秸秆预处理对土壤微生物量及呼吸活性的影响

冬小麦秸秆经8．0g·L^-1H2O2(pH11．0)溶液、12．5g·L^-1 NaOH溶液或H2SO4溶液浸泡8h并80℃烘干后,与无机N一起加入土壤,进行室内25℃恒温培养试验,在不同时间测定土壤微生物量C、N和CO2释放速率。结果表明,培养前期,秸秆预处理使土壤微生物量C数量增加了1．0～1．4倍,但降低了土壤微生物的呼吸活性;培养后期,NaOH和H2SO4处理使土壤微生物量C分别下降了28％和42％,但增加了土壤微生物的呼吸活性;H2O2处理则使土壤微生物量N增加90％;土壤微生物区系中的真菌比例在不同时刻有所增加,表明将秸秆预处理后施入土壤,将对土壤中微生物数量和呼吸活性产生一定影响。     

秦岭火地塘森林生态系统不同层次的水质效应

根据降水与森林生态系统相互作用的空间顺序,分别对火地塘林区火地沟流域大气降水、林内雨、枯透水、支沟溪流水和流域出口径流水质进行了比较分析和变化机理分析。结果表明：森林生态系统不同层次均有使微酸性降水pH值升高的作用,但以林冠层和森林土壤的作用最大,升幅分别为0．58和0．61;森林生态系统对NO3^-、NH4^＋、K、PO4^3均有净化作用,净化NO3^-的关键阶段为沟道径流阶段,净化NH4^＋、K、PO4^3的主要方式则为土壤吸附;森林生态系统各层次均增加Ca含量,除土壤外,也增加Mg,但Ca主要来源于土壤和岩石,Mg主要来源于岩石;降水中的Cd、Pb、Mn、Zn经过森林生态系统不同层次的阻减,含量分别降低了0．721μg·L^-1、6．528μg·L^-1、0．0128mg·L^-1和1．4674mg·L^-1,其中以林冠层的阻减作用最大,阻减效果分别为83％、76．7％、54％和99％。总体上,林冠层是净化水质的关键层次,其次为森林土壤。     

有机酸对土壤无机态磷转化和速效磷的影响

土壤有效磷含量低是影响作物生产的重要限制因素之一.作物根分泌活化难溶性磷的有机酸对改善其磷素营养具有重要意义.采用张守敬和Jackson无机磷分级方法,以湖北省3种pH值土壤为材料,加入不同磷源和有机酸,经过室温培养后,测定速效磷含量和无机磷组分的变化.结果表明:施磷显著提高了土壤中速效磷含量,中性土、酸性土Fe-P和Al-P含量大幅上升, Fe-P占增加量的50%以上,而碱性土Ca-P含量显著增加.加施有机酸使中性土速效磷含量增多,除苹果酸处理的变幅较小外,草酸和柠檬酸的加入速效磷显著增加.由于有机酸的作用,中性土Al-P含量下降,Ca-P含量上升,变幅大小依次为草酸＞柠檬酸＞苹果酸;酸性土中Al-P含量呈下降趋势,碱性土中Ca-P含量有不同程度的减少,3种土壤中O-P含量均有所增加.说明有机酸活化的磷主要来源于中性土和酸性土Al-P、Fe-P及碱性土Ca-P中的磷,同时有机酸能够促进土壤中闭蓄态磷(O-P)的形成与积累.     

氮肥添加对黑钙土酸度变化及酸碱缓冲性能的影响

以pH为5.38、6.54、7.16和8.11(依次编号为A、B、C和D)的黑钙土为研究对象, 采用室内恒温培养法, 研究氮肥(尿素、磷酸二铵)添加对黑钙土酸度变化及酸碱缓冲性能的影响。结果表明, 模拟3年施肥量条件下, 施加尿素和磷酸二铵分别使4种黑钙土的pH值下降了0.44、0.51、0.61、0.36和0.52、0.55、0.86、0.42个单位。对4种土壤而言, pH值降低程度的大小顺序依次为C＞B≥A＞D。施加氮肥后, D土壤样品的pH值仍呈碱性, 故未检测出交换性酸、H+、Al3+。施加尿素和磷酸二铵使A、B、C土壤样品的交换性酸含量分别增加了0.07、0.94、3.62倍和0.23、0.74、2.93倍, 交换性H+含量分别增加了0.12、1.14、7.27倍和0.26、0.97、4.73倍, 交换性Al3+含量分别增加了0.15、0.77、2.35倍和0.21、0.54、2.29倍。交换性酸、H+、Al3+含量增加程度的大小顺序均为C＞B＞A。添加尿素的黑钙土交换性酸、H+、Al3+含量与添加磷酸二铵的无显著差异。尿素和磷酸二铵添加后, 4个土壤样品的酸碱缓冲容量分别下降了2.82%、10.27%、3.24%、2.99%和2.26%、3.80%、3.70%、3.94%, 且两种肥料的影响无显著差异。黑钙土酸碱缓冲容量与土壤pH、有机质含量呈极显著正相关, 与土壤交换性H+、AI3+含量呈显著负相关。总之, 氮肥添加不同程度上提升了不同酸度黑钙土的交换性酸、H+、Al3+含量, 降低了土壤pH值和酸碱缓冲容量。     

城市土壤磷素特性及其与地下水磷浓度的关系

采集了8个南京市的城区土壤剖面及同位置地下水样品,进行了P素特性的研究,结果表明,城市土壤的全P,有效P和可溶性P含量分别为1．26－11．41g.kg^-1,19.48-166.74mg.kg^-1和0．5、－5．41mg.kg^-1,远高于相同地区的农业土壤,土壤有效P与全P呈极显著正相关,土壤可溶性P与全P,有效P的相关性达到极显著水平,而土壤有机C,全N与土壤全P,有效P,可溶性P不相关,城市地下水中溶解态P和总P的浓度分别为0．010－1．759mg/L^-1和0．079－1．876mg.L^-1,它们之间呈极显著相关性,地下水中溶解态P,总P浓度与土壤剖面全P,有效P,可溶性P的加权平均值的相关性达到极显著或显著水平。     

鼎湖山森林土壤渗透水酸度和无机氮含量对模拟氮沉降增加的早期响应

在林地分别喷加0、50、100和150kg N hm^-1a^-1,研究鼎湖山马尾松林、马尾松针阔混交林和季风常绿阔叶林中土壤20cm深渗透水酸度和无机氮含量在开始9个月的变化。结果表明,3种森林对照样方土壤渗透水pH值为3．82—4．24,外加氮处理使其平均降低了0．08—0．18。3个森林对照样方土壤渗透水无机氮平均含量分别为6．14、6．66和11．64mg L^-1,铵态氮占15．0％、11．9％和3．0％。外加氮处理使3种森林土壤渗透水铵态氮和硝态氮含量均有不同程度的提高,这表明外加氮处理不但增加了无机氮从森林土壤流失的潜力,而且使土壤进一步酸化。     

日本曲霉产生的黑麦酮酸F对玉米的化感作用

日本曲霉（Aspergillus japonicus)是土壤和谷物种子表面的一种常见真菌。研究结果表明。日本曲霉所产生的大量黑麦酮酸F(SAF)对玉米(Zea mays)有很强的化感作用,低浓度显著促进玉米幼苗生长,高浓度则抑制．在0．0375mmol·L^-1SAF下,玉米幼苗根长增长31．7％,根数量增加13．2％,根活力提高4．73倍,并促进玉米对P、K、Ca、Mg、S等5种营养元素的吸收．高浓度SAF(0．3mmol·L^-1)下玉米根活力受抑制(72．1％),根对N、P、K、Ca、Mg、Fe等营养元素的吸收也受抑制.0．6mmol·L^-1的SAF下根完全失去活力,电镜观察表明,有SAF的情况下玉米叶绿体片层结构模糊、混乱,双层膜不完整。     

溶磷菌和固氮菌溶解磷矿粉时的互作效应

采用4株溶磷菌（Lx81、Dm84、Jm92、Lx191）、和3株固氮菌（ChW5、ChW6、ChO6）单独和混合接种后测定培养液有效磷含量、pH值及总有机酸含量的方法,研究溶磷菌和固氮菌溶解磷矿粉时的互作效应。结果表明,相对于单独接种溶磷菌：Lx81与3株固氮菌分别混合培养能提高磷矿粉的溶解能力,4株溶磷菌与ChW6,Lx81、Dm84、Lx191与Ch06分别混合培养及Jm92＋ChW5组合溶磷量极显著增加（P〈0．01）;Dm84＋ChW5、Lxl91＋ChW5、Jm92＋Ch06组合的溶磷量下降（P〈0．01）。除Lx81＋ChW6、Lx81＋Ch06培养液pH值降低外,混合培养的其它组合培养液pH值均较单独接种溶磷菌时升高。有机酸测定结果表明,Lx81、Jm92与ChW5、Ch06分别混合培养、ChW6＋Lx81组合有机酸含量升高（P〈0．01）,其它7种组合的有机酸含量均较单独接种溶磷菌的值下降（P〈0．01）。溶磷菌和固氮菌单菌培养时溶磷量与pH值、溶磷量与总有机酸含量及pH值与总有机酸含量之间呈现线性相关;Dm84、Lx191与3株固氮菌分别混合培养溶磷量与pH值之间、Lx81与3株固氮菌分别混合培养溶磷量与总有机酸含量之间呈现线性相关,其它组合的溶磷量与pH值、总有机酸含量间没有相关性。溶磷菌和固氮菌混合培养对溶解磷矿粉既有协同作用也有拮抗作用。     

大鼠冷束缚应激时胃粘膜损伤与外周β—内啡肽关系的实验研究

目的：探讨冷束缚应激大鼠血浆及胃黏膜中β－内啡肽（β－endorphine)的变化及作用。方法：制作大鼠冷束缚应激模型,以放免法测定应激0,1／4,2,8h血浆及胃黏膜中β－内啡肽的含量,同时测定胃液pH,胃黏膜溃疡指数（UI）,另设两预处理组,分别于应激前15分钟用纳洛酮（1．6mg/kg)和等容量生理盐水颈静脉注射,测定其UI及胃液pH,结果：整个应激过程中血浆及胃黏膜中β－内啡肽的含量无显著变化（P＞0．05）,应激各组胃黏膜UI均显著高于未应激组（P＜0．01）,应激15分钟组胃液pH显著高于未应激组（P＜0．01）,临终前（应激8h组）胃液pH显著高于对照组（P＜0．05）,阻断阴UI及胃液pH较对照组均无显著变化（P＞0．05）,结论：应激过程中血浆及胃黏膜β－内啡肽含量稳定,阻断β－内啡肽不影响胃液pH及UI,外周β－内啡肽变化对应激所致胃黏膜损伤可能不起重要作用。     

厌氧胁迫下芝麻不同耐渍基因型形态、生理及矿质元素变化的比较研究

在部控制氧下比较4种不同耐渍基因型芝麻的形态,生理指数及营养器官矿质元素含量变化。结果表明,耐渍品种种野芝7号与豫芝1号不定根条数增加4－5倍,净光合速率（Ph)下降幅度小,ADH活性增加约2倍,根据Ca,P含量显著升高,K降幅较小,根中其元素以及茎、叶中8种元素呈下降趋势。非耐渍品种丹巴格与遂平小籽黄,不定根条数无明显增加,Pn下降50％－60％,ADH活性可升高5－9倍;根中Ca,P含量亦增高,K下降较多,耐渍基因型有明显的结构适应特征,厌氧代谢的能量补偿作用相对次要,Ca,P在芝麻对厌氧胁迫的生理适应中起重要作用。     

Genotypic variability in phosphorus solubilizing activity of root exudates by pigeonpea grown in low-nutrient environments

A pot experiment confirmed that pigeonpea could efficiently utilize various sources of phosphorus (P) (aluminium phosphate, iron phosphate and apatite), irrespective of genotype. A qualitative assay method for iron (Fe)-P solubilizing activity showed that root exudates collected from P-deficient pigeonpea contained Fe-P solubilizing substances and that they were released mainly from root tips. Citric, malic, malonic, succinic and piscidic acids were identified in root exudates. Citric and piscidic acids release from roots was increased by low-P treatment in all the genotypes tested. The release rates of citric and piscidic acids were affected by the P concentration of shoots rather than that of roots. The pigeonpea roots released approximately 5–100 times more piscidic acid than citric acid depending on P stress status, plant age and genotype. When organic acids were added to Alfisols, citric acid was most capable of mobilizing P from the soil, followed by piscidic acid and malic acid. No correlation was found between genotypic variability in the release rates of citric and piscidic acids from the roots under low-P treatment at hydroponic culture and in the growth and P uptake of plants on Alfisols. Although citric and piscidic acids released from pigeonpea roots may play a partial role in solubilizing unavailable insoluble P in soils, the releases were thought to be an unsatisfactory strategy for explaining genotypic variation in low P availability of pigeonpea.     

低磷胁迫下AM真菌对枳实生苗吸磷效应及根系分泌有机酸的影响

在温室沙培灭菌条件下,以Al-P为磷源、枳为试材、Glomus mosseae (G.m)和G.versiforme (G.v)为菌剂,研究低磷胁迫下AM真菌对枳实生苗干物重、吸磷效应及根系分泌有机酸的影响。结果表明,接种AM真菌显著增加枳地上部、地下部干物重,增幅16.79%~135.25%;同时显著增加其吸磷量,菌丝对植株的吸磷贡献率为17.04%~71.95%(G.m>G.v),施Al-P显著提高菌丝吸磷贡献率。接种AM真菌的根系分泌的有机酸种类与对照有所不同,未接种处理枳分泌的有机酸有草酸、苹果酸、乳酸、乙酸、顺丁烯二酸和柠檬酸等6种,而接种G.m的则检测到草酸、酒石酸、苹果酸、乳酸、乙酸、柠檬酸、丁二酸等7种,G.v处理的检测到酒石酸,接种处理均未检测到顺丁烯二酸;接种丛枝菌根真菌增加了枳根系分泌有机酸的量(比未接种处理增加19.80~56.87 mg/kg,且施用AlPO₄后有机酸含量显著增加(增加20.06~21.84 mg/kg);未接种植株根系仅分泌少量有机酸;接种植株根系分泌的有机酸以苹果酸(42.87%)、柠檬酸(39.22%)和草酸(12.06%)为主。     

喀斯特不同植被恢复阶段土壤有机酸季节变化与有效氮磷的关系

植物分泌有机酸在提高土壤养分有效性方面起到重要作用。为了解喀斯特地区不同植被恢复阶段土壤有机酸含量季节性变化与氮磷有效性的关系,在灌木林和原生林各选择3种优势植物,测定雨季和旱季两个季节根际土和非根际土的有机酸含量、碳氮磷含量和比值、有效性氮磷含量及微生物生物量碳。结果表明:原生林植物根际土的草酸含量高于灌木林,而苹果酸和乙酸含量则低于灌木林;根际土草酸含量均高于非根际土;2个植被根际土和非根际土的草酸含量在雨季高于旱季,而苹果酸和乙酸含量则低于旱季;土壤草酸含量与有机碳、全氮、全磷和N∶P值呈显著正相关,与C∶N呈显著负相关;土壤有效氮和有效磷与草酸和微生物生物量碳呈显著正相关。上述结果表明,植物分泌有机酸的季节性变化与土壤养分状态和自身养分需求相关,而有机酸耦合微生物对养分有效性的提高具有积极的作用。因此,根际土的有机酸季节变化可能是喀斯特生态系统中植物适应土壤养分限制的一种重要机制。     

Influence of phenolic acids on phosphorus mobilisation in acidic and calcareous soils

Phenolic acids and phenols are abundant in soils. However, little information is available on the role of these compounds in mobilisation of soil phosphorus (P). The present study examined the effects of three phenolics on P mobilisation in comparison with citric acid in three soils differing in chemical properties. The soils were incubated with organic compounds at concentrations of 0 to 100 mol g^–1 soil for 30 min. While the addition of phenolic acid anions and phenol decreased soil pH, citrate either increased or did not affect soil pH depending on the soil type. All the organic compounds increased the amounts of easily-mobilised P fractions in the order of catechol citric acid proto-catechuic acid caffeic acid for the acid soils and citric acid > catechol = proto-catechuic acid > caffeic acid for the calcareous soil. Phosphorus mobilisation did not correspond to the amounts of Ca, Fe or Al ions released from the soils. These results suggest that organic acids and phenols altered the P fractions from stable, sparingly-soluble forms to easily dissolvable forms, and that chelation or precipitation of cations with organic ligands occur before biodegradation of the ligands.     

Low-molecular-weight aliphatic carboxylic acids in soil solutions under different vegetations determined by capillary zone electrophoresis

Concentrations of low-molecular-weight aliphatic carboxylic acids in soil solution were determined by a newly developed capillary zone electrophoresis method. Soil solution samples were collected by centrifugation of soil from the A horizon of a Danish, homogeneous, nutrient-rich Hapludalf in adjacent forested and arable plots. The forested plots of 0.5 ha were 33-year old stands of beech (Fagus sylvatica L.), oak (Quercus robur L.), grand fir (Abies grandis Lindl.), and Norway spruce (Picea abies (L.) Karst.), while sugar beet (Beta vulgaris L.) and winter wheat (Triticum aestivum L.) were the agricultural crops this year. High variability in soil solution concentrations of metal cations (Al, Ca, K, Mg, Na), monocarboxylic acids (formic, acetic, lactic, and valeric acids), and di- and tricarboxylic acids (oxalic, malic, succinic, and citric acids) were found within each plot. Despite this short-range within-plot variability, higher concentrations of di- and tricarboxylic acids were found in the forested soils than in the arable soils. The vegetation seemed to favour some monocarboxylic acids, but the total monocarboxylic acid concentrations showed little relation to the vegetation. Probably due to much less soil water in the Norway spruce plot, the low-molecular-weight aliphatic carboxylic acid concentrations in the samples from that plot were much higher than those found in samples from the other plots. Carbon in low-molecular-weight aliphatic carboxylic acids only accounts for a few percent of dissolved organic carbon, and no general relation was found between carbon in low-molecular-weight aliphatic carboxylic acids and dissolved organic carbon, although the correlation between carbon in di- and tricarboxylic acids and dissolved organic carbon was significant. This revised version was published online in June 2006 with corrections to the Cover Date.     

Aluminum resistance in two cultivars of Zea mays L.: Root exudation of organic acids and influence of phosphorus nutrition

Root exudation of organic acids as Al-chelating compounds and P nutrition have been suggested to play a major role in Al-resistance in higher plants. Effects of Al exposure on maize plant growth, and organic acid root content and root exudation under various levels of P nutrition were examined. Sikuani, a Colombian maize cultivar tolerant to acid soils with high Al saturation, and Corso, a Swiss cultivar, were grown in sterile hydroponic conditions for 21 days. Al-caused inhibition of root growth was lower in Sikuani than in Corso. Al effect on plant growth was decreased with increasing P content in roots. Al content in roots increased with increasing P content and was higher in Sikuani than in Corso. When exposed to Al, the contents in root apices as well as the root exudation of citric and malic acids in Corso and citric, malic and succinic acids in Sikuani increased, and were higher in Sikuani than in Corso. Increased PEP carboxylase (PEPC) activity in root apices after Al exposure partially explained the variations of organic acid content in the roots. These Al-induced changes in PEPC activity, organic acid content and exudation were reduced in plants supplied with higher P concentrations during the 21 days prior to treatment. Increased secretion of organic acids after exposure to Al appeared to be specific to Al and was not totally explained by increased root content in organic acids.     

Effects of Low-Molecular-Weight Organic Acids on Gadolinium Accumulation and Transportation in Tomato Plants

Effects of low-molecular-weight organic acids on the accumulation and transportation of gadolinium (Gd) in tomato plants were studied under hydroponic condition. The results indicated that changes of organic acids occurred in the processes of Gd accumulation and transportation in tomato plants which were treated with extraneous Gd solutions. Malic, citric, and succinic acids contributed to both Gd accumulation in roots and transportation in xylem vessels. When Gd was unloaded from the xylem to the leaf cells, formic, lactic, citric, and succinic acids played important roles in Gd accumulation in leaves. When tomato plants were cultured in the uptake solution of Gd-containing malic, citric, or succinic acid for 48 h, the succinic acid in roots and leaves and the malic acid in xylem saps both increased obviously. From the results above, we can conclude that succinic acid had the most important role in Gd accumulation in tomato roots and leaves, while malic acid transported Gd via xylem vessels more effectively.     

Effect of organic acids on the biosynthesis of macrotetralide antibiotics by an Actinomyces chrysomallus var. carotenoides strain

The biosynthesis of macrotetrolides by Actinomyces chrysomalus var. carotenoides was stimulated by acetic, succinic, propionic, oxalic, malic, tartaric, citric, pyruvic, alpha-ketoglutaric and fumaric acids. Incorporation of 14C-acetate into the molecule of the antibiotic and the data on dependence of the stimulating effect upon the quantitative ratio and time of the organic acid addition were indicative of the role of acetic, succinic and propionic acids as precursors of macrotetrolides. The other organic acids increased the biosynthesis of macrotetolides when added to the culture within wide time ranges of the culture development and prolonged the period of the mycelium productive state.     

Organic Acids of Ditylenchus triformis and Turbatrix aceti

Pyruvic acid, lactic acid and several tricarboxylic acid cycle acids were extracted from Ditylenchus triformis and Turbatrix aceti and identified. Fumaric acid was predominant in both nematodes. Small amounts o f malic and α-ketoglutaric acids and intermediate quantities o f lactic, citric, succinic, and pyruvic acids occurred in D. triformis. In T. aceti citric, lactic, and α-ketoglutaric acids were less abundant than succinic, malic and pyruvic acids. Only traces of aconitic and oxalacetic acids occurred in both nematodes. All the organic acids detected accounted for only about one per cent of the dry weight of nematodes o f the two species.