某硫矿重金属分级及土柱淋溶

Fractions of various heavy metals in a sulfidic minespoil were investigated.Column leachine experiment was also conducted to simulate “acid mine drainage“(AMD) from the minespoil.The results show that leaching of heavy metals from the minespoil was extremely significant during the initial water flushing.The amounts of heavy metals leached out dramatically reduced after leaching twice.It is worthwhile to note that in this study,Zn,Mn,Fe,As and Ni in the first leachate exceeded the total amount of each corresponding water-extractable(1:5,soil:water)metal contained in the minespoil sample.This appears to suggest that 1:5 water extraction did not allow accurate estimation of water-leachable concentrations of the above heavy metals.This work has implications for the management of sulfidic minespolis.Acid drainage of great environmental concerns is likely to occur only during heavy rainfall events after substantial soluble and readily exchangeable acid and metals are accumulated in the minespoils.The slow-reacting fractions other than water-soulble and readily exchangeable fractions may pose little environmental hazards.This is particularly true for Pb,As and Ni.     

Characterization and Heavy Metal Retention Capacity of Soils in Mangrove Forest of the Niger Delta,Nigeria

Abstract

Soils under the main mangrove (Rhizophora racemosa and Avicennia germinans) forest in the Niger Delta, Nigeria, were characterized, and their capacities to retain heavy metals were examined by using soil column leaching experiments, using 20 mg L^?1 Cu, 50 mg L^?1 Zn, 20 mg L^?1 Cd, and 100 mg L^?1 Mn solutions. At the end of the leaching experiments, soil samples from each column were divided into two layers (0–5 cm and 5–10 cm) and analyzed for total metal retained. The fractionation of heavy metals in the surface soil samples (0–5 cm) was investigated by the sequential extraction technique. The study showed that the soils were influenced by tidal flow and characterized by the presence of very fine textured, thin (0–5 cm) to moderately thick (10–15 cm) layer of alluvium (mud) on the surface. The fibric soil material beneath the surface mud varies in thickness from about 70 to 100 cm, and beyond the histic layer is the plastic, very sticky, massive clay. In situ, the soils were neutral in reaction (pH 7.0–7.2), but became strongly acid (pH 3.3–4.8) upon drying. They are saline, high in soluble salts, highly reduced, with CEC that is low in the fibric layer, but high in the mineral, clayey subsoil horizon. The soils are saturated with water for much more than 30 days in a year and have fiber content that is more than 40 cm thick, with the fibric sphagnum constituting more than three‐fourths by volume to a depth greater than 90 cm. The soils, classified as Typic Sphagnofibrists, sequestered considerable amounts of copper (Cu), zinc (Zn), cadmium (Cd), and manganese (Mn) with most of the metals retained in the surface soils. The anthropogenic heavy metals were mostly adsorbed probably to the negatively charged sites of organics and clay. These loosely bound metals may be desorbed and reenter the aqueous phase, thus becoming a secondary source of metal pollution.     

Seasonal soil nitrogen dynamics affect yields of lowland rice in the savanna zone of West Africa

Background : Rice production in low‐input systems of West Africa relies largely on nitrogen supply from the soil. Especially in the dry savanna agro‐ecological zone, soil organic N is mineralized during the transition period between the dry and the wet seasons. In addition, in the inland valley landscape, soil N that is mineralized on slopes may be translocated as nitrate into the lowlands. There, both in‐situ mineralized as well as the laterally translocated nitrate‐N will be exposed to anaerobic conditions and is thus prone to losses. Aim : We determined the dynamics of soil NO₃‐N along a valley toposequence during the dry‐to‐wet season transition period and the effects of soil N‐conserving production strategies on the grain yield of rainfed lowland rice grown during the subsequent wet season. Methods : Field experiments in Dano (Burkina Faso) assessed during two consecutive years the temporal dynamics and spatial fluxes of soil nitrate along a toposequence. We applied sequential and depth‐stratified soil nitrate analysis and nitrate absorption in ion exchange resin capsules in lowlands that were open to subsurface interflow and in those where the interflow from the was intercepted. During one year only we also assessed the effect of pre‐rice vegetation on conserving this NO₃‐N as well as on N addition by biological N₂ fixation in legumes using δ¹⁵N isotope dilution. Finally, we determined the impact of soil N fluxes and their differential management during the transition season on growth, yield and N use of rainfed lowland rice. Results : Following the first rainfall event of the season, soil NO₃‐N initially accumulated and subsequently decreased gradually in the soil of the valley slope. Much of this nitrate N was translocated by lateral sub‐surface flow into the valley bottom wetland. There, pre‐rice vegetation was able to absorb much of the in‐situ mineralized and the laterally‐translocated soil NO₃‐N, reducing its accumulation in the soil from 40–43 kg N ha^?1 under a bare fallow to 1–23 kg N ha^?1 in soils covered by vegetation. Nitrogen accumulation in the biomass of the transition season crops ranged from 44 to 79 kg N ha^?1 with a 36–39% contribution from biological N₂ fixation in the case of legumes. Rice agronomic performance improved following the incorporation as green manure of this “nitrate catching” vegetation, with yields increasing up to 3.5 t ha^?1 with N₂‐fixing transition seasons crops. Conclusion : Thus, integrating transition season legumes during the pre‐rice cropping niche in the prevailing low‐input systems in inland valleys of the dry savanna zone of West Africa can temporarily conserve substantial amounts of soil NO₃‐N. It can also add biologically‐fixed N, thus contributing to increase rice yields in the short‐term and, in the long‐term, possibly maintaining or improving soil fertility in the lowland.     

Use of the nitrate electrode for determination of nitrates in soils

Abstract

A procedure for the rapid and accurate determination of water‐extractable soil nitrates is described. Use of this procedure resulted in quantitative recovery of nitrates added to soil. Reproducibility of results was high, with nitrate‐nitrogen in 40 soil samples determined on successive days differing by a maximum of 4 ppm with 33 determinations differing by 2 ppm or less. Comparison with a phenoldisulfonic acid method on 513 soil samples had a maximum difference of 7 ppm with a majority of determinations having a difference of 4 ppm or less.     

Effect of Clinoptilolite Addition to Soil on Wheat Yield and Nitrogen Uptake

Abstract

During the past years, appreciable amounts of zeolite‐rich tuff that contains more than 70% clinoptilolite (Cp) have been discovered in Greece. The present study evaluates the ability of natural Greek Cp to increase the efficiency of nitrogen (N) fertilizer uptake in wheat. A pot experiment with winter wheat was conducted in a Typic Xerorthent that was fertilized with ammonium sulfate and amended with 0 to 60 ton/ha of Cp. Clinoptilolite application resulted in an increase of the cation exchange capacity of the soil from 9.5 to 13.6 meq/100 g (i.e., 43%). Soil ammoniacal N was greater in the samples amended with Cp at the boot stage, as was NO₃‐N. Clinoptilolite addition increased total wheat yield (dry matter of hay plus seed) 52% (from 21.1 g/pot in the control to 32.0 g/pot) in the treatment with 60 ton/ha of Cp. The influence was greater for seed yield than hay yield. Clinoptiloite addition resulted in high increase in total N uptake, about 141% (from 156 mg/pot in the control to 376 mg/pot) in the treatment with the highest Cp rate. For hay, the increase was 133% (from 125 mg/pot to 291 mg/pot), whereas for seed it was 126% (from 31 mg/pot to 70 mg/pot) from control to the treatment with the highest Cp rate, resulting in a more efficient N fertilizer use. The optimum Cp addition rate was estimated as large as 15 ton/ha.     

Physiological and Molecular Response of Wheat Roots to Nitrate Supply in Seedling Stage

The objective of this study was to understand the morphological, physiological, and molecular responses of wheat roots to nitrate supply at seedling stage. Two wheat genotypes, Jimai 22 and Shannong 15, were grown in Hoagland's nutrient solution with different nitrate levels at seedling stage. Results indicated that the plant dry weight and N accumulation increased with the increase of nitrate supply. The number of axial root, total uptake area (TUA), and active uptake area (AUA) increased with more nitrate supply. Correlation analysis indicated that significant positive correlations existed between N accumulation and dry weight, N accumulation and AUA, and N accumulation and AUA/TUA. Although, the expressions ofNRT2.1, NRT2.2, and NRT2.3 decreased with nitrate supply increased, the expressions of NRTI, NRT2.1,and NRT2.3 could maintain high level at N3 treatment. The free amino acid and NO3- content in shoot also increased with the increased nitrate application, but no significant difference was found in root among the treatments. These results implied that the increase of N uptake by nitrate supply was due to the morphological and physiological responses of wheat roots and the high expression level of TaNRT genes. Similarly, the contribution of morphological, physiological,and molecular parameters was different between two genotypes of wheat.     

添加不同形态化学氮肥对杏鲍菇菌渣堆肥的影响

以杏鲍菇菌渣为堆肥原料,分别添加硝酸钾、硫酸铵和尿素,调节堆体碳氮比(C/N)至20,研究添加不同化学氮肥对杏鲍菇菌渣堆肥的温度、p H、电导率(EC)、氧化还原电位(ORP)及有机(无机)态氮等的影响。结果表明:添加尿素和硫酸铵的堆肥升温较快,达到的最高温度较高,并且具有较低的p H值和较高的ORP值,堆肥最终的腐熟程度比添加硝酸钾的堆肥高;添加3种化学氮肥后,随着堆肥时间的推进,堆肥中的DOC、DON、NH4+–N、NO3––N、NO2––N含量都发生了变化,到堆肥结束时,添加硝酸钾的堆肥中DOC和DON含量高于添加硫酸铵和尿素的堆肥中的含量。综合分析,添加不同形态的化学氮肥对堆肥过程中的温度、酸碱度和氧化还原电位等产生影响,进而导致堆肥的腐熟程度不同。     

Measurement and simulation of herbicide transport in macroporous soils

Lysimeter experiments were carried out to study pesticide transport through macroporous soils. In order to differentiate between the effects of soil structure and chemical behaviour, the leaching experiments were conducted using disturbed and undisturbed soil samples. Two herbicides with different sorption behaviours, and bromide as tracer were applied. The results were used to validate a dynamic simulation model which considers bypass flow in macropores. The simulation results show that the model is able to reproduce the soil suction within the soil as well as the spatial distribution of bromide and the herbicides. The continuity of the macropores is most important for the efficiency of bypass flow. The results indicate that cultivation practices like ploughing significantly influence the temporal and spatial distribution of the macropores. © 1998 SCI.     

复合阻燃剂对思茅松胶合板性能的影响

选用5种磷-氮-硼复合体系阻燃剂对思茅松单板进行真空加压处理,用于制备阻燃胶合板,测试思茅松阻燃胶合板的胶合强度、燃烧性能、吸湿性和抗流失性.结果表明:当阻燃剂载药率为10%时,阻燃胶合板的胶合强度均≥1.15 MPa,超过Ⅱ类胶合板标准0.8 MPa;极限氧指数值均>38%,达到日本JIS难燃一级指标要求.当载药率为15%时,FR-a,FR-b和FR-c 3种阻燃剂处理的阻燃胶合板的极限氧指数值为53%~59%.5种阻燃剂中,FR-a会显著增加木材的吸湿性,其他阻燃剂对吸湿性影响不大.与阻燃剂的水溶性相对应,FR-a和FR-b抗流失性较差,FR-d和FR-e具有优良的抗流失性,FR-c则有一定的抗流失性.5种阻燃剂相比较,FR-c的综合性能最优.     

苯系化合物在硝酸盐还原条件下的生物降解性能

运用驯化的反硝化混合菌群进行了苯系化合物(BTEX)的厌氧降解试验.结果表明,混合菌群能够在反硝化条件下有效降解苯、甲苯、乙苯、邻二甲苯、间二甲苯和对二甲苯.BTEX的降解规律符合底物抑制的Monod模型,当初始浓度小于50mg·L^-1时,6种受试基质的厌氧降解速率顺序为:甲苯>乙苯>间二甲苯>邻二甲苯>对二甲苯>苯.整个试验过程中NO₃^-的消耗与苯、甲苯、乙苯、邻二甲苯、间二甲苯及对二甲苯生物降解之间的摩尔比分别为:9.47,9.26,1