Bioavailability of Vanadium Extracted by EDTA, HCl, HOAC, and NaNO3 in Topsoil in the Panzhihua Urban Park, Located in Southwest China

Bioavailable vanadium was evaluated on the basis of soil vanadium single-extraction with ethylenediaminetetraacetic acid (EDTA), hydrochloric acid (HCl), acetic acid (HOAc), and sodium nitrate (NaNO(3)) in Panzhihua urban park. The soil vanadium concentration extracted by HOAc was 0.01-2.07?mg?kg(-1), by EDTA 0.28-7.03?mg?kg(-1), by NaNO(3) 0.07-0.53?mg?kg(-1), and by HCl 0.19-1.36?mg?kg(-1). The bioavailable vanadium (bioavailable fraction) obtained with HOAc was 0.01-1.33%, with EDTA 0.27-4.09%, with NaNO(3) 0.13-0.72%, and with HCl 0.06-0.28%. In addition, the impact of soil properties, soil nutrients, and soil enzyme activities on bioavailability of vanadium is discussed in this study. Based on the characteristics of bioavailable vanadium in the soil, ecological and health risks should have been given more attention in the studied area.     

重庆岩溶区土壤景观多样性

不同土壤发生类型塑造了异质的景观格局,而土壤类型上不同的土地利用实践又对原有景观格局进行重构。研究的目的是利用景观指数识别重庆岩溶区土壤多样性的景观特征。结果表明：重庆市岩溶区土壤景观多样化和空间异质化程度不高,各景观分布比例不均匀;土壤景观嵌块体呈现复杂的几何形状,黄壤、石灰土和黄棕壤是主要的土壤类型;除山地草甸土以林地和草地,棕壤以林地为主要景观外,其余9种土壤类型都以耕地和林地为主要景观;农、林用地在重庆岩溶区土壤景观空间格局的结构和功能中起主导作用;但因各类土壤性质和分布特点的不同,耕地和林地在各类土壤上的分配比例上存在明显差异;人类活动在诱导耕地嵌块体数急剧增多的同时,居民工矿用地、林地、未利用地嵌块体数目也相应增加;研究可为岩溶区土地利用决策与调控提供科学依据,加深人们对岩溶区土壤多样性的理解。     

喀斯特区不同退化程度植被群落植物-凋落物-土壤-微生物生态化学计量特征

为摸清喀斯特植被退化对群落各组分C、N、P生态化学计量特征及内稳态特征的影响,为喀斯特退化生态系统植被恢复与重建提供科学依据,以桂西北喀斯特地区5种退化程度植被群落为研究对象,测定了不同退化程度植被群落植物叶片、凋落物、土壤和微生物生物量的C、N、P含量,分析其化学计量比特征、相互关系及植物内稳性特征。结果表明：(1)随着退化程度加剧,叶片C、N、P含量、N∶P和凋落物N∶P、微生物量C显著下降,而叶片C∶N、C∶P则显著增加,且植物叶片N∶P<14;随退化程度加剧,凋落物N、P含量、土壤C、N、P含量、微生物量N、P呈先略有增后显著降低的趋势,且不同退化程度群落土壤N∶P和微生物量C∶N无显著差异。(2)叶片N、P含量与土壤N、P含量,叶片C∶P与土壤C∶N、C∶P、N∶P,叶片N∶P与凋落物N、N∶P,叶片C、N、P含量与微生物量C呈显著或极显著正相关关系;叶片C∶N与土壤C、N,叶片C∶P与土壤N、P,叶片N∶P与土壤P呈显著或极显著负相关关系。(3)喀斯特地区植物叶片N、P元素的内稳性指数(H)平均值分别为2.74和2.31,属于弱稳态型,叶片N∶P的H值为5.14,为稳...     

长期施肥下农田土壤-有机质-微生物的碳氮磷化学计量学特征

探讨外源养分的输入对土壤系统内碳、氮、磷化学计量特征的影响,对于深刻认识农田土壤有机碳(C)和养分循环及其相互作用过程具有重要意义。以26年的农田长期定位施肥试验为平台,分析长期不同施肥条件下土壤、有机态及微生物生物量碳、氮、磷含量及其化学计量学特征,并根据内稳性模型y=c x~(1/H)计算其化学计量内稳性指数H。结果表明:与长期撂荒处理(CK_0)相比,种植作物条件下26年化肥配施有机肥处理(MNPK和1.5MNPK)显著降低微生物生物量氮含量,但显著提高了微生物生物量磷的含量。相对于撂荒处理,即使长期配施化肥磷处理(NP、PK、NPK),其土壤有机磷降低显著。对于C∶N比而言,化肥配施有机物料处理(秸秆或有机肥)的土壤C∶N比、有机质C∶N及微生物生物量C∶N比均显著低于化肥处理(N、NP、PK和NPK)。对于C∶P比而言,相对于撂荒处理,26年施用磷肥(化肥磷或有机磷)显著降低了土壤C∶P比和微生物生物量C∶P比,而CK和偏施化肥处理(N、NP和PK)显著降低了土壤有机质C∶P比。对于土壤N∶P比而言,撂荒处理土壤N∶P比显著高于其他处理,而撂荒处理土壤有机质N∶P比显著高于CK和化肥处理,表明不施肥或化肥条件下作物种植加剧了土壤有机质中氮素的消耗。微生物生物量C∶N、C∶P、N∶P比的内稳性指数H分别为0.24、0.75、0.64,不具有内稳性特征。微生物生物量C∶N、C∶P、N∶P比分别与土壤C∶N、C∶P、N∶P比呈显著正相关关系,但与土壤有机质碳氮磷化学计量比之间无显著相关性。表明土壤碳、氮、磷元素的改变会直接导致微生物生物量碳、氮、磷化学计量比的改变,但微生物生物量碳氮磷化学计量比对土壤有机质碳氮磷化学计量比无显著影响,土壤有机质的碳氮磷计量比可能更多是受到作物和施肥等养分管理措施的影响。     

广西木论喀斯特森林土壤养分水平与植被及地形的关系

研究了广西木论喀斯特森林原生植被和次生植被的土壤养分特征,测定了陡坡、缓坡、洼地3种主要地形内林地0～5 cm表层土壤中的有机质(SOM)、氮、磷、钾含量,以及它们在石土面、土面两类主要小生境间的差异.结果表明:林分成熟度高、优势种不明显的原生林积累了高水平的SOM,缓坡石土面最高,达345 g kg-1,洼地的含量较低,但仍在80 g kg-1以上;土壤全氮(TN)、碱解氮(AN)含量也较高.以红背山麻杆(Alchornea trewioides)、广西野桐(Mallotus conspuyrcatus)、伞花木(Eurycorymbus cavderiei)等为优势种的次生林,物种多样性较原生林低,SOM、TN、AN含量也低,缓坡石土面和土面小生境的SOM分别为110 g kg-1和77 g kg-1,是原生林的32%和35%,下降幅度最大,其次为陡坡,而洼地的差异不明显.全磷(TP)、有效磷(AP)、全钾(TK)、有效钾(AK)含量在两林型间差异无明显规律.原生林和次生林土壤养分含量(除TK外)以缓坡>陡坡>洼地;但次生林中三者间无显著差异.同类型样地内小生境土壤养分含量(除TK外)均为石土面含量高于土面.     

Survival of, and induced stress resistance in, carbon-starved Pseudomonas fluorescens cells residing in soil.

We investigated the survival, cell length, and development of general stress resistance in populations of Pseudomonas fluorescens R2f and its rifampin-resistant mutant, R2f Rpr, following exposure to carbon starvation conditions in liquid cultures and residence in two different soils, Flevo silt loam (FSL) and Ede loamy sand (ELS). In much the same way as was recently shown for P. putida KT2442, carbon-starved P. fluorescens R2f populations revealed enhanced resistance to otherwise lethal treatments, such as exposure to ethanol, high temperature, osmotic tension, and oxidative stress. A large population of nonculturable P. fluorescens R2f Rpr cells arose shortly after their introduction into ELS soil, whereas the formation of nonculturable cells was not observed in FSL soil. Also, the inoculant cell (based on immunofluorescence) and CFU counts decreased faster in ELS soil than in FSL soil. Introduction of carbon-starved instead of exponential-growth-phase R2f Rpr cells into ELS soil did not affect bacterial survival. The inoculant cell length decreased in soil, and no large differences in cell length in the two soil types were observed. Addition of glucose to ELS soil resulted in a stable cell length of R2f Rpr cells, whereas carbon-starved cells introduced into ELS soil remained small. Exponentially growing R2f Rpr cells developed enhanced resistance to ethanol, high temperature, osmotic tension, and oxidative stress within 1 day in both soils, whereas cells introduced into ELS soil amended with glucose showed decreased resistance. Cells that were carbon starved prior to introduction into ELS soil showed unchanged stress resistance levels upon residence in soil.     

Natural Attenuation, Biostimulation, and Bioaugmentation in 4-Chloroaniline-Contaminated Soil

Bioremediation treatments including natural attenuation (NA), biostimulation (BS), and bioaugmentation (BA) were performed and compared regarding the degradation of 4-chloroaniline (4CA) contaminating two types of agricultural soil collected from Nakornnayok (NN) and Chiangmai (CM) provinces, Thailand. Despite the different soil properties, both soil types exhibited intrinsic potential for biodegradation. 4CA degradation by NA in loam soil-NN was fairly effective (ca. 40%), while in sandy-clay loam soil-CM it occurred poorly (<10%). Compared to NA, BS with aniline and BA with 4CA-degrading Klebseilla sp. CA17 were comparatively more effective techniques, although the degradation occurred differently in each soil type. In soil-NN, the biodegradation of 4CA took place at a higher rate, achieving biodegradation of 70–75% within 4 weeks, than in soil-CM, i.e., up to 40–46% within 8 weeks. During each treatment, changes in soil microbial activity, numbers of 4CA-degrading micro-organisms, and dynamic modification of soil microbial community structure were also monitored. The results suggest that both BS and BA are feasible techniques for bioremediation of 4CA accumulated in soil, although the biodegrading efficiency in soil environment depends not only on site characteristics but also on the characteristics of either indigenous microbial population or the survival and stability of bioaugmented cultures.     

Populations of the spinach wilt pathogen, Fusarium oxysporum f. sp. spinaciae, in the root tissues, rhizosphere, and soil in the field.

Populations of Fusarium oxysporum f. sp. spinaciae in root tissues and rhizosphere soil of diseased spinach plants were higher than in the root tissues and rhizosphere soil of healthy plants. Populations in soil rhizosphere were higher than in nonrhizosphere soil. The fungus populations were very low in the root tissues of the nonsusceptible strawberry, broccoli, chinese cabbage, and mustard grown in the infested field. The populations were low at the beginning of the season, increased, and remained high during the summer, then dropped in the fall. The fungus populations ranged from 1600 to 2600 propagules/g in the top 10 cm of soil, declined sharply between 11 and 20 cm, and were nondetectable between 41 and 60 cm.     

黄土高原典型植物根际对土壤微生物生物量碳、氮、磷和基础呼吸的影响

选择黄土高原7种典型植物的根际与非根际土壤为研究对象,对土壤的养分含量、微生物生物量碳、氮、磷和基础呼吸的影响进行了初步研究。结果表明,7种不同植物根际土壤与非根际土壤的养分含量、微生物生物量和基础呼吸均存在显著差异;除冷蒿的土壤微生物生物量磷以外,其他各种植物的根际土壤的养分含量、微生物生物量和基础呼吸均比非根际土壤的高;土壤有机碳、全氮与土壤微生物生物量碳、氮及基础呼吸之间均具有极显著或显著相关关系,表明了土壤微生物生物量碳、氮可以作为判断土壤肥力状况的生物学指标,同时也可为提高土壤肥力水平和土壤培肥效果提供依据。     

Contrasting effects of municipal compost on alfalfa growth in clay and in sandy soils: N, P, K, content and heavy metal toxicity

The limits for loading soils with Tunisian urban compost for cultivating Medicago sativa were determined in a 6-month experiment in a greenhouse. Mature municipal solid waste compost (MSWC) from Tunis city was applied to clay and sandy soils from cultivated fields at rates equivalent to 40, 80, 120tha(-1). In the absence of MSWC, the shoot biomass (dry weight) cumulated over four cuts was 2-2.5 lower in sandy soil than in clay soil. It was 20-25% augmented upon MSWC addition in clay soil, independently of MSWC dose. The opposite trend was observed in sandy soil, the shoot yields being diminished by MSWC in a dose dependent manner. In MSWC-amended clay soil but not in sandy soil, Cd, Cu, Zn, and Pb concentrations in shoots remained below or close to the tolerated values according to EEC norms. The MSWC might be used as conditioner for clay soil, but not for sandy soil.     

西宁南山4种灌木根际和非根际土壤微生物、酶活性和养分特征

西宁南山区植被退化情况严重,人工造林植被恢复被看作是最有效的恢复手段,其中选择合适造林树种尤为关键。选择人工种植的唐古特白刺Nitraria tangutorum、柠条Caragana korshinskii、西北小蘗Berberis vernae和短叶锦鸡儿Caragana brevifolia共4种灌木树种造林试验区为研究对象,通过测定根际和非根际土壤微生物数量、酶活性及养分含量,综合比较种植4种灌木树种根际和非根际土壤肥力差异,科学评价其对土壤的改善效果。研究表明:(1)土壤微生物数量和酶活性总体呈现出根际高于非根际的规律,仅放线菌数量和脲酶活性出现了根际低于非根际现象。(2)土壤养分方面,4种灌木根际土壤和非根际土壤p H值、全N、全P、全K含量差异不显著,有机质、有效P、速效K含量均呈现出根际非根际,而碱解N则是根际非根际。(3)土壤酶活性与土壤微生物数量相关性不显著,土壤有机质含量与土壤细菌、真菌数量呈极显著正相关,有效P含量与土壤细菌、真菌和放线菌数量呈极显著正相关,速效K含量与过氧化氢酶、酸性磷酸酶活性呈显著正相关,全N、碱解N含量均与脲酶活性呈显著正相关。(4)从土壤肥力综合水平来看,根际非根际,其中根际土壤中西北小蘗柠条短叶锦鸡儿唐古特白刺,研究结果表明西北小蘗和柠条能大幅提高土壤肥力,改良土壤效果较好。     

新疆玛纳斯流域非农业种植地盐碱性空间变异特征

土壤盐渍化是导致干旱区土地退化的主要原因之一,也是影响干旱区可持续发展和环境改善的基本问题。充分挖掘不同分类体系下盐渍土空间变异性可以为实施开垦或恢复生态措施提供科学依据。以干旱区开垦近50a的玛纳斯流域为研究区,在不同分类体系下,以土壤盐度,p H值,离子类型为指标,分析该区域非农业种植地(弃耕地,盐碱地,裸地,沙地)盐渍土类型的空间分布特征。结果表明:(1)研究区68%的样本属于非盐渍化,不同类型的盐渍土主要以链状分布于泉水溢出带-冲积平原-干三角洲地带,由南向北,区域整体盐分大致遵循先升高后降低再升高趋势,半方差函数分析土壤盐分呈现弱变异,说明这种分布情况是受随机(人为)因素的影响;而p H整体由南向北递增,传统统计学和地统计学的分析结果都表明土壤碱化呈现中等变异,受结构(自然)因素和随机(人为)因素的共同影响。表层土壤除在溢出带为氯化物型盐渍土外,其他地区自南向北由硫酸-氯化物型逐渐变为氯化-硫酸盐型和硫酸盐土、苏打盐土,离子的半方差函数拟合模型结果均是弱变异和中等变异,与美国盐度实验室分类体系的变异性结果相同,此类分布特征也是结构因素和随机因素共同作用的结果。(2)分析五种典型地貌的盐渍土分布,方差分析结果表明,5种地貌类型均呈现盐分表聚特征,碱化度则由南向北递增;其中盐碱特征最为显著的是泉水溢出带。泉水溢出带的盐土垂直方向的变化趋势为由表层至深层,盐土类型由硫酸-氯化物盐土变为氯化盐土;冲积平原和干三角洲样点处全剖面为氯化物-硫酸盐土,冲积洪积扇和沙漠地区则包含所有阴离子盐土类型。对玛纳斯流域盐渍土特性的空间异质性进行分析,可以为下一步有针对性地治理与改善土壤盐渍化提供科学依据。     

甘肃敦煌西湖荒漠-湿地生态系统土壤水分空间异质性及其影响因子研究

土壤水分是内陆荒漠区湿地生态系统中重要的限制因子,为了揭示该区域土壤水分空间分布特征,采用传统统计学和地统计学相结合的方法,对甘肃敦煌西湖国家级自然保护区0~200cm内各层土壤水分的空间变异性及海拔、土壤质地和植被对其的影响进行了研究,旨在为极干旱区湿地生态系统植被修复和保育提供科学依据。结果表明:(1)本研究所得各变量的变异系数、块金方差、基台值、变程和结构比分别为36.51%~88.65%、0.007~0.098、0.112~0.549、116~453和76.6%~97.6%,各变量均为中等变异,存在高度异质性,具有较强空间自相关。(2)深层(60~200cm)土壤水分含量较浅层(0~60cm)变异大,且不同层次土壤水分含量的空间异质性差别也较大,空间变异主要发生在较小尺度上(分维数D在1.902~1.989之间)。(3)海拔是影响该区域深层土壤水分空间变异的主导因子。(4)土壤质地与浅层(0~60cm)土壤水分含量的相关性大于与深层(60~200cm)土壤含水量的相关性,它们与海拔相关性表现相反;草本植被盖度与浅层土壤水分含量呈较高的正关联关系,灌木根量与深层土壤水分含量呈较高的负关联关系。     

京东板栗主产区土壤氮磷钾的空间变异

采用经典统计学和地统计学相结合的方法,对京东板栗主产区迁西县土壤氮、磷、钾的空间变异进行了分析.结果表明：迁西县土壤全量氮、磷、钾和速效氮、钾的含量普遍较低,但表层土壤速效磷含量较高;氮、磷、钾的空间分布均表现为中等变异,且以磷的变异最大.表层土壤全氮和碱解氮的分布符合高斯模型,其空间变异主要由结构性因素决定;全钾和速效钾的分布分别符合球状模型和高斯模型,前者空间变异受结构性因素和随机性因素的共同影响,空间相关性为中等;后者主要受结构性因素的影响,空间相关性强烈.氮、钾在全县范围内的空间分布特征相似,高值区均出现在县域南部和西北部,而中部和东北部的含量较低.全磷的高值区主要分布在该县北部,速效磷高值区则分布在县区南部.氮、钾全量和有效态含量之间存在极显著正相关关系,但全磷和速效磷含量的相关性不显著.     

Partitioning of Zn,Cd, Pb,and Cu in organic-rich soil profiles in the vicinity of a zinc smelter

Abstract

A five-step sequential extraction procedure was applied to organic-rich soil samples from five soil profiles situated 1–8 km from a zinc smelter. The partitioning of Zn, Cd, Pb, and Cu into five operationally defined fractions (exchangeable, “carbonate’’-bound, reducible, oxidizable, and residual) was studied at different soil depths down to 35cm. In the surface soil (0–1 cm) a major part of Pb and Cu was extracted in the oxidizable fraction, whereas for Zn and Cd slightly more was extracted in the ‘‘carbonate”-fraction than in the other four fractions. Extracted metal proportions in the oxidizable fraction were respectively of the order of 30%, 20%, 50%, and 80% for Zn, Cd, Pb, and Cu in the surface soil for all sites, but these proportions decreased with soil depth. In the surface soil less than 20% of all the elements were extracted in the residual fraction, but the proportions associated with this fraction generally increased with soil depth. In the C-horizon, differences in extracted proportions of Pb and Cu in the residual fraction were probably due to geochemical factors, whereas for Zn the low extracted proportion at a highly contaminated site (20%) may be due to Zn migration to the C-horizon at this site. For Cd the extracted proportions in the C-horizon were lower than for the other elements, generally below 20%, presumably because Cd is weaker in terms of its adsorption to the soil than the other elements studied. Total concentrations of the metals decreased strongly with increasing distance from the smelter, but less systematic differences were observed for their distributions among fractions. Potentially bioavailable metal proportions (exchangeable + “carbonate”-bound fraction) in the surface soil were about 50%, 60%, 20%, and 10% for Zn, Cd, Pb, and Cu, respectively. In C-horizon soil the mobility sequence Cd>Zn>Pb = Cu was generally observed. The present results indicate that the concentrations and chemical fractionation of Zn, Pb, and Cd in these soils represent a considerable risk to natural terrestrial food chains.     

Fine Root Decomposition and Cycling of Cu,Ni, Pb,and Zn at Forest Sites Near Smelters in Sudbury,ON, and Rouyn-Noranda,QU, Canada

This study determined rates of in situ fine root decomposition and changes in trace metals concentration during decomposition at sites in Sudbury, ON, and Rouyn-Noranda, QU, with elevated or background concentrations of Cu, Ni, Pb, and/or Zn in the soil, and correlated the depth gradients of Cu, Ni, Pb, and Zn for soils and roots at the same sites. Fine roots were extracted from soil cores within root traps several times over 12 months; biomass and metal concentrations were measured. Live roots were collected from 30-cm soil cores, separated into three depths. Elevated soil metal concentrations did not necessarily reduce fine root decomposition, and effects on decomposition were similar to those previously reported for surface foliar litter at the same sites. Decomposing roots at only the high metal sites demonstrated increased metal concentrations with time. Root tissue concentrations of Cu, Ni, and Zn, but not Pb, at lower soil depths were generally higher than expected from soil metal concentrations. This could be explained by reallocation of essential metals, although these metals were likely also more available for uptake at depth due to lower DOC concentrations. This study means that for risk assessment, separate determinations of altered decomposition for roots and leaf litter are likely not necessary for predicting ecosystem effects, a pragmatically useful conclusion given the labor intensity of the fine root studies. This study also suggests that for risk assessment of plant community exposure to metals, prediction of exposure to metals should probably consider soil layers that do not have substantially elevated metal concentrations, as their soil characteristics, or plant processes, may result in unexpected exposure.     

Alfalfa,Medicago sativa L., in highly weathered,acid soils

Summary Seedlings of a broad based population of alfalfa, (Medicago sativa L.), were visually selected for 2 generations (cycles) in an acid Cecil soil (pH=4.8). Simultaneously, 2 generations of selections were made in a limed Cecil soil (pH=6.2) amended with phosphorus. When tested in acid soil (pH=4.8) with added P, the cycle 2 acid selections yielded significantly more top yield than either the limed selections or the original seed. When grown in the limed soil (pH=6.2) without added P, the acid selections yielded significantly less. There were no significant differences among selections in other soil conditions (pH=4.8, no P added and pH=6.2, P added). Root weight and length and nodule fresh weight correlated well with top yield in all treatments. The yield of the 10 parent varieties and polycrossed seed of their cycle 1 acid and cycle 1 limed selections were compared under two soil conditions (acid and limed). The results of this test indicate that some varieties were more responsive to acid soil selection than other. Overall, none of the 10 varieties showed any decreases in total top yield due to one cycle of selection in either the acid or limed soil conditions.     

不同龄级速生杨人工林土壤微生物数量与养分动态变化

通过稀释平板法和常规化学分析法, 对伊犁河谷地区3种龄级(5年、10年、15年)的速生杨欧美黑杨(Populus × euramericana)人工林的土壤微生物数量、组成和土壤养分变化进行了研究。结果表明, 3种不同林龄林地土壤微生物集中分布在10-40 cm土层, 数量和种类组成随季节变化有明显差异。随着林龄的增长, 土壤微生物总数、细菌数量减少, 真菌和放线菌数量在10年生人工林最高, 这一规律随季节变化。三大类土壤微生物的组成比例相对稳定, 不随季节变化而变化。土壤有机碳、氮含量主要集中在0-20 cm土层, 随土壤深度的增加逐渐减少, 其含量及分布受季节和土壤深度不同程度的影响。土壤有机碳含量随林龄的增长而逐渐增高, 有机氮则先减后增。相关分析表明, 土壤微生物总数与土壤有机碳呈负相关, 真菌数量与土壤有机氮呈正相关。3种林地土壤有机C/N比与土壤细菌数量/真菌数量比例一致, 说明速生杨人工林在一定生长年龄内能提高土壤的固碳能力, 改善土壤肥力。     

Vertical and Horizontal Distributions of Zn,Cd, Pb,Cu, and Hg in Uncultivated Soil in the Vicinity of a Zinc Smelter at Odda,Norway

In the present work the extent and variation of Zn, Cd, Pb, Cu, and Hg loading in undisturbed surface soil (0–5 cm) and the vertical transport of the metals in soil profiles are studied in the vicinity of a zinc smelter in Norway. Three major controlling factors on the metal concentrations in soil have been assessed: 1) distance from the anthropogenic point source; 2) organic matter content (O.M.); and 3) the prevailing wind directions. Moreover metal distributions in proximal soil profiles in 1972 and 2003 are compared. Current concentrations of Zn, Cd, Pb, Cu, and Hg in surface soil reach 14000, 60, 980, 430, and 7.0 mg·kg ^{? 1} , respectively, near the smelter and decrease regularly with distance in the northerly direction according to the regression model (y = ax^{? b} ). The Zn concentrations are significantly different from the background range up to 30 km from the smelter, whereas the other metals approach background at only 10 km distance. Subsurface concentration peaks of Pb, Cu, and Hg are found at greater depth in soil profiles than peaks of Zn and Cd. Levels of Zn, Cd, and Pb in surface soil seem to have decreased from 1972 to 2003, whereas for Cu the levels appear not to be significantly different.     

DNA in soil: adsorption,genetic transformation,molecular evolution and genetic microchip

This review examines interactions between DNA and soil with an emphasis on the persistence and stability of DNA in soil. The role of DNA in genetic transformation in soil microorganisms will also be discussed. In addition, a postulated mechanism for stabilization and elongation/asserbly of primitive genetic material and the role of soil particles, salt concentrations, temperature cycling and crystal formation is examined.