糠醛渣生态肥对风沙土理化性质和茄子效益的影响

采用田间试验方法,研究了糠醛渣生态肥对河西内陆灌区风沙土改土培肥效应和茄子效益的影响。结果表明:糠醛渣生态肥原料间的效应是:茄子专用肥糠醛渣5406生物菌肥,糠醛渣生态肥配方比例为:5406生物菌肥0.0103:茄子专用肥0.1291:糠醛渣0.8606。施用糠醛渣生态肥与传统化肥比较,风沙土体积质量、pH、EC和可溶性盐分别降低了13.85%、1.07%、6.22%和6.92%;Hg、Cd、Cr和Pb离子分别降低了21.21%、40.00%、18.70%和21.94%;总孔隙度、团聚体和饱和持水量分别增加了13.35%、16.98%和13.35%;CEC、有机质、碱解氮、速效磷、速效钾、有效锌和有效钼分别增加了19.20%、25.93%、0.29%、1.89%、0.17%、2.08%和8.33%;真菌、细菌和放线菌分别增加了59.00%、41.94%和24.32%;蔗糖酶、脲酶和磷酸酶分别增加了57.51%、5.88%和10.35%;茄子单果重、单株果重、产量和施肥利润分别增加了5.27%、5.35%、3.01%和0.51×104元/hm~2。糠醛渣生态肥施用量与风沙土总孔隙度、团聚体、饱和持水量、有机质、速效养分和茄子产量呈显著的正相关关系;与体积质量、pH呈显著的负相关关系;糠醛渣生态肥施用量与茄子产量间的线性回归方程为y=51.2300+1.5151x–0.0408x2,经济效益最佳施用量为17.40 t/hm~2,茄子理论产量为65.24 t/hm~2。在风沙土上施用糠醛渣生态肥,有效的改善了土壤理化性质和生物学性质,提高了土壤有机质和番茄产量。     

Redox potential of bulk soil and soil solution concentration of nitrate,manganese, iron,and sulfate in two Gleysols

While the reduction of nitrate‐N, Mn(III,IV), Fe(III), and sulfate‐S in soil has been studied intensively in the laboratory, field research has received only limited attention. This study investigated the relationship between redox potential (E_H) measured in bulk soil and concentrations of nitrate, Mn²⁺, Fe²⁺, and sulfate in the soil solution of two Gleysols differing in drainage status from the Marsh area of Schleswig‐Holstein, Northern Germany. The soils are silty‐sandy and developed from calcareous marine sediments. Redox potentials were monitored weekly with permanently installed Pt electrodes, and soil solution was obtained biweekly by ceramic suction cups from 10, 30, 60, and 150 cm depth over one year. Median E_H at 10, 30, 60, and 150 cm depths was 470, 410, 410, and 20 mV in the drained soil and 500, 480, 30, and –170 mV in the undrained soil, respectively. A decrease in E_H below critical values was accompanied in the soil solutions (pH 7.4 to 7.8) by disappearance of nitrate below 0 to 200 mV, appearance of Mn²⁺ below 350 mV, and Fe²⁺ below 0 to 50 mV. Both metals disappeared from soil solution after aeration. In the sulfide‐bearing environment of the 150 cm depth of the undrained soil, however, the sulfate concentrations were highest at such E_H values at which sulfate should be unstable. This discrepancy was reflected in the fact that at this depth bulk soil E_H was about 400 mV lower than soil solution E_H (250 mV). When investigating the dynamics of nitrate, Mn, and Fe in soils, bulk soil E_H provides semi‐quantitative information in terms of critical E_H ranges. However, in sulfidic soil environments the interpretation of E_H measured in bulk soil is uncertain.     

模拟池塘中锶-89的迁移和积累动力学

采用放射性同位素示踪技术研究了核污染关键核素之一——~(89)Sr在水生生态系中的动力学行为。当示踪剂~(89)Sr一次性引入水系后,即向系统内的动植物及底泥迁移,从而使系统各组分中~(89)Sr-Sr的量均随时间变化。结果表明:1.在试验期间,池水中~(89)Sr-Sr的含量随时间减少,6d后由原来的1.76 ppm降至1.01ppm,11d后已不到原来的一半,第35d时只及原始量的30％。2.池水中的~(89)Sr-Sr向系统各组分中的迁移速率和数量因组分的性质而异。比如底泥,1d后由原始的0增加到7.07 ppm,11d后趋向平衡,以后几乎不再增加;~(89)Sr-Sr在鱼和螺蛳体内的含量在试验期间均随时间增加,35d时分别由原始的0增加到18.73ppm和48.28ppm;在处理当天,金鱼藻中~(89)Sr-Sr虽增加较快,由原始的0增至6.68 ppm,但4h后却几乎不再增加。3.水生动植物对放射性锶都有一定的浓集作用,最大的浓集系数分别为:螺蛳94.7,鱼36.7,金鱼藻只有12.6。可见,贝壳类动物对水系中的放射性锶有较强的去污能力。     

农业生产中的铁锰平衡问题

本文根据对菠萝和水稻的研究,论述了土壤和植物体内铁与锰的关系,认为在植物体内铁与锰的比例应保持一个平衡的关系。如果锰多铁少、比例失调,作物的正常生长将受到危害。     

Promotion of the seed germination and seedling growth of cabbage by root-colonizing fungi isolated from oat and Eucalyptus roots

(Jpn. J. Soil Sci.Plant Nutr., 77, 257–263, 2006)
The symptom of blighted leaves was observed for the melon plants grown on an isolated soil bed after steam sterilization (SS) in a greenhouse in Kochi Prefecture, Japan. To clarify the causes of this symptom, soil and plant analyses were conducted in the first experiment. Manganese concentrations in the leaves with the symptom were higher than 1,000 mg kg−1and exchangeable Mn in the soil was higher than 30 mg kg−1, which indicated the observed symptom was due to Mn excess. In the second experiment, formation of Mn oxide-dissolving substances after SS was examined for several organic amendments, because large amounts of palm chips had been supplied to the soil before SS in the first experiment. As a treatment similar to SS, palm chips, bark compost, and cattle feces manure were autoclaved. The water extracts were collected before and after the autoclave treatment and the Mn oxide-dissolving capacities of the extracts were evaluated. The Mn oxide-dissolving capacity of the water extracts after SS was remarkably higher than before SS, and the value was highest in palm chips, and followed by bark compost, and cattle feces manure. Fractionation and HPLC analysis of the water extracts after SS revealed that the main substance behind Mn oxide reduction in palm tips was arabinose and that in bark manure was malic acid. Further, Mn oxide-dissolving capacities of the water extracts were almost completely explained by the amounts of arabinose or malic acid found in these materials. From these results, it was considered that reducing substances such as arabinose were released by SS from the palm chips which had been applied in large quantity before SS and these reducing substances dissolved the soil Mn oxides and increased the amounts of available Mn, which led to the occurrence of Mn toxicity to the plants.     

Growth and phosphorus uptake of maize cultivated alone,in mixed culture with other crops or after incorporation of their residues

Intercropping or rotating of P‐efficient crop species which mobilize sparingly soluble P by their root exudates can have beneficial effects on growth and P uptake of P‐inefficient species. We aimed at studying the effect of intercropping or incorporating of crop residues of P‐efficient crops on the components of maize P‐uptake, i.e. the root‐system size and P influx (P‐uptake rate per unit root length). This was studied in 3 pot experiments in a low‐P sandy soil. In the first experiment, maize was intercropped with white lupine, sugar beet or oilseed rape, and with groundnut in the second experiment. In the third experiment, maize was grown after incorporating the crop residues of white lupine, sugar beet or oilseed rape. Maize growth and yield was strongly inhibited when intercropped with white lupine, sugar beet or oilseed rape, probably because of competition for nutrients. But with groundnut as the accompanying species, maize yield was increased by a factor of 3, mainly because of an enhanced P influx. Crop residues of oilseed rape and sugar beet increased the yield of maize by factors 2 and 1.6, respectively, because of a 3 and 2 times higher P uptake as compared to maize grown after maize without incorporation of crop residue. The reason for the higher maize P‐uptake after oilseed rape was an 11 times higher P influx as compared to maize without crop residues, and after sugar beet residues because of an enhanced root growth and a 4 times higher P influx. Lupine residues did not improve maize growth, mainly because of a low P influx, which was even less than that of maize grown without crop residues. The soil solution P concentration and calcium acetate lactate‐extractable P (CAL P) measured in this study did not reflect the P availability as indicated by the plants (P uptake, P influx). This indicates that other mechanisms such as P mobilization in the rhizosphere by root exudates or cell‐wall components were responsible for the increased P availability. These mechanisms need further investigation.     

Manganese availability and microbial populations in the rhizosphere of wheat genotypes differing in tolerance to Mn deficiency

Plant genotypes differ in their capacity to grow in soils with low manganese (Mn) availability. The physiological mechanisms underlying differential tolerance to Mn deficiency are poorly understood. To study the relationship between Mn content in soil, plant genotypes, and rhizosphere microorganisms in differential Mn efficiency, two wheat (Triticum aestivum L.) cultivars, RAC891 (tolerant to Mn deficiency) and Yanac (sensitive), were grown in a Mn‐deficient soil to which 5, 10, 20 or 40 mg Mn kg^–1 were added. The shoot dry matter of both cultivars increased with increasing Mn addition to the soil. At all soil Mn fertilizer levels, the tolerant RAC891 had a greater shoot dry matter and a higher total shoot Mn uptake than the sensitive Yanac. The concentration of DTPA‐extractable Mn in the rhizosphere soil of RAC891 at Mn20 and Mn40 was slightly lower than in the rhizosphere of Yanac. The population density of culturable microorganisms in the rhizosphere soil was low (log 6.8–6.9 cfu (g soil)^–1) in both cultivars and neither Mn oxidation nor reduction were observed in vitro. To assess the non‐culturable fraction of the soil microbial community, the ribosomal intergenetic spacer region of the bacterial DNA in the rhizosphere soil was amplified (RISA) and separated in agarose gels. The RISA banding patterns of the bacterial rhizosphere communities changed markedly with increasing soil Mn level, but there were no differences between the wheat cultivars. The bacterial community structure in the rhizosphere was significantly correlated with the concentration of DPTA‐extractable Mn in the rhizosphere, fertilizer Mn level, shoot dry matter, and total shoot Mn uptake. The results obtained by RISA indicate that differential tolerance to Mn deficiency in wheat may not be related to changes in the composition of the bacterial community in the rhizosphere.     

Can conservation tillage and residue management enhance energy use efficiency and sustainability of rice-pea system in the Eastern Himalayas?

ABSTRACT

Low productivity and energy use efficiency (EUE) of rice farming are the major concerns for agricultural sustainability in the Eastern Himalayan region of India. A field experiment on rice (Oryza sativa L.)-pea (Pisum sativum L) system was conducted for three consecutive years during 2012–15 in lowland ecosystem to assess the direct and residual impact of tillage and residue management (RM) practises on productivity and sustainability. Significantly higher grain yield of rice was achieved under no-till (NT) than minimum tillage (MT) and conventional tillage (CT). Among RM practises, 50% NPK + green leaf manure, 50% NPK + weed biomass and 50% NPK + in-situ residue retention recorded significantly higher mean grain yields than application of 50% NPK and 100% NPK without residues. Residual effect of MT in preceding rice gave significantly higher green pod yield of succeeding pea than NT and CT. The system EUE was significantly higher under MT (rice)-NT (pea) compared to those of NT-NT and CT-NT systems. The sustainable yield index of rice and pea was maximum under MT-NT followed by NT-NT. Thus, NT/MT with suitable RM practises is a pertinent strategy for sustainable productivity of rice-pea system in the Eastern Himalayas and in similar adjoining regions.     

Influence of cropping on the content,composition and dynamics of organic residue in the soil of the plough layer

Organic residue (OR) forms the undecomposed part of soil organic matter (SOM). The majority of it originates from plant remains, but to a certain extent it may also be derived from manure and from the remains of heterotrophic soil organisms. The OR content and dynamics are influenced by management practices (crop rotation, tillage, manuring). The main objective of this work was to study the effect of cropping on the content, fractional composition (coarse and fine fragments) and annual turnover of nonhumified SOM or OR in arable Podzoluvisol in the conditions of south Estonia and to evaluate the role of OR in the humus status of soil. Using the soil-coring method, the OR content and composition and underground phytomass (UGP) as a source of OR in the plough layer were studied. The soil cores (252) were taken during 1991–1992 from three long-term field trials cropped with wheat, barley, rye, potatoes and short-term clover-grass mixtures. The sample plots selected from field trials were tilled conventionally and fertilized according to normal Estonian soil management practice (with a mean rate of N₈₀P₂₃K₄₀ kg ha^-1 year^-1). The average OR content in arable soil ranged from 1.0 to 1.6 g ash-free dry matter (DM_af) kg^-1 soil. The greatest amount of UGP (2.85 g DM_af kg^-1), as a source of OR in soil, was estimated for the 2-year clovergrass mixture. Soil organic carbon accumulated in the composition of OR forms 5.7% of the total organic carbon pool of the plough layer. In regular cropping systems the OR content and pool seem to fluctuate within limits determined by the pedoecological conditions of the soil.     

植物修复对锰尾渣污染土壤特性的影响

采用盆栽法研究栽培美洲商陆和大豆进行植物修复后,锰尾渣污染土壤特性的变化。栽培美洲商陆和大豆可增加土壤的碱解氮、速效磷、速效钾和有机质。栽培植物后,土壤pH值变化不显著,但土壤磷酸酶、尿酶、蛋白酶、蔗糖酶、硝酸还原酶和脱氢酶的活性都高于对照。栽培植物可影响土壤锰和镉的形态分布,降低土壤锰和镉总含量,减少土壤水溶性锰和镉含量。在锰尾渣污染区域,混种美洲商陆与大豆进行植物修复,改良土壤特性更佳。