青藏高原东北缘不同土地利用类型土壤质量综合评价

土壤质量评价是合理利用土壤资源的重要前提。通过采集青藏高原东北缘甘肃省天祝县境内林地(n=9)、草地(n=18)和耕地(n=38)土壤样品,并测定土壤容重、田间持水量和有机质等13项土壤理化性质指标,采用主成分分析和相关性分析构建最小数据集(MDS),建立土壤质量评价指标体系,对3个不同土地利用类型的土壤质量进行综合评价。结果表明: 林地的总孔隙度、毛管孔隙度、田间持水量、毛管持水量、饱和含水量、有机质、全氮和速效钾含量显著高于草地和耕地。林地土壤质量评价指标体系包括田间持水量、有机质、全氮、速效氮和速效钾,土壤质量指数(SQI)介于0.329～0.678,平均值为0.481;草地土壤质量评价指标体系包括田间持水量和速效氮,SQI介于0.302～0.703,平均值为0.469;耕地土壤质量评价指标体系包括毛管持水量、非毛管孔隙度、速效氮、速效磷和速效钾,SQI介于0.337～0.616,平均值为0.462。影响林地、草地和耕地土壤质量的最大障碍指标分别为速效钾、田间持水量和毛管持水量。基于MDS的土壤质量指数能够实现研究区不同土地利用类型土壤质量的准确评价,土壤质量整体上表现为林地>草地>耕地,评价结果对该区域土壤可持续管理具有重要参考价值。     

川中丘陵区土地利用方式对土壤理化性质影响的灰色关联分析

以川中丘陵区小流域为研究对象,研究了坡耕地、坡改梯、甜橙林和水保林4种土地利用方式以及裸地(对照)对0～10和10～20 cm土壤容重、土壤孔隙度及土壤养分含量的影响.结果表明: 同一土地利用方式下,毛管孔隙度、非毛管孔隙度、总孔隙度、有机质、全氮、全磷、碱解氮、有效磷、速效钾随土层加深而减小,而土壤容重则相反,全钾层间差异不大.相同土层甜橙林毛管孔隙度、非毛管孔隙度、总孔隙度、全磷、有效磷含量最大,容重最小,水保林全氮、碱解氮含量最高,水保林0～10 cm土层的有机质含量最高,甜橙林10～20 cm土层的有机质含量最高.0～10 cm土层,灰色关联度从大到小依次为水保林(0.9441)、甜橙林(0.8858)、梯平地(0.6300)、裸地(0.5397)、缓坡耕地(0.4714);10～20 cm土层,灰色关联度依次为水保林(0.8919)、甜橙林(0.8401)、梯平地(0.5773)、裸地(0.5301)、缓坡耕地(0.5175).水保林改善土壤理化性质作用最佳,缓坡耕地改良效果最差.     

华南地区八种人工林的土壤物理性质

研究了华南地区8种林地的土壤物理性质,根据其土壤特点分为4类。第1类为马占相思林地、黎蒴-加勒比松林地、火力楠-木荷林地、木荷林地和湿地松林地,特点是上层的土壤容重小于中层和下层,毛管孔隙度中等或较小,非毛管孔隙度中等或较大,非毛管孔隙度和总孔隙度为上层大于中层和下层,自然含水量中等或较大,随着土壤深度的增加而下降或稳定。除了马占相思林地上层外,毛管持水量为中等或较小;第2类为柚木林地,土壤容重较大,且3层土壤的容重相近,毛管孔隙度和毛管持水量较大,非毛管空隙度和自然含水量较小;第3类为落羽杉林地,各层土壤的自然含水量远远大于其他林地。上层和中层的土壤容重、毛管孔隙度和非毛管空隙度中等,毛管持水量大。下层的土壤容重和非毛管空隙度大、毛管空隙度和毛管持水量小。第4类为尾叶桉林地,上层的土壤容重大于中层和下层,毛管孔隙度和毛管持水量较大,非毛管空隙度和自然含水量较小。     

亚热带不同树种土壤水源涵养功能

亚热带地区由于大面积的砍伐使天然林被人工林所代替,对森林土壤水源涵养功能造成了很大影响。树种可以通过自身特性来改变土壤物理结构进而影响土壤持水能力,因此合理选择树种对区域水源涵养具有重要意义。然而,立地条件的差异往往会对实验结果产生影响。为减少立地条件的差异,2012年2月在土壤发育和经营历史相同的林地上建立了中亚热带常见树种同质园。2019年8月测定了种植12个树种后不同土层(0—10、10—20、20—30、30—40 cm和40—50 cm)的土壤容重、含水量、总/毛管/非毛管孔隙度、最大/毛管/非毛管持水量和蓄水量。结果表明,种植不同树种7年后,土壤容重、含水量、总/毛管/非毛管孔隙度、最大/毛管/非毛管持水量和蓄水量均在表层(0—20 cm)土壤中差异显著,而在深层(20—50 cm)土壤中差异不显著。土壤孔隙度、持水量和蓄水量均与土壤容重呈显著负相关关系,而与土壤含水量呈显著正相关关系。与其他树种相比,种植鹅掌楸、枫香和全缘叶栾树等落叶阔叶树种可在较短时间内增加土壤孔隙度,提高土壤持水量和蓄水量。因此,在亚热带人工林经营管理中,可在杉木、马尾松纯林中适当引入鹅掌楸、枫香和全缘叶栾树等落叶阔叶树种,提升亚热带森林土壤水源涵养功能。     

上海外环线绿地群落凋落物对土壤水分物理性质的影响

选取上海外环线绿化带8个人工植物群落为对象,以裸地为对照,研究了凋落物量、土壤孔隙性状和持水特性,探讨了城市绿地群落凋落物对土壤水分物理性质的影响.结果表明:各群落0～10 cm土壤的最大持水量、毛管持水量、最小持水量、质量含水量、体积含水量、毛管孔隙度、非毛管孔隙度、总孔隙度和土壤通气度均显著高于裸地(P<0.05),而容重均显著低于裸地(P<0.05);10～20 am土壤水分物理性质差异不显著;凋落物年凋落量与绿地群落0～10 cm土壤毛管孔隙度呈显著负相关,而与绿地群落0～10 cm土壤持水特性相关性均不显著;凋落物现存量与绿地群落0～10 cm土壤总孔隙度和通气度呈显著正相关,与0～10 cm土壤容重呈显著负相关;而凋落物年凋落量、现存量与绿地群落10～20 cm土壤水分物理性质相关性均不显著;绿地群落凋落物蓄积能有效改善绿地群落内表层土壤(0～10 cm)水分物理性质,主要是改良土壤孔隙状况;在绿地养护中应保留绿地群落凋落物.     

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。     

冰雪灾害对粤北杉木林土壤物理性质的影响

2008 年1 月至2 月, 雨雪冰冻天气袭击广东粤北地区。冻雨在枝叶上形成冰柱, 造成大量的折干残体。冰雪灾害对森林土壤的影响是森林恢复和管理的关键所在, 然而对灾害引起土壤物理性质的变化研究甚少。为了研究冰雪灾害对土壤物理性质的影响, 在粤北乐昌林场杉木林内建立三个面积为20 m×20 m 的固定标准地, 分别在标准地中心以及四个角采集上土层(0-20 cm)和下土层(20-40 cm)的土样, 测定土壤物理性质: 土壤容重、毛管持水量、总孔隙度、毛管孔隙度、非毛管孔隙度和通气孔隙度。研究结果表明: 与2008 年相比, 2011 年杉木林地土壤容重降低, 而土壤毛管持水量、总孔隙度、毛管孔隙度、非毛管孔隙度和通气孔隙度均升高, 说明冰雪灾害对土壤物理性质有重要影响。     

不同植被恢复模式下煤矸石山复垦土壤性质及煤矸石风化物的变化特征

为了探讨植被恢复模式对煤矸石山复垦土壤和矸石风化物的影响,对煤矸石山6种主要植被类型(刺槐林、刺槐-柠条混交林、榆树-紫穗槐混交林、侧柏-刺槐混交林、荆条林、紫花苜蓿草丛)下土壤和煤矸石风化物的理化性状及重金属进行了比较研究。结果表明:(1)煤矸石山上种植植被可使土壤容重、土壤持水量和孔隙度明显改善。乔木模式更明显。矸石山植被恢复后,可明显增加土壤养分含量。不同植被模式下,土壤养分增加存在显著差异。侧柏-刺槐和榆树-紫穗槐混交模式效果较好。(2)植被对煤矸石风化物容重和机械组成改善作用依次为针阔混交林>乔灌林>乔木纯林>灌木林>草本。植被促进有机质与全氮积累依次为:侧柏-刺槐>刺槐>刺槐-柠条>榆树-紫穗槐>荆条>紫花苜蓿。荆条林下煤矸石风化物全P含量最大。荆条林与侧柏-刺槐混交林利于速效P积累。对速效K积累有利的是荆条林与榆树-紫穗槐混交林。(3)植被种植可以减少煤矸石风化物中重金属含量。榆树-紫穗槐混交模式对减低超标重金属Cd的效果好,其次是针阔混交林(侧柏-刺槐)。对于超标重金属As而言,侧柏-刺槐模式优于其它植被模式,基本达到重金属As不超标。     

辽西低山丘陵区人工油松林和沙棘林的水文生态效应

利用设置在不同地类内的径流小区,对辽西大凌河流域的沟壑丘陵区进行定位观察,探讨辽西半干旱区主要造林树种油松和沙棘的水文生态效应.结果表明：2002年6月～2004年6月平均降水量为238.9mm时,油松和沙棘平均林冠截留量分别为55.5mm和76.05mm,其截留率分别为23.08%和32.28%,即约有1/4～1/3降水被林冠截留.油松林中凋落物平均截留率为14.17%,沙棘林为20.8%.油松林和沙棘林年均径流深分别为2.516mm和0.893mm;侵蚀量为15.57t km^-2和0.76t km^-2;林地内径流深和侵蚀量约为荒地（对照）的1/20和1/50.林地土壤理化性质,除土壤容重之外,0～20cm土层的总孔隙度、非毛管孔隙度、饱和含水量和非毛管持水量都高于2～40cm土层;油松林和沙棘林土壤有机质、全氮、全钾和速效钾含量均显著高于荒地;pH、全磷和速效磷在地类和不同土层深度中没有显著差异.沙棘林和油松林的非毛管持水量分别是荒地的275.9%和182.1%.     

添加山皮土和秸秆对铁尾矿基质性质及植物生长的影响

铁尾矿砂作为复垦基质是实现其资源化利用的有效途径。本研究以室内盆栽法探究山皮土和秸秆对铁尾矿基质性质及紫穗槐幼苗生长的影响。处理因素为山皮土添加比例(0%、25%、50%、75%、100%)和秸秆添加比例(1%、3%、5%)。结果表明:添加山皮土能降低基质容重、全P、速效P含量,提高了田间持水量、阳离子交换量、全K和速效K含量;添加秸秆降低了基质容重,提高了田间持水量、阳离子交换量、全N、全P、速效N、速效K和TOC含量。在紫穗槐生长效果上,添加山皮土提高了紫穗槐幼苗的株高、根长、地径、冠幅和生物量;添加秸秆使紫穗槐幼苗的株高、根长、地径、冠幅和生物量呈现先增大后减小的趋势(3%1%、5%)。综合分析表明,紫穗槐幼苗在3%秸秆+100%山皮土处理下生长情况最佳,而3%秸秆+50%山皮土处理的各个指标均与1%秸秆+0%山皮土处理差异显著(P0.05),紫穗槐幼苗生长状况良好。因此,在实践中,在铁尾矿砂中添加3%秸秆+50%山皮土作为复垦配方可以更大限度地实现铁尾矿砂资源化利用。     

尾矿区不同植被恢复模式下高效固氮菌的筛选及Biolog鉴定

为了从铁尾矿中获得高效土著固氮菌,采用选择性无氮培养基从不同恢复模式下铁尾矿土样中筛选高效固氮菌,并且通过乙炔还原法对分离出的48株固氮菌进行固氮酶活性测定。结果表明:筛选出两株具有较高固氮活性菌株Db1与Ec1,Biolog鉴定为固氮菌属(Azotobacter),固氮比活力分别为203.20 nmol·mg-1·h-1和307.23 nmol·mg-1·h-1。不同植被恢复模式、物种多样性、尾矿坡向、工程措施、恢复年限均对尾矿固氮菌株数量有影响。样地处于尾矿阳坡,或属于人造混交林,或植被恢复年限长,又或者实施六孔砖、坡岩造地等工程措施的尾矿植被恢复模式下筛得的固氮菌菌株数较多或固氮活力较高。     

Taxon specific response of carabids (Coleoptera,Carabidae) and other soil invertebrate taxa on invasive plant Amorpha fruticosa in wetlands

False indigo (Amorpha fruticosa L.) is an invasive exotic plant introduced to Europe in the early eighteenth century. Its spread has been rapid, particularly in disturbed wetland habitats, where it forms dense impermeable monospecific stands and modifies habitat conditions. The impact of A. fruticosa on native plant communities has been well analyzed, however knowledge concerning the possible effects on soil invertebrates and particularly carabid beetles is completely lacking. This study analyzed the impact of an A. fruticosa invasion on carabid beetles and other soil invertebrates. Soil fauna was sampled by pitfall traps at natural habitats, initially colonized by A. fruticosa, and habitats largely invaded by A. fruticosa. In total 2,613 carabid beetles belonging to 50 species and 72,166 soil invertebrates were collected. The invasion of A. fruticosa strongly affected the carabid beetle species composition, which clearly differed between all studied sites. Widespread euritopic carabid beetle species showed positive responses to A. fruticosa invasion, while the activity density of open habitat species strongly declined. Mean individual biomass was significantly higher at invaded sites due to increased incidence of large carabids (genus Carabus Linné, 1758). Carabid beetle activity density and abundance of soil invertebrates were considerably higher at invaded sites than in natural sites. Conversely, the impact of A. fruticosa on carabid beetle species richness and diversity was less pronounced, most likely due to immigration from adjacent habitats. Changes in carabid beetle species composition and abundance of soil invertebrates were most likely due to changes in vegetation structure and microclimate. The results suggest that A. fruticosa invasion considerably affected carabid beetles, an insect group that is only indirectly related to plant composition. Therefore, severe future changes can be expected in invertebrate groups that are closely related to plant composition, since A. fruticosa cannot be completely removed from the habitat and covers relatively large areas.     

Phytoremediation potential of transplanted bare-root seedlings of trees for lead/zinc and copper mine tailings

Selecting plant species that can overcome unfavorable conditions and increase the recovery of degraded mined lands remains a challenge. A pot experiment was conducted to evaluate the feasibility of using transplanted tree seedlings for the phytoremediation of lead/zinc and copper mine tailings. One-year-old bare-root of woody species (Rhus chinensis Mill, Quercus acutissima Carruth, Liquidambar formosana Hance, Vitex trifolia Linn. var. simplicifolia Cham, Lespedeza cuneata and Amorpha fruticosa Linn) were transplanted into pots with mine tailings and tested as potential metal-tolerant plants. Seedling survival, plant growth, root trait, nutrient uptake, and metal accumulation and translocation were assessed. The six species grew in both tailings and showed different tolerance level. A. fruticosa was highly tolerant of Zn, Pb and Cu, and grew normally in both tailings. Metal concentrations were higher in the roots than in the shoots of the six species. All of the species had low bioconcentration and translocation factor values. However, R. chinensis and L. formosana had significantly higher translocation factor values for Pb (0.88) and Zn (1.78) than the other species. The nitrogen-fixing species, A. fruticosa, had the highest tolerance and biomass production, implying that it has great potential in the phytoremediation of tailing areas in southern China.     

根系固土主导力学因素与差异性评价

为了探究影响根系固土的主导力学因素,并为侵蚀区固土抗蚀植物种的筛选提供部分依据。以3—4年生(4年生为主)5种内蒙古干旱、半干旱地区常见的水土保持植物:柠条(Caragana microphylla Lam.)、沙柳(Salix psammophila C.wang et Ch.Y.Yang)、沙地柏(Sabina vulgaris Ant.)、白沙蒿(Artemisia sphaerocephala Krasch.)、沙棘(Hippophae rhamnoides Linn.)为研究对象,针对春季土壤干旱和夏季暴雨(土壤湿润)两种自然条件,对影响5种植物根系固土的10项指标进行主成分分析。结果表明,根系抗拉力学特性是影响植物根系固土的主导力学因素,其次为根-土界面摩阻特性,最后是根-土复合体抗剪特性。在此基础上,从根系力学特性的角度出发,运用层次分析法对两个时期5种植物根系固土能力的差异性进行评价。在评价过程中,为了保证评价数据完整性,减小专家主观因素所带来的误差,使评价结果更具科学性,该文将两个时期主成分分析所得3个力学特性的方差贡献率作为权重。评价结果显示,根系固土指数为:春季土壤干旱时期,柠条(0.834)沙柳(0.330)沙地柏(-0.066)白沙蒿(-0.206)沙棘(-0.864);夏季暴雨时期分别为,柠条(0.876)沙地柏(0.218)沙柳(0.065)白沙蒿(-0.404)沙棘(-0.755)。5种植物中,柠条根系的抗拉力学特性显著优于其他植物,可作为干旱、半干旱地区固土抗蚀的重要参考树种。     

Plant species effect on the spatial patterns of soil properties in the Mu-us desert ecosystem,Inner Mongolia,China

Although Artemisia ordosica Krasch. and Sabina vulgaris Ant. are the dominant shrub species in the Mu-us desert ecosystem, they differ in their botanical traits. We investigated the spatial patterns of soil properties using geostatistical analysis to examine the effect of plant species on these spatial patterns. Comparison among three microsite types (under A. ordosica, under S. vulgaris, and the opening between vegetation) showed that A. ordosica generally had less effect than S. vulgaris on local soil properties. The long life-span, prostrate life-form, and evergreen leaf-habit of S. vulgaris may lead to a higher accumulation of organic and fine materials under S. vulgaris. The range of spatial autocorrelation found in the mass of organic matter on the soil surface was smaller than that of the coverage of S. vulgaris (11.5 m) which corresponded to the canopy patch size of this species, and was longer than the canopy patch size of A. ordosica. The ranges of total C and N, and pH (11.7–15.6 m) were similar to that of S. vulgaris. The range of available P (106.3 m) was comparable to that of the coverage of A. ordosica (86.2 m) considered to be the scale of the distribution of this species. The ranges of silt+clay and exchangeable K, Ca, and Mg (31.0–46.7 m) were not related to plant presence, and were similar to that of topography (43.1 m).     

赣榆县厉庄地埂利用型式试验

在赣榆县厉庄以大金鸡菊、紫穗槐和红柳三种经济植物进行了地埂利用型式试验,取得了比较明显的水土保持效果和改善农田小环境的生态效益。栽植后第三年植物覆盖率达90％或100％;地面蒸发量减少15.2～17.7％;截留降水量为0.5～0.7mm;大气相对湿度提高3.7～5.4％;土壤养分也有不同程度的增加。经济效益估测每亩地埂可收到300～600元,比种黄豆高5～9倍。效益最好的是红柳,大金鸡菊次之,紫穗槐较低。     

Autecology, distributional expansion and negative effects of Amorpha fruticosa L. on a river ecosystem: a case study in the Sendaigawa River, Tottori Prefecture

Amorpha fruticosa L., introduced from the eastern part of North and Central America as a revegetation material for artificial slopes, has escaped into riverbeds in Japan, and its negative effects are of concern. In this study, an attempt has been made to clarify the actual extent of escape and establishment of A. fruticosa, through a case study of the Sendaigawa River, Tottori Prefecture, coupled with a survey of national distribution using the National Censuses on River Environments. The autecology of A. fruticosa, including phenology, germination, allelopathy and coppicing ability, was also studied by observation and experiments. The following conclusions were drawn: A. fruticosa preferred sunny sites; the total established area in the study site was 7,500 m²; A. fruticosa showed strong coppicing ability; there was lower species diversity in and around areas populated by A. fruticosa; and A. fruticosa has been expanding its area both in the watershed of Sendaigawa River region and nationwide. The authors emphasize the importance of quick control of A. fruticosa.     

臭柏群落在不同演替阶段某些群落特征的研究

毛乌素沙地臭柏群落自发演替的基本过程为：半流动沙地沙竹 +沙米（有时是白沙蒿）群落→半固定沙地油蒿+臭柏群落→固定沙地臭柏+硬质早熟禾群落→固定沙地臭柏群落→老固定沙地臭柏+苔藓群落,最后可能发展成为地带性的本氏针茅草原。演替早期向演替亚顶级群落发展过程中物种多样性逐步增加,生态环境逐渐变湿。随着臭柏的衰退,某些喜湿植物的退出,物种多样性开始减少,群落生境向旱生化发展。     

乡土植物生活型构成对川渝地区边坡植被水土保持效益的影响

乡土植物灌木化建植是高速公路边坡防护的重要生态模式。为了探讨生态恢复过程中乡土植物的生活型构成对边坡植被水土保持效益的影响,揭示乡土植物生活型-物种多样性-生态系统功能间的偶合关系,借助3个物种配置试验,于2009年4月构建了以草本、灌木或乔木为主体的草本型、灌木型、乔木型绿化配置及草-灌-乔混合型试验区。自建植次年(2010年)起,对试验区进行持续5a生态监测。结果表明:1)边坡植被的物种丰富度与乡土植物的生活型有关,呈现乔木型灌木型草-灌-乔混合型草本型趋势;2)植被的物种多样性(Shannon-Wiener指数、Pielou指数)与乡土植物生活型构成及建植年限有关:建植后第1、第2年,多样性水平呈草本型草-灌-乔混合型灌木型乔木型变化趋势;自建植后第三起(2012—2014年),呈草-灌-乔混合型草本型灌木型乔木型波动;3)植被的水土保持性能(径流系数、侵蚀模数)与群落的物种多样性密切相关:多样性水平越高,水土保持性能越强。可见,乡土植物的生活型构成对提高边坡植被的物种多样性、改善生态性能至关重要。