临沂烟田耕层土壤综合保育类型研究

为更好地指导临沂烟区土壤综合保育,为其他烟区提供参考与依据,在定量分析评价临沂烟区2 249份土壤样品的pH和有机质、碱解氮、有效磷和有效钾含量、面积及分布情况的基础上,借助地统计学方法和ArcGIS平台,划分出10类保育类型:提有机质–改碱、增氮–改碱、增氮–提有机质、增氮–提有机质–改酸、增氮–提有机质–改碱、增氮磷–提有机质–改碱、增钾–提有机质–改酸、增氮钾–提有机质–改酸、增氮钾–提有机质–改碱、增氮磷钾–提有机质–改碱,并根据不同类型提出了初步的相应保育措施。     

冀东滨海盐碱区耕层土壤盐碱变化规律研究

采取定点、定期取样方法,研究了冀东滨海盐碱区地下水以及0~5 cm、5~10 cm、10~20 cm和20~30 cm耕层土壤的盐碱变化。结果表明:0~5 cm耕层含盐量最高,平均达到了0.66%,是其他3个耕层含盐量的4~5倍,而其他3个耕层的含盐量差异不大。从盐分季节性变化看,5月中旬~6月中旬耕层土壤含盐量较高。而耕层土壤pH值较稳定,基本维持在7.8水平,且季节性变化不大。说明土壤碱性不是影响该区作物生长的主要因子,在实际生产措施中应以降低土壤盐分为主。     

黄河下游三角洲盐渍区表层土壤积盐影响因子及其强度分析

采用通径分析方法研究了黄河下游三角洲盐渍区表层土壤(0～10cm)积盐的影响因子及其强度的主次关系,结果表明:表土积盐过程受到盐源分布、盐分离子化学特征、土壤理化性质、地下水状况以及区域性气候条件的综合影响;旱季条件下研究区土壤盐渍化程度较高且盐分表聚性明显;土壤盐源分布对表土层积盐的影响强度最大,其次是盐分离子组成化学特征,表土层理化属性和地下水状况主要通过其它因素对表土层积盐产生间接影响;反映盐源分布的亚表土层(10～20cm)盐分和反映土壤盐分离子化学组成特征的钠吸附比SAR、氯硫比Cl-/SO42-是表土层积盐的主要控制因素。该研究结果为黄河三角洲地区盐渍土地的科学管理与改良利用提供参考依据。     

新疆喀纳斯景区表层土壤磁学特征及环境意义

为探究环境磁学方法在景区土壤污染监测中的可行性,以新疆5A级景区喀纳斯为研究区域,采集表层土壤样品72个,并对其进行系统的环境磁学分析。结果表明:喀纳斯景区土壤磁性矿物平均含量较高,磁学矿物主要由亚铁磁性矿物构成,并含有少量的不完全反铁磁性矿物。磁晶颗粒主要为粗颗粒多畴,同时存在较少的超顺磁颗粒。磁参数空间分布表明,磁性矿物含量参数(χLF、SIRM、SOFT、HIRM)在湖口旅游区表现出高值,新村、老村和旅游接待地呈现相对低值;其他参数(χFD%、S-ratio、SIRM/χLF)空间分布规律与含量磁性参数基本呈相反趋势;研究区的磁性高值点分布与景区人类活动密集区、建筑物及道路的分布具有一致性;湖口旅游区较高的磁性值主要与较强的自然成土作用有关,其他区域的磁性高值点主要受旅游活动的影响。因此,借助土壤磁学方法能够有效区分和圈定景区土壤人为污染范围,为景区土壤污染防治和旅游规划提供参考依据。     

Impacts of urbanization on topsoil nutrient balances—a case study at a provincial scale from Fujian,China

With increasing urbanization, the demands for high quality agricultural products induced changes in local cropping patterns. Although grain production still occupied a large portion in sown and planted areas, the share of sown areas declined from 67% to 44% for total grain crops, and 54% to 35% for rice between 1989 and 2002 in Fujian province. The change in crop spectrum and land use by urbanization has resulted in two extreme trends in topsoil — nutrient depletion in grain-dominated regions and nutrient overload in city suburbs. The positive correlation between nitrogen balance and local urban population in some years showed that urbanization affected nutrient balance in topsoil. The rapid changes in land use and crop spectrum caused by urbanization therefore created a challenge to the traditional soil nutrient management derived mainly from paddy fields and an urgent need for new management schemes in the province. The study provides valuable insights into nutrient management and soil sustainability in the context of rapid urbanization and population growth in Fujian.     

长期施磷稻田土壤磷素累积及其潜在环境风险

应用常规化学分析法和数学统计方法,基于太湖地区13年的长期定位试验,研究长期不同施磷水平下[0(不施磷)、30 kg.hm 2.a 1(低磷)、60 kg.hm 2.a 1(适磷)、90 kg.hm 2.a 1(高磷)]稻麦轮作系统稻田土壤磷素累积规律及磷素流失引发的环境风险。在本试验区土壤环境条件下,可能发生稻田磷素淋溶及径流的土壤耕层(0~15 cm)Olsen-P临界值分别为26.0 mg.kg 1和24.8 mg.kg 1。连续13年适磷、高磷施肥,土壤耕层Olsen-P含量分别达到26.9 mg.kg 1和33.2 mg.kg 1,均高于临界值浓度,且已导致稻田田面水与30 cm渗漏水中总磷浓度显著升高,大大提高了稻田磷素淋溶及径流的风险。低磷施肥土壤Olsen-P长期稳定在(10.1±2.0)mg.kg 1水平,并且每年的稻麦产量与高磷、适磷处理相比并无显著差异,而长期低磷施肥土壤磷的流失风险也较小。因此,在太湖地区稻麦轮作体系下,磷肥不宜以常规适磷水平长期施用,建议以低磷水平(30 kg.hm 2.a 1)长期施用或以适磷水平(60 kg.hm 2.a 1)间歇式施用。     

Natural revegetation of indigenous roadside vegetation by propagules from topsoil

Road construction degrades large areas of indigenous vegetation. Better understanding of ecosystem restoration after degradation will require development and assessment of improved restoration techniques. The potential of natural revegetation based on propagules from topsoil as a restoration technique, to achieve succession towards indigenous vegetation, is not fully understood and accepted as an alternative method for vegetation establishment. The aim of this study was to evaluate this restoration technique by comparing different topsoils with respect to their potentials for revegetation and to describe the early succession on these topsoils by recording change in vegetation cover and the number of species.The study road RV23 is situated in south-east Norway and runs mainly through mixed, mostly coniferous forest. The topsoil (the upper 30 cm) was removed before road construction started, stockpiled during the construction period and then redistributed on the road verge afterwards. In 1999, 10 macroplots of 25 m² were placed randomly on selected topsoils of different qualities, to represent the soil variation in the study area. The soil quality varied from organic-rich to organic-poor soils. Each macro plot contained four 1-m² mesoplots in which the species composition was recorded in 2000 and 2001.Univariate statistical tests were applied to reveal change in vegetation cover between macroplots within 1 year and between years 2000 and 2001. Furthermore, statistical tests were used to reveal the change in single-species frequencies between the study years.Two years after deposition of topsoils, the vegetation cover was generally satisfactory from an aesthetical point of view. However, the variation in vegetation cover and species composition was considerable on different topsoils, reflecting both the local variation of the indigenous vegetation and the soil quality. A total of 121 species of vascular plants were recorded in all 10 macroplots, although not more than 59 species were found in one macroplot. Species composition and single-species frequencies changed considerably from the first year to the second. Among the 61 species that were recorded in more than five mesoplots, the frequency of 16 species increased and the frequency of 10 species decreased significantly (P<0.05). Most of the decreasing species can be considered as weed species and are not represented in the present indigenous vegetation, while most of the increasing species are. The vegetation change from 2000 to 2001 apparently represents the first steps in a succession towards an ecosystem dominated by species of the indigenous vegetation.     

Re-establishing life in restored topsoils

Surface mining activities and other large civil engineering works often involve the removal, storage and reinstatement of topsoil. Disturbance disrupts normal biological functions within the soil and can markedly change the environment within which soil organisms must exist. This has implications for soil fertility and for the overall ecology of replaced land. A number of studies have investigated the impact of opencast coal mining practices on soil organisms and their capacity for recovery following site reinstatement. The extent and duration of any adverse effect varies from one group of organisms to another according to their vulnerability to damage, their capacity for recovery and their ability to recolonize areas from which they have been eliminated. Three groups of organisms—earthworms, aerobic bactería and vesicular arbuscular endophytes—are considered, to illustrate their differing responses to soil disturbance and the various factors limiting their early recovery throughout a restored area. Given favourable management, consistent with good general rehabilitative practice, the re-establishment of normal earthworm populations depends entirely on the distribution of an inoculum. For aerobic bacteria adverse physical conditions in reinstated soils are the overriding influence determining levels of activity. For mycorrhizal fungi both soil conditions and the absence of an inoculum may delay recovery, although the evidence in support of this view is inconclusive.     

Soil stress as affected by wheel load and tyre inflation pressure

The relative importance of wheel load and tyre inflation pressure on topsoil and subsoil stresses has long been disputed in soil compaction research. The objectives of the experiment presented here were to (1) measure maximum soil stresses and stress distribution in the topsoil for different wheel loads at the same recommended tyre inflation pressure; (2) measure soil stresses at different inflation pressures for the given wheel loads; and (3) measure subsoil stresses and compare measured and simulated values. Measurements were made with the wheel loads 11, 15 and 33 kN at inflation pressures of 70, 100 and 150 kPa. Topsoil stresses were measured at 10 cm depth with five stress sensors installed in disturbed soil, perpendicular to driving direction. Contact area was measured on a hard surface. Subsoil stresses were measured at 30, 50 and 70 cm depth with sensors installed in undisturbed soil. The mean ground contact pressure could be approximated by the tyre inflation pressure (only) when the recommended inflation pressure was used. The maximum stress at 10 cm depth was considerably higher than the inflation pressure (39% on average) and also increased with increasing wheel load. While tyre inflation pressure had a large influence on soil stresses measured at 10 cm depth, it had very little influence in the subsoil (30 cm and deeper). In contrast, wheel load had a very large influence on subsoil stresses. Measured and simulated values agreed reasonably well in terms of relative differences between treatments, but the effect of inflation pressure on subsoil stresses was overestimated in the simulations. To reduce soil stresses exerted by tyres in agriculture, the results show the need to further study the distribution of stresses under tyres. For calculation of subsoil stresses, further validations of commonly used models for stress propagation are needed.     

应用标准化方法评价攀枝花地区表层土壤的重金属污染

应用标准化方法建立了攀枝花地区土壤环境地球化学基线模型，在此基础上，评价了表层土壤的重金属污染状况。结果表明：该区Cd没有污染，Co、Cr、Ni、Pb为轻微污染，As、Zn以轻微污染到中度污染为主，污染程度较高的地区主要分布在工矿区。