甘肃兴隆山森林演替过程中的土壤理化性质

在森林群落恢复演替过程中,由于森林类型及其所处立地环境不同,森林与土壤相互作用过程具有复杂性。以甘肃兴隆山6种森林类型(青杄林、青杄-白桦林、山杨-白桦林、灌丛林、落叶松林和油松林)0—60 cm土壤层为研究对象,探讨森林恢复演替过程中土壤理化性质的变化规律,旨在为该区域退化森林生态系统恢复与重建提供依据。结果表明:1)在土壤剖面上,兴隆山森林土壤容重随深度的增加而逐渐增大,总孔隙度、毛管孔隙度、自然含水量、最大持水量、毛管持水量、田间持水量均随深度的增加而减小;pH值差异不显著,无明显变化规律;土壤有机质、全N、水解N、有效P、速效K均随深度的增加而变小,表聚效应明显;全P差异不显著,呈"圆柱体"分布模式;2)在森林恢复演替过程中,天然林容重、孔隙度、持水能力、渗透性明显好于人工林,随森林正向演替的进行,天然林容重不断减少,孔隙度明显改善,通透性能不断增强,而人工林土壤物理性质出现明显退化现象;天然林pH值在演替方向上并未表现出酸化现象;天然林土壤有机质、全N、水解N、有效P和速效K变化规律不明显,但总的变化趋势为先增加后减小;3)有机质与全N、水解N、最大持水量、毛管持水量、田间持水量呈显著正相关,而与容重呈显著负相关;全N与水解N呈显著正相关;土壤有机质在改善土壤理化性质和促进养分循环方面具有重要作用,已成为植被恢复过程中土壤变化的一个重要标志。     

陕西定边盐渍土土壤含盐量和pH的空间分布特征

为给陕西省定边县堆子梁镇盐渍土综合整治提供基础资料,对该地区盐渍土土壤含盐量和pH的空间分布特征进行研究。运用地统计学方法对研究区土壤含盐量和pH的空间分布特征进行分析。结果表明,研究区土壤含盐量的平均值为0.54%,高于强度盐渍化土标准（>0.4%）,属于强度盐渍化土;pH的平均值为8.90,属于碱性土壤;同时,pH空间分布格局总体呈高含盐量区域pH低的特点。分析半方差函数可知,土壤含盐量变化符合指数模型,自相关距为2 010 m,块金系数C₀/(C₀+C)为0.50,表现出中等变异程度;pH变化符合线性模型,自相关距为2 377 m,块金系数C₀/(C₀+C)为0.21,具有强烈的空间相关性。根据盐渍土土壤性质的空间分布特征,在研究区盐渍土土壤综合整治中,可采取分区域、分方法、有针对性地进行改良与利用的措施。     

火烧对黔中喀斯特山地马尾松林土壤理化性质的影响

在黔中喀斯特山地马尾松人工次生林内取样分析火烧和对照样地间土壤理化指标的变化,研究了火烧对林地土壤理化性质的影响。结果表明马尾松火烧林地表层土壤毛管孔隙度和总孔隙度升高、最大持水量和最小持水量增加,土壤密度和非毛管孔隙度降低、土壤质量含水量和体积含水量减少;土壤有机质、全N量、全P量、全K量,水解N量、有效P量、速效K量、交换性盐基量和pH值增大,阳离子交换量降低。林火对马尾松林地土壤主要理化指标影响的趋势为或表层土壤影响率大于剖面影响率、或表层土壤影响率小于剖面影响率,不同指标在土壤剖面的变化趋势或增加、或降低,对数或幂函数拟合曲线均达相关显著性水平。火烧和对照样地间的表层土壤理化指标变化主要反映了林火影响,近岩层土壤理化指标变化主要是成土母质在空间上的分异,也受生物的影响。乔木层植株死亡率同表层土壤最大持水量、最小持水量、有机质量和全N量的正相关性显著,同土壤密度的负相关性显著;灌木层植株死亡率同表层土壤密度正相关性显著,同毛管孔隙度、总孔隙度、质量含水量、最大持水量、最小持水量、有机质量、全N量、全P量和速效K量的负相关性达显著或极显著水平;灌木层生物损失量同表层土壤密度和有机质量正相关显著,同速效K量的负相关性显著,枯物层生物损失量同pH值的正相关性显著。火烧马尾松林分平均胸径同表层土壤密度正相关性显著,同毛管孔隙度、总孔隙度、质量含水量、最大持水量、最小持水量和有机质量的负相关性显著。     

豫中褐土耕地土壤性质空间分异及质量评价

以河南省中部褐土集中分布区禹州县文殊镇为例,基于GIS对该镇进行500 m×500 m规则网格布点248个,将布点图层与土壤图进行叠加分析建立空间数据库,作为野外GPS定位精确采样的依据.野外实际共采集202个点的土壤样品（0～20 cm）,其中随机均匀选取34个点进行容重环刀采样.获取有机质、速效K、速效P、pH值、全N、全P、质地、阳离子交换量(CEC)、缓效K和容重10项土壤指标作为耕地土壤质量评价的因素.对指标进行数据统计分析,运用层次分析法（AHP）计算排列出评价因子的权重,运用普通Kriging插值法得出研究区10项土壤理化性质空间分异及土壤质量等级分布和面积.结果表明：研究区褐土耕地土壤质量属于较好的水平,其中优、中等占95%以上,差等只有不到5%.     

不同入侵程度下飞机草对喀斯特地区土壤理化性质的影响

外来生物入侵威胁着全球的生物多样性和生态系统的功能,研究外来入侵植物对土壤理化性质的影响有助于理解外来入侵植物的入侵机制。以广西喀斯特地区飞机草（Chromolaena odorata）入侵生境为研究对象,比较分析了不同飞机草入侵程度下（对照、轻度入侵、中度入侵、重度入侵）土壤物理和化学指标变化特征。结果表明：随着飞机草的入侵程度加重,土壤容重显著增加,轻度入侵、中度入侵和重度入侵生境下土壤容重分别比对照增加了10.3%、16.7%、22.3%,土壤非毛管孔隙度、总孔隙度和土壤含水量显著降低,土壤毛管孔隙度无显著变化;飞机草入侵对土壤pH值无显著影响,随着入侵程度加重,土壤速效磷和速效钾的含量显著升高,在重度入侵生境下土壤速效磷和速效钾含量分别比对照增加了4.3倍、3.8倍,土壤全氮和有机质含量显著降低。飞机草入侵显著改变了土壤理化性状,导致喀斯特地区土壤物理结构退化,生态系统水土保持能力下降,同时飞机草通过改变土壤养分循环提高了土壤可直接利用养分的水平,创造对自身有利的土壤环境,进而促进其生长和扩散。     

云顶山不同人工林林下植物多样性及其与土壤理化性质的关系

以成都云顶山5种人工林（Ⅰ：柏木枫杨林;Ⅱ：银杏楠木林;Ⅲ：光皮梾木香樟林;Ⅳ：枫杨桤木林;Ⅴ：柏木林）为研究对象,重点研究不同人工林林下植物多样性与土壤理化性质差异以及二者间的关系。结果表明：不同人工林灌草层重要值最高的物种不同,光皮梾木香樟林林下植物组成最丰富,而银杏楠木林最贫乏。各人工林灌木层多样性指数H、优势度指数H''、丰富度指数D均以光皮梾木香樟林最大,而均匀度指数J_sw无显著差异;草本层H、D、J_sw均以柏木林最大,银杏楠木林最小,而H''差异不显著。不同人工林土壤pH值、有机质、全氮、全磷、速效钾、速效磷含量差异显著,pH值、全磷含量柏木枫杨林最高,有机质、全氮、速效钾、速效磷含量银杏楠木林最高。显著影响灌木层物种多样性的土壤因子为有机质、速效磷,草本层为pH、全磷、速效磷。结论：光皮梾木香樟林林下整体植物多样性水平最高,经营此种林分有利于林下植物多样性维持及发展,pH、有机质、全磷、速效磷是影响研究区林下植物多样性的主要土壤因子。     

甘肃中东部地区9种薹草属植物分布区群落特征和土壤养分状况

为探究薹草属(Carex L.)植物在不同植被类型中的分布状况,该研究对甘肃中东部地区9种薹草属(Carex L.)植物分布区的群落特征进行调查,并对土壤养分状况进行比较分析,以揭示野生薹草群落物种多样性和分布特征与土壤环境因子间的关系。结果表明：(1) 9种薹草群落物种多样性差异性较大,Shannon-Wiener多样性指数(H)、Simpson优势度指数(D_si)均以青绿薹草群落最高,亚柄薹草最低;Patrick丰富度指数(R)以异穗薹草群落最高,细叶薹草群落最低;Pielou均匀度指数(J_sw)以凹脉薹草群落最高,亚柄薹草最低。(2) 9种野生薹草属植物适宜生长的土壤pH呈中性或弱碱性,且有机质、氮素、钾素含量较丰富,磷含量偏低;土壤有机质、pH、全氮、全磷、全钾、碱解氮、速效磷、速效钾含量的平均值分别为41.07 g·kg^-1、8.35、1.16 g·kg^-1、0.65 g·kg^-1、5.60 g·kg^-1、47.94 mg·kg^-1、5.82 mg·kg^-1和100.60 mg·kg^-1。(3) 9种薹草属植物群落物种多样性与全氮、全磷、全钾、碱解氮、有机质、降雨量和海拔呈正相关关系,而与土壤pH、速效磷、速效钾呈负相关关系,且降雨量、土壤pH、速效磷和有机质对9种野生薹草属植物群落物种多样性影响较大。     

带状采伐后不同时期毛竹林恢复和土壤养分特征

为研究带状采伐毛竹林对竹林恢复和土壤养分的影响,以福建省建瓯市毛竹林为研究对象,设置5 m(处理1,C₁)和7 m(处理2,C₂)2种采伐宽度,以不进行采伐处理为对照(CK),研究采伐后当年新鞭生长期(I时期,2018年10月)和采伐后次年新立竹生长期(Ⅱ时期,2019年6月)新竹生长相关指标和土壤养分变化特征。结果表明：(1)C₁、C₂、CK处理的出笋数量分别为2 227、2 650和1 955株·hm^-2,且C₂与C₁、CK差异显著(P<0.05);退笋率各处理之间无显著差异(P>0.05),表现为C₁2。(2)2种采伐处理的胸径(DBH)显著低于CK,表现为CK>C₂>C₁。(3)采伐后Ⅰ时期和Ⅱ时期相比,土壤全磷(TP)和全钾(TK)含量增加,全氮(TN)和全碳(TC)含量降低;采伐后I时期的C₁、C₂处理中土壤TN、TP、TK和TC含量均大于CK,但采伐后Ⅱ时期的土壤TC含量小于CK。研究认为,带状采伐能提高出笋量和立竹数,增加土壤氮磷钾养分含量;7 m带状采伐竹林恢复状况整体上优于5 m带状采伐。     

冰雪灾害对杉木林土壤特性的影响

2008年初,在波及我国南方大部分地区的雨雪冰冻灾害中,冻雨在杉木枝叶上形成冰柱,造成大量的杉木个体折冠。通过开展杉木林凋落物和树干残体的养分及土壤理化性质的研究,可以了解冰雪灾害后杉木林的土壤肥力动态。冰雪灾害造成的林冠折损引起了林地的光照增强,导致了土壤温度上升及土壤水分增加,从而促进了凋落物的分解,凋落物经过1a的分解后,N、P和K含量分别下降了7%、12%和21%。凋落物储量减少了22%,N、P和K的储量分别下降了27%、31%和38%。2009年树干残体的N和P含量分别上升5%和6%,而K含量降低15%。树干残体由于分解缓慢,其储量下降3%,N储量增加了2%,P储量不变,而K储量下降了18%。冰雪灾害后森林凋落物积累于地表,分解后形成较厚的有机质层,土壤结构因此变得疏松。2009年的土壤容重和毛管孔隙度减小,总空隙度和毛管持水量增加,非毛管孔隙显著增加。林冠残体在分解过程中促进了土壤有机质和养分的积累。2009年的土壤pH降低,有机质、全N、全P和全K含量分别增加了16%、11%、14%和8%,碱解N和速效P含量分别增加了113%和17%,而速效K含量下降了36%。     

基于主成分分析的古树土壤肥力综合评价

以广州市海珠区登记在册的40株古树为研究对象,调查其生长状况,采集土壤测定pH、EC值、容重、通气度、有机质、全N、全P、全K、水解N、有效P、速效K含量等11项理化指标,采用主成分分析和聚类分析对古树土壤肥力进行综合评价.结果表明:海珠区大多数古树土壤EC值偏低(<0.35 mS·cm-1),表现为强变异;土壤有机质...     

黔中喀斯特山区村级尺度土壤养分空间变异性及其与水稻产量的关系

以贵州省安顺市西秀区旧州镇文星村为研究区域,采用地统计学方法,研究了黔中喀斯特山区土壤pH值、有机质、碱解氮、有效磷、速效钾、全氮、全磷、全钾、有效铜、有效锌、有效铁、有效锰和水稻产量的空间变异规律及其相互关系.结果表明: 土壤pH值、碱解氮、有效磷、速效钾、全磷、有效铜及水稻产量构成因素的C₀/(C₀+C)<25%,表现为强烈的空间相关性,有机质、全氮、全钾、有效锌、有效铁、有效锰及水稻产量的C₀/(C₀+C)为25%~75%,具有中等空间相关性.土壤速效钾含量与水稻产量关系最为密切,偏相关系数达到极显著水平(r=0.4669,P<0.0001),土壤碱解氮、速效钾和有效磷对有效穗数和千粒重的直接通径系数均为正值,其大小顺序与偏相关分析结果一致.克里金插值结果表明,土壤有机质、碱解氮、速效钾、全氮、有效铜、有效锌的含量在研究区均存在从西南向东北逐渐递减的趋势;产量在西北部及东南部较高.     

Effects of Soil Properties on the Transfer of Cadmium from Soil to Wheat in the Yangtze River Delta Region, China—a Typical Industry–Agriculture Transition Area

In order to identify the effects of soil properties on the transfer of Cd from soil to wheat under actual field conditions, 126 pairs of topsoil and wheat samples were collected from the Yangtze River delta region, China. Relevant parameters (Cd, Ca, Mg, Fe, Mn, Zn, N, P, K, S, pH, total organic carbon, and speciation of soil Cd) in soil and wheat tissues were analyzed, and the results were treated by statistical methods. Soil samples (19.8%) and 14.3% of the wheat grain samples exceeded the relevant maximum permissible Cd concentrations in China for agricultural soil and wheat grain, respectively. The major speciations of Cd in soil were exchangeable, bound to carbonates and fulvic and humic acid fraction, and they were readily affected by soil pH, total Ca, Mg, S and P, DTPA-Fe, Ex-Ca, and Ex-Mg. Cadmium showed a strong correlation with Fe, S, and P present in the grain and the soil, whereas there was no significant correlation in the straw or root. Generally, soil pH, Ca, Mg, Mn, P, and slowly available K restricted Cd transfer from soil to wheat, whereas soil S, N, Zn, DTPA-Fe, and total organic carbon enhance Cd uptake by wheat.     

涪陵茎瘤芥种植区土壤肥力与产量的关系

采用田间调查研究和室内化学分析方法,研究了涪陵区主要茎瘤芥种植区土壤肥力因子及其与茎瘤芥产量的关系.结果表明: 茎瘤芥种植区土壤有效钙、镁、铁、锰、铜和锌含量较丰富,分别为3034、260、11.2、26.1、1.15和1.50 mg·kg^-1,有效磷适中,为19.3 mg·kg^-1;但有机质、碱解氮、速效钾和有效硫含量较为缺乏,分别为9.05 g·kg^-1、89.2 mg·kg^-1、106 mg·kg^-1和27.0 mg·kg^-1.茎瘤芥产量与土壤pH、有效钙呈极显著正相关,而与有效铁呈极显著负相关关系.土壤肥力因子对茎瘤芥产量的影响为：有效锰>有效铜>pH>有效铁>速效钾>有效钙>有效镁>有效硫>碱解氮>有效锌>有机质>有效磷;通过逐步回归分析剔除不显著变量,建立了土壤有效钙与茎瘤芥产量间的线性方程:Y=31636+3.63X₆.
     

Effect of annual variation in soil pH on available soil nutrients in pear orchards

Soil pH is an important factor affecting the availability of soil nutrients that impact plant growth. Given the susceptibility of soil pH to excessive fertilization and the widespread use of manures, it is essential to examine the influence of soil pH on the distribution and availability of soil nutrients. We sampled and analyzed brown soils from pear orchards in thirteen towns in Wendeng county. Samples were obtained from areas along or between rows of trees at specified distances and depths. The results showed that the soil pH fluctuated from 4.06 to 6.59 in October 2008 and from 4.24 to 7.57 in April 2009. The quantity of soil samples with pH below 5.50 increased by 34.6%. Analysis of the soil pH for samples obtained along the rows of trees showed that the pH decreased as the depth increased (except for the range 5.5 to 6.0); soil pH in the samples obtained between the rows of trees demonstrated different trends. The average organic matter (O.M.) content as well as the N (NH₄⁺) and available P, K, Cu, Zn, Fe, and Mn contents in the samples collected in October 2008 were higher than those observed in April 2009. Conversely, the values for other available nutrients were lower than those in the samples collected in April 2009. The available nutrients and organic matter (O.M.) content in different pH ranges varied. The soil pH was significantly or very significantly correlated with N (NH₄⁺ and NO₃^-), available K, Cu, Fe, and exchangeable Ca for the October 2008 samples, while a significant or very significant correlation existed between N (NH₄⁺), available P, Zn, exchangeable Ca, and exchangeable Mg for the April 2009 samples. The correlations between soil pH and the amounts of available nutrients and organic matter (O.M.) along the rows of trees in September 2009 were nearly consistent with those between the rows.     

Effect of annual variation in soil pH on available soil nutrients in pear orchards

Soil pH is an important factor affecting the availability of soil nutrients that impact plant growth. Given the susceptibility of soil pH to excessive fertilization and the widespread use of manures, it is essential to examine the influence of soil pH on the distribution and availability of soil nutrients. We sampled and analyzed brown soils from pear orchards in thirteen towns in Wendeng county. Samples were obtained from areas along or between rows of trees at specified distances and depths. The results showed that the soil pH fluctuated from 4.06 to 6.59 in October 2008 and from 4.24 to 7.57 in April 2009. The quantity of soil samples with pH below 5.50 increased by 34.6%. Analysis of the soil pH for samples obtained along the rows of trees showed that the pH decreased as the depth increased (except for the range 5.5 to 6.0); soil pH in the samples obtained between the rows of trees demonstrated different trends. The average organic matter (O.M.) content as well as the N (NH₄⁺) and available P, K, Cu, Zn, Fe, and Mn contents in the samples collected in October 2008 were higher than those observed in April 2009. Conversely, the values for other available nutrients were lower than those in the samples collected in April 2009. The available nutrients and organic matter (O.M.) content in different pH ranges varied. The soil pH was significantly or very significantly correlated with N (NH₄⁺ and NO₃^-), available K, Cu, Fe, and exchangeable Ca for the October 2008 samples, while a significant or very significant correlation existed between N (NH₄⁺), available P, Zn, exchangeable Ca, and exchangeable Mg for the April 2009 samples. The correlations between soil pH and the amounts of available nutrients and organic matter (O.M.) along the rows of trees in September 2009 were nearly consistent with those between the rows.     

黑土开垦后水稳性团聚体与土壤养分的关系

研究了黑土开垦后水稳性团聚体变化规律及其与土壤养分状况的关系．结果表明,黑土开垦初期,水稳性团聚体的含量迅速下降．在开垦的第一个10年,水稳性团聚体下降约10％;随着开垦时间的延长,其下降幅度趋缓,第10年～第50年,水稳性团聚体仅下降10％,之后下降幅度更加缓慢,接近一个稳定的水平．黑土中>0．25mm水稳性团聚体与土壤的有机碳、全氮、全磷和CEC具有良好的相关性,相关系数分别为0．7625、0．6794、0．6084和0．8134,均达到极显著水平;与交换性钙、交换性镁、交换性钾和交换性钠的相关性也达到极显著水平;在回归关系中,与有机碳和CEC之间的关系更密切,与全钾、速效磷、速效K和缓效K没有明显的相关性．要保持黑土良好的结构状况,土壤有机碳变化应处于平衡状态。     

祁连山西水林区土壤阳离子交换量及盐基离子的剖面分布

以祁连山西水林区分布的棕钙土、灰褐土、栗钙土和高山草甸土为对象,研究了阳离子交换量和盐基离子(K+、Na+、Ca2+、Mg2+)的剖面分布规律及其与土壤理化因子的关系。结果表明:土壤阳离子交换量(CEC,介于4.80—48.10 cmol/kg)和盐基总量(TEB,介于4.67—21.34 cmol/kg)随剖面深度的增加逐渐减小,不同土壤类型的大小顺序为:灰褐土>高山草甸土>栗钙土>棕钙土;土壤盐基组成以Ca2+、Mg2+为主(占TEB的比例平均为71.6%、22.9%),K+、Na+所占比例较低(占TEB的比例平均为3.3%、2.2%);棕钙土、灰褐土和栗钙土盐基离子的剖面分布由浅至深呈现:K+≈Ca2+>Na+≈Mg2+,高山草甸土盐基离子则呈现:K+>Na+>Mg2+>Ca2+。不同土壤类型间盐基离子的含量及饱和度随发生层次不同存在较大差异。土壤有机质是CEC的主要贡献因素,粉粒对CEC也有显著的促进作用,而砂粒、CaCO3对CEC有显著抑制作用。土壤生物复盐基作用弱于淋溶作用,造成盐基饱和度较大(BSP,介于44.4%—97.2%),并随剖面深度的增加逐渐增大。相关性分析表明,土壤交换性Na+、Mg2+的含量及饱和度均呈极显著正相关,交换性Na+、Mg2+饱和度与CaCO3含量呈极显著正相关;pH值与BSP呈极显著正相关;土壤速效P含量与CEC呈极显著正相关,速效K含量与交换性K+含量呈极显著正相关。     

我国23个土壤磷素淋失风险评估Ⅱ.淋失临界值与土壤理化性质和磷吸附特性的关系

从13个省（市）采取23个耕地表层土壤,通过室内模拟试验测定其磷素淋失临界值和pH、有机质、＜0.01mm、＜0.002mm、交换性钙镁、活性铁铝、磷等温吸附特性等,以建立土壤磷素淋失临界值与土壤基本理化性质和磷吸附特性之间的关系.结果表明：土壤pH＜6.0时,随土壤pH提高临界值增加,土壤pH与临界值之间呈显著的指数关系;而当土壤pH＞6.0时,随土壤pH提高临界值减小,在pH6.5左右土壤磷素淋失临界值最高.土壤磷素淋失临界值与土壤有机质、活性铁（铝）、交换性钙之间存在显著的相关,而与交换性镁、CEC、＜0.01mm、＜0.002mm、K、Qm的相关性受土壤酸碱度影响.可以通过测定土壤有机质或活性铁的含量,来计算土壤磷素淋失临界值,评价土壤磷素淋失的风险.供试的23个土壤,除了采自湖北潜江的20号水稻土存在比较大的磷素淋失风险,其余土壤发生磷素淋失的风险很小.     

Gains and losses in soil nutrients associated with harvesting and burning eucalypt rainforest

In mixed eucalypt/rainforest in southern Tasmania, samples of surface soil 0 to 2 cm, 2 to 5 cm, and 5 to 10 cm were taken from a clear-felled coupe before and after burning in 1982, from a similar coupe after burning in 1979, and from an uncut area adjacent to each coupe. Factors compared were bulk density; total organic C, N, P, Ca, Mg, and K; pH; exchangeable Ca, Mg, and K; cation exchange capacity; extractable P; and N-mineralisation rates. The effect of burning was found to be restricted mainly to the upper 2 cm of soil. The combustion of organic matter caused losses of 7360 kg organic C and 211 kg N/ha; 348 kg Ca and 282 kg Mg and 151 kg K/ha were added to the soil in ash. Burning caused significant increases in pH, exchangeable Ca, Mg, and K, and in extractable P; cation exchange capacity was reduced. In the 6 months after burning only K was leached from the upper 2 cm of soil. Equilibrium levels of NH₄?N increased initially after the fire, but between 6 and 18 months, equilibrium levels and rate of production of NH₄?N during anaerobic incubation in soil of burned coupes differed little from that in adjacent uncut forest. Rates of production of NO₃?N during aerobic incubation were very low throughout the period of study. It is concluded that for soils developed on dolerite in mixed eucalypt/rainforest, a single regeneration burn probably improves the nutritional status of the soil. Nutrients lost from the area as particulate ash are in quantities that will probably be replaced in rainfall in 15 to 20 years.     

阿拉善荒漠灌木根际中、微量元素含量特征

探讨了阿拉善干旱荒漠区霸王、白刺、红砂、沙冬青、沙木蓼、梭梭和驼绒藜7种旱生灌木根际与非根际土壤Ca、Mg、Fe、Mn、Zn、Cu的含量特征.结果表明:(1)除梭梭根际pH值高于非根际之外,其余6种灌木根际土壤均表现出不同程度的酸化作用.(2)7种灌木根际全钙和交换性钙的含量均低于非根际.除沙木蓼和驼绒藜外,其余5种灌木根际全镁含量均高于非根际,白刺的富集率最高,为43.04%;除沙木蓼外,其余灌木根际交换性镁的含量均有所富集,梭梭的富集率最高,为26.52%.(3)7种灌木根际全铁、全锰、全锌含量总体上小于非根际,但是根际有效铁、有效锰、有效锌含量均大于非根际,表现出明显的富集效应,沙木蓼根际有效铁、有效锰、有效锌的富集率最高,分别为:29.76%、20.92%、86.99%.(4)沙木蓼根际全铜和有效铜含量略高于非根际.梭梭根际全铜含量低于非根际,但梭梭根际有效铜含量却有富集的趋势.其余五种灌木根际全铜和有效铜含量均低于非根际.(5)根际及非根际土壤各养分性状之间,存在复杂的相关性.