黄土高原旱地长期种植作物对土壤微量元素形态和有效性的影响

在长期定位试验的基础上,用连续浸提方法对土壤微量元素进行形态分级,研究了长期种植作物条件下黄土高原旱地土壤中微量元素的形态组成及其在不同土壤组分间的分配特征,探讨了种植系统对土壤微量元素有效性的影响。土壤中有效态微量元素含量的剖面分布除与土壤中微量元素的全量有关外,还与不同的种植系统有关。各种植系统有效锌和有效铜含量均低于休闲土壤,有效锌以小麦连作和苜蓿连作降低最多,有效铜以小麦连作和粮豆轮作降低最多。小麦连作系统40 cm以上土层土壤有效锰含量和休闲土壤接近,40~100cm土层低于休闲土壤,苜蓿连作和粮豆轮作整个剖面土壤有效锰含量均有所增加。各种植系统40cm以上土层土壤有效铁含量均高于休闲土壤,40~100cm土层土壤有效铁分布趋势相同,其含量均随土层深度的增加而增加,并且小麦连作低于休闲土壤,粮豆轮作高于休闲土壤,苜蓿连作与休闲相近,这些结果表明长期种植作物可以显著改善土壤锰素营养和铁素营养状况。苜蓿连作和小麦连作使锌和铁从矿物态向有机结合态转化,增加了土壤有效锌和有效铁的储备,粮豆轮作系统各形态锌低于休闲土壤,并且土壤中锌的总贮量有所减少;各种植系统土壤氧化物结合态铁在耕层增加,在古耕层降低,这也表明种植作物可以活化深层土壤难溶态铁。长期种植作物使耕层土壤各形态铜含量降低,粮豆轮作和小麦连作系统古耕层土壤各形态铜含量较休闲土壤有所增加。3种种植系统碳酸盐结合态、氧化物结合态和有机结合态锰含量均有不同程度的下降,且耕层土壤交换态、碳酸盐结合态和有机结合态锰高于古耕层,氧化物结合态和矿物态锰含量低于古耕层。     

不同母质柑橘园土壤养分特征及肥力综合评价

为探究不同母质柑橘园土壤养分特征,阐明土壤母质对肥力影响,为果园精准施肥提供参考依据,本研究采集了5种不同母质的柑橘土壤,共计217个样点,分析了土壤pH、有机质以及大、中、微量元素有效态含量。结果表明：柑橘园土壤平均pH<5.5,土壤呈酸性;除板页岩、石灰岩外,其他母质土壤有机质匮乏;第四纪红土交换性钙、镁含量丰富,其他母质较为匮乏;各母质土壤的碱解氮、有效锌、硼、钼含量适宜,速效钾、有效磷、硫、铁、锰、铜过量。方差分析表明,除有效铜、锌外,其他各养分含量在不同母质间均存在显著差异,板页岩发育的土壤有机质、碱解氮、有效磷、速效钾以及有效铁、铜、钼高于其他母质土壤,交换性钙、镁含量低于其他母质。通过主成分综合评分得出,5种母质土壤综合肥力大小为板页岩>砂岩>第四纪红土>河湖冲沉积物>石灰岩。随着柑橘种植年限延长,板页岩、河湖冲沉积物、石灰岩土壤肥力有极显著提升,第四纪红土肥力有显著提升。综合分析,板页岩发育的土壤养分最为丰富。土壤有机质、碱解氮、速效钾、有效硼、有效磷、有效硫是影响肥力的重要因子,针对不同母质土壤养分间的差异,可因地制宜地对果园土壤进行精准...     

南疆地区巴仁杏果园土壤矿质元素与叶片营养水平分析

为探讨果园土壤矿质元素与叶片营养水平的相互关系,于巴仁杏盛果期采集南疆阿克陶县巴仁杏果园的壤土和沙土土样,以及植株叶片,测定土壤与叶片矿质元素质量分数,结果表明,该地区2种类型土壤巴仁杏果园叶片全氮质量分数均偏低,沙土果园叶片镁质量分数偏低。不同土壤类型果园叶片全氮、钾、钙、镁质量分数差异显著。该地区果园土壤养分整体较低,其中,土壤有机质、氮、磷、锌、锰、铜质量分数均偏低,此外不同矿质元素在不同土层的分布规律因土壤类型不同而各有差异。2种土壤类型果园的土壤有机质质量分数与叶片磷质量分数均呈正相关,叶片其他矿质元素质量分数与土壤有机质质量分数的相关性与土壤类型有关;土壤矿质元素与叶片相应矿物质元素的相关性因土壤质地不同而存在较大差异。因此,在巴仁杏果园的土肥管理中应增施有机质及氮、磷、锌、锰、铜、硼等矿质元素。此外,对不同土壤类型果园的管理应根据果园土壤类型进行针对性施肥。     

土壤与烤烟中微量元素含量的相关性

通过分析四川省会理烟区土壤及红花大金元烟叶各30份样品中微量元素含量,研究了会理烟区植烟土壤与烟叶中中微量元素含量之间的定量关系。结果表明:会理烟区大部分土壤中微量元素含量在较适宜的范围内,但部分土壤水溶性硼、有效锌含量较低,烟叶中铜元素、镁元素含量较缺乏;利用多元线性逐步回归分析得到土壤与烟叶中微量元素的回归方程,其中烟叶中的锰、锌含量均受到土壤中5个中微量元素的综合影响,而钙含量仅受到土壤中有效锰和交换性钙的影响;偏相关和通径分析结果表明,烟叶中微量元素与其对应的土壤内中微量元素呈极显著正相关,且直接作用系数最大。土壤中的中微量元素之间存在着广泛的协同或拮抗效应,其中土壤有效锰的含量对烟叶所有中微量元素含量的影响最大,而烟叶锌含量受土壤中其他中微量元素的影响最大。     

红壤剖面土壤养分对土地利用变化响应的敏感性

为了解红壤剖面土壤养分及其有效形态的分布以及对高强度土地利用的响应,本研究选取位于湘东大围山低丘陵地带同一景观单元内花岗岩红壤发育的4种毗邻的典型土地利用方式(包括樟树天然林以及由此转变而来的杉木人工林、板栗园和坡耕地),采用自制土钻以20 cm等间隔采集0~100 cm土壤样品,测定各土层的p H、有机质、大量元素(全氮、全磷、全钾)及其有效态(碱解氮、有效磷、速效钾)、中量(钙、镁)和微量元素(铁、锰、铜、锌)有效态的含量,并计算不同养分的敏感性指数(SI),分析土壤养分对土地利用变化响应的敏感性。结果表明,天然林地改为其他土地利用方式,0~100 cm土壤剖面有机质、全氮含量分别降低9%~55%和28%~57%,全磷含量则升高0.3~52倍,高强度的人类活动(如施肥)导致土壤剖面有机质和全氮的损失,但却引起磷素的累积。较之土壤全量养分(SI介于-0.6~1.5),有效态养分含量(SI介于-0.8~51.8)对土地利用变化的响应更为敏感。土壤有效磷(SI介于-0.8~51.8)、速效钾(SI介于-0.5~2.9)、有效态铁(SI介于-0.6~3.1)、有效态铜(SI介于-0.8~2.2)含量对土地利用变化以正响应为主,反映土地利用方式的转变提高了土壤剖面上养分的有效性。与表土相比,花岗岩红壤底土有效态养分(如碱解氮、有效磷、速效钾、有效态锰、锌)含量对土地利用变化的响应更敏感。不能简单地将不同土地利用方式浅层表土养分的研究结论外推到深层底土,应重视土地利用变化引起的底土养分(尤其是有效态和中、微量元素)的演变趋势。     

玻璃肥料肥效试验(报告一)

微量元素(锰、锌、铜、钼、硼等)为植物正常生活所必需。在缺乏微量元素的土壤上栽培农作物产量很低,为了保证丰产必须施用微量肥料(含有微量元素的肥料)。植物体内微量元素的不足,可能由于它们生长的土壤中缺乏这些元素;但往往不是完全缺乏,而是微量元素以不溶解的状态存在,因而这些物质不能为植物所利用。例如土壤中石灰含量     

外源硫输入对草地土壤-植物系统养分有效性的影响

外源硫输入增加是草地生态系统土壤酸化的一种重要诱因,在一定程度上抑制了土壤有机质的矿化从而有利于有机碳积累,但可导致石灰性土壤中碳酸盐的分解;硫输入可提高土壤中氮及微量元素铁、锰、铜、锌、硼的有效性,降低钼的有效性;导致交换性盐基离子淋失并降低钙、镁、钾的有效性;增加石灰性和中性土壤磷的有效性,而降低酸性或强酸性土壤磷的有效性。外源硫输入可促进草地植物对氮和磷的协同吸收,总体上可以促进草地植物对金属微量元素的吸收,但土壤酸化可能引起植物锰毒害,增加植物锰吸收的同时抑制了对铁的吸收。高量硫输入及土壤重度酸化可导致草地生产力和物种多样性降低;低剂量硫输入对草地生产力有一定的促进作用,但对物种多样性及群落稳定性的影响目前尚缺乏系统的研究资料。     

江西省茶园土壤肥力特征及其影响因子

为探明江西省典型茶园土壤养分状况和肥力特征,选取江西省21个地区372个典型茶园,分析茶园土壤养分的差异性、空间性、相关性及与地形、土壤类型、海拔和建园时间的关联性。结果表明: 江西省茶园土壤pH、有机质、碱解氮、速效磷、速效钾、全氮、全磷和全钾分别达到优质高效高产茶园土壤营养指标的53.9%、60.1%、56.1%、22.9%、38.5%、43.7%、11.1%和95.5%,其中速效磷为强变异;有效铜、锌、铁、锰和硼达到土壤微量元素含量分级一级标准的占比分别为76.3%、74.2%、96.8%、73.1%和0.0%。江西茶园土壤养分以赣中地区最高,其次是赣东北和赣西北地区,赣南地区最低。除全钾外,土壤pH与有机质、碱解氮、速效磷、速效钾、全氮和全磷均呈显著正相关。不同地形土壤养分以平地最高,高山次之,山地和丘陵最低;不同土壤类型土壤养分以水稻土、砂壤和山地黄棕壤较高,其次是黄壤、红黄壤和紫色土,红壤最低;土壤pH、有机质和全钾随海拔上升而递增,而速效磷随海拔上升而递减;土壤有机质、碱解氮、全氮、速效磷和全磷随建园时间的增加而递增,而土壤pH随建园时间的增加而递减。综上,江西省茶园土壤肥力总体水平良好,有机质、全钾、有效铜、锌、铁和锰均较丰富,但土壤偏酸,速效磷和全磷偏低,有效硼严重缺乏。赣中应提高土壤pH和钾肥,赣东北增加钾和氮肥,赣西北增加有机质和磷肥,赣南应增加氮磷钾肥并配施有机肥;高山茶园补充速效磷和钾肥,山地茶园提高氮和磷肥;红黄壤茶园提高土壤pH和全钾,红壤茶园应提高氮磷钾肥并配施有机肥,黄壤和山地黄棕壤茶园需要增施磷肥,紫色土茶园需提高土壤有机质;茶园需要逐年增加白云石粉、生理碱性肥料和有机肥等,防治茶园土壤酸化。     

微量元素对水稻幼苗生长和呼吸作用的影响及其相互关系

用不同浓度的各种微量元素CuSO_4·5H_2O、MnSO_4·4H_2O、ZnSO_4·7H_2O、H_3BO_3·H_2O、MoO_3处理水稻种子24小时,放在25℃恒温箱内萌发,10天后除去胚乳分别测定地上部和地下部的干重。微量元素促进生长和呼吸的最适浓度是铜2p.p.m.,锌、锰100p.p.m.,钼、硼50p.p.m.。用最适浓度浸种得到的幼苗分别测定微量元素对呼吸抑制剂(氰化钾、丙二酸、氟化纳等)的相互作用以及对琥珀酸氧化酶的影响,结果如下: 1.5种微量元素中除锌对水稻地上部有抑制作用外,其他都对生长有促进作用,一般幼苗干重可增加10％左右,最高可增加地上部27％(硼50p.p.m.)。 2.各种微量元素对生长有促进作用的浓度一般也促进呼吸,两者基本是平行的,随着浓度的增加对生长和呼吸均表现有抑制作用。 3.铜、锌、锰、钼对呼吸抑制剂氰化钾的抑制作用有明显的拮抗作用,它们随时间的延长而逐渐恢复。 4.各种微量元素均有加重丙二酸抑制作用的现象,这可能是因为微量元素对琥珀酸去氢酶就有抑制作用。 5.锰对琥珀酸氧化酶表现有好的作用,而铜却表现不利的影响。     

黄土高原小流域土壤养分空间变异特征及预测

在黄土高原小流域尺度上,地形和土地利用是影响土壤属性变异的重要因素.在横山县朱家沟小流域采集111个表层土样,比较不同土地利用及景观位置土壤养分变异及分布特征,分析土壤养分与地形因素的关系并利用相关环境信息进行空间预测.结果表明,不同土地利用类型土壤养分存在显著性差异.有机质和全氮含量表现为坝地最高,灌木地最低,而全磷含量以梯田最高.在不同景观位置,沟平地有机质和全氮含量显著高于其他景观位置,而全磷差异不显著.土壤有机质与复合地形指数CTI、汇流动力SPI、沉积物运移指数STI显著负相关,全氮与沉积物运移指数STI显著负相关,而全磷只与坡度β显著负相关.多元线性逐步回归模型预测土壤有机质和全氮较好,而全磷预测结果较差;回归-克里格预测有效地减小了残差,与实测值较为接近,预测精度高于回归预测.     

川西北草原土壤及冷暖季牧草微量元素含量比较

改善土壤的理化环境及提高牧草的营养水平必须了解草地土壤及牧草微量元素的分布与含量。试验从川西北草地的亚高山丘原草甸、亚高山平坝草甸和沼泽平坝草甸采集土样和冷暖季草样。土样采集深度范围是0～10cm,10～20cm,20～30cm。应用火焰原子吸收光谱法测定了草样中铜、铁、锰、锌和钴的含量和土样中这些元素的有效态含量,应用氟离子选择电极法测定了土样中的氟离子浓度和草样中的氟含量。土壤pH高低顺序为草甸土>冲积土>泥炭草甸土,pH随土壤深度变深而下降;土壤和牧草的钴含量都处于缺乏状态,分别为0.64mg/kg和0.26mg/kg。牧草铁和锰含量都高于正常水平,铁为414.51～565.06mg/kg,锰为138.68～247.09mg/kg.     

Trace elements in aerial parts and rhizosphere of <Emphasis Type="Italic">Thymus pannonicus</Emphasis> All.

This paper brings out the results of the study on the levels of selected trace elements (Cu, Fe, Mn, Zn and Cr) in aerial parts of Thymus pannonicus All. (Lamiaceae) and rhizosphere soil from twelve locations in Serbia. Prior to assays by flame and flameless atomic absorption spectrometry, samples were subjected to microwave-assisted acid digestion. Real and potential acidity of soil samples were also measured. Obtained results for soil samples, although slightly higher for some elements (Cu: 12.38–45.18 mg/kg; Fe: 22102–46193 mg/kg; Mn: 776.95–4901.27 mg/kg; Zn: 62.27–214.02 mg/kg; Cr: 48.86–69.13 mg/kg), were found to fit into biogeochemical background. Element contents in plant samples differed depending on collecting site (Cu: 5.26–14.07 mg/kg; Fe: 25.92–1454.07 mg/kg; Mn: 89.29–278.25 mg/kg; Zn: 1.81–10.64 mg/kg; Cr: 1.11–3.51 mg/kg), which can be partly explainable by different nutrient availability influenced by soil acidity. Zinc levels in T. pannonicus were below expected and seem to be strongly influenced by plant physiological properties.     

Deposition of copper, iron, manganese and zinc in the empty body of growing lambs of the breed German Merino Landsheep

A growth experiment with 108 lambs (breed: German Merino Landsheep) was carried out to examine the effect of gender, body weight (BW) and feeding intensity on the deposition of Fe, Zn, Cu and Mn in the empty body (whole animal minus contents of the gastrointestinal tract and bladder). The lambs (50% female and 50% male animals) were fed at three feeding levels ('low', 'medium' and 'high' by varying daily amounts of concentrate and hay) and slaughtered at different final BWs (30, 45 or 55 kg). Six male and six female animals were killed at a BW of 18 kg representing the animals' BW at the beginning of the comparative slaughter experiment. There were significant main effects for the treatments growth rate and final weight on the daily rate of accretion of the trace elements examined. Feeding intensity had a marked influence on the accretion rate for Fe (P < 0.001), Zn (P < 0.001), Cu (P < 0.001) and Mn (P = 0.003). With increasing feeding intensity (low, medium, high) the daily deposition of these trace elements increased (4.4, 5.2, 6.6 mg/day for Fe; 4.9, 5.5, 6.9 mg/day for Zn; 0.20, 0.36, 0.44 mg/day for Cu; 0.14, 0.16, 0.21 mg/day for Mn). Heavier final BW led to increased daily retention of Zn (P < 0.001) and Mn (P = 0.002). Gender had a marked influence only on the accretion rate for Zn (P < 0.001). Ram lambs had a higher daily deposition of this element than female lambs. Related to 1000 g empty body gain, the following concentrations were found for the trace elements examined: Fe 26.1 mg, Zn 30.0 mg, Cu 1.41 mg and Mn 1.04 mg. A feeding influence was given for Zn (P < 0.001) and Cu (P = 0.039). Feeding level low had higher Zn and lower Cu concentrations. Male animals showed less Fe (P < 0.001) and Zn (P = 0.034) per kg empty body gain than females.     

鼎湖山南亚热带常绿阔叶林植物和土壤微量元素含量

报道了鼎湖山南亚热带常绿阔叶林各层次植物和表层土壤(0～20 cm)四个微量元素(Cu、Fe、Mn和 Zn)的含量和分配格局。结果表明:(1)土壤有效Cu、Fe、Mn和Zn含量(mg／kg)平均值依次为0．72、140．85、 1．42和1．92;(2)所有植物叶片Cu、Fe、Mn和Zn元素含量(mg／kg)分别介于6．1～100．6、6．5～1027．5、46．3 ～1196．7和27．0～338．6,其中乔木层植物叶片微量元素含量(mg／kg)平均值表现为Mn(305．3)>Fe (259．3)>Zn(109．9)>Cu(19．3),而其它植物表现为Fe(586．4)>Mn(336．9)>Zn(141．4)>Cu(36．6);(3) 植物微量元素在各器官的分配格局随元素和植物所在的层次不同而异:乔木层植物Cu含量高低排序为干> 根>枝>叶>皮,Fe为根>皮>叶>枝>干;Mn为叶>皮>枝>根>干;Zn为叶>根>枝>皮>干;(4)在 群落垂直结构上,Fe元素含量表现为自上而下递增的趋势,而Cu、Mn和Zn含量规律不明显;(5)植物和土壤 的微量元素与微量元素间相关性均较差;(6)与亚热带其它森林相比,鼎湖山季风常绿阔叶林土壤Cu、Mn和 Zn含量较低,但乔木层植物因具有很强的吸收或富集能力而含量较高。     

Effect of Na/Ca and Na/K ratios in saline culture solution on the growth and mineral nutrition of rice (Oryza sativa L.)

Summary A study was conducted to evaluate the effect of manganese on accumulation of Zn, Fe, Cu, and B by different soybean genotypes under varying soil pH conditions, in view of determining tolerance towards extremes in soil pH and mineral toxicities. Enon sandy loam soil was used for the investigation in a greenhouse. Manganese rates were 0, 10, and 20 kg/ha. The pH levels were 5.3, 6.3, and 7.0. The soybean genotypes tested were PI 159319, PI 324924, PI 960895, and L-76-0132. Results indicate that Zn concentration in the genotypes leaf and seed was not affected by Mn application whereas the Cu concentration in the leaf was affected. In general, there was an increase in concentration of Fe in the genotypes seed with Mn application. Boron concentration in the genotypes leaf and seed was unaffected by Mn application. The effect of soil pH on Zn, Fe, Cu, and B in the genotypes tissue was significant. This did not result in toxic levels of the elements in the tissues.Contribution of the Department of Plant Science and Technology, North Carolina Agricultural and Technical State University, Greensboro, N.C. 27411, and Agronomic Division, North Carolina Department of Agriculture, Raleigh, NC 27611, USA     

Particle size and metal distributions in anaerobically digested pig slurry

Particle size distribution and trace element patterns were studied in a full-scale anaerobic digestion plant treating pig slurry. Mass balance was established for major (N, P, K, Ca, Fe, Mg and S) and minor (Al, Cu, Mn and Zn) elements. Most of the elements were conserved through the process but part of the P, Ca, Mg and Mn was deposited as crystals lining the digester. In the dry matter of the slurry, Cu and Zn occurred at between 170 and 2600 mg kg(-1) due to pig diet supplements. Analyses of particle size distributions in raw and digested slurries showed a general shift in distribution towards larger sizes due to degradation of small and easily degradable particles as well as formation of large microbial filaments. Graded sieving of digested slurry showed metals to be mainly present on 3-25 microm particles. Less than 2% Cu and Zn was removed by passage through a 250 microm rotary screen.     

不同利用强度下绿洲农田土壤微量元素有效含量特征

以地处极端干旱背景下的塔里木盆地南缘策勒绿洲为研究区,以绿洲化为视角,根据当地农民耕作习惯于2005年选择4块试验农田,分别代表当地典型的农田利用强度。基于单项指数(Ei)和综合指数(Ec)相结合的评价方法,分析了绿洲农田在不同利用强度下的土壤Fe、Cu、Mn、Zn等微量元素有效性,探讨了土壤微量元素与人为耕作管理措施之间的关系。结果表明:人为耕作管理强度会对土壤微量元素有效含量产生重要影响,绿洲不同位置农田因施肥强度和管理方式的差别,其土壤微量元素有效含量特征存在显著差异。绿洲内部农田土壤有效Fe、Cu、Mn、Zn含量显著高于绿洲边缘各样地,新垦农田土壤有效Fe、Cu、Zn含量均低于对照样地;绿洲内部农田土壤微量元素有效性最高,新垦农田最低;农田土壤微量元素有效性与土壤有机质存在显著的正相关关系。     

Essential trace elements in milk and blood serum of lactating donkeys as affected by lactation stage and dietary supplementation with trace elements

The aim of this trial was to study the concentration of zinc (Zn), iron (Fe), copper (Cu), manganese (Mn), selenium (Se), cobalt (Co) and iodine (I) in milk and blood serum of lactating donkeys, taking into account the effects of lactation stage and dietary supplementation with trace elements. During a 3-month period, 16 clinically healthy lactating donkeys (Martina-Franca-derived population), randomly divided into two homogeneous groups (control (CTL) and trace elements (TE)), were used to provide milk and blood samples at 2-week intervals. Donkeys in both groups had continuous access to meadow hay and were fed 2.5 kg of mixed feed daily, divided into two meals. The mixed feed for the TE group had the same ingredients as the CTL, but was supplemented with a commercial premix providing 163 mg Zn, 185 mg Fe, 36 mg Cu, 216 mg Mn, 0.67 mg Se, 2.78 mg Co and 3.20 mg I/kg mixed feed. The concentrations of Zn, Fe, Cu, Mn, Se, Co and I were measured in feeds, milk and blood serum by inductively coupled plasma-MS. Data were processed by ANOVA for repeated measures. The milk concentrations of all the investigated elements were not significantly affected by the dietary supplementation with TE. Serum concentrations of Zn, Fe, Cu Mn and Se were not affected by dietary treatment, but TE-supplemented donkeys showed significantly higher concentrations of serum Co (1.34 v. 0.69 μg/l) and I (24.42 v. 21.43 μg/l) than unsupplemented donkeys. The effect of lactation stage was significant for all the investigated elements in milk and blood serum, except for serum manganese. A clear negative trend during lactation was observed for milk Cu and Se concentrations (−38%), whereas that of Mn tended to increase. The serum Cu concentration was generally constant and that of Co tended to increase. If compared with data reported in the literature for human milk, donkey milk showed similarities for Zn, Mn, Co and I. Furthermore, this study indicated that, in the current experimental conditions, the mineral profile of donkey milk was not dependent on dietary TE supply.     

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.