铅锌矿废弃地尾矿砂对银合欢幼苗定居的影响

研究了广东省仁化县韶关凡口铅锌矿废弃地尾矿砂对银合欢（Leucaena glauca)幼苗定居的影响。结果表明，尾矿砂各Pb、Zn、Cu、Cd等重金属含量极高，Pb、Zn比对照土壤高100倍左右，Cu、Cd高4－5倍，植物对重金属的吸收、积累量较大，且多集中于根部。尾矿砂中硝态氮（NO3^--N)和铵态氮（NH4^ -N)含量很低，仅为对照土壤的13％－23％。银合欢幼苗在尾矿砂中能生长，但其叶片光合色素含量较少，株高、复叶数、植株干物质量等生物量显著降低，这主要是由于重金属含量过高导致根系活力降低，限制了植物对水分和营养物质的吸收，其次是土壤贫瘠的影响。     

铅锌矿废弃地尾矿砂对银合欢幼苗定居的影响

研究了广东省仁化县韶关凡口铅锌矿废弃地尾矿砂对银合欢(Leucaena glauca)幼苗定居的影响。结果表明，尾矿砂中Pb、Zn、Cu、Cd等重金属含量极高，Pb、Zn比对照土壤高100倍左右，Cu、Cd高4～5倍，植物对重金属的吸收、积累量较大，且多集中于根部。尾矿砂中硝态氮(NO^-₃-N)和铵态氮(NH⁺₄-N)含量很低，仅为对照土壤的13%～23%。银合欢幼苗在尾矿砂中能生长，但其叶片光合色素含量较少，株高、复叶数、植株干物质量等生物量显著降低，这主要是由于重金属含量过高导致根系活力降低，限制了植物对水分和营养物质的吸收，其次是土壤贫瘠的影响。     

金属尾矿砂的改良和植被重建研究进展

针对金属尾矿砂的理化性状以及所带来的环境影响进行了简要介绍和评述,着重从改良的角度论述了我国治理修复金属矿区尾矿砂的研究进展、存在的问题和将来的发展方向。     

泥炭和化学肥料处理对黑麦草在铜矿尾矿砂上生长影响的研究

金属采矿产生的尾矿不但粒度小、重量轻、表面积大 ,堆放时易流动和形成塌漏 ,而且含有高浓度的重金属 ,对附近的村镇、农田、水源等构成极大威胁[1～ 3] 。因此 ,为保护环境、减小矿业开发对自然生态的破坏 ,金属尾矿库的土地复垦将非常必要[4 ,5] 。早期的结果表明 ,重金属的毒性和营养物质的缺乏是矿区植物定植的主要限制因子[6 ,7] 。添加改良剂和化学肥料来改变矿砂性质从而改善植物生长条件 ,实现尾矿库的植被恢复是一个可行的途径[8,9] 。有机物料的施用不但改善了尾矿砂较恶劣的物理性状 ,并且其分解产物具有一定的活性基团 ,很容易…     

钝化剂对铅锌尾矿砂中重金属的固化作用

铅锌尾矿砂重金属含量高,对环境危害大。为了减缓铅锌尾矿砂的重金属污染风险,采用室内培养实验方法,在铅锌尾矿砂中添加油菜秸秆、芒草秸秆、水稻秸秆、石灰和磷酸一铵等钝化剂,并通过DTPA及Tessier连续提取铅、锌、镉的化学形态,评价钝化剂对铅、锌、镉的移动性和生物有效性的影响。结果表明,油菜秸秆、芒草秸秆、水稻秸秆、石灰和磷酸一铵均显著地降低Cd的生物有效性及其迁移能力;磷酸一铵、油菜秸秆均能有效地降低尾矿砂中Pb的生物有效性及其迁移能力,尤其是磷酸一铵有极显著的效果;油菜秸秆、芒草秸秆、水稻秸秆和磷酸一铵均能有效地降低尾矿砂中Zn的生物有效性及其迁移能力。尾矿砂中DTPA态Cd、Zn与交换态、碳酸盐结合态Cd、Zn极显著正相关,DTPA态Pb与碳酸盐结合态Pb极显著正相关。从Pb、Cd、Zn生物有效态含量的减少方面考虑,油菜秸秆和磷酸一铵是较好的铅锌尾矿砂原位钝化剂。     

天然蒙脱石和沸石改良对黑麦草在铜尾矿砂上生长的影响

通过温室盆栽试验,开展了天然蒙脱石和沸石处理对黑麦草在铜矿尾矿砂上生长影响的研究。结果表明:蒙脱石和沸石改良对黑麦草的地上部生物量没有显著影响,但改变了黑麦草的根重;而施用肥料促进了黑麦草生长。蒙脱石的加入使尾矿砂的有效态锌含量显著降低,但对有效态铜的含量影响不明显;而沸石的加入均显著降低了尾矿砂的有效态铜和锌的含量;另外,矿物的加入降低了尾矿砂的pH值,但其变化与尾矿砂重金属有效态含量变化之间无相关性。矿物的加入降低了黑麦草根中的铜锌吸收,但蒙脱石增加了第一茬黑麦草地上部铜锌吸收,对第二茬黑麦草地上部铜锌吸收无影响;而沸石对两茬黑麦草地上部铜锌含量均无显著影响。不同生长期黑麦草对铜锌吸收量有差异,第二茬黑麦草的地上部锌含量明显高于第一茬,而铜含量则变化不大。     

重金属对土壤微生物酶活性的影响

本文通过含有不同浓度的铜、铅、砷、镉 4种重金属的大豆、小麦盆栽试验 ,采用气相色谱方法测定土壤微生物酶活性 .结果表明 :低浓度的重金属能够提高固氮酶和反硝化酶的活性 ,而高浓度的重金属对上述二种酶有强烈的抑制作用     

生物有机肥对秦巴山区核桃园土壤微生物群落和酶活性的影响

采用大田试验,探讨生物有机肥对秦巴山区核桃园土壤微生物群落结构及其代谢、 酶活性和土壤理化性质的影响。结果表明,施入生物有机肥可改变土壤微生物群落结构,改变微生物对各大类碳源的利用,提高微生物碳源利用率、物种多样性和丰富度,常规施肥对土壤微生物群落结构影响不显著。生物有机肥可显著提高土壤蔗糖酶、酸性磷酸酶和脱氢酶活性,但对过氧化氢酶的影响不显著;常规施肥可提高土壤脲酶和脱氢酶活性,对其他酶活性没有显著影响。生物有机肥可显著提高土壤有机质, 全量氮、磷、钾和速效磷含量,提高土壤pH值,使土壤理化性质得到改善;常规施肥也可在一定程度上提高土壤养分含量,但其效果不如生物有机肥。     

荒地不同压砂年限对土壤微生物区系、酶活性与土壤理化性状的影响

以宁夏中卫市香山地区荒地压砂3,8,15,25 a和邻近未压砂(对照)的土壤为研究对象,研究了压砂对土壤微生物区系、酶活性和土壤理化性状的影响.结果表明,与对照相比,压砂后微生物总数减少;土壤脲酶活性随着压砂年限的延长呈下降趋势;前15 a压砂地土壤有机碳、全氮、碱解氮和速效钾随着压砂年限的延长呈下降趋势;压砂地土壤含水量高于对照;压砂地全盐含量远远低于对照;说明荒地压砂种植能蓄水保墒,防止土壤次生盐碱化,但连续种植肥力下降,微生物量减少.     

重金属污染矿区复垦土壤微生物生物量及酶活性的研究

对铜矿废弃地复垦土壤微生物生物量及酶活性研究结果表明 ,与对照土壤相比 ,矿区复垦土壤微生物生物量C、N和P均有所降低 ,微生物商Cmic Corg可作为矿区重金属污染土壤微生物学敏感指标之一 ;酶活性变化与此相似 ,脲酶、脱氢酶和酸性磷酸酶与对照差异显著 ,其他则与对照差异明显 ,一定程度削弱了矿区土壤中C、N营养元素周转速率和能量循环     

Grasses, litter, and their interaction affect microbial biomass and soil enzyme activity

Plant effects on ecosystem processes are mediated through plant-microbial interactions belowground and soil enzyme assays are commonly used to directly relate microbial activity to ecosystem processes. Live plants influence microbial biomass and activity via differences in rhizosphere processes and detrital inputs. I utilized six grass species of varying litter chemistry in a factorial greenhouse experiment to evaluate the relative effect of live plants and detrital inputs on substrate-induced respiration (SIR, a measure of active microbial biomass), basal respiration, dissolved organic carbon (DOC), and the activities of β-glucosidase, β-glucosaminidase, and acid phosphatase. To minimize confounding variables, I used organic-free potting media, held soil moisture constant, and fertilized weekly. SIR and enzyme activities were 2-15 times greater in litter-addition than plant-addition treatments. Combining live plants with litter did not stimulate microbial biomass or activity above that in litter-only treatments, and β-glucosidase activity was significantly lower. Species-specific differences in litter N (%) and plant biomass were related to differences in β-glucosaminidase and acid phosphatase activity, respectively, but had no apparent effect on β-glucosidase, SIR, or basal respiration. DOC was negatively related to litter C:N, and positively related to plant biomass. Species identity and living plants were not as important as litter additions in stimulating microbial activity, suggesting that plant effects on soil enzymatic activity were driven primarily by detrital inputs, although the strength of litter effects may be moderated by the effect of growing plants.     

Snow removal alters soil microbial biomass and enzyme activity in a Tibetan alpine forest

Projected future decreases in snow cover associated with global warming in alpine ecosystems could affect soil biochemical cycling. To address the objectives how an altered snow removal could affect soil microbial biomass and enzyme activity related to soil carbon and nitrogen cycling and pools, plastic film coverage and returning of melt snow water were applied to simulate the absence of snow cover in a Tibetan alpine forest of western China. Soil temperature and moisture, nutrient availability, microbial biomass and enzyme activity were measured at different periods (before snow cover, early snow cover, deep snow cover, snow cover melting and early growing season) over the entire 2009/2010 winter. Snow removal increased the daily variation of soil temperature, frequency of freeze–thaw cycle, soil frost depth, and advanced the dates of soil freezing and melting, and the peak release of inorganic N. Snow removal significantly decreased soil gravimetric water, ammonium and inorganic N, and activity of soil invertase and urease, but increased soil nitrate, dissolve organic C (DOC) and N (DON), and soil microbial biomass C (MBC) and N (MBN). Our results suggest that a decreased snow cover associated with global warming may advance the timing of soil freezing and thawing as well as the peak of releases of nutrients, leading to an enhanced nutrient leaching before plant become active. These results demonstrate that an absence of snow cover under global warming scenarios will alter soil microbial activities and hence element biogeochemical cycling in alpine forest ecosystems.     

Effects of tree harvesting, forest floor removal, and compaction on soil microbial biomass, microbial respiration, and N availability in a boreal aspen forest in British Columbia

The effects of timber harvesting and the resultant soil disturbances (compaction and forest floor removal) on relative soil water content, microbial biomass C and N contents (C_mic and N_mic), microbial biomass C:N ratio (C_mic-to-N_mic), microbial respiration, metabolic quotient (qCO₂), and available N content in the forest floor and the uppermost mineral soil (0-3 cm) were assessed in a long-term soil productivity (LTSP) site and adjacent mature forest stands in northeastern British Columbia (Canada). A combination of principal component analysis and redundancy analysis was used to test the effects of stem-only harvest, whole tree harvest plus forest floor removal, and soil compaction on the studied variables. Those properties in the forest floor were not affected by timber harvesting or soil compaction. In the mineral soil, compaction increased soil total C and N contents, relative water content, and N_mic by 45%, 40%, 34% and 72%, respectively, and decreased C_mic-to-N_mic ratio by 29%. However, these parameters were not affected by stem only harvesting or whole tree harvesting plus forest floor removal, contrasting the reduction of white spruce and aspen growth following forest floor removal and soil compaction reported in an earlier study. Those results suggest that at the study site the short-term effects of timber harvesting, forest floor removal, and soil compaction are rather complex and that microbial populations might not be affected by the perturbations in the same way as trees, at least not in the short term.     

Fumigation-extraction and substrate-induced respiration derived microbial biomass C,and respiration rate in limed soil of Scots pine sapling stands

The effect of liming on microbial biomass C and respiration activity was studied in four liming experiments on young pine plantations. One of the experimental sites had been limed and planted 12 years before, two 5 years before, and one a year before soil sampling. The youngest experimental site was also treated with ash fertilizer. Liming raised the pH_KCl of the humus layer by 1.5 units or less. Microbial biomass was measured using the fumigation-extraction and substrate-induced respiration methods. Liming did not significantly affect microbial biomass C, except in the experiment which had been limed 11 years ago, where there was a slight biomass increase. Basal respiration, which was measured by the evolution of CO₂, increased in the limed soils, except for the youngest experiment, where there was no effect. Ash fertilization raised the soil pH_KCl by about 0.5 unit, but did not influence microbial biomass C or basal respiration. Fumigation-extraction and substrate-induced respiration derived microbial biomass C values were correlated positively with each other (r=0.65), but substrate-induced respiration gave approximately 1.3 times higher results. In addition, the effect of storing the soil samples at +6 and -18°C was evaluated. The effects were variable but, generally, the substrate-induced respiration derived microbial biomass C decreased, and the fumigation-extraction derived microbial biomass C and basal respiration decreased or were not affected by storage.     

Effects of multiple soil conditioners on a mine site acid sulfate soil for vetiver growth

A pot experiment was conducted to investigate the effects of various soil treatments on the growth of vetiver grass ( Vetiveria zizanioides (L.) Nash) with the objective of formulating appropriate soil media for use in sulfide-bearing mined areas. An acidic mine site acid sulfate soil (pH 2.8) was treated with different soil conditioner formula including hydrated lime, red mud (bauxite residues), zeolitic rock powder, biosolids and a compound fertilizer. Soils treated with red mud and hydrated lime corrected soil acidity and reduced or eliminated metal toxicity enabling the establishment of vetiver grass.Although over-liming affected growth, some seedlings of vetiver survived the initial strong alkaline conditions. Addition of appropriate amounts of zeolitic rock powder also enhanced growth, but over-application caused detrimental effects. In this experiment, soil medium with the best growth performance of vetiver was 50 g of red mud, 10 g of lime, 30 g of zeolitic rock powder and 30 g of biosolids with 2 000 g of mine soils (100% survival rate with the greatest biomass and number of new shoots), but adding a chemical fertilizer to this media adversely impacted plant growth. In addition, a high application rate of biosolids resulted in poorer growth of vetiver, compared to a moderate application rate.     

Effects of plant species on microbial biomass phosphorus and phosphatase activity in a range of grassland soils

Soil P transformations are primarily mediated by plant root and soil microbial activity. A short-term (40 weeks) glasshouse experiment with 15 grassland soils collected from around New Zealand was conducted to examine the impacts of ryegrass (Lolium perenne) and radiata pine (Pinus radiata) on soil microbial properties and microbiological processes involved in P dynamics. Results showed that the effect of plant species on soil microbial parameters varied greatly with soil type. Concentrations of microbial biomass C and soil respiration were significantly greater in six out of 15 soils under radiata pine compared with ryegrass, while there were no significant effects of plant species on these parameters in the remaining soils. However, microbial biomass P (MBP) was significantly lower in six soils under radiata pine, while there were no significant effects of plant species on MBP in the remaining soils. The latter indicated that P was released from the microbial biomass in response to greater P demand by radiata pine. Levels of water soluble organic C were significantly greater in most soils under radiata pine, compared with ryegrass, which suggested that greater root exudation might have occurred under radiata pine. Activities of acid and alkaline phosphatase and phosphodiesterase were generally lower in most soils under radiata pine, compared with ryegrass. The findings of this study indicate that root exudation plays an important role in increased soil microbial activities, solubility of organic P and mineralization of organic P in soils under radiata pine.     

不同土壤改良剂处理对连作西洋参根际微生物数量、土壤酶活性及产量的影响

以北京地区连作西洋参为研究对象, 通过3种土壤改良剂(熟石灰、EM菌剂、沼液)随机区组试验对其土壤理化性状、酶活性、根际微生物区系及产量进行了系统研究。结果表明: 低浓度熟石灰、中浓度EM菌剂及高浓度沼液处理最有利于提高西洋参产量; 施加熟石灰处理后, 土壤微生物主要类群数量显著减少, 土壤pH显著升高, 并对土壤脲酶活性有明显抑制作用; 施加沼液和EM菌剂处理后, 土壤有效微生物菌群显著增加(P<0.05), 土壤有机质和营养物质含量也显著增加(P<0.05), 并对土壤脲酶和多酚氧化酶活性有一定的促进作用。相关性分析发现, 土壤微生物主要类群的数量与蔗糖酶、脲酶、多酚氧化酶活性均有一定的相关性, 其中, 土壤细菌数量与蔗糖酶、多酚氧化酶活性呈极显著正相关(r分别为0.895^**和0.808^**), 土壤真菌和放线菌数量与蔗糖酶、脲酶、多酚氧化酶活性呈极显著正相关(r分别为0.932^**、0.769^**、0.840^**和0.837^**、0.891^**、0.797^**)。另外, 土壤细菌数量与有机质含量呈极显著正相关(r=0.863^**)。表明连作西洋参根际微生物区系及土壤酶活性与土壤理化性状之间紧密联系, 通过施加不同土壤改良剂, 可以为耐连作种植西洋参提供适宜的土壤环境。     

连年翻压绿肥对植烟土壤微生物量及酶活性的影响

通过3年田间定位试验,研究连年翻压绿肥对植烟土壤微生物量碳、氮及酶活性的影响。结果表明,连年翻压绿肥能提高土壤微生物量碳、氮及土壤脲酶、酸性磷酸酶、蔗糖酶、过氧化氢酶的活性,且随翻压年限的增加而增加。整个生育期,翻压3年绿肥的处理与对照相比微生物量碳、氮分别提高31.0%~67.1%、23.0%~145.1%;土壤脲酶、酸性磷酸酶、蔗糖酶、过氧化氢酶活性分别提高34.4%~51.9%、11.0%~18.6%、58.0%~172.7%、24.0%~50.0%,表明翻压绿肥后土壤生物过程活跃,利于有机物质的转化和烤烟正常生长所需的营养供应。动态变化特征表明,翻压绿肥1、2、3年的各处理微生物量碳、氮均在团棵期出现峰值,土壤脲酶、酸性磷酸酶、过氧化氢酶均在旺长期出现峰值。在出现峰值时翻压3年的处理与对照相比微生物量碳、氮分别提高67.1%、60.7%;土壤脲酶、酸性磷酸酶、过氧化氢酶活性分别提高51.9%、14.2%、30.6%。此时正值生育旺期,利于烟株生长发育,说明连年翻压绿肥后培肥土壤效果显著。土壤微生物量C、N和酶活性能灵敏反映土壤肥力的变化,可作为评价土壤质量的生物学指标。     

复垦年限及植被模式对煤矿复垦土壤微生物多样性的影响

了解露天煤矿区复垦状况及其对土壤微生物的影响机制,对于估算受损生态系统的恢复程度至关重要。该文以采用多种模式复垦的安太堡露天煤矿为研究区域,通过野外调查与采样分析,借助于Biolog EcoPlatesTM方法对复垦区和原地貌(对照)表层土壤中的微生物功能多样性状况进行了探索,评价了复垦年限和复垦植被模式对土壤微生物特征的恢复效应;并从土壤物理化学性质(土壤容重、pH值、土壤有机碳、总氮、速效氮、速效磷和速效钾)和生物性质(土壤微生物量碳和微生物量氮)中筛选可反映土壤微生物功能多样性变化的代表性指示物质。结果表明:1)露天煤矿复垦年限和复垦植被模式均对土壤微生物的功能多样性有明显影响。复垦年限越长的样地中土壤微生物有较高的活性和均匀度,但丰富度较低;若样地的复垦年限较长,复垦植物种植模式对土壤微生物多样性的作用强于复垦时长对其的影响。2)从土壤微生物多样性恢复层面分析,单一植物复垦配置的优化次序为杏树、榆树和柠条,混交林配置较优的选择为柠条×刺槐。3)土壤微生物生物量碳的含量与土壤微生物功能多样性指标Shannon-Wiener指数(ρ=–0.69,P0.01)和McIntosh指数(ρ=–0.69,P0.05)显著负相关,在一定程度上可作为复垦区生物多样性指示物质。研究成果将为露天煤矿及其所在区域的生态恢复、治理和监测提供参考。     

丘陵红壤不同人工林型土壤微生物类群、酶活性与土壤理化性状关系的研究

在中国科学院红壤生态试验站优化农业生态模式的长期定位试验地选取恢复14年的常绿针叶林地(马尾松)、落叶阔叶林地(小叶栎)、针阔混交林地(湿地松-小叶栎)和自然恢复地(受到人为干扰)为样地,并以附近疏草荒地作为对照,研究了不同人工林型对土壤微生物类群、酶活性以及土壤理化性质的影响.结果表明:与对照相比,不同林型下土壤细菌、真菌和放线菌总数均有很大程度的增加,依次为针阔混交林>阔叶林>针叶林>自然恢复地>疏草荒地.土壤蔗糖酶、脲酶和酸性磷酸酶活性表现为阔叶林>针阔混交林>针叶林>自然恢复地>疏草荒地.在剖面分布上,土壤微生物类群和酶活性也有明显的层次差异,即随土层的增加而减少.在0～10 cm土层中,土壤细菌、真菌与脲酶、酸性磷酸酶之间具有显著或极显著相关性.土壤微生物类群和酶活性与土壤有机质、全氮和有效氮之间具有极显著相关性.