Mobility and Distribution of Zinc,Cadmium and Lead in Calcareous Soils Receiving Spiked Sewage Sludge

Leaching column experiments were conducted to determine the degree of mobility and the distribution of zinc (Zn), cadmium (Cd), and lead (Pb) because of an application of spiked sewage sludge in calcareous soils. A total of 20 leaching columns were set up for four calcareous soils. Each column was leached with one of these inflows: sewage sludge (only for two soils), spiked sewage sludge, or artificial well water (control). The columns were irrigated with spiked sewage sludge containing 8.5 mg Zn l^?1, 8.5 mg Cd l^?1, and 170 mg Pb l^?1 and then allowed to equilibrate for 30 days. At the end of leaching experiments, soil samples from each column were divided into 18 layers, each being 1 cm down to 6 cm and 2 cm below that, and analyzed for total and extractable Zn, Cd and Pb. The fractionation of the heavy metals in the top three layers of the surface soil samples was investigated by the sequential extraction method. Spiked sewage sludge had little effect on metal mobility. In all soils, the surface soil layers (0-1 cm) of the columns receiving spiked sewage sludge had significantly higher concentrations of total Zn, Cd and Pb than control soils. Concentration of the heavy metals declined significantly with depth. The mobility of Zn was usually greater than Cd and Pb. The proportion of exchangeable heavy metals in soils receiving spiked sewage sludge was significantly higher than that found in the control columns. Sequential extraction results showed that in native soils the major proportion of Zn and Pb was associated with residual (RES) and organic matter (OM) fractions and major proportion of Cd was associated with carbonate (CARB) fraction, whereas after leaching with spiked sewage sludge, the major proportion of Zn and Pb was associated with Fe-oxcide (FEO), RES, and CARB fractions and major proportion of Cd was associated with CARB, RES and exchangeable (EXCH) fractions. Based on relative percent, Cd in the EXCH fraction was higher than Zn and Pb in soils leached with spiked sewage sludge.     

Effect of high rates of sulphur on the CaCO3 and CaSO4 content of calcareous soils

Samples of two calcareous soils from central Iraq were amended with 2, 6 and 10 mg g⁻¹ soil of agriculturegrade sulphur and incubated for 4, 8 and 12 weeks at 30°C and 70% water-holding capacity. At the end of each incubation period, soils were analyzed for sulphate, CaCO₃ and CaSO₄. The sulphate content of the soils increased, whereas the CaCO₃ content decreased, with increasing S levels and incubation time. The gypsum formed was in proportion to the sulphur oxidised and the calcium released from CaCO₃.     

Effects of Plant Residue and Salinity on Fractions of Cadmium and Lead in Three Soils

Bioavailability and mobility of heavy metals (HMs) in soils are determined by their partitioning between solution and solid-phase and their further redistribution among solid-phase components. A study was undertaken to determine the effects of organic matter (OM) and salinity on cadmium (Cd) and lead (Pb) distribution among soil fractions. Three agricultural soils were treated with 20 mg Cd/kg as Cd (NO₃)₂·4H₂O, 150 mg Pb/kg as Pb (NO₃)₂, 20 g/kg alfalfa powder, and 50 mmol/kg of NaCl, and then incubated at 60% water holding capacity (60% WHC) and constant temperature (25°C) for 12 weeks. Various fractions of Cd and Pb were extracted from the soils after 2 and 12 w of incubation using a sequential extraction technique. Results showed that in the early stage of incubation (2 w), added Pb were found mainly in the specifically sorbed (SS) and amorphous Fe oxides (AFeO) fractions and added Cd found in SS and Mn oxides (MnO) fractions. Addition of 2% OM decreased the exchangeable (EXC) Pb fraction almost in all soils, whereas it had a different effect on the EXC Cd fraction depending on soil pH. Addition of NaCl increased the EXC Cd fraction in two soils, but it did not alter Pb fractions. At the end of the incubation period, Pb decreased in the EXC and MnO fractions except in the neutral soil and Cd decreased mainly in the SS fraction.     

玉米和大豆秸秆还田初期对黑土CO2排放的影响

通过恒温培养试验,研究了不同类型秸秆还田后的土壤CO₂排放特征及其与秸秆C、N含量的关系,以明晰黑土区不同类型秸秆还田后的分解特征,探明还田秸秆的C、N含量对固碳效果的影响.结果表明： 在61 d的培养试验中,土壤CO₂排放速率随时间呈现出“下降 稳定 增大(出现‘较高值’) 下降”的过程.不同类型秸秆还田后土壤CO2排放速率随时间变化的特征存在明显差异,主要体现在“较高值”出现和持续的时间不同.秸秆类型对土壤CO₂累积排放量具有显著影响,前21 d和前61 d的土壤CO2累积排放量对秸秆添加的响应不同.在前21 d,玉米根、玉米茎下部、玉米叶、大豆叶的CO₂累积排放量(约160 μmol·g^-1)显著大于其他秸秆;而除大豆叶外,大豆秸秆61 d的CO₂累积排放量均比玉米秸秆大.前21 d CO₂累积排放量与秸秆含碳量的比值(CR)和秸秆的C/N、含氮量之间均呈显著的线性相关;而61 d的CO₂累积排放量与秸秆的C、N含量之间不存在线性关系.综上,在还田条件下,秸秆类型对土壤CO₂的排放有明显影响;大豆秸秆比玉米秸秆容易分解,但与长时间分解不同,大豆秸秆还田最初阶段的分解速率小于玉米秸秆;秸秆的C/N、含氮量只对还田最初阶段的土壤CO₂排放有较大影响.     

玉米和大豆秸秆还田初期对黑土CO2排放的影响

通过恒温培养试验,研究了不同类型秸秆还田后的土壤CO₂排放特征及其与秸秆C、N含量的关系,以明晰黑土区不同类型秸秆还田后的分解特征,探明还田秸秆的C、N含量对固碳效果的影响.结果表明： 在61 d的培养试验中,土壤CO₂排放速率随时间呈现出“下降 稳定 增大(出现‘较高值’) 下降”的过程.不同类型秸秆还田后土壤CO2排放速率随时间变化的特征存在明显差异,主要体现在“较高值”出现和持续的时间不同.秸秆类型对土壤CO₂累积排放量具有显著影响,前21 d和前61 d的土壤CO2累积排放量对秸秆添加的响应不同.在前21 d,玉米根、玉米茎下部、玉米叶、大豆叶的CO₂累积排放量(约160 μmol·g^-1)显著大于其他秸秆;而除大豆叶外,大豆秸秆61 d的CO₂累积排放量均比玉米秸秆大.前21 d CO₂累积排放量与秸秆含碳量的比值(CR)和秸秆的C/N、含氮量之间均呈显著的线性相关;而61 d的CO₂累积排放量与秸秆的C、N含量之间不存在线性关系.综上,在还田条件下,秸秆类型对土壤CO₂的排放有明显影响;大豆秸秆比玉米秸秆容易分解,但与长时间分解不同,大豆秸秆还田最初阶段的分解速率小于玉米秸秆;秸秆的C/N、含氮量只对还田最初阶段的土壤CO₂排放有较大影响.     

The input and fate of new C in two forest soils under elevated CO2

The aim of this study was to estimate (i) the influence of different soil types on the net input of new C into soils under CO₂ enrichment and (ii) the stability and fate of these new C inputs in soils. We exposed young beech–spruce model ecosystems on an acidic loam and calcareous sand for 4 years to elevated CO₂. The added CO₂ was depleted in ¹³C, allowing to trace new C inputs in the plant–soil system. We measured CO₂‐derived new C in soil C pools fractionated into particle sizes and monitored respiration as well as leaching of this new C during incubation for 1 year. Soil type played a crucial role in the partitioning of C. The net input of new C into soils under elevated CO₂ was about 75% greater in the acidic loam than in the calcareous sand, despite a 100% and a 45% greater above‐ and below‐ground biomass on the calcareous sand. This was most likely caused by a higher turnover of C in the calcareous sand as indicated by 30% higher losses of new C from the calcareous sand than from the acidic loam during incubation. Therefore, soil properties determining stabilization of soil C were apparently more important for the accumulation of C in soils than tree productivity. Soil fractionation revealed that about 60% of the CO₂‐derived new soil C was incorporated into sand fractions. Low natural ¹³C abundance and wide C/N ratios show that sand fractions comprise little decomposed organic matter. Consistently, incubation indicated that new soil C was preferentially respired as CO₂. During the first month, evolved CO₂ consisted to 40–55% of new C, whereas the fraction of new C in bulk soil C was 15–23% only. Leaching of DOC accounted for 8–23% of the total losses of new soil C. The overall effects of CO₂ enrichment on soil C were small in both soils, although tree growth increased significantly on the calcareous sand. Our results suggest that the potential of soils for C sequestration is limited, because only a small fraction of new C inputs into soils will become long‐term soil C.     

Fate of [carbonyl-14C]methabenzthiazuron in an arid region soil — effect of organic amendment,soil disturbance and fumigation

[Carbonyl-¹⁴C] methabenzthiazuron (MBT) was applied to an arid region soil at a rate of 5mg kg⁻¹ soil to give a¹⁴C content of 2400 KB kg⁻¹ soil. After 15 weeks of incubation at 22°C and 50% of the maximum water holding capacity of the soil, 7.2% of the applied¹⁴C was mineralized to¹⁴CO₂. Where the soil was amended with wheat straw, total mineralization increased to 17.3%. Soil disturbance caused a significant increase while chloroform fumigation caused a significant decrease in the rate of¹⁴CO₂ production, both from amended and unamended soils. These results suggest that MBT is degraded mainly through microbial co-metabolism. Wheat straw amendment resulted in increased transformation of MBT into soil humus. In unamended soil, a major portion of¹⁴C was recovered in fulvic acid and in fractions extracted with organic solvents. Recovery of¹⁴C in non-extractable bound residues (humins) increased as incubation progressed and seemed to be derived from the fulvic acid fraction, which showed a concomitant decrease. More than 99% of the residual¹⁴C in unamended soil consisted of unaltered MBT; the remainder occurred as 1-methyl-1 (benzthiazolyl) urea. In amended soil, a relatively higher percentage of the extractable¹⁴C was found in the metabolite. Small amounts of three unidentified¹⁴C-labelled compounds were also observed. In amended soil, disturbance caused a decrease in extractable-¹⁴C whereas fumigation caused a significant increase, as compared to the untreated control. The effects were more pronounced when the soils were reated at an early stage of incubation. In general, soil disturbance increased the availability of MBT for further transformations while chloroform fumigation decreased the process.     

Effects of incubation temperature on the organic amendment‐mediated control of Fusarium wilt of tomato

Organic soil amendments play important roles in the reduction of plant diseases caused by soil‐borne plant pathogens. This study examined the combined effects of concentrations of organic amendments, temperature and period of incubation in soil on the management of Fusarium wilt of tomato caused by Fusarium oxysporum f. sp. lycopersici (Fol). In an experiment with substrate mixture, Fol reduction was higher when the soils were incubated at 35°C than at 30°C. Disease severity was proportionally reduced as the volume of amendment added increased. Furthermore, disease was significantly lower in substrates incubated for 30 days at both temperatures, as compared to substrates incubated for only 15 days. The most effective control was achieved with pelletised poultry manure (PPM). In experiments with natural sandy soil, the effects of amendments on Fol populations, measured by real‐time quantitative PCR with TaqMan probes, were significant. The highest decreases in Fol DNA resulted when the soil was amended with 2% PPM and incubated at 35°C. The reductions in DNA concentrations was most likely related to the accumulations of high concentrations of NH₃ (27.3 mM) in soils treated with 2% PPM and incubated at room temperature (RT; 23 ± 2°C), or at 35°C. Severity of plants grown in soils incubated at RT decreased by over 40%, and more than 73% when incubated at 35°C, regardless of the rate of PPM. The results indicate that the management with PPM, when combined with heating or solarisation, is an effective control measure against Fusarium wilt of tomato.     

Simultaneous Simulations of Uptake in Plants and Leaching to Groundwater of Cadmium and Lead for Arable Land Amended with Compost or Farmyard Manure

The water budget of soil, the uptake in plants and the leaching to groundwater of cadmium (Cd) and lead (Pb) were simulated simultaneously using a physiological plant uptake model and a tipping buckets water and solute transport model for soil. Simulations were compared to results from a ten-year experimental field study, where four organic amendments were applied every second year. Predicted concentrations slightly decreased (Cd) or stagnated (Pb) in control soils, but increased in amended soils by about 10% (Cd) and 6% to 18% (Pb). Estimated plant uptake was lower in amended plots, due to an increase of K_d (dry soil to water partition coefficient). Predicted concentrations in plants were close to measured levels in plant residues (straw), but higher than measured concentrations in grains. Initially, Pb was mainly predicted to deposit from air into plants (82% in 1998); the next years, uptake from soil became dominating (30% from air in 2006), because of decreasing levels in air. For Cd, predicted uptake from air into plants was negligible (1–5%).     

Screening of Indigenous Ornamental Species from Different Plant Families for Pb Accumulation Potential Exposed to Metal Gradient in Spiked Soils

Contamination of surface soils with lead (Pb) is a global concern due to the release of hazardous materials containing the metal element. In order to explore ways to remediate contaminated soils with less impact on environment and costs, this study aimed at screening ornamental plant species exposed to Pb gradient in spiked soils for Pb phytoextraction. Twenty-one ornamental plant species that currently grow in Pakistan, were selected to assess their potential for Pb accumulation. Pot experiments were conducted to evaluate the accumulative properties of the different plant species in unspiked control (Pb = 0) and spiked soils with different levels of Pb at 500, 1000, 1500 and 2000 mg Pb kg^?1 of soil. Biotranslocation factor (TF), Enrichment factor (EF) and Bioconcentration factor (CF) were calculated to assess the phytoremediation potential of tested plant species after seven weeks of exposure. Out of 21 plant species, Pelargonium hortorum and Mesembryanthemum criniflorum performed better and accumulated more than 1000 mg Pb kg^?1 of shoot dry biomass when they were grown in 500, 1000 and 1500 mg Pb kg^?1 contaminated soils. Both plants had no significant (P < 0.05) variation in the total dry biomass with increasing soil Pb concentration indicating a high tolerance to Pb. Considering the capacity of Pb accumulation, total dry biomass, TF, EF &; CF indices, Pelargonium hortorum and Mesembryanthemum criniflorum could be considered as Pb hyperaccumulators and could have the potential to be used in phytoremediation.     

Effects of Amendments and Water Conditions on the Chemical Speciation of Cd and Pb in Contaminated Paddy Soil in a Mining Area

Lime, sepiolite and peat were used as amendments to study their effects on the chemical speciation of Cd and Pb in a polluted paddy soil under moist and water-logged conditions. The results showed that application of amendments reduced acid-extractable Cd (up to 12.56% and 5.07%) and Pb (up to 6.69% and 2.68%) in moist and water-logged soils, respectively. The reducible Cd and residual Cd was increased while the oxidizable Cd was decreased after adding amendments. However, the oxidizable Pb was increased while the residual Pb was decreased in amended soil, and the reducible Pb presented a different changing trend under moist and water-logged conditions. The soil pH was significantly correlated with different fractions of Cd and Pb in soil, which indicated a distinct influence of soil pH on the redistribution process of Cd and Pb fractions in amended soil.     

Binding of cardiolipin/lecithin and monoamine oxidase to lipid-depleted mitochondrial membrane structure.

Lipid-depleted pig liver mitochondrial residues were incubated with different proportions of the acidic phospholipid cardiolipin and the zwitterionic phospholipid lecithin in either separate or mixed liposomes. When cardiolipin and lecithin were present in separate liposomes all of the cardiolipin but no lecithin bound to the residues. When present in the same liposomes, cardiolipin also caused binding of lecithin to the mitochondrial residues. When monoamine oxidase solubilized from pig liver mitochondria by extraction of the phospholipids was included in the incubation, binding of the enzyme to the residues occurred in the presence of cardiolipin. The percentage of enzyme bound followed the same trend as the binding of phospholipids to the mitochondrial residues.     

Temperature responses of carbon mineralization in conifer forest soils from different regional climates incubated under standard laboratory conditions

¹⁴C‐labelled straw was mixed with soils collected from seven coniferous forests located on a climatic gradient in Western Europe ranging from boreal to Mediterranean conditions. The soils were incubated in the laboratory at 4°, 10°, 16°, 23° and 30 °C with constant moisture over 550 days. The temperature coefficient (Q₁₀) for straw carbon mineralization decreased with increasing incubation temperatures. This was a characteristic of all the soils with a difference of two Q₁₀ units between the 4–10° and the 23? 30 °C temperature ranges. It was also found that the magnitude of the temperature response function was related to the period of soil incubation. Initial temperature responses of microbial communities were different to those shown after a long period of laboratory incubation and may have reflected shifts in microbial species composition in response to changes in the temperature regime. The rapid exhaustion of the labile fractions of the decomposing material at higher temperatures could also lead to underestimation of the temperature sensitivity of soils unless estimated for carbon pools of similar qualities. Finally, the thermal optima for the organic soil horizons (Of and Oh) were lower than 30 °C even after 550 days of incubation. It was concluded that these responses could not be attributed to microbial physiological adaptations, but rather to the rates at which recalcitrant microbial secondary products were formed at higher temperatures. The implication of these variable temperature responses of soil materials is discussed in relation to modelling potential effects of global warming.     

Decomposition and sorption characterization of plant cuticles in soil

The sorption of organic compounds by plant cuticular matter has been extensively investigated; however, little has been studied regarding the effect of plant cuticle degradation on their role in the sorption of organic compounds in soils. The sorption of phenanthrene was studied in soil samples which had been incubated for up to 9 months with three different types of plant cuticle isolated from tomato fruits, pepper fruits and citrus leaves. The main change in the diffuse reflectance Fourier-transform infrared (DRIFT) spectra during incubation of the cuticles was related to cutin decomposition. The peaks assigned to methyl and ethyl vibration and C=O vibration in ester links decreased with decomposition. In general, with all samples, the phenanthrene sorption coefficients calculated for the whole incubated soils (K _d) decreased with incubation time. In contrast, the carbon-normalized K _d values (K _oc) did not exhibit a similar trend for the different cuticles during incubation. The origin of the cuticle also affected the linearity of the sorption isotherms. With the tomato and citrus cuticle samples, the Freundlich N values were close to unity and were stable throughout incubation. However with the green pepper cuticle, the N values exhibited a significant decrease (from 0.98 to 0.70). This study demonstrates that the structural composition of the plant cuticle affects its biodegradability and therefore its ability to sorb organic compounds in soils. Of the residues originating from plant cuticular matter in soils, the cutan biopolymer and lignin-derived structures appear to play a dominant role in sorption as decomposition progresses. Responsible Editor: Alfonso Escudero.     

Heavy metals fractionation and organic matter mineralisation in contaminated calcareous soil amended with organic materials

Degradation of organic matter (OM) from organic amendments used in the remediation of metal contaminated soils leads to changes in soil chemical properties shortly after their addition, which may affect the soil metal distribution. The effects of two differing organic amendments on OM mineralisation and fractionation of heavy metals in a contaminated soil were investigated in an incubation experiment. The treatments were: control unamended soil, soil amended with fresh cow manure, and soil amended with a compost having a high maturity degree. The soil used was characteristic of the mining area at La Unión (Murcia, Spain) with 28% CaCO(3) and sandy-loam texture (pH 7.7; 2602 mg kg(-1)Zn; 1572 mg kg(-1)Pb). Manure and compost C-mineralisation after 56 days (24% and 3.8%, respectively) were below values reported previously for uncontaminated soils. Both amendments favoured Zn and Pb fixation, particularly the manure. Mn solubility increased at the beginning of the experiment due to a pH effect, and only Cu solubility increased through organic matter chelation in both amended soils.     

The dynamics of microflora and the occurrence of phytotoxic substances in different soils with corn residues and inorganic nitrogen

In an incubation experiment the development dynamics of bacterial and fungal communities as well as the level of phytotoxicity were analysed in sand and three soils differing in mechanical structure and amended with corn residues and mineral nitrogen. Bacterial biomass was positively correlated with the degree of dispersion of the solid phase of the soil, whereas the ratio of fungal to bacterial biomass (F:B) was found to be negatively correlated. Fungi were much more tolerant to carbon or nitrogen deficit than bacteria. Introduction of the plant material alone, characterized by a broad carbon to nitrogen ratio, led to the domination of fungi in microbial communities. The level of soil phytotoxicity built up with increasing level of crop residues. Phytotoxicity was observed for the longest time period in soil with the highest silt and clay content. The narrowing of the C:N ratio at introduction of the appropriate amount of mineral nitrogen (larger in heavier soils) resulted in accelerated disappearance of phytotoxicity and at the same time favoured bacterial development. This points to a significant participation of bacteria in the degradation of phytotoxic substances in the soil.     

Suitable Chemical Properties of Animal Manure Compost to Facilitate Pb Immobilization in Soil

Chemical immobilization using animal manure compost is one of the most useful for low-cost, in-situ soil remediation techniques. The present study aimed to determine suitable chemical properties of animal manure compost to facilitate lead (Pb) immobilization in soil. The level of mobile Pb in soil amended with swine compost was higher than that amended with cattle compost during the early stage of incubation. However, the level of mobile Pb was almost the same in soil amended with both types of compost on day 184 of incubation. The ratio of the residual fraction after sequential extraction was enhanced in soil amended with both types of compost, particularly swine compost. X-ray diffractometer (XRD) results demonstrated the precipitation of Pb phosphate minerals, such as pyromorphite, in Pb-sorbed composts, particularly swine compost. Amendment using swine compost could reduce Pb solubility even when it had a high content of water-soluble organic matter because it significantly lowered Pb phase solubility. The amendment with swine compost improved plant growth and microbial activity. This study suggests that composts with high phosphorus (P) content are suitable for Pb immobilization amendment even if they have a high water-soluble organic matter content.     

Optimization of soil physical and chemical conditions for the bioremediation of creosote-contaminated soil

Mispah type soil (FAO : Lithosol) contaminated with >250 000 mg kg^-1 creosote was collected from the yard of a creosote treatment plant. The soils carbon, nitrogen and phosphorus contents were determined. Due to creosote contamination, thecarbon content of the soil was found to be 130,000 mg C kg^-1. This concentration was found to greatly affect the nitrogen content (0.08%). The phosphorus content was less affected (4.5%). It was estimated that a nutrient amendment to bring the soil to a C : N 10 : 1 would be adequate to stimulate microbial growth and creosote degradation. The soil was amended with a range of C : N ratios below and above the estimated ratio. In one of the treatments, the phosphorus content was amended. Sterile and natural controls were also set up. The soil was incubated at 30 °C on a rotaryshaker at 150 rpm in the dark for six weeks. Water content was maintained at 70% field capacity. The lowest nitrogen supplementation (C : N = 25 : 1) was more effective in enhancing microbial growth (3.12E + 05) and creosote removal (68.7%) from the soil. Additional phosphorus was not very effective in enhancing the growth of microorganisms and removal of creosote. The highest nitrogen supplementation(C : N = 5 : 1) did not enhance microbial growth and creosote removal.A relationship between mass loss and creosote removal was also observed. Phenolics and lower molecular mass polycyclic aromatic hydrocarbons (PAHs) were observed to be more susceptible to microbial degradation than higher molecular mass compounds. Nutrient concentration, moisture content and pH were thus observed to play very significant roles in the utilization of creosote in soil. These results are being used for the development of a bioremediation technology for the remediation of creosote contaminated soils in a treatment plant in South Africa.     

模拟酸雨对不同土壤有机碳和作物秸秆分解的影响

为研究酸雨对不同pH值水稻土中有机碳分解的影响,选择酸性（pH 5.48）、碱性（pH 8.18）和中性（pH 6.70）水稻土（分别设置施用秸秆0、15 g·kg^-1土处理）在20 ℃条件下进行40 d的培养试验,各土壤组分别用pH值为6.0、4.5、3.0的模拟雨水将土壤含水量调为400 g·kg^-1(以风干土计).结果表明：秸秆、酸雨和土壤共同对土壤系统CO₂释放产生影响,秸秆的添加可显著提高土壤CO₂释放速率.培养期间,酸雨未显著影响土壤有机碳分解,但对土壤中作物秸秆的分解影响显著. pH 3.0酸雨处理下酸性和碱性土壤中秸秆40 d总分解量比pH 6.0处理高8%;酸雨抑制了中性水稻土中秸秆的分解,pH 3.0酸雨处理下秸秆40 d总分解量比pH 6.0处理低15%.pH 3.0酸雨处理下,酸性水稻土有机碳分解速率分别比中性和碱性水稻土高43%和50%（P<0.05）,秸秆在中性水稻土中分解量分别比其在酸性和碱性水稻土中低17%和16%（P<0.05）.     

Lipids in plant tissue cultures. VI. Effect of temperature on the lipids of Brassica napus and Tropaeolum majus cultures

The lipid contents of callus cultures of rape (Brassica napus) and nasturtium (Tropaeolum majus) increase in response to decreasing the temperature, though to different degree. Irrespective of the incubation temperature the lipids in cultures of both plants contain as predominant classes steryl glycosides, esterified steryl glycosides, sterols, steryl esters and fatty acids and, as minor constituents, various proportions of triacylglycerols, phospholipids and several unidentified fractions.The ratio of phospholipids to triacylglycerols as well as the ratio of diacylglycerophosphorylethanolamines to dicylglycerophosphorylcholines increase with time both in rape cultures incubated at 30°C and in those kept at 5°C.The lipids in rape and nasturtium cultures grown at 30°C contain smaller proportions of polyunsaturated fatty acids than the lipids in cultures incubated at 5°C. Erucic acid, the major constituent fatty acid of the seed lipids, in both plants, occurs only in trace amounts in the lipids of callus cultures. In contrast, linoleic and linolenic acids, which occur only in traces in the seed lipids of nasturtium, are major constituent fatty acids in the lipids of callus cultures derived from seedlings of this plant.The levels of constituent polyunsaturated fatty acids in the diacylglycerophosphorylethanolamines and the diacylglycerophosphorylcholines increase with time whereas in the triacylglycerols only linolenic acid is slightly increased.