Mapping critical levels of ozone,sulfur dioxide and nitrogen dioxide for crops,forests and natural vegetation in the United States

Air pollution abatement strategies for controlling nitrogen dioxide, sulfur dioxide, and ozone emissions in the United States focus on a ‘standards-based’ approach. This approach places limits on air pollution by maintaining a baseline value for air quality, no matter what the ecosystem can or cannot withstand. In this paper, we present example critical levels maps for the conterminous U.S. developed using the ‘effects-based’ mapping approach as defined by the United Nations Economic Commission for Europe's Convention on Long-Range Transboundary Air Pollution, Task Force on Mapping. This approach emphasizes the pollution level or load capacity an ecosystem can accommodate before degradation occurs, and allows for analysis of cumulative effects. We present the first stage of an analysis that reports the distribution of exceedances of critial levels for NO₂, SO₂, and O₃ in sensitive forest, crop, and natural vegetation ecosystems in the contiguous United States. We conclude that extrapolation to surrounding geographic areas requires the analysis of diverse and compounding factors that preclude simple extrapolation methods. Pollutant data depicted in this analysis is limited to locationally specific data, and would be enhanced by utilizing spatial statistics, along with converging associated anthropogenic and climatological factors. Values used for critical levels were derived from current scientific knowledge. While not intended to be a definitive value, adjustments will occur as the scientific community gains new insight to pollutant/receptor relationships. We recommend future analysis to include a refinement of sensitive receptor data coverages and to report relative proportions of exceedances at varying grid scales.     

Nutrient depletion in Ferralsols under hybrid sisal cultivation in Tanzania

Abstract. Sisal production in Tanzania has declined sharply in the past two decades because of a decrease in the area grown and a decrease in yields. As sisal is cultivated without manuring, depletion of soil fertility is considered one of the main causes of the declining yields. This paper presents a balance of the macronutrients N, P, K, Ca and Mg for sisal grown in a plantation in NE Tanzania on deep, red clay soils (Ferralsols). Annual fibre yields declined from 2.5 t/ha in the 1960s to about 1 t/ha in the 1980s. Hybrid sisal is a demanding crop and in ten years, with a total fibre yield of 11 t/ha, about 260 kg of N, 40 kg of P, 385 kg of K, 890 kg of Ca and 330 kg of Mg are removed in the harvested leaves. A comparison of soils after two and three 10-yr cycles of sisal production showed that in the third cycle the pH decreased by 0.5 units and that exchangeable bases were decreased by fifty per cent or more. The amounts of K, Ca and Mg removed from the soil were similar to those in leaves. However, soil analyses could not detect changes in total N and available P, possibly because of the large amount of total N in the soil and the lack of precision in the N and P analyses. In the Ferralsols, potassium is likely to become deficient first, followed by magnesium and calcium. The soil has little available P, and an increase in soil acidity may decrease it further and also create aluminium and manganese toxicities. In order to maintain sisal production, fertilization with P, K, Ca and Mg is necessary, and to improve yields N must also be applied.     

Toxic metals in amenity soil

Abstract. The soil of amenity areas is important in the urban landscape. Some is natural, some is man-made. Both contribute greatly to the environment of our cities through the grass, shrubs and trees which they support. Results of research from agriculture and urban gardens have been extrapolated in this review to consider the significance of toxic metals in amenity soil. The metals of most concern for plant growth are zinc, copper and nickel as they are phytotoxic, but additionally lead, cadmium, arsenic, and mercury are of concern due to their effects on human health. The currently acceptable threshold values for metals in the soil of public open spaces, playing fields and parks are presented, and consideration is given to the toxic metal content of an assortment of materials likely to be used in constructing amenity soil.     

Characteristics of bacteria in the forest soils under natural vegetation

Characteristics of the predominant bacteria isolated in November and May from the forest soils of both dry and wet types under natural vegetation were studied.

Although Gram-negative rods were the most abundant bacteria in both soil types and in both seasons, their contents were less and other bacteria especially spore-forming ones increased in May.

Among Gram-negative rods in the soil of the dry type in November, the most predominant was those with nonchromogenic rods motile with polar flagella which grew in a simple synthetic media containing glucose or p-hydroxybenzoate and ammonium as the sole carbon and nitrogen sources. In May, the ratio of the bacteria which require amino nitrogen or those with more chomplex nutritional requirement increased. In the soil of moderately wet type, the difference in kinds of bacteria between the two seasons was not so clear as that in the dry type.

Most of Bacillus species obtained in these soils were those requiring amino acids or other growth factors among which B. cereus was most abundant.     

Thermal regime of tundra soils under reclamation and restoration of natural vegetation

This paper covers the specifics of the temperature regime in reclaimed tundra soils under a sown perennial herb meadow and a restored (secondary) ecosystem as compared to the small-shrub yernik (birch)-willow-moss and shrub yernik-willow-moss tundra types. The taxonomic position of the anthropogenic soils and those of the secondary (restored) biogeocenosis is discussed as related to the transformation or regeneration of the biotic and thermal components of the biogeocenosis. The soil development causes profound changes in the freezing-thawing regime, which gives grounds to distinguish the developed soils as an individual soil type.     

Redox conditions and heavy metals distribution in mangrove forests receiving effluents from shrimp farms (Teremba Bay,New Caledonia)

Purpose  

The mangroves of New Caledonia, in the south Pacific, act as a buffer between a lagoon of more than 20,000 km² and the island, which is characterized by ultramafic rocks and lateritic soils that are exploited for their richness in heavy metals. We will provide a better understanding of the redox conditions, and of heavy metal distributions in mangroves receiving shrimp farm effluents.     

Plant parasitic nematodes and spatio-temporal variation in natural vegetation

In this paper, the possible role of plant parasitic nematodes as a driving force of change in natural vegetation is analysed using the succession at coastal foredunes as a model. In pot trials, when grown in natural substrates from mature stands, seedlings of dominant foredune plants showed poor growth when compared to sterilised substrates. In natural substrates from preceding stages, growth reduction was far less, or even non-significant. Chemical soil treatment with nematicides resulted in enhanced growth of the seedlings. Inoculation of ectoparasitic nematodes reduced plant growth, but only at densities much higher than those occurring in control pots with unsterilised field soil. Identification at species level showed that endoparasitic nematodes are specifically associated with particular plant species. Therefore, it is hypothesised that the distribution of endoparasitic nematodes may be an important factor leading to the specific nature of soil pathogen complexes in coastal foredunes. We discuss the role of endoparasitic nematodes as possible key species in soil communities and compare the possible effects of specific vs. generalistic plant parasitic nematodes in soil communities on vegetation processes.     

Carbon storage and other properties of soils under agriculture and natural vegetation in São Paulo State, Brazil

Abstract. Topsoil (0–20 cm) and subsoil (60–100 cm) properties are compared at agricultural and nearby natural vegetation sites in São Paulo State. Differences are related to land use and climate, in order to estimate soil carbon storage under various ecosystems and also to study the effects of high-input agriculture on the chemical composition of soils with low activity clays. Within each land use, organic carbon in the topsoil is most strongly related to clay + silt content. This relationship is stronger for cropped, short savannah (cerrado) and tall savannah (cerradão) sites than for semi-deciduous and evergreen forest sites. Losses of topsoil carbon with cropping can be predicted if the initial carbon and the clay+silt contents are known. The greatest carbon losses after long term cultivation occurred in forest mineral topsoils, ranging from 6% for perudic clayey soils to 37% for ustic sandy soils. No significant difference in carbon content was found between the paired savannah-cultivated sites. In most of the originally less fertile soils cation exchange capacity was greater in the cultivated topsoil (Ap) than in the topsoil under savannah or forest (A1), probably because of liming and phosphate fertilization. Most subsoils at agricultural sites show increases in exchangeable bases (mainly Ca) and base saturation, but no significant change in pH.     

A review of natural vegetation openness in north-western Europe

Secondary succession is threatening many species of open habitats in north-western Europe. This problem has caused an intense debate over whether the present-natural vegetation in this region would be closed forest or more open vegetation. Native large herbivores have been proposed as the key agents creating such open vegetation. Here I address this question by reviewing the palaeoecological evidence regarding vegetation openness in past oceanic interglacials and the pre-agricultural Holocene, i.e. before the onset of strong human impact. I conclude that closed forest would predominate, but include localized longer-lasting openings. Further, open vegetation would be frequent on floodplains, infertile soils, chalklands, and in continental and submeditteranean areas. Large herbivores and fire emerge as likely potential key factors in creating open vegetation in north-western Europe. Fire would probably also be important in the maintenance of light-demanding or short-statured woody species within closed upland forests.     

Heavy metals in crops as affected by soil types and sewage sludge rates

Abstract

A municipal sewage sludge was applied at three application rates to three soils in field lysimeters to study the effects of soil and sludge application rate on cadmium (Cd), copper (Cu), nickel (Ni), and zinc (Zn) absorbed by ‘Larker’ barley (Hordeum vulgare L.) and by Swiss chard (Beta vulgaris L. ‘Cicla'). Sludge applied at 20, 40, and 100 Mg/ha oven‐dry equivalent were mixed into the top 0.15 m of soil in each lysimeter. In addition, a nil sludge rate (control) received 125 kg N/ha. Metal contents were relatively low in barley grain, higher in barley straw, and highest in Swiss chard. Metal contents in plants increased with increasing sludge loading. Most plants grown on soil amended with the higher sludge rates were too high in Cd (greater than 0.5 mg/kg of dry feed material) to be suitable for animal consumption. No plant materials tested exceeded the suggested maximum Zn, Cu, or Ni levels.     

农作物叶片对大气沉降重金属的吸收转运和积累机制

近年来,农产品的重金属超标问题已经引起了公众的广泛关注,也是国内外学者研究的热点.要实现农产品重金属污染的有效防控,首先需要解决的就是重金属来源问题.目前已有的研究大多集中在根系对土壤中重金属的吸收机制研究,且已基本探明作物根系对重金属的吸收转运机制,包括根际离子的活化,根细胞的吸附和扩散、跨膜运输,根皮层细胞的横向运...     

NaCl胁迫下作物对离子的吸收及分配

盐渍化土壤在世界上分布广泛,在我国也有很大的面积。为了开发利用盐渍化的土地资源,传统的治理途径是采用工程和农业措施相结合的方法。然而,近年来越来越多的研究表明,发掘利用现有的生物资源,应用现代生物技术,通过培育抗盐品种来提高植物抗盐性也是开发利用盐碱土的一个重要方面。本文通过对作物耐盐品种和盐敏感品种的比较,综述了盐胁迫下粮食、果树、蔬菜及棉花等作物对K+、Na+、Ca2+、Mg2+等离子吸收及分配的影响,并提出了进一步的研究方向。     

Potassium release and fixation in Ferralsols (Oxisols) from Southern Togo

Potassium release and fixation were studied on Ferralsols (typic Eutrustox) of Southern Togo both by isotopic exchange with ⁴²K+ ions and by exchange with 1 M ammonium acetate. Experiments were conducted on soil samples taken from surface (0–30 cm) and subsoil (80–100 cm) layers of four plots. These plats, with the same soil type, were subjected to various kinds of use: forest and crops, with or without fertilizers. A single wetting and drying of the soil samples increased the amounts of exchangeable K. This exchangeable K release could stem from clay protonation during drying. However, the K release is insufficient to allow permanent intensive agriculture without K fertilizer addition. Soil samples were therefore treated with KCI in order to study K fixation. About 20% of the applied K was fixed and the percentage increased with wetting and drying. The fixation can be explained by the presence of about 2% of interstratified clay minerals in these kaolinitic soils. Comparison of the kinetic characteristics of the isotopically exchangeable K with the amounts of ammonium exchangeable K revealed the existence of several kinds of exchange site for K ions.     

Soil physical quality of Luvisols under agroforestry,natural vegetation and conventional crop management systems in the Brazilian semi-arid region

The imposition of agricultural systems changes the natural equilibrium of the soil to an extent that it becomes dependant on management practices and soil resilience. Agroforestry systems (AFs) mimic characteristics of natural ecosystems such as multistrata canopy and deep rooting and may minimize the consequences of these changes by providing soil protection and maintenance of conditions similar to those under natural vegetation. This study evaluates the physical properties of a Luvisol at a site where since 1997 alternative agroforestry systems (AFs) (agrosilvipasture—AGP and silvipasture—SILV), conventional crop management (CCM) and natural vegetation (NV) have been maintained. Undisturbed soil cores were collected in 2005 and submitted to a range of matric suction for which soil bulk density (BD), soil penetration resistance (Q) and soil water content (θ) were determined. Water retention and penetration resistance were used to determine the least limiting water range (LLWR) and the slope of the soil water retention curve at its inflection point (S-value). Particle size, total organic carbon (TOC) and particle density were determined using the disturbed soil samples. Water retention and porosity followed the sequence NV > SILV > CCM > AGP. The AFs studied (AGP and SILV) improved or maintained soil physical quality when compared to NV with no significant differences between the S-values of 0.044, 0.042 and 0.050, respectively. However, the S-value of 0.035 for CCM indicates that this management was unable to maintain soil physical quality on the same levels as AFs and NV. The decrease of LLWR with BD occurred for all treatments, and the BD at a maximum effect (LLWR = 0) which is called the critical BD (BD_c), was, respectively, 1.69, 1.62, 1.56 and 1.56 Mg m^?3 for AGP, SILV, NV and CCM. The larger values of LLWR for AFs (AGP and SILV) are similar to the value for NV, with associated superior aeration, matric suction and reduced resistance to penetration by roots. Indices such as LLWR and S-value were suitably sensitive and could be used in future research, but it is important to identify other potential indices for these situations that can show how quickly changes in soil quality may occur.     

基于高光谱植被指数的黑河流域作物叶绿素含量制图

Recent advances in optical remote sensing led to improved methodologies to monitor crop properties.The red-edge-based vegetation index considered to be one of the most powerful tools for estimating the chlorophyll content(Chl) was usually constructed from in-situ hyperspectral reflectance.In this paper, we present the work done to compare the Chl predictive quality by various red-edge-based vegetation indices based on the CASI data.The results indicated that among the selected vegetation indices, TCARI/OSAVI-based model estimated Chl(R2=0.46, RMSE =0.60 and P<0.01) with the best accuracy.To search the optimal vegetation index for Chl estimation, the normalized difference spectral index(NDSI) and ratio spectral index(RSI) were developed by using the waveband combination algorithm.A high linear correlation(R2=0.79, RMSE=0.38 and P<0.01) was acquired by combining the 869.20 and 754.90 nm wavebands, then NDSI(869.20, 754.90) was applied to the CASI image to generate the Chl distribution map.It suggests that more fertilizer should be provided for the southwest areas due to the lower Chl.     

肥料重金属含量状况及施肥对土壤和作物重金属富集的影响

本文对肥料中重金属的含量状况以及施肥对土壤和农作物重金属累积影响的研究进展进行了系统分析和总结。过磷酸钙中锌（Zn）、 铜（Cu）、 镉（Cd）、 铅（Pb）含量高于氮肥、 钾肥和三元复合肥,有机-无机复混肥料中的Pb含量高于其他化肥。有机肥如畜禽粪便、 污泥及其堆肥中的重金属含量高于化肥,猪粪中的Cu、 Zn、 砷（As）、 Cd含量明显高于其他有机废弃物,鸡粪中铬（Cr）含量高;污泥和垃圾堆肥中Pb或汞（Hg）含量高。商品有机肥Zn、 Pb和镍（Ni）含量高于堆肥,Hg含量高于畜禽粪便。多数研究表明,氮磷钾配施与不施肥相比土壤Cd和Pb含量增加,施用有机肥比不施肥提高土壤Cu、 Zn、 Pb、 Cd含量。施用化肥对农作物重金属富集的影响不明确,而施用有机肥可提高作物可食部位Cu、 Zn、 Cd、 Pb 的含量,影响大小与有机肥种类、 用量、 土壤类型和pH以及作物种类等有很大关系。在今后的研究中应着重以下几个方面, 1）典型种植体系下土壤重金属的投入/产出平衡; 2）不同种植体系下长期不同施肥措施对土壤重金属含量、 有效性影响的动态趋势; 3）典型种植体系和施肥措施下土壤对重金属的最高承载年限; 4）现有施肥措施下肥料中重金属的最高限量标准。