免耕覆盖对不同质地土壤水分与作物产量的影响

采用空间位移法,将河北省吴桥县3种质地(砂土、砂质壤土、砂质粘壤土)的原状土转移到同一地点,研究了华北平原免耕覆盖下3种质地土壤的水分特征与作物产量。试验于2010—2013年开展,地点设在河北省吴桥县中国农业大学吴桥实验站。结果表明:相对传统翻耕,免耕覆盖可以增加土壤体积含水量,且在砂质壤土上的保水效果比其他2种土质更明显;砂质粘壤土免耕覆盖处理0~20 cm土层土壤体积含水量较传统翻耕处理低,不同于其他2种土壤;根据试验前2年结果,免耕覆盖并未显著提高作物的水分利用效率,小麦季趋势较为一致,砂土、砂质壤土和砂质粘壤土免耕覆盖的WUE比翻耕分别低13.95%、9.76%和8.61%;玉米季不同土质的趋势有差异,其中砂土免耕覆盖处理的WUE比翻耕低6.45%,而砂质粘壤土免耕覆盖处理的WUE比翻耕高4.89%,但差异均不显著;3种土质下,免耕覆盖相对传统翻耕没有表现出增产优势,小麦产量比传统翻耕分别降低7.09%、4.26%和0.39%,玉米产量分别减少9.81%、4.11%和10.19%。本试验条件下,免耕覆盖措施在3种土质均具有较好的保水效果,但短期内没有表现出增产趋势。     

Effect of temperature on rice growth in nutrient solution and in acid sulphate soils from Vietnam

Climatic and soil factors are limiting rice growth in many countries. In Vietnam, a steep gradient of temperature is observed from the North to the South, and acid sulphate soils are frequently devoted to rice production. We have therefore attempted to understand how temperature affects rice growth in these problem soils, by comparison with rice grown in nutrient solution. Two varieties of rice, IR64 and X2, were cultivated in phytotrons at 19/21°C and 28/32°C (day/night) for 56 days, after 3 weeks preculture in optimal conditions. Two soils from the Mekong Delta were tested. Parallel with the growing experiments, these two soils were incubated in order to monitor redox potential (E _h ), pH, soluble Al and Fe, soluble, and available P. Tillering retardation at 20°C compared to 30°C was similar in nutrient solutions and in soils. The effect of temperature on increasing plant biomass was more marked in solutions than in soils. The P concentrations in roots and shoots were higher at 20°C than at 30°C, to such an extent that detrimental effect was suspected in plants grown in solution at the lowest temperature. The translocation of Fe from roots to shoots was stimulated upon rising temperature, both in solutions and in soils. This led to plant death on the most acid soil at 30°C. Indeed, the accumulation of Fe in plants grown on soils was enhanced by the release of Fe²⁺ due to reduction of Fe(III)-oxihydroxides. Severe reducing conditions were created at 30°C: redox potential (E _h ) dropped rapidly down to about 0 V. At 20°C, E _h did not drop below about 0.2 V, which is a value well in the range of Fe(III)/Fe(II) buffering. Parallel to E _h drop, pH increased up to about 6–6.5 at 30°C, which prevented plants from Al toxicity, even in the most acid soil. Phosphate behavior was obviously related to Fe-dynamics: more reducing conditions at 30°C have resulted in enhancement of available P, especially in the most acid soil.     

Effect of zinc sources and levels on the growth and Zn nutrition of soybean (Glycine max. L.) in the presence of chloride and sulphate salinity

A study was conducted in a screen house in pots on a sandy loam soil deficient in Zn. Salinity was induced by adding 44, 88 and 132 me/l of chloride and sulphate salts in the saturation extract. To these treatments, 0, 5 and 10 ppm Zn were added as ZnSO₄·7H₂O or Zn-EDTA. The results indicated that the yield of soybean shoot was lowest at the highest salinity level and highest at the lowest level. Shoot yield improved markedly with Zn application. Both sources of Zn were equally effective in augmenting crop yields. Yields were low in Cl-salinity when compared with equivalent levels of SO₄-salinity. Application of ZnSO₄·7H₂O produced higher yields in SO₄-dominant salinity. Zinc content increased and Zn uptake decreased with increase in Cl-salinity regardless of Zn sources. In SO₄-salinity, ZnSO₄·7H₂O did not influence the Zn content, but uptake was suppressed with increase in SO₄-salinity. Increasing rates of SO₄-salinity enhanced Zn content in the presence of Zn-EDTA.     

猪粪和土霉素对不同肥力土壤微生物数量及活性的影响

在不施肥和施用猪粪两种情况下,采用培养试验研究了不同浓度土霉素污染(0、0.1、1、10、100和1000 mg·kg^-1)对土壤细菌丰度、酶活性和NO₃-N浓度等的影响.试验培养温度为25 ℃,培养时间为30 d,取样分析时间分别为1、4和30 d.结果表明：在不施肥条件下,土霉素污染对土壤细菌数量及微生物活性的影响较小,土壤S₁、S₂和S₃细菌数量、呼吸强度、酶活性和NO₃-N浓度下降10%时土霉素的剂量（EC₁₀）分别为36～1000 mg·kg^-1、20～1000 mg·kg^-1和4～1000 mg·kg^-1;而在施用猪粪的情况下,对应的数值分别为2～656 mg·kg^-1、2～81 mg·kg^-1和1～42 mg·kg^-1.添加土霉素对土壤细菌及酶活性的影响随土壤肥力的提高而增大,且其对土壤细菌数量和呼吸强度的影响大于对酶活性和NO₃-N浓度的影响.土霉素污染对土壤微生物数量和活性的影响随时间变化而变化,一般在培养4 d时的影响最为明显.土霉素对土壤微生物的影响总体上表现为抑制作用.     

Strong coupling between natural Planctomycetes and changes in the quality of dissolved organic matter in freshwater samples

Dilution-regrowth experiments coupled to fluorescence in situ hybridization were conducted with samples from two humic reservoirs in order to examine how inorganic nutrients (N, P) affect free-living bacterioplankton phylogenetic groups and subsequently the quality of dissolved organic matter (DOM). The experiments were complemented by analyses of the empirical relationships between the targeted bacteria, nutrients, DOM and grazers. The ratio of absorbance of waters (A) at 250 and 365 nm (A(250 nm):A(365 nm)), which has been found to increase with the proportion of small molecules in the DOM pool in other humic waters, was used as an index of DOM quality. When nutrient stimulated bacteria, both the responses of bacterial groups (in the absence of grazers) and the ratio A(250 nm):A(365 nm) were generally different between treatments (+N, +P, +NP), suggesting that in nutrient-poor systems, differences in the type of inorganic nutrient supply will ultimately cause differences in DOM quality. The ratio A(250 nm),:A(365 nm) peaked in the +N treatments where members of the Planctomycetes (PLA) were the most stimulated group, and across treatments, PLA best explained (positive relationship) variations in this ratio. Consistent with this, the in situ data showed that the removal of the negative effects of flagellates on PLA yielded the highest R(2) in attempts to use bacterial groups to explain variations in A(250 nm):A(365 nm). These findings provide lines of evidence, not previously demonstrated in natural waters, that Planctomycetes may be an important factor changing the DOM quality, particularly in nutrient-poor systems when supplied with inorganic N.     

人为营养物质输入对汉丰湖不同营养级生物的影响--稳定C、N同位素分析

以长江一级支流小江上游的汉丰湖为研究对象,设置了4个采样点(影响组:A, B;对照组:C, D),应用碳、氮稳定性同位素探讨人类生活污水和农业面源污染对汉丰湖水生生态系统中不同营养级水平生物类群的影响。结果表明:影响组POM(颗粒有机物)和螺类碳、氮稳定性同位素比值范围分别为-25.93‰--24.63‰、4.12‰-9.86‰,-14.28‰--21.60‰、7.97‰-19.99‰;对照组POM(颗粒有机物)和螺类碳、氮稳定性同位素比值范围分别为-25.62‰--22.51‰、0.01‰-6.56‰,-22.96‰--19.21‰、6.75‰-8.89‰;不同组间POM和初级消费者螺类碳同位素比值无明显空间变化(P>0.05), 而氮稳定性同位素比值空间变化显著(P<0.05)。因此,在汉丰湖食物网中,氮稳定性同位素特征更好地反应了营养物质(人为输入)吸收和富集的信息。与固着藻类、鱼类等相比,POM和软体动物螺类更适合作为环境评价的指示物。影响组A、B样点的部分生物类群已经受到了人为营养物质输入的影响,影响强度B样点区域>A样点区域。结果建议加强汉丰湖水环境保护,控制污水排放量及提高污水处理水平,对于保护小江和三峡库区水质具有十分重要的意义。     

Effect of different levels of water salinity on the decomposition of organic manures in a brackish water fish pond soil

Effects of different water salinity levels on the decomposition of the two organic manures cowdung and poultry manure were studied under laboratory condition. Application of the manures increased the free CO₂ content and decreased D.O. levels of water. pH values of soil and water declined slightly on addition of the manures. The amount of nitrogen, released from the organic manures to water and soil phases, increased gradually with the period of incubation but decreased with increase in water salinity levels. NH₄ ⁺ was found to occur in comparatively higher amount than NO₃ ^–, due to prevailing anaerobic environmental conditions. The amount of added organic carbon remaining in the soil decreased gradually as the decomposition proceeded, but recorded slightly higher values with increase in water salinity levels.The results showed that the rates of decomposition of added organic manures were comparatively lower under higher water salinity levels and hence indicated that use of well decomposed manures might be more suitable for use under such water salinities in brackish water fish ponds.This work formed a part of a thesis submitted for the Degree of Doctor of Philosophy to Bidhan Chandra Agricultural University, West Bengal in 1978This work formed a part of a thesis submitted for the Degree of Doctor of Philosophy to Bidhan Chandra Agricultural University, West Bengal in 1978     

亚热带森林不同植物及器官来源的可溶性有机质输入对土壤激发效应的影响及其作用机理

外源有机物的输入可以通过正负激发效应影响土壤有机碳(SOC)的矿化。然而, 当前的研究较少考虑不同植物及器官来源可溶性有机质(DOM)输入对土壤激发效应的影响及其作用机理。该研究以武夷山森林土壤为研究对象, 以室内培养的方式向土壤中添加¹³C标记青冈(Cyclobalanopsis glauca)、杉木(Cunninghamia lanceolata)、木莲(Manglietia fordiana)和相思(Acacia confusa)这4种植物的根和叶来源DOM, 研究不同植物及器官来源DOM输入对土壤激发效应的影响及其作用机理。主要结果: 不同植物及器官来源DOM添加初期加快了SOC的矿化, 呈现正激发效应, 随后转为负激发效应。从整个培养期(90天)的累积激发效应来看, DOM的输入均抑制了SOC的矿化, 使其矿化量减少22%-49%, 其中青冈根DOM输入使SOC的矿化量减少最多, 而由木莲叶DOM输入减少的SOC矿化量最少。DOM输入引起的土壤激发效应强度受不同植物器官影响明显, 具体表现在植物根来源DOM输入所引起的土壤激发效应强度显著高于植物叶来源DOM输入所引起的激发效应强度(相思除外)。DOM的输入总体上提高了土壤微生物生物量碳(MBC)含量、土壤β-葡萄糖苷酶活性、纤维素酶活性以及土壤有效氮含量, 而对微生物群落组成无明显影响。从结构方程模型来看, DOM输入所引起的土壤激发效应主要受土壤微生物对外源碳的利用(¹³C-MBC)、纤维素酶活性以及土壤有效氮含量的影响, 这些因子的变化可解释植物叶来源DOM和根来源DOM添加处理下土壤激发效应变化的68%和86%。该研究结果表明在土壤氮充足的条件下, DOM的输入可以通过提高微生物生物量、土壤酶活性来加快分解所添加的外源有机物, 从而减少了对SOC的分解。因此, 在该研究中“底物优先利用”是土壤激发效应的主要作用机理。     

Studies on the biotin flow at the duodenum of dairy cows fed diets with different concentrate levels and types of forages

Abstract

Biotin is involved in many vital metabolic pathways and must be provided for an efficient fermentation in the rumen, as well as for the intermediary metabolism of the host animal. Factors influencing ruminal biotin metabolism and output are widely unknown at present. Therefore, dairy cows fitted with permanent cannulas in the dorsal rumen and in the proximal duodenum were fed differently composed diets, and the biotin flow at the proximal duodenum was measured. The diets (on DM basis) consisted of 8.9 kg grass hay (Diet 1), 8.9 kg corn silage plus 2.0 kg concentrate (Diet 2), or 7.3 and 7.4 kg grass silage plus 10.0 kg concentrate (Diets 3 and 4). The concentrate in Diets 3 and 4 contained 87% wheat and corn grain, respectively. The cows were pre-fed the rations for 21 days. Thereafter duodenal digesta was sampled every two h for 5 days. Cr₂O₃ served as a flow marker and the microbial proportion of total nitrogen at the duodenum was estimated by near infrared spectroscopy (NIRS). The duodenal flow of biotin was not related to biotin intake, but to the amount of fermented organic matter (FOM) and the amount of microbial protein (Biotin [mg/d] = 0.518 · kg FOM?0.300; r = 0.85 and biotin [mg/d] = 0.012 · g microbial protein + 1.478; r = 0.84), irrespective of the composition of the diet fed. Mean daily biotin flow was 0.48 ± 0.11 mg/kg FOM without any systematic effect of diet composition. The ruminal biotin balance, calculated as the difference between biotin flow at the duodenum and biotin intake, was positive (1.4 – 2.0 mg/d) in cows fed the mixed roughage/concentrate diets and negative (?0.71 mg/d) when the pure hay diet was fed.     

不同施肥模式下稻田土壤微生物生物量磷对土壤有机碳和磷素变化的响应

通过15年的红壤稻田长期定位试验,研究了不同施肥模式下土壤微生物生物量磷(MB-P)对土壤有机碳和磷素变化的响应.结果表明红壤稻田有机碳源的长期投入和土壤有机碳的逐年升高使土壤微生物生物量碳(MB-C)维持在较高水平(＞800 mg·kg-1),是稻田土壤MB-P(＞16.0 mg·kg-1)提高的主要原因.长期不施磷肥条件下,土壤全磷含量与试验前相比显著降低(P＜0.05),而土壤有机磷含量平均提高了29.3%;土壤亏损的磷形态主要是无机磷(Al-P、Fe-P、Ca-P和O-P),其中Al-P含量处于最低水平(平均0.5 mg·kg-1).另外,长期不施磷肥土壤的MB-P远高于Olsen法提取态磷(Olsen-P)(＜7.0 mg·kg-1),而稻田土壤MB-P与Al-P呈显著相关(P＜0.05),表明土壤微生物对稻田土壤Al-P、Fe-P、Ca-P和O-P的利用是促进其向有效磷方向转化的关键途径.磷肥配合有机养分循环利用不仅提高了土壤磷库的积累,而且通过土壤微生物的活化有效地提高了土壤磷的有效性.     

氮添加对森林土壤有机碳库固存及CO2排放的影响研究进展

氮添加会引起土壤理化性质和养分有效性的改变。受此影响,森林植物的地上碳同化能力和地下碳分配格局也会相应地发生变化,总体表现为促进植物生长固碳,增加凋落物和植物根系沉积碳输入土壤,并改变上述植物源有机质的数量和化学成分。与此同时,土壤微生物的群落结构和生态功能也会受到氮添加的影响,由于土壤中的有机碳分解、转化和稳定等过程均受到微生物的驱动,因此,氮添加所引起的底物供应差异和微生物响应会影响森林土壤有机碳的矿化,并最终影响森林土壤有机碳库固存、稳定和CO₂排放。但目前关于氮添加对森林土壤有机碳库固存能力和CO₂排放特征的影响机制仍不清楚,为此,以森林土壤的碳循环过程为线索,综述了氮添加对底物供应、土壤有机碳激发效应、微生物碳代谢等过程的影响,并尝试梳理在氮添加影响下森林土壤有机碳分解、转化和稳定的微生物驱动机制。这有助于预测氮添加对森林土壤"氮促碳汇"的实际效果,以便研究人员在未来氮沉降日益严重背景下更好地预测森林土壤的碳循环特征,寻找提高森林土壤有机碳库固存能力和降低CO₂排放相关途径提供参考。同时,还分析了目前相关研究中存在的问题,并对该领域未来的研究热点进行了展望。     

Correlation between pyridoxal-5'-phosphate levels and the percentage activation of aspartate aminotransferase enzyme in haemolysate and plasma during in vitro incubation studies with different B6 vitamers

Conflicting results using erythrocyte aminotransferase (eAST) stimulation to assess vitamin B6 nutritional status in patients with less severe B6 deficiencies are common. It has been claimed that the presence of different B6 vitamers may modify the activation of eAST by pyridoxal-5'-phosphate (PLP) leading to stimulatory or even inhibitory effects. To investigate the possible role of this phenomenon in producing inconsistent AST stimulations, aliquots of whole blood were incubated with equivalent amounts of different B6 vitamers, and the AST stimulation was correlated with the concentrations of PLP, measured by high-performance liquid chromatography. At the end of the incubation period the erythrocytes and plasma were separately analyzed. The conversion of non-PLP B6 vitamers to PLP, by the erythrocytes, was similar (approximately 70%) for all B6 vitamers used in the incubation experiments. The newly formed PLP accumulated in the erythrocytes, but the percentage activation of AST did not change significantly from the basal levels, in spite of the presence of increased levels of PLP and other B6 vitamers used for incubation. When PLP was used in the incubation studies, all of it was retained by the plasma and was associated with a marked suppression of plasma AST stimulation. To determine the degree to which plasma and erythrocyte AST was dose-dependent, plasma and haemolysates were incubated with increasing concentrations of PLP. A very significant inverse relationship was obtained in plasma between AST stimulation and PLP even at modest PLP levels, while haemolysates required incubation with much higher PLP concentrations to demonstrate the same effect. Since plasma PLP is considered to be the most reliable indicator of B6 nutritional status in man, our findings suggest that plasma percentage AST stimulation more closely reflects the B6 nutritional status than erythrocyte AST stimulation test which may reflect B6 status only in severe, longstanding B6 deficiencies. Conflicting results using erythrocyte AST stimulations may be attributed to the insensitivity of red cell AST to changes in PLP content. It is unlikely that the presence of non-PLP B6 vitamers in haemolysate may affect the percentage stimulation of aminotransferase enzymes by PLP.     

Effect of short interspersed element sequences on the integration and expression of a reporter gene in the preimplantation-stage mouse embryos

Based on the assumption that foreign DNA sequences may have increased chance of integration into the host genome if they are flanked by high copy-numbered genomic sequences such as SINEs (short interspersed elements), we investigated the integration frequency of Lac Z reporter gene flanked by a fused B1/B2 in an in vivo system using pronuclear microinjection technique in the mouse. The SINE-flanked DNA showed a 4-fold increased integration frequency of the reporter gene than the control DNA (63% vs. 16%). Moreover, the level of beta-galactosidase expression, estimated from the X-Gal staining intensity in transgenic embryos, was greatly higher in SINE-carrying DNA. These results suggest that the SINE sequences can serve a very useful tool in improving the efficiency of current transgenic animal technology.     

Carbon translocation to the rhizosphere of maize and wheat and influence on the turnover of native soil organic matter at different soil nitrogen levels

Wheat and maize were grown in a growth chamber with the atmospheric CO₂ continuously labelled with ¹⁴C to study the translocation of assimilated carbon to the rhizosphere. Two different N levels in soil were applied. In maize 26–34% of the net assimilated ¹⁴C was translocated below ground, while in wheat higher values (40–58%) were found. However, due to the much higher shoot production in maize the total amount of carbon translocated below ground was similar to that of wheat. At high N relatively more of the C that was translocated to the root, was released into the soil due to increased root respiration and/or root exudation and subsequent microbial utilization and respiration. The evolution rate of unlabelled CO₂ from the native soil organic matter decreased after about 25 days when wheat was grown at high N as compared to low N. This negative effect of high N in soil was not observed with maize.     

Effects of different molecular weight fractions of dissolved organic matter on the growth of bacteria,algae and protozoa from a highly humic lake

Effects of different molecular size fractions (< 1000 MW, < 10 000 MW, < 100 000 MW and <0.1 μm) of dissolved organic matter (DOM) on the growth of bacteria, algae and protozoa from a highly humic lake were investigated. DOM from catchment drainage water as well as from the lake consisted mostly (59–63%) of high molecular weight (HMW) compounds (> 10 000 MW). With excess inorganic nutrients, the growth rate and yield of bacteria were almost identical in all size fractions. However, in < 1000 MW fractions and with glucose added, a longer lag phase occurred. Without added nutrients both the growth rates and biomasses of bacteria decreased towards the smaller size fractions and the percentage of dissolved organic carbon (DOC) used during the experiment and the growth efficiency of bacteria were lower than with excess nutrients. The growth efficiency of bacteria was estimated to vary between 3–66% in different MW fractions, largely depending on the nutrient concentrations, but the highest growth efficiencies were observed in HMW fractions and with glucose. The growth of algae was clearly lowest in the < 1000 MW fraction. In dim light no net growth of algae could be found. In contrast, added nutrients substantially enhanced algal growth and in deionized water with glucose, algae achieved almost the same growth rate and biomass as in higher MW fractions of DOM. The results suggested that bacteria and some algae were favoured by DOM, but protozoans seemed to benefit only indirectly, through bacterial grazing. The utilization of DOM by bacteria and algae was strongly affected by the availability of phosphorus and nitrogen.     

Effect of starch addition on the biological conversion and microbial community in a methanol-fed UASB reactor during long-term continuous operation

The effect of starch addition on the microbial composition and the biological conversion was investigated using two upflow anaerobic sludge bracket (UASB) reactors treating methanolic wastewater: one reactor was operated with starch addition, and another reactor was operated without starch addition. Approximately 300 days of operation were performed at 30 kg COD/m³/d, and then, the organic load of the reactors was gradually increased to 120 kg COD/m³/d. Successful operation was achieved at 30 kg COD/m³/d in both reactors; however, the methanol-fed reactor did not perform well at 120 kg COD/m³/d while the methanol-starch-fed reactor did. The granule analysis revealed the granule developed further only in the methanol-starch-fed reactor. The results of the microbial community analysis revealed more Methanosaeta cells were present in the methanol-starch-fed reactor, suggesting the degradation of starch produced acetate as an intermediate, which stimulated the growth of Methanosaeta cells responsible for the extension of granules.     

藏北高寒草地土壤有机质化学组成对土壤蛋白酶和脲酶活性的影响

土壤酶作为生态系统的生物催化剂, 是土壤有机体的代谢驱动力, 在土壤物质循环和能量转化过程中起着重要作用。该研究以藏北5种不同类型高寒草地(高寒草甸、高寒草原、高寒草甸草原、高寒荒漠草原和高寒荒漠)为研究对象, 利用热裂解气质联用技术(Py-GC/MS)分析不同类型草地土壤有机质化学组成, 并建立其与土壤蛋白酶和脲酶活性之间的相互关系。结果表明, 5种高寒草地土壤(0-15 cm)的酶活性表现出一定差异性, 高寒荒漠草原土壤的脲酶活性显著高于蛋白酶活性, 而其余类型高寒草地的脲酶和蛋白酶活性之间的差异未达到显著水平; 蛋白酶活性在5种高寒草地土壤之间的差异显著, 而脲酶活性在5种草地土壤之间的差异未达到显著水平。相关分析发现, 土壤蛋白酶活性与土壤有机质烷烃、烯烃和芳香烃的相对丰度和糠醛:吡咯的值密切相关, 土壤脲酶活性与土壤有机质化学组成之间相关性未达到显著水平。综上所述, 高寒草地类型和土壤有机质化学组成是影响高寒草地土壤蛋白酶活性的重要因素, 而对土壤脲酶活性的影响均未达到显著水平, 其影响因素有待进一步深入的研究。     

Cultivation effects on the nature of organic matter in soils and water extracts using CP/MAS 13C NMR spectroscopy

The objective of this study was to examine the chemical structure of the organic matter (SOM) of Oxisols soils in slash and burn agriculture, in relation to its biological properties and soil fertility. The CP/MAS ¹³C technique was used to identify the main structural groups in litter and fine roots as SOM precursors; to identify the changes on the nature of the SOM upon cultivation and the proportion of labile and stable components; and to identify the nature of the organics present in water extracts (DOC). Carbohydrates were the main structural components in litter whereas components such as carbonyl C, carboxyl C,O-alkyl C and alkyl C were more common in SOM. Phenolic C and the degree of aromaticity were similar in litter and SOM. Cultivation resulted in a small decrease in the relative proportion of carbohydrates in SOM, little change in the levels of O-alkyl C and carbonyl C, but an increase in carboxyl C, phenolic C and aromaticity of the SOM. The level of alkyl C in soil was higher than the level of O-alkyl C, indicating the importance of long-chain aliphatics along with lignins in the stabilization of the SOM in Oxisols. The SOM of Mollisols from the Canadian Prairies differed from the Oxisol, with a generally stronger expression of aromatic structures, particularly in a cultivated soil in relation to a native equivalent. Carbohydrate components were the predominant structures in the DOC, indicating their importance in nutrient cycling and vertical translocations in the Oxisol.     

Effect of Wortmannin on the repair profiles of DNA double-strand breaks in the whole genome and in interstitial telomeric sequences of Chinese hamster cells

The DNA breakage detection-fluorescence in situ hybridization (DBD-FISH) procedure was applied to analyze the effect of Wortmannin (WM) in the rejoining kinetics of ionizing radiation-induced DNA double-strand breaks (DSBs) in the whole genome and in the long interstitial telomeric repeat sequence (ITRS) blocks from Chinese hamster cell lines. The results indicate that the ITRS blocks from wild-type Chinese hamster cell lines, CHO9 and V79B, exhibit a slower initial rejoining rate of ionizing radiation-induced DSBs than the genome overall. Neither Rad51C nor the catalytic subunit of DNA-dependent protein kinase (DNA-PKcs) activities, involved in homologous recombination (HR) and in non-homologous end-joining (NHEJ) pathways of DSB repair respectively, influenced the rejoining kinetics within ITRS in contrast to DNA sequences in the whole genome. Nevertheless, DSB removal rate within ITRS was decreased in the absence of Ku86 activity, though at a lower affectation level than in the whole genome, thus homogenizing both rejoining kinetics rates. WM treatment slowed down the DSB rejoining kinetics rate in ITRS, this effect being more pronounced in the whole genome, resulting in a similar pattern to that of the Ku86 deficient cells. In fact, no WM effect was detected in the Ku86 deficient Chinese hamster cells, so probably WM does not add further impairment in DSB rejoining than that resulted as a consequence of absence of Ku activity. The same slowing effect was also observed after treatment of Rad51C and DNA-PKcs defective hamster cells by WM, suggesting that: (1) there is no potentiation of the HR when the NHEJ is impaired by WM, either in the whole genome or in the ITRS, and (2) that this impairment may probably involve more targets than DNA-PKcs. These results suggest that there is an intragenomic heterogeneity in DSB repair, as well as in the effect of WM on this process.