl~-,显示出底聚特征,而K+、SO_4~(2-)和HCO_3~-含量则随着土层的加深而降低,具有表聚特征。降水淋溶、盐分离子迁移速率的差别和各土层中不同生物量根系对盐分吸收的差异可能是造成盐分在垂直方向上含量变化的主要因素。     

盐胁迫下外源褪黑素和Ca~(2+)对甜瓜幼苗的缓解效应

以甜瓜品种‘羊角酥瓜’为试材,利用人工气候室控制环境条件(昼/夜25/18℃),研究盐胁迫条件下外源褪黑素(MT)和Ca~(2+)对甜瓜幼苗根系和叶片中Cl~-、Na~+、K~+、Mg~(2+)、Ca~(2+)离子含量,Na~+/K~+、Na~+/Ca~(2+)、Na~+/Mg~(2+)值,以及H~+-ATP酶活性、渗透调节物质积累和细胞膜质过氧化的影响.结果表明:与对照相比,盐胁迫处理显著抑制甜瓜幼苗生长,增加根系和叶片中Cl-、Na~+含量,降低K~+、Mg~(2+)、Ca~(2+)含量.盐胁迫下,喷施外源MT或Ca~(2+)处理均可以显著降低甜瓜根系和叶片中Cl~-、Na~+含量,提高K~+、Mg~(2+)、Ca~(2+)含量,植株体内Na~+/K~+、Na~+/Ca~(2+)和Na~+/Mg~(2+)值下降;同时也提高了根系和叶片H~+-ATP酶活性及叶片渗透调节物质的含量,降低盐胁迫对细胞膜的伤害,表现在甜瓜叶片相对电导率和丙二醛含量降低.总之,在盐胁迫条件下,外源MT、Ca~(2+)单独和复配处理均可通过提高H~+-ATP酶活性来降低盐害离子的含量,改善甜瓜幼苗中的离子平衡,同时增加渗透调节物质的含量,降低膜质过氧化水平,从而增强其对盐胁迫的适应性,其中MT和Ca~(2+)复配处理时的效果更好.复配外施MT和Ca~(2+)在诱导甜瓜幼苗提高耐盐方面具有协同增效作用.     

盘锦红海滩湿地沉积物常量元素化学成分调查

为了探究翅碱蓬死亡原因,开展了对红海滩湿地沉积物中常量化学成分研究。实验结果表明,Ca~(2+)、Mg~(2+)、Cl~-、HCO_3~-含量随着沉积物深度的增加而逐渐降低,分析可能是由于海水在沉积物表面蒸发导致的盐分积累所致。Ca~(2+)、Mg~(2+)、Cl~-由河口下游向河口上游方向均出现了不同程度降低的变化趋势;4月份沉积物中镁钙比从河口下游向河口上游显著下降,5月份则没有显著的变化规律。沉积物中5月份的含盐量与4月份相比有上升趋势,沉积物中Ca~(2+)、Mg~(2+)、Cl~-含量也有相同变化趋势。沉积物中Cl~-的变化趋势与含盐量的变化趋势相同,呈现正相关关系。本研究为红海滩湿地生态修复理论研究提供了基础数据支持。     

不同淋洗水量下胶州湾养殖池塘土壤盐分淋洗规律

针对养殖池塘严重盐渍化现象,为确保土地资源和水资源的有效利用,通过室内土柱试验探讨不同淋洗水量下胶州湾养殖池塘土壤盐分淋洗规律,并确定最佳用水量。结果表明:随着淋洗水量的增加,土壤及其淋滤液的含盐量均以指数形式下降,为兼顾淋洗效果和节约用水,接近1:1的水土比可以达到较好的改良效果;在脱盐过程中,土壤中Ca~(2+)、Mg~(2+)、K~+、Na~+、Cl~-含量均呈下降趋势,SO_4~(2-)含量呈先上升后下降的趋势,CO_3~(2-)、HCO_3~-含量呈上升趋势;淋滤液中各盐离子浓度与土壤各盐离子变化规律类似;土壤各盐离子脱盐率大小大致表现为Cl~-Na~+K~+Ca~(2+)Mg~(2+)SO_4~(2-)HCO_3~-;随着淋洗水量的增加,土壤中离子组成由原来的Cl~-和Na~+为主先转变为以Na~+、K~+和SO_4~(2-)为主,最后转变为Na~+、HCO_3~-和K~+为主。土壤脱盐过程伴随着土壤碱化现象,因此需要对盐渍土脱盐过程中的碱化现象进行进一步研究。     

猪精子体外获能前后离子成分变化

应用扫描电镜和镜射电镜能谱技术,为猪精子获能前后质膜表面和内部的离子成分进行了研究,结果表明,猪精子获能后质膜表面的Na~+和Al~(3+)升高,而Cl~-和Ca~(2+)降低;精子顶体内Na~+和Cl~-降低,Ca~(2+)、K~+和Fe~(2+)升高;中段线粒体内的Na~+、Ca~(2+)和Fe~(2+)升高,而K~+和Cl~-降低。文章分析了精子获能后顶体内Na~+、Cl~-、K~+、Ca~(2+)和Fe~(2+)变化的浓度比和摩尔比。     

九种金属离子对桑椹红色素稳定性影响的研究

本文报道Fe~(2+),Fe~(3+)……Ca~(2+)等9种金属离子对桑椹红色素稳定性影响的研究。结果表明:Fe~(2+),Fe~(2+),Cu~(2+),Zn~(2+)对该色素颜色的稳定性有不利影响;Mg~(2+),Al~(3+),K~+,Na~+,Ca~(2+)等5种金属离子有增强其吸收值的作用,其中Al~(3+)增色作用最为明显,Ca~(2+)护色作用较为突出,但它们的作用都随时间延长而逐渐降低。     

盐胁迫对高丛越橘幼苗生长及离子平衡的影响

以高丛越橘"双迪"2年生扦插苗为材料,在盆栽条件下经0、100、200和300mmol·L~(-1)Na Cl溶液处理40天后,研究了幼苗干物质积累量、叶片受害情况以及矿质离子(Na~+、K~+、Ca~(2+)、Mg~(2+)和Cl~-)含量变化及其在根、茎、叶中积累、运输与分布特征,以揭示其盐适应生理机制,为耐盐越橘品种选育及合理栽培提供依据。结果表明:在低盐(100mmol·L~(-1))处理下总干物质量没有明显降低,在中高盐(200～300 mmol·L~(-1))处理下总干物质量明显降低,盐害指数随盐胁迫的加重而明显增大;在低盐处理下,茎和叶对K~+、茎对Mg~(2+)以及根对Ca~(2+)的吸收保持稳定;在中高盐胁迫下,Na~+和Cl~-在叶中大量积聚,显著降低了根对K~+、Ca~(2+)和Mg~(2+)以及茎和叶对K~+的吸收能力,显著降低了植株从根到叶K~+、Ca~(2+)和Mg~(2+)的整体运输能力,从而破坏了叶的离子平衡,导致离子毒害和生长受阻。     

青海布哈河丰水期水化学特征

运用相关分析、因子分析和富集因子等对布哈河流域2014年丰水期河水样品主要离子浓度特征及来源进行了分析。结果表明:布哈河流域河水p H值的变化范围为7.91~9.21,平均值为8.43;EC的变化范围为133~871μS·cm~(-1),平均值为383μS·cm~(-1);河水中SO_4~(2-)、Ca~(2+)、Cl-、Na~+、 Mg~(2+)、NO3-、K+和NH_4~+的平均离子浓度分别为60.2、33.1、31.1、14.8、12.8、8.1、1.5和0.3μeq·L-1;阳离子浓度的大小顺序为Ca~(2+)Na~+ Mg~(2+)K+NH_4~+,而主要阴离子浓度的大小顺序SO_4~(2-)Cl-NO_3~-; Mg~(2+)、Ca~(2+)和SO_4~(2-)的离子浓度随着海拔的增加呈增加的趋势,Na+、Cl-和NO_3~-随着海拔的增加表现出减小的趋势,但K~+和NH_4~+不随海拔梯度的改变而变化;布哈河全流域的水化学类型为SO_4~(2-)-Ca~(2+)-Cl-- Mg~(2+);布哈河流域的水化学主要受控于蒸发岩和碳酸盐岩风化产物的影响。     

盐渍土壤大果沙枣树主要矿质阳离子的吸收和分配特征

为探明大果沙枣树体矿质离子渗透调节机制,比较分析了盐渍化生境中1～12a生树的根、枝和叶部主要矿质阳离子的吸收、分配特征。结果表明:(1)大果沙枣树体内Ca~(2+)的积累量最高(13.79 g/kg),K~+次之(5.92 g/kg),Na~+最低(1.00 g/kg);随着树龄的增大,大果沙枣根部的Na~+以及枝和叶部的K~+、Ca~(2+)、Mg~(2+)的积累量均逐渐增大,而根部的K~+含量则逐渐减少;高龄段(10～12a)树体根部的Na~+累积量显著(P0.05)高于中低龄(1～9a)段。(2)大果沙枣树体内K~+/Na~+最大(15.36),Mg~(2+)/Na~+次之(12.25),Ca~(2+)/Na~+最小(10.51),根和枝部的K~+/Na~+均随着树龄的增大而降低,叶部则表现相反。(3)土壤中的K~+和Mg~(2+)向根方向、根部K~+、Mg~(2+)和Ca~(2+)向枝方向以及根部的K~+和Mg~(2+)向叶方向的选择运移系数均随着树龄的增大呈直线上升趋势。(4)土壤中Na~+与根部Na~+含量呈极显著正相关关系(0.687,P0.01),与叶部的K~+含量呈显著正相关(0.605,P0.05);土壤中K~+含量与根部的Na~+、叶部的K~+分别呈显著和极显著正相关(0.544,0.676),与根部的Mg~(2+)呈显著负相关关系(-0.499)。研究发现,大果沙枣树生长过程中主要通过根部对Na~+的聚积作用,以及K~+、Mg~(2+)和Ca~(2+)在枝、叶部的吸收积累来维持植物体离子平衡,以适应盐渍土壤环境。     

钙对盐胁迫下冰叶日中花不同器官离子含量和根部K~+、Na~+吸收的影响

以冰叶日中花(Mesembryanthemum crystallinum L.)实生苗为材料,经NaCl、NaCl+ CaCl_2、NaCl+LaCl_3处理后,利用电感耦合等离子发射光谱仪检测叶、茎、根中Na~+、K~+、Ca~(2+)、Mg~(2+)含量,计算K~+/Na~+、Ca~(2+)/Na~+和Mg~(2+)/Na~+比值,利用非损伤微测技术测定根尖Na~+流和K~+流,研究盐胁迫下钙在维持离子平衡中的作用。结果显示,NaCl处理后,冰叶日中花各器官中Na~+含量增加,K~+、Ca~(2+)、Mg~(2+)含量降低,离子比值降低;CaCl_2处理降低了Na~+含量,提高了K~+、Ca~(2+)、Mg~(2+)含量,离子比值升高,而LaCl_3处理后的结果相反。经NaCl处理24 h后,冰叶日中花根尖Na~+和K~+明显外流,加入CaCl_2后,Na~+外流速度显著增加,K~+外流速度受到抑制,而加入LaCl_3后则降低了Na~+的外流速度,促进了K~+的外流。研究结果表明冰叶日中花受到盐胁迫后,钙参与了促进根部Na~+外排、抑制K~+外流的过程,进而保持各器官中较低的Na~+含量,表明钙在维持和调控离子平衡中起到重要作用。     

黄河口湿地柽柳灌丛土壤盐渍化特征

为探究黄河三角洲湿地柽柳灌丛下土壤的盐渍化特征，在黄河三角洲国家级自然保护区(37°35''-12''N，118°33''-119°20''E)黄河入海口附近，根据长势基本一致的原则分别在碱蓬群落、柽柳群落和芦苇群落各选3株柽柳，采集柽柳灌丛下土壤样品，分析土壤盐分和盐碱化参数的空间分布以及距基茎不同距离处研究对象(土壤总盐(TS)、电导率(EC)、pH、交换性钠百分率(ESP))和环境因子(Na⁺、K⁺、Ca²⁺、Mg²⁺、Cl^-、HCO₃^-、SO^2-₄)之间的关系。结果表明：(1)研究区土壤为弱碱化盐土，离子含量由高到低依次为Cl^->Na⁺>SO^2-₄ >Ca²⁺>Mg²⁺>HCO^-₃>K⁺。除pH在土壤表层数值最低外，表层土壤TS、EC、ESP和盐分离子大于深层土壤，显示表聚性。(2)土壤盐分和盐碱化参数空间分布总体为：在柽柳基茎周围形成"盐谷"、"碱谷"效应， Na⁺、Mg²⁺、Cl^-表现为"盐谷"，K⁺ 、SO^2-₄ 、Ca²⁺ 表现为"盐岛"。(3)在整个土壤剖面中，与TS、EC相关性最强的阴阳离子为Mg²⁺、Cl^-，从灌丛中心到灌丛间裸地Ca²⁺、SO^2-₄与TS、EC的相关性逐渐减弱，Mg²⁺、Cl^-与TS、EC的相关性逐渐增强。Ca²⁺和SO^2-₄与pH表现为较强的负相关性；与ESP相关性最强的阴离子为HCO^-₃，与之相关性最强的阳离子为Na⁺和K⁺，并且Na⁺和K⁺与ESP的相关性表现出从灌丛中心向外逐渐增强。(4)土壤盐渍化主要受控于Na⁺，从灌丛下到灌丛间裸地Cl^-对盐渍化程度的影响逐渐增加，SO^2-₄的影响逐渐降低。     

The Occurrence,Sources and Spatial Characteristics of Soil Salt and Assessment of Soil Salinization Risk in Yanqi Basin,Northwest China

In order to evaluate the soil salinization risk of the oases in arid land of northwest China, we chose a typical oasis-the Yanqi basin as the research area. Then, we collected soil samples from the area and made comprehensive assessment for soil salinization risk in this area. The result showed that: (1) In all soil samples, high variation was found for the amount of Ca²⁺ and K⁺, while the other soil salt properties had moderate levels of variation. (2) The land use types and the soil parent material had a significant influence on the amount of salt ions within the soil. (3) Principle component (PC) analysis determined that all the salt ion values, potential of hydrogen (pHs) and ECs fell into four PCs. Among them, PC1 (C1^-, Na⁺, SO₄ ^2-, EC, and pH) and PC2 (Ca²⁺, K⁺, Mg²⁺and total amount of salts) are considered to be mainly influenced by artificial sources, while PC3 and PC4 (CO₃ ^- and HCO₃ ^2-) are mainly influenced by natural sources. (4) From a geo-statistical point of view, it was ascertained that the pH and soil salt ions, such as Ca²⁺, Mg²⁺ and HCO₃ ^-, had a strong spatial dependency. Meanwhile, Na⁺ and Cl^- had only a weak spatial dependency in the soil. (5) Soil salinization indicators suggested that the entire area had a low risk of soil salinization, where the risk was mainly due to anthropogenic activities and climate variation. This study can be considered an early warning of soil salinization and alkalization in the Yanqi basin. It can also provide a reference for environmental protection policies and rational utilization of land resources in the arid region of Xinjiang, northwest China, as well as for other oases of arid regions in the world.     

淋洗与植物作用耦合对盐渍化土壤的改良效应

以甘肃秦王川引大灌区盐渍化土壤为背景,以当地5种耐盐植物为材料,采用根袋法盆栽试验动态研究了淋洗结合植物种植对盐渍化土壤改良的效应。结果表明:与种前相比,单纯的淋洗作用对土壤pH值影响不大,而淋洗结合植物种植明显降低了土壤pH值,且根际土壤pH值小于非根际土壤的,5种耐盐植物中霸王根际土壤pH值降低幅度最大,达0.6个单位。K+、Ca2+、Na+、Mg2+、Cl-和SO2-4在5种植物根际土壤中均有不同程度的富集,富集程度因物种的不同而不同,随培养时间的延长而呈波动状态。5种供试植物和对照组土壤中的6种主要的可溶性盐分离子随淋洗次数和培养时间的延长呈下降趋势。在培养120d后,单纯淋洗的土壤中K+、Ca2+、Na+、Mg2+、Cl-和SO2-4的含量相比种前平均分别降低了33.3%、26.1%、35.6%、32.5%、35.5%和36.3%,植物吸收带走的上述各离子的含量平均分别占种前的46.2%、8.1%、30.2%、7.2%和21.6%,其中霸王吸收带走的盐分离子最多,而淋洗结合种植植物的土壤中上述各离子的含量与种前相比平均分别降低了67.25%、63.73%、83.8%、67.5%、81.55%和78.46%,由此可见,淋洗结合植物种植的脱盐效果优于单纯淋洗,且土壤中主要的盐分离子Na+、Cl-和SO2-4的含量降低幅度最大,通过计算得出,在Cl-、SO2-4和Na+减少的总量中还有37.73%的Na+、38.22%的Cl-和35.14%的SO2-4的减少量是由植物根系的物理化学作用机制引起的。     

Seasonal changes of ionic concentrations in the vacuolar sap of Chara vulgaris L. growing in a brackish water lake

Summary The composition of the vacuolar sap of Chara vulgaris growing in a brackish water lake was estimated weekly over 2 years (1984–1985). The ionic concentrations of the main cations Na⁺, K⁺, Ca²⁺, and Mg²⁺ and the anion Cl^- varied depending on cell age, developmental state, and season. The average of all measurements (in mM) was Na⁺: 35, K⁺: 106, Ca²⁺: 7, Mg²⁺: 23, Cl^-: 101, SO _2- ⁴ : 20, and PO _3- ⁴ : 5. At the onset of growth in May/June the ionic content was lower compared to the mean value for the year, steadily increasing until it reached its maximum above the annual mean in winter. During the period of fructification (sexual reproduction: formation of antheridia and oogonia), when up to 100 mM sucrose was accumulated in the vacuolar sap, ionic content was lowest. This resulted in a fairly constant osmotic potential throughout the year. Mg²⁺ and Ca²⁺ concentrations were correlated with the physiological age of the cells.     

模拟酸沉降对鼎湖山季风常绿阔叶林地表径流水化学特征的影响

通过模拟酸沉降实验,研究了旱季期间(10-3月份)鼎湖山季风常绿阔叶林在4种不同pH模拟酸雨处理(对照、pH 4.0、pH 3.5、pH 3.0)下地表径流水化学输出特征.结果显示:(1)地表径流pH随酸处理强度增强呈“U”型变化模式,酸沉降对地表径流pH的影响不显著(P＞0.05),表明模拟酸沉降尚未引起地表水的酸化.(2)地表径流中NO3-、SO24-浓度随酸处理强度增强略有增加;HCO3-浓度的变化模式与地表径流pH类似.酸根离子浓度与地表径流pH相关性分析表明,SO24-、HCO3-有助于提高地表水抗酸化能力而NO3-则有助于促进地表水酸化.(3)地表径流中盐基离子对酸沉降的响应不尽相同.pH 3.0处理显著提高地表径流中Ca2+、Na+浓度;Mg2+浓度具有随酸处理梯度增强而增加的趋势;K+受模拟酸度的影响小.表明强酸(pH3.0)处理将导致土壤Na+、Ca2+、Mg2+盐基离子流失.(4)酸沉降具有诱发土壤可溶性有机碳(DOC)流失的倾向,增加地表水受有机污染的风险.     

渗透胁迫和离子毒害对转Bt基因棉幼苗生长及离子分布的影响

研究了渗透和盐胁迫处理对转Bt基因抗虫棉(Gossypium hirsutum) 99B种子的萌发和幼苗生长的影响,以及幼苗不同器官离子吸收和分配的差异。结果表明:渗透和盐胁迫均对转Bt基因抗虫棉幼苗的生长有抑制作用,其中PEG的抑制作用最强,而3种盐的抑制程度以CaCl₂>NaCl>Na₂SO₄,且在Na⁺含量相同时,Cl^-的毒害大于SO₄^2-。渗透胁迫下使根、茎和叶中的Na⁺和Cl^-含量提高,K⁺、Ca²⁺、SO₄^2-含量和K⁺/Na⁺、Ca²⁺/Na⁺和SO₄^2-/Cl^-比值降低,且地上部的变化幅度大于地下部的,其中以PEG的影响最为显著,其次是CaCl₂,Na₂SO₄处理最弱。这些说明,转Bt基因抗虫棉99B的耐盐性较弱。     

Nutrient budgets in a dry heathland watershed in northeastern Spain

Dissolved nutrient inputs in bulk precipitation and outputs in streamwater were measured during 3 years of contrasting hydrological conditions in a 6.3-ha, grazed heathland watershed on schists in the Montseny mountains (NE Spain), drained by an intermittent stream. On average, 39% of the precipitation became streamflow. Bulk precipitation delivered positive net alkalinity (mean 0.22 keq/ha/yr), sulphate input was moderate (9.0 kg SO₄-S/ha/yr), and the mean input of inorganic N was not exceptionally high (6.6 kg/ha/yr). Ion concentrations were relatively low in streamwater; SO₄ ^2- was the dominant anion. Most concentrations in streamwater varied seasonally, with maxima in late summer or early autumn and minima in spring. This pattern probably resulted from increased availability of ions for leaching due to decomposition of organic matter and chemical weathering during the warm period. Nitrate concentrations were relatively high in winter and dropped sharply in early spring, probably because of biological uptake. Annual element outputs in streamwater varied between years and seemed to be controlled by both the amount of annual streamflow and its seasonal distribution. Annual inputs exceeded outputs for dissolved inorganic N. The watershed accumulated H⁺ and Ca²⁺, had net losses of Na⁺ and Mg²⁺, and was close to steady state for K⁺, SO₄ ^2-, Cl^- and alkalinity. The chloride budgets gave no evidence of substantial dry deposition in this system. The cationic denudation rate was negative (-0.14 keq/ha/yr) because Ca²⁺ retention was higher than net exports of Na⁺ and Mg²⁺ from silicate weathering. Low nutrient export and little production of alkalinity suggest that this watershed has a low buffering capacity.     

杨树人工林生态系统降水再分配及主要离子特征

大气降水是森林生态系统养分输入的主要途径之一,对养分的生物地球化学循环有着重要的意义。对13年生杨树人工林林外雨、树干流、林内雨和地表径流等水文过程中的养分特征进行了调查分析,旨在了解该生态系统的养分输入与输出规律,为杨树人工林可持续经营提供依据。结果表明,从2013年11月至2014年10月,杨树人工林生态系统林外雨量为1154.1 mm,树干流量仅占大气降水量的2.3%,15.4%的大气降水被杨树人工林的冠层截留;林内雨、树干流与大气降水量(林外雨)的动态变化规律相似。各类降水年加权平均pH值表现为林内雨林外雨树干流;各类降水的离子浓度动态变化规律基本一致,即在降水量较小的11月至次年1月份,各阴阳离子的浓度普遍较高,在降水量较大的2—9月份,阴阳离子浓度普遍较低。SO_4~(2-)-S和Ca~(2+)分别是各类降水中的主要阴离子和阳离子;整体上,树干流的离子浓度林内雨大气降水;林内雨是养分输入的主要形式,通过林内雨输入林地较多的养分离子是Ca~(2+)和K~+,分别为70.83 kg hm~(-2)a~(-1)和63.31 kg hm~(-2)a~(-1);地表径流和土壤渗漏是养分输出的主要形式,输出林地较多的离子是Cl~-和Ca~(2+),分别为196.47 kg hm~(-2)a~(-1)和123.09 kg hm~(-2)a~(-1),其次为SO_4~(2-)-S、Mg~(2+)、Na~+、K~+;NH_4~+-N和NO_3~--N的输出量不足输出离子总量的1%。所以,从水文过程看,杨树人工林生态系统无机氮(NH_4~+-N和NO_3~--N)和K~+表现为净积累,净积累量分别为10.9 kg hm~(-2)a~(-1)和56.4 kg hm~(-2)a~(-1),其他离子表现为净损失,其中Cl~-的净损失量达179.8 kg hm~(-2)a~(-1)左右,其他离子损失量50 kg hm~(-2)a~(-1)。     

The ionic components of the current pulses generated by developing fucoid eggs.

Using a newly developed, extracellular vibrating electrode, we studied the ionic composition of the current pulses which traverse the developing Pelvetia embryo. External Na⁺, Mg²⁺, or SO₄^2?, are not needed for the first 20 min of pulsing. In fact, lowering external Na⁺ or Mg²⁺ (or K⁺) actually stimulates pulsing. Since tracer studies show that Ca²⁺ entry is speeded by Na⁺, Mg²⁺, or K⁺ reduction, these findings suggest that Ca²⁺ entry triggers pulsing. A sevenfold reduction in external Cl^? raises pulse amplitudes by 60%. Moreover, Cl^? is the only major ion with an equilibrium potential near the pulse reversal potential. These facts suggest that Cl^? efflux carries much of the “inward” current. We propose a model for pulsing in which increased Ca²⁺ within the growing tip opens Cl^? channels. The resulting Cl^? efflux slightly depolarizes the membrane and thus drives a balancing amount of K⁺ out. Thus, the pulses release KCl and serve to relieve excess turgor pressure. By letting Ca²⁺ into the growing tip, they should also strengthen the transcytoplasmic electrical field which is postulated to pull growth components toward this tip.     

Long-term and seasonal changes in the chemical composition of precipitation and surface waters of lakes and tarns in the English Lake District

SUMMARY. The composition of bulk (wet and dry) precipitation in 1975 and 1976 was similar to that found 22 years previously. In 1975, mean values for nine precipitation samplers at one site (Wraymires) ranged from pH 4.3 to 4.5; similar values were obtained in 1976. Samplers covered with fine-mesh plastic gauze caught substantially more Ca²⁺ and K⁺ than open samplers, but pH and SO^2-₄+ NO₃^- concentrations were similar in open and covered samplers. In precipitation, c. 50% of H⁺ was balanced by NO₃^- and c. 50% by SOi; 80% of the SO^2-₄ was balanced by Ca²⁺ and Mg²⁺. Conccntrations of major cations (H⁺, Na⁺, K⁺,Ca²⁺, Mg²⁺) and anions (CI^-, NO₃^- SO^2-₄ and alkalinity [Alk—largely HCO₃^-]) in upland water- bodies were similar to those found in precipitation, but pH levels were generally higher and above 6.0 m some tarns. At lower altitudes, on base-rich roeks and soils, Ca²⁺ and Alk become dominant. Results of a survey of lakes and tarns in 1974–78 are compared with a survey in 1953–56 and published data (chiefly for pH and Alk) for 1947–50, 1932 and 1928. Comparisons are also made with other measurements of Alk in three productive lakes (Blelham Tarn, Esthwaite Water and Windermere) for 1936–39 and 1945–80. Winter levels of NO₃-N, PO₄-P and Si are given for these lakes; although the first two have increased during the late 1960s and the 1970s there has been no significant change in the last. NO₃^- and probably some SO^2-₄. In productive lakes a substantial (c. 50%) rise in mean Alk occurred during the late 1960s and the 1970s, possibly related to increased winter levels of NO₃-N and PO₄-P derived from sewage and fertilizers. In this period the maximum pH levels reached in summer were notably high, sometimes exceeding pH 10. The rise in Alk, conductivity and pH of surface waters is influenced by climatic factors (a decade of drier years), sewage input and biological productivity within the lakes. Considerable seasonal fluctuations in the concentrations of major ions, a characteristic feature of surface waters in the English Lake District, are illustrated and some implications for cation-anion balance briefly discussed. Mid-winter concentrations are usually high forNa⁺, K⁺, Cl^-. NO₃^-and low for Ca²⁺, Mg²⁺, Alk. SO^2-₄. Alkalinity. pH and conductivity of Lake District tarns and lakes show no signs of acidification during the period 1928–80. On the contrary, productive lakes have become more alkaline and some unproductive low-alkalinity (< 100 μ-equiv. 1^-1) lakes also show signs of alkalization, with increased mean concentrations of Na⁺. Ca²⁺ and Mg²⁺, balanced by Alk.