湘潭锰矿废弃地栾树人工林微量元素生物循环

对湘潭锰矿废弃地5年生栾树人工林内微量元素的含量、积累、空间分布和生物循环进行了研究。结果表明：土壤中各微量元素含量顺序为：Fe>Mn>Zn>Pb>Ni>Cu>Co>Cd,均低于对照地,但仍未低于湖南省背景值(Fe除外)。枯枝落叶层中,仅Mn和Co从半分解到已分解阶段向土壤中转移,其他元素在分解过程中都出现了不同程度的富集,各元素在不同阶段含量没有显著差异,在分解过程中,Mn元素含量最高且与Cu、Pb、Co、Ni、Cd均存在数量级差异。栾树各组分元素含量顺序为：叶>枝>细根>皮>粗根>大根>根头>干,各元素总含量顺序为：Mn>Fe>Zn>Pb> Cu>Cd>Ni>Co;林分微量元素总贮量为15.272kg/hm_-2,其中干和枝贮存量最高,占总贮存量的54.204%。各器官微量元素贮存量顺序为：枝>干>叶>皮>根头>大根>粗根>细根;林分微量元素吸收量为5.200kg/hm₂.a,存留量为2.504kg/hm₂.a,归还量2.751kg/hm₂.a,总利用系数为2.394,循环系数为3.138,周转期为11.203a。栾树对Mn的吸收能力最强,Fe、Ni的返还系数要高于吸收系数,所有元素的分解系数都高于返还系数。Fe、Mn的迁移系数要高于分解系数,Mn、Zn、Pb、Cd的富集系数要高于其他元素。     

海南岛兴隆地区巴戟天属若干植物的微量元素

本文研究海南兴隆地区巴戟天属4种植物微量元素含量变化特性,结果表明同属异种植物对同一元素的吸收量、变化范围差异悬殊,种间元素含量水平以Mn>Fe>Mg>Al>Zn>Cu为序;同种植物不同器官微量元素的吸收量也各有差别,例如海南巴戟的含量以根(60224×10-6)>叶(36108×10-6)>花(34609×10-6)>茎(32407×10-6)。同属异种植物与土壤中元素含量消长变化关系密切,相比之下,植物中Mn、Fe、和Mg含量均高于Al、Zn、Cu。     

鼎湖山自然保护区不同演替阶段森林土壤中有效微量元素状况研究

三种森林表层土壤中有效微量元素的平均含量顺序为 :Fe >Zn>Mn>B >Cu >Mo,马尾松林的含量顺序为 :Fe>Zn>Cu >B >Mn >Mo,混交林和阔叶林与平均含量一致。三种森林有效Fe的含量均极高 ,表现出富铁状况 ,而有效Mn含量甚微 ,表明该区森林均严重缺Mn,有效Cu和Zn的含量处于中等水平 ,均高于其临界值。但处于演替初期阶段的马尾松林还缺B和Mo,混交林也略缺Mo。相关分析结果表明 ,土壤pH值与所考察的所有微量元素有效量之间均呈负相关 ,且与有效B、Cu和Fe相关极显著 (P <0 .0 1 ) ,与有效Mo相关显著 (P <0 .0 5 ) ;有机质与所考察的所有微量元素有效量之间均呈正相关 ,且与有效B和Fe相关极显著 ,与有效Mn相关显著     

黄土丘陵区不同植被根际土壤微量元素含量特征

为了解黄土高原不同植被土壤微量元素的根际效应,分析了该地区柠条、沙棘、沙打旺、柳枝稷、阿尔泰狗娃花和茵陈蒿6种植被根际与非根际土壤中有机碳、全氮、Mn、Cu、Fe、Zn含量.结果表明： 6种植被中,柠条、阿尔泰狗娃花和茵陈蒿根际土壤的有机碳、全氮含量高于非根际土壤;除柠条和沙棘外,其余4种植被非根际土壤pH值均显著高于根际土壤.6种植被根际土壤有效Mn含量均低于非根际;柠条、沙打旺和柳枝稷根际有效Cu含量显著高于非根际,表现出强烈根际富集现象.除沙打旺外,其他5种植被根际有效Fe含量均略高于非根际.沙打旺、柳枝稷、茵陈蒿和阿尔泰狗娃花表现出强烈的有效Zn根际富集现象.根际与非根际土壤有机碳、全氮与有效Mn、有效Zn,以及有效Mn与有效Zn呈极显著正相关.根际土壤pH值与有效Mn和有效Zn呈显著负相关.由于不同植物根系的生长特征、根际pH值及微生物种类等的差异,不同植被根际的微量元素含量不同,茵陈蒿根际4种微量元素含量高于其他植被.     

不同植被恢复模式下中亚热带黄壤坡地土壤微量元素效应

以武陵山区女儿寨小流域为例,研究了中亚热带黄壤坡地7种典型植被恢复模式下土壤微量元素有效性及其与土壤有机质、pH值之间的关系.结果表明： 0～20 cm土层荒草灌丛的B、Mn含量、油桐人工林Mo、Cu含量、杜仲人工林Zn含量和毛竹 杉木混交林Fe含量最高;20～40 cm土层润楠次生林B、Fe、Mn含量、荒草灌丛模式Mo含量、油桐人工林Zn含量和杜仲人工林Cu含量最高;毛竹 杉木混交林B、Mo、Cu、Mn含量在各层土壤均最低.各元素有效性指数以Mn最高,Cu最低,排序为Mn>Zn>Fe>Mo>B>Cu;土壤微量元素有效性综合指数以荒草灌丛模式最高(12.28),毛竹 杉木混交林最低(2.95),排序为Ⅶ>Ⅴ>Ⅲ>Ⅳ＞Ⅰ＞Ⅱ＞Ⅵ.土壤有机质含量与B、Zn有效态含量之间线性关系显著,二次多项式亦可较好地描述有机质与有效态Mn之间的关系,而有机质与Mo、Fe、Cu之间曲线回归关系不显著.土壤pH值与土壤Zn、Cu呈显著正相关,与Mn、Mo也有较好的相关性,而与B相关性较低,与Fe为弱负相关.     

泉州湾河口红树林湿地重金属的分布与迁移

通过测定泉州湾河口湿地2种红树植物(桐花树和秋茄)不同部位(根、枝和叶)及其根际沉积物中重金属酸可提取态含量,探讨该区域重金属元素的分布、在植物不同部位富集和迁移的情况。结果表明:2种红树植物根际沉积物中酸可提取态重金属含量顺序均为FeMnZnPbCuCrNi;秋茄根际沉积物中Cu、Zn、Pb、Ni和Cr两两之间呈正相关,桐花树根际沉积物中Cu与Zn呈正相关,Pb与其他重金属的相关性不显著;2种红树植物根中大多数重金属含量与根际沉积物中重金属酸可提取态含量之间呈正相关,而枝中的相关性不显著;2种红树植物重金属富集的情况较接近,Mn富集系数最大,其次是Cu和Zn;Mn、Cu、Zn、Cr主要富集在叶中,而Pb、Fe、Ni主要富集在根部;2种植物中Mn的迁移能力最强,易于从根部运输到叶中。     

奉节脐橙不同器官元素含量分布特征

对奉节脐橙果、叶、干、根中的必需大量元素 (N、K、Ca、Mg、P、S)、微量元素 (Fe、Mn、Cu、Zn、B、Mo)、有益元素 (Si、Co、F、Se、Ni、Sr)、有毒有害元素 (Hg、As、Cr、Cd、Pb、Sb、Bi)的分布特征进行分析 ,结果表明 :果、叶、干、根对各元素的吸收与富集特征具有明显的规律性 ,如叶、干、根中大量元素含量次序均为 Ca>N>K>Mg,叶、干、根中微量元素含量均有 Fe>Mn>Zn>Cu>Mo的规律 ,根、干、叶中有益微量元素含量次序均为 Si>Sr>F>Ni>Co>Se,叶、干、根中有毒有害元素含量次序均有 Pb>As>Sb >Hg的规律 ;在脐橙各器官中 ,叶是大量元素与有毒有害元素最富集的器官 ,根则是有益元素最富集的器官 ,有毒有害元素的 Cr、微量元素的 Mn、Fe、Mo也以根最为富集 ,干则是上述元素最不富集的器官 ,所有元素中 ,仅 Zn在干中最富集 ;大量元素 (除 N外 )、微量元素、有益元素在脐橙各器官的分配含量与地壳土壤背景值的分异含量趋势基本一致 ,土壤背景是这三类元素的主要控制因素。但有毒有害元素的分配形式则明显受人类活动的影响     

磁化微咸水灌溉对欧美杨I-107微量元素和碳氮磷养分特征的影响

为探讨盐分环境下,磁化作用对土壤和植株养分特征的影响,以欧美杨I-107为试材,采用磁化和非磁化微咸水灌溉处理,通过对土壤和植物组织中微量元素和碳氮磷含量的测定,以揭示土壤-植物的养分供求关系。研究发现:(1)微咸水灌溉处理中叶片和根系Fe含量均下降;叶片Zn、Mn和Cu含量提高,根系Mn和Zn含量降低、Cu含量提高。叶片和根系中总碳含量均提高,全氮和全磷含量均降低;叶片C/N下降,根系C/N和C/P则提高。(2)磁化微咸水灌溉处理叶片和根系中Fe、Zn、Cu含量均提高,Mn含量降低;叶片C、P及C/N提高,N含量下降;根系C、C/N和C/P含量提高。(3)微咸水灌溉土壤中Fe、Mn、Zn和Cu微量元素全量均降低,有效态含量均提高;OC和N、C/P和N/P下降,全磷和C/N提高。(4)磁化微咸水灌溉中土壤Fe、Mn和Zn全量提高,Cu降低;Fe、Mn、Zn和Cu有效态含量提高;OC和N、C/P和N/P提高。可见,磁化作用有利于调节植株对微量元素的吸收和分配,提高土壤的固氮能力以及对植株的碳供应能力。此外,盐分环境下,植物体通过提高元素Fe含量以及C/N比值维持光合作用的正常进行,以满足植株正常生长发育的需要。     

多枝桉叶营养元素含量的季节变化与施肥效应研究(Ⅱ)

研究了五种施肥处理(NPK、NP,N、P、对照)多枝按叶Ca、Mg、Zn、Fe、Cu、Mn等营养元素含量的季节动态。结果表明：多枝按叶片各营养元素含量的相对稳定期分别为Ca、Mn：11～3月;Mg：9～1月;Cu：11～1月;Fe：9～11月;Zn：3～5月。施肥后,多枝按叶各营养元素的季节动态均发生了一定程度的变化。     

大冶铜绿山矿区海州香薷(Elsholtzia hai-chowensis)植物地球化学特征分析

研究了大冶钢绿山矿区海洲香薷(Elsholtziahaichowensis)及其群落中几种主要植物Cu、Mn、Zn、Cd、Pb的累积分布,植物与土壤元素、Cu矿的关系,并对海洲香薷的重金属耐受性、铜矿的指示作用作了初步探讨.结果显示海洲香薷植物中的元素表现为Cu＞Mn＞Zn＞Pb＞Cd.其中Cu、Mn、Pb元素含量表现为根＞叶＞茎,Zn、Cd表现为叶＞根＞茎.和其它植物相比,海洲香薷中的Cu、Mn、Cd含量均高于其它植物,是其它植物的1～10倍.海洲香薷与土壤元素关系中,Cu的相关性最显著,其次为Pb.海洲香薷集中分布于矿区内含Cu较高的土壤上(1645～8950ug/g),其分布与Cu密切相关.     

青藏高原掌叶大黄和丽江大黄及其土壤的主要元素含量

采集掌叶大黄（Ｒｈｅｕｍ ｐａｌｍａｔｕｍ）和丽江大黄（Ｒｈｅｕｍ ｌｉｋｉａｎｇｅｎｓｅ）根茎、叶及根部土壤,应用ＩＣＰ测定主要元素含量特征,研究了２种大黄及其土壤的元素含量特征。结果表明,２种大黄土壤Ｐ含量远低于大黄根茎和叶,Ｆｅ含量则为土壤〉根茎〉叶,其中根茎与叶相差不大,但它们与土壤相差５０～１１０倍;Ｎａ、Ｍｎ、Ｃｕ含量在２种大黄中都表现为土壤〉叶〉根茎,Ｃａ含量在掌叶大黄中为土壤〈叶〈     

Evaluation of changes in the element content and biomass of invaded with Meloidogyne arenaria Tiny Tim tomato plants under NH4VO3 treatment

The parasite-host system Meloidogyne arenaria--Tiny Tim tomato plants has been studied in order to investigate the influence of the process of invasion on the chemical composition and biomass of plants. The concentrations of seven chemical elements Cu, Zn, Mg, K, Na, Mn and Fe have been determined using AAS in controls and invaded plants, and their changes have been evaluated under treatment with NH4VO3 in three different concentrations 0.01, 0.1 and 0.13 mg/100 ml H2O. The process of treatment with NH4VO3 disbalances significantly the trace element content of plants. The lowest concentration (0.01 mg NH4VO3) causes bigger changes in the concentrations of Mn, Fe and Na in non-invaded plants. The highest concentration (0.13 mg NH4VO3) balances the content of the elements back to their levels in the control plants for the elements Zn, Fe and Na. The pure effect of the process of invasion with Meloidogyne arenaria on the biomass (leaves, stems, roots and total biomass) of Tiny Tim plants is expressed in a significant increasing, mainly due to the development of the parasites. After treatment with different concentrations of NH4VO3 the decreasing in the biomass of leaves, stems and roots is observed which reflects on the total biomass of plants. The concentration of NH4VO3 eliminates the unfavourable changes not only in the chemical content of plants but also in their biomass. It could be taken into consideration as an alternative method used instead of treatment with nematocides.     

喀斯特城市杨树人工林微量元素的生物循环

对喀斯特城市25年生杨树人工林内Cu、Fe、Zn、Mn、Ni、Pb、Co、Cd微量元素的含量、积累、空间分配和生物循环进行了研究。结果表明,林地土壤中,微量元素含量Fe最高,Mn次之,Cd最低,且呈现随土层深度增加而减少的垂直分布规律。在枯枝落叶层的分解过程中,Pb、Ni、Mn、Cd、Cu、Co、Zn分解速度比Fe快。林木各器官微量元素含量为细根>树叶>粗根>树皮>树枝>大根>根桩>干材,Cu在叶中高于其他器官。林分微量元素的总贮量为14.086 kg.hm^-2,微量元素在各器官中贮存量排序为Mn>Zn>Cu>Fe>Cd>Co>Pb>Ni,树干和树皮的贮存量最多,占总贮存量的43.4%。林分微量元素的年吸收量为3.079 kg.hm^-2,年归还量为2.663 kg.hm^-2,年存留量为0.417 kg.hm^-2,总利用系数为0.219,循环系数为0.865,周转期为5.29年,林分对土壤中Cd的吸收能力强,微量元素的生物分解率均高于生物迁移率。杨树林分中微量元素具有较大的循环速率和较短的周转期,而且林分对养分的稳定性、自我调节能力和培肥土壤的能力强,有利于林地生产力维持。     

黄山松年轮硫及重金属元素含量动态特征

对黄山松80年的年轮序列中S及重金属元素Mn、Fe、Zn、Cu和Pb含量分析结果表明,年轮中S浓度可划分为3个等级:58.5%年轮段,S浓度<2mg·kg^-1;24.4%年轮段,S浓度3.65～6.0mg·kg^-1;17.1%年轮段,S浓度>11mg·kg^-1.年轮序列中S的积累有较大幅度的波动,可分为波动型(1917～1960年)、相对稳定型(1961～1980年)和持续增长型(1981年以后)3种类型;在1935～1938年、1959～1960年以及最近10年的年轮中,S含量均>11mg·kg^-1,表明该时段大气中S的浓度较高.统计分析表明,近18年来,旅游人数的增加与年轮中S含量呈显著相关性,一些景点较集中的燃料消耗可能造成局部大气污染,从而影响到树木.年轮序列中Pb的积累浓度低于土壤背景值;Mn、Fe、Zn和Cu在年轮中的积累均有明显的波动性;统计上无显著的相关性,表明这4种元素在年轮中的积累是独立的;Zn和Cu在年轮序列中积累的波动与树龄无关;Mn在年轮序列中的浓度随树龄增加而降低,在最新的几个年轮段又略有增加,Fe则相反.     

南四湖区农田土壤有机质和微量元素空间分布特征及影响因素

基于地统计学和GIS技术相结合的方法,研究了南四湖区农田土壤有机质和微量元素的空间分布特征及其影响因素。结果表明,土壤有机质和微量元素均属中等变异程度,除硼符合正态分布外,其余土壤属性均符合对数正态分布。结构分析表明,除硼为纯块金效应外,土壤有机质和其它微量元素空间自相关性较强,其中结构性因素起主导作用。克里格插值结果表明,土壤有机质分布总体趋势为由北向南逐渐降低,锰、铜、锌分布总体趋势为中部高,南北两端低。影响因素分析表明,土壤类型、耕层质地、坡度、土地利用类型和地貌类型对土壤有机质均有显著影响。土壤类型主要是由于成土母质的差异影响土壤有机质的高低与分布,随质地由砂变粘、坡度由低变高,土壤有机质含量逐步升高,田间管理水平的差异是造成不同土地利用类型下土壤有机质含量差异的主要原因。微量元素中,除硼不受影响外,铁、锰、铜和锌与土壤类型、耕层质地、坡度、土地利用类型和地貌类型密切相关。     

鼎湖山南亚热带常绿阔叶林植物营养元素含量分配格局研究

在鼎湖山南亚热带常绿阔叶林中,植物叶片营养元素含量为Ｎ ０．９４６％－２．５３５％,Ｐ ０．０３０－０．１２７％,Ｋ ０．６１４％－１．８３３％,Ｃａ ０．４４２％－１．９９５％,Ｍｇ ０．０２４％－０．１８８％。叶片各营养养元素间相关性较差,仅Ｐ与Ｍｇ及Ｍｇ与Ｋ之间存在显著的线性相关。叶片Ｎ元素平均含量在各层中的序列为：乔木Ⅲ〉乔木Ⅱ〉乔木Ⅰ〉灌木〉藤本〉草本;其它营养元素浓度随层次分配的规律性     

Glutathione metabolism in Urtica dioica in response to cadmium based oxidative stress

To investigate the antioxidative response of glutathione metabolism in Urtica dioica L. to a cadmium induced oxidative stress, activities of glutathione reductase (GR), glutathione-S-transferase (GST), and glutathione peroxidase (GSH-Px), content of reduced (GSH) and oxidized (GSSG) glutathione, lipid peroxidation (LPO), and also accumulation of Fe, Zn, Mn, Cu besides Cd were determined in the roots, stems, and leaves of plants exposed to 0 (control), 0.045, and 0.09 mM CdCl₂ for 58 h. Whereas the Cd content continuously increased in all organs, the Fe, Zn, Mn, and Cu content decreased in dependence on the applied Cd concentration and incubation time. The Cd treatment resulted in increased GR and GST activities in all organs, however, GSH-Px activity was dependent on Cd concentration and plant organ. The GSH/GSSG ratio maintained above the control level in the stems at both Cd concentrations. The LPO was generally close to the control values in the roots and stems but it increased in the leaves especially at 0.09 mM Cd.     

Trace elements in the hydrologic cycle of a forest ecosystem

Summary Concentrations of Cu, Fe, Mn, and Zn were measured in bulk atmospheric precipitation, throughfall, stemflow, and soil solutions at 10−, 15−, 25−, and 30-cm depths, in aEucalyptus globulus forest in the Berkeley hills, California, during the 1974–75 wet season after each main storm event. Litter and plant samples were analyzed. There was some similarity in the behavior of Cu, Fe, and Zn, but Mn behaved differently. Mn and Zn are largely deposited on the forest canopy by impaction during dry-deposition episodes, whereas most of the Cu and Fe input occurs in rain. For the hydrologic components measured, concentrations of Cu and Fe increase in the order: precipitation<throughfall<stemflow <soil solutions. For Zn the order is: precipitation<stemflow<throughfall<soil solutions. Concentrations of Cu, Zn, and Fe in the soil solution fluctuate with downward movement of wetting fronts and are negatively correlated with pH. Concentrations of Fe in soil solution are about 10 times greater than those of throughfall and stemflow; the corresponding relative differences for Cu and Zn were much less. Plant uptake of Mn exceeds that of Cu, Zn, and Fe. The increases in Mn concentrations from precipitation to throughfall and stemflow are much greater than those for Cu, Zn, and Fe because precipitation has very low Mn concentrations. The concentration series for Mn is: precipitation<soil solutions<throughfall<stemflow. Concentrations of Mn in the soil solution are negatively correlated with pH. During the dry summer Mn accumulates in the soil, but is quickly flushed by early rains of the wet season.     

The effects of copper, manganese and zinc on plant growth and elemental accumulation in the manganese-hyperaccumulator Phytolacca americana

Synchrotron radiation X-ray fluorescence (SRXRF) and inductively coupled plasma mass spectrometry were used to estimate major, minor and trace elements in Cu-, Zn- and Mn-treated Phytolacca americana. The effects of the addition of Cu, Zn and Mn on morphological parameters, such as root length, shoot height, and fresh and dry weights of shoots and roots, were also examined. In addition, the activities of superoxide dismutase (SOD), ascorbate peroxidase (APX), guaiacol peroxidases (GPX) and catalase (CAT) and the expression of Fe-SOD, Cu/Zn-SOD, metallothionein-2 and glutathione S-transferase (GST) exposed to the highest amounts of Cu, Zn or Mn were detected. Our results confirmed the following: (1) Zn supplementation leads to chlorosis, disturbed elemental homeostasis and decreased concentrations of micro- and macroelements such as Fe, Mg, Mn, Ca and K. Cu competed with Fe, Mn and Zn uptake in plants supplemented with 25μM Cu. However, no antagonistic interactions took place between Cu, Zn, Mn and Fe uptake in plants supplemented with 100μM Cu. Mn supplementation at various concentrations had no negative effects on elemental deficits. Mn was co-located with high concentrations of Fe and Zn in mature leaves and the concentrations of macro elements were unchanged. (2) P. americana supplemented with increased concentrations of Zn and Cu exhibited lower biomass production and reduced plant growth. (3) When plants were supplemented with the highest Zn and Cu concentrations, symptoms of toxicity corresponded to decreased SOD or CAT activities and increased APX and GPX activities. However, Mn tolerance corresponded to increased SOD and CAT activities and decreased POD and APX activities. Our study revealed that heavy metals partially exert toxicity by disturbing the nutrient balance and modifying enzyme activities that induce damage in plants. However, P. americana has evolved hyper accumulating mechanisms to maintain elemental balance and redox homeostasis under excess Mn.