土壤腐殖质组成对大气二氧化碳浓度升高的响应

为了探求大气CO2浓度升高对土壤腐殖质及其组成的影响，为大气CO2浓度升高条件下土壤生物化学过程的变化提供依据，通过稻-麦轮作FACE（Free-air CO2 enrichment）平台研究了正常施氮水平下水稻土壤有机碳及其各组分对大气CO2浓度升高的响应。研究结果表明：不同土层的腐殖质组分含量有所差异，表层（0～15cm）土壤腐殖化程度较高，表层的土壤有机碳（SOC）、水溶性碳（WSOC）、胡敏酸（HA）、富里酸（FA）、胡敏素（HM）数量均高于下层（15～30cm）。大气CO2浓度升高，增加了表层和下层的SOC，促进了土壤有机质的积累；使表层WSOC有增加趋势，但对下层没有显著影响；降低了土壤中可提取腐殖物质中HA的比例（PQ），土壤的腐殖化度下降，有利于HA的分解与转化和FA的积累；对土壤HM没有显著影响。     

施用有机物料对土壤镉形态的影响

采用室内培养试验,研究作物新鲜秸秆和腐熟猪粪对模拟镉（Cd）污染的土壤中Cd形态转化的动态影响。结果表明,各处理土壤交换态Cd含量随培养时间均逐渐降低。碳酸盐结合态和铁锰氧化物结合态Cd含量先增加后降低, 而有机质结合态和残渣态Cd含量则逐渐增加。添加秸秆可增加土壤交换态Cd含量,但随时间延长,增幅逐渐降低, 猪粪则可降低土壤交换态Cd含量。添加有机物后土壤交换态Cd含量的变化主要是由有机质结合态或残渣态Cd含量的变化而引起。秸秆和猪粪对土壤Cd形态的转化与土壤胡敏酸（HA）和富里酸（FA）的变化有关。秸秆对能活化土壤Cd的FA增加幅度大于对能钝化土壤Cd的HA增加幅度,降低HA/FA比,但降幅随时间逐渐减少; 猪粪在整个培养阶段对HA增加幅度均大于FA的增加幅度,增加HA/FA比。秸秆和猪粪均可降低潮土pH而提高红壤pH,但只有猪粪可通过提高红壤pH降低Cd向交换态转化。添加秸秆和猪粪后,Cd由低活性态向交换态转化与HA/FA呈显著负相关。     

开垦年限对稻田土壤腐殖质组成和胡敏酸结构特征的影响

以吉林省磐石市朝阳山镇青山村开垦年限分别为5 a、20 a和50 a的稻田土壤为研究对象,研究了0~15 cm和15~30 cm土层的土壤有机碳含量(SOC)、水溶性物质(WSS)、富里酸(FA)、胡敏酸(HA)和胡敏素(Hu)组成和HA结构特征及土壤养分含量的变化。结果表明:随稻田开垦年限增加(5~50 a),表层(0~15 cm)与亚表层(15~30 cm)土壤变化如下:(1)电导率分别增加74.8%和113.7%,p H均基本稳定。土壤速效氮、有效磷和速效钾含量分别增加0.24%、15.8%、29.7%和1.33%、6.92%、14.7%。(2)有机碳总量分别增加42.1%和47.9%,WSS、HA和Hu含量分别增加28.4%、51.9%、76.2%和87.7%、84.9%、70.1%,而FA含量分别下降了9.2%和1.74%。说明稻田耕作年限越长越有利于土壤有机碳的积累。(3)胡敏酸占腐殖质的比例(PQ)值均增大,土壤腐殖化程度加深。(4)HA的氢碳元素物质的量之比(H/C)、色调系数(?lg K)、半定量分析得红外光谱在2 920和1 720峰处吸收强度之比(E2 920/1 720)与在2 920和1 620峰处吸收强度之比(E2 920/1 620)均减小,HA分子芳化度增强,缩合度上升,结构变得复杂。     

不同CO2浓度对玉米秸秆分解期间土壤腐殖质形成的影响

以往人们较多的研究了土壤有机碳与温室气体的源、汇关系问题,却很少研究温室气体对土壤有机碳本身分解转化和各组分性质的影响。为了探讨CO2浓度升高对腐殖物质形成转化的作用,本文通过室内人为高浓度CO2的培养试验,用腐殖质组成修改法研究了玉米秸秆分解期间（1~180d）土壤总有机碳（TOC）、水溶性物质（WSS）、碱提取腐殖物质（HE）、胡敏酸（HA）和胡敏素（HM）数量的动态变化规律及不同CO2浓度对有机碳各组分形成与转化的影响。结果表明：玉米秸秆分解期间,“新形成”的净TOC逐渐降低,净HE表现为先增加而后下降的趋势,HM的绝对数量逐渐下降。可提取腐殖物质中HA的比例（PQ）先增加后下降,最终趋于平稳,说明最初富里酸（FA）的形成速度大于HA,随培养时间的延长,FA和HA经历了一段相互转化的过程,最终达到动态平衡。30%CO2浓度（V/V）处理的TOC、WSS、HE和HM数量明显高于3%CO2浓度处理和正常CO2浓度（0.0375%）处理,其中WSS和HM反应更为敏感。但3%CO2浓度处理与正常CO2浓度处理的差异不明显。可提取腐殖物质的PQ的顺序是30%CO2浓度处理〉3%CO2浓度处理〉正常CO2浓度处理,说明CO2浓度增加更有利于FA而不利于HA的形成和稳定。     

不同种植年限设施菜地土壤有机质组成与结构变化

试验采集不同种植年限设施菜地土壤样品,测定土壤有机质(SOM)、可溶性有机碳(DOC)、胡敏酸(HA)、富里酸(FA)、微生物量碳(MBC)、微生物商(C_(mic)-to-C_(org))、C矿化和E4/E6值等指标,结合傅立叶变换红外光谱技术解析不同种植年限土壤有机质组成与结构变化的规律。结果显示,随着种植年限的增加,SOM、DOC、HA、HA/FA、MBC、C_(mic)-to-C_(org)、E4/E6值、C矿化率和CO_2释放速率均出现明显下降趋势,其中MBC、C_(mic)-to-C_(org)、C矿化率、CO_2释放速率和HA/FA在种植6 a时下降最明显,之后变化缓慢。与露天农田土壤(CK)相比,设施菜地呈现较高的SOM、DOC、Humus、HA、FA、HA/FA和E4/E6。胡敏酸红外光谱图谱显示设施菜地种植20 a处理土壤芳构化程度高,结构稳定,难以降解,其他三种种植年限(3 a、6 a和10 a)的芳构化程度相对较低,脂肪族成分相对较高。综上可知,设施菜地土壤有机质组成与结构随着种植年限的增加具有规律性变化,结果加深了对设施菜地土壤有机质演变规律的认知。     

秸秆和猪粪的施用对土壤镉有效性的影响和机理研究

用盆栽试验研究作物秸秆和腐熟猪粪对土壤镉（Cd）有效性的影响及机理。结果表明,施用秸秆促进油麦菜对Cd的吸收,而施用猪粪降低油麦菜对Cd的吸收,这主要是由于秸秆显著地增加了交换态Cd含量,而猪粪则显著降低交换态Cd含量。秸秆或猪粪对交换态Cd含量的影响则主要与土壤胡敏酸（HA）和富里酸（FA）的变化有关。施用秸秆对土壤中FA增加幅度大于对HA的增加幅度,即HA/FA比值降低。而施用猪粪则增加了HA/FA比值。相关分析表明,施用秸秆和猪粪情况下土壤HA/FA与交换态Cd含量之间呈显著负相关关系（P＜0.05）。结果还表明,秸秆和猪粪对土壤交换态Cd含量的影响还与其对腐殖酸芳构化程度的影响有关,添加猪粪比添加秸秆的土壤腐殖酸芳构化程度大。因此,有机物质对土壤Cd有效性的影响与土壤有机质组成的变化密切相关。     

热辐射对水稻土有机质组成的影响

本文研究了受不同程度热辐射后的水稻土中有机质组分的变化情况,结果表明:随温度升高,土壤中水溶性有机碳(DOC)含量先增加后减少,200℃变化尤为显著,增加为CK的3.68 ～ 7.45倍,中性糖、糖醛酸与DOC的变化趋势一致.辐射温度不同,土壤中的胡敏酸、富里酸组成和含量亦发生不同程度的变化,300℃胡/富比值最大(1.79 ～ 5.04),土壤腐殖质聚合程度增加;200℃胡敏酸的E4/E6比值最大,反映此温度下土壤芳香缩合度低、具有较多的脂族结构物质、土壤腐殖化程度低.     

秸秆深还不同年限对黑土腐殖质组成和胡敏酸结构特征的影响

秸秆深还(Corn stover deep incorporation,CSDI)指将作物秸秆深埋于土壤亚表层20~40 cm深处,用以解决秸秆焚烧和土壤肥力退化的可持续利用模式。本文以吉林农业大学玉米连作耕地试验田未施用秸秆和秸秆深还不同年限的土壤为研究对象,设置CK、CSDI(2014)、CSDI(2013)和CSDI(2012)共4种处理,分别代表未施入秸秆、2014年秸秆深还(深还第1年)、2013年秸秆深还(深还第2年)、2012年秸秆深还(深还第3年),研究秸秆深还不同年限对黑土腐殖质组成和胡敏酸结构特征的影响。通过腐殖质组成修改法提取富里酸(Fulvic acid,FA)、胡敏酸(Humic acid,HA)和胡敏素(Humin,HM),国际腐殖质协会(International Humic Substances Society,IHSS)推荐的方法提取HA样品,通过元素组成、红外光谱和差热分析测定HA结构。结果表明:与CK相比,秸秆深还1年后显著提高了土壤和腐殖质各组分有机碳含量,亚表层累积效果更明显,其土壤有机碳(SOC)、HA、FA和HM有机碳含量分别增加了23.7%、30.5%、27.3%和46.1%,但PQ值(HA在可提取腐殖物质的比例)没有显著变化;HA氧化度和缩合度降低明显,表层和亚表层(O+S)/C比值分别降低14.31%和14.68%,H/C比值分别增加27.74%和28.86%,脂族链烃和芳香碳含量增加,热稳定性降低,HA结构趋于简单化。随着年限增加,深还3年后SOC、FA和HM有机碳含量呈下降趋势,HA有机碳含量呈上升趋势,PQ值变化显著,HA缩合度、氧化度呈上升趋势,脂族性减弱,芳香性增强,HA结构趋于复杂化。说明随着年限增加,秸秆不断矿化分解,秸秆深还对土壤腐殖质组成和结构特征的影响效果减弱。     

用δ13C法研究黑土有机碳组分的变化规律

通过室内短期培养实验，利用δ^13C的方法研究了小麦秸秆分解过程中黑土有机碳组分的变化规律。结果表明：有机物料本身含有相当数量的腐殖物质，这些物质的加入对土壤中有机碳的更新与活化有重要的作用。黑土中添加小麦秸秆后，土壤有机碳各组分的含量明显增加。随着培养时间的延长，土壤有机碳各组分的含量在不断变化，新形成的和原土中的HA与FA间发生转化，而且主要以FA向HA转化为主，原土的HA与FA间的转化速度比新形成的HA和FA的转化速度相对较慢。最初FA的形成速度大于HA的速度。随着培养时间的延长，由于部分FA向HA转化，加速了HA的形成，最终土壤HA与FA皆呈积累趋势，且HA的增加量显著大于FA。土壤中新形成的FA比原有的FA分解速度快。     

泥炭和褐煤对土壤有机碳和腐殖物质组成的影响

在相同温湿度环境条件下,研究泥炭和褐煤与土壤混合后对土壤有机碳及其腐殖物质组成变化的影响,为改善耕地土壤有机碳库的管理提供理论依据。结果表明:随着培养时间的延长,添加褐煤、木本泥炭的土壤有机碳含量分别上升了0.66%和17.41%,添加草本泥炭的土壤有机碳含量下降了3.15%;胡敏酸含碳量呈逐渐增加的趋势,富里酸含碳量呈逐渐减小的趋势;添加草本泥炭的胡敏素含碳量呈下降趋势,添加褐煤和木本泥炭的土壤胡敏素含碳量呈逐渐上升趋势。土壤胡富比和PQ值整体上都表现出随着培养时间的延长而逐渐增加的趋势。由此可知,泥炭和褐煤能提高土壤有机碳,改良土壤腐殖物质组分,且添加木本泥炭的土壤有机质含量和腐殖物质组分改善效果最好。     

有机酸处理条件对玉米秸秆热解特性的影响

酸洗预处理能有效改善K^+对生物质热解的影响,该文利用热重分析仪和裂解-气相色谱质谱联用仪进行了玉米秸秆的热解试验,研究了不同有机酸酸洗浓度(3%、5%和7%)、酸洗温度(25、50和75℃)和酸洗时间(1、2和3 h)对玉米秸秆热解特性的影响。结果表明:酸洗能显著降低玉米秸秆内在K^+的含量;经过不同条件的有机酸洗预处理后,玉米秸秆的TG/DTG(thermogravimetry/differential thermogravimetry)曲线均向高温段移动,最大热解速率随着酸洗浓度和酸洗温度的增加逐渐增大,随着酸洗时间的增加先增大后降低,在酸洗温度为75℃时,最大热解速率达到最大值15.49%/min;与此同时,玉米秸秆热解主要产物为酚类、酮类和呋喃类化合物,酸洗后,其酚类物质产率明显增加,在酸洗浓度为7%时达到最大值16.75%,而酮类和呋喃类化合物产率减少,分别在酸洗时间为1 h和酸洗浓度为7%时达到最小值0.10%和7.13%。酸洗后,焦炭产率减少,在酸洗浓度为3%时达到最小值18.79%。通过研究不同处理条件下有机酸对玉米秸秆热解特性的影响,为生物质预处理中酸溶液的选择提供了参考。     

Endogenous organic acid variations in different chickpea (Cicer arietinum L.) genotypes

Abstract

Changes in cropping systems during the past century have led to selective pressure on weed flora. Species and ecotypes with characteristics enabling them to survive in high-input farmland have increased in numbers, at the cost of plants lacking these characters. Since the 1950s, the perennial weed species Cirsium arvense (L.) Scop. and Sonchus arvensis L. have mainly been controlled by the herbicide group synthetic auxins like MCPA. During recent decades, C. arvense seems to have become less susceptible to MCPA in both Europe and North America but the reasons are unclear.

To study the importance of selective pressure on weed ecotypes, both short- and long-term studies were carried out in Uppsala, Sweden. The first consisted of two growth-characteristic greenhouse experiments. The hypothesis was that ecotypes of C. arvense and S. arvensis from high-input farmland were different and displayed a more competitive growth pattern than did ecotypes from low-input farmland.

The second study was a field experiment with four ecotypes of C. arvense from low-input farmland to study if selective pressure was in force, over a period of six years. The four ecotypes had different growth characteristics and herbicide sensitivity and they were exposed to crop competition and MCPA treatments during the experimental period. The hypothesis was that ecotypes with a more competitive growth pattern and MCPA tolerance would survive to a greater extent than would other ecotypes. For C. arvense, the results from the growth-characteristic experiment showed that the growth pattern of ecotypes from high-input farmland differed, showing a more directly elongated growth pattern with fewer spines on the leaves compared with ecotypes from low-input farmland, which usually were of rosette-type. Results from the field experiment with C. arvense showed that after six years MCPA-sensitive and/or rosette-type ecotypes had almost disappeared while ecotypes with a more directly elongated growth pattern and less sensitive to MCPA survived to a much greater extent. The conclusion was therefore that when exposed to selective pressure like crop competition and herbicide treatments, ecotypes of C. arvense with a more directly elongated growth pattern and less sensitive to herbicide treatment survived to a greater extent compared with ecotypes missing these traits. Ecotypes from high-input farmland had generally fewer leaf spines than did ecotypes from low-input farmland. This may suggest a trade-off between spine formation and rapid competitive growth. In the growth-characteristic experiment with S. arvensis, no differences between ecotypes from high- and low-input farmland regarding growth characteristics or leaf spines could be detected. This might partly be due to a lower exposure of S. arvensis to selective pressure compared with C. arvense, since S. arvensis generally is less sensitive to MCPA.     

Interactive effects of organic acids in the rhizosphere

Organic acids released into the rhizosphere may perform many beneficial functions to the plant including metal detoxification and enhancement of nutrient acquisition. Typically, these organic acids are studied in isolation; however, roots simultaneously exude a cocktail of organic acids and other substances, and their combined impact on rhizosphere processes may be quite different. It has been hypothesized that some exudates may play secondary roles (e.g. inhibitors of microbial activity, blockage of sorption sites), which might enhance the longevity and nutrient-mobilization capacity of others. Here we investigated how the decomposition, sorption and P-solubilizing effects of citrate, malate and oxalate are affected by the presence of malonate and shikimate. We found that in a range of agricultural soils the decomposition of citrate, malate and oxalate was rapid, but not influenced by the presence of large quantities of shikimate or malonate. This suggests that the individual organic acids are taken up by different transport mechanisms or components of the microbial community. At large concentrations, malonate decreased sorption of citrate, malate and oxalate on the soil, whilst shikimate had little effect. The capacity of citrate, malate and oxalate to desorb P was significantly greater in cocktails containing malonate compared with the single organic acid; no effect was seen with shikimate. We conclude that neither malonate nor shikimate at realistic concentrations will significantly affect the biodegradation of citrate, malate or oxalate in the rhizosphere, and while malonate did enhance P desorption, this effect is additive rather than synergistic. Overall, we found little evidence that malonate and shikimate act as secondary regulators of citrate, malate and oxalate behavior in soil.     

Effect of humic acid and fulvic acid based liquid and foliar fertilizers on the yield of wheat crop

Abstract

An organic-mineral liquid fertigation fertilizer containing humic acid, nitrogen (N)–phosphorus (P)–potassium (K), zinc (Zn), sulfur (S), manganese (Mn) and a liquid foliar fertilizer consisting of fulvic acid and gibberellic acids were formulated and applied to wheat. The purpose of this study was to develop an efficient and cost effective liquid and foliar fertilizer and compare their potential with commercially available urea and DAP. The fulvic acid and humic acids were obtained by alkaline extraction of lignite coal. All the treatments were significant over the control. The application of the liquid fertigation fertilizer and liquid foliar fertilizer along with 50?kg of urea per acre showed the best results biological yield (grain plus straw yield). It was found that the highest yield was obtained in T₆ treatment and the second best results were obtained with T₂ treatment, but has a high cost, while treatment T₆ was the most significant economical and yielded a high income when compared to other treatments.     

Organic Acids and Diffusive Flux of Organic and Inorganic Phosphorus in Sandy-Loam and Clayey Latosols

This study evaluated the effects of organic acids on the diffusive flux of phosphorus (DFP) along time. Treatments were a factorial 2?×?2?×?2?×?2?×?5 design: two soils (clayey Red Latosol and a sandy-loam Red-Yellow Latosol), two organic acids (citric acid, CA, and humic acid, HA), and two phosphorus (P) sources [monopotassium phosphate (KH₂PO₄) and inositol hexaphosphate (IHP)] either with or without heating (100 °C) of the soil. The soil plus treatments, in all combinations, were placed in contact with an anion exchange resin and the P in the resin was measured after 2, 4, 6, 10, and 15 days. The DFP was greater when the soils were treated with CA than when treated with HA. Citric acid was more effective in increasing the DFP from KH₂PO₄, whereas HA was the organic ligand that promoted a larger DFP when the source was IHP.     

Low pH and aluminum tolerance of Bradyrhizobium strains isolated from acid soils in Indonesia

Sixty-seven strains of Bradyrhizobium isolated from soybean plants growing on acid soils in West Java and Sumatra, Indonesia, were examined for the effect of the pH and aluminum concentration on their growth in nutrient media, compared with 61 strains of Bradyrhizobium from soils in Japan. The results in this study indicated that the indigenous population of Bradyrhizobium in the soils of Indonesia showed a large difference in acid- and Al-tolerance from that of Japan. Eighty-five and 48% of the isolates from Japanese soils and Indonesian soils, respectively, were unable to grow in YEM broth at pH below 4.5. The acid-tolerance was correlated with AI-tolerance of the isolates on YEM agar plates at pH 4.4. Seventy-five percent of the isolates that grew in YEM broth at pH 4.5 were also resistant to 400 µM Al on the YEM plates. Acetylene reduction assay of the root nodules revealed that 3 of the acid- and Al-tolerant isolates from Indonesian soils showed a significantly high nitrogen fixation activity.     

粘土矿物对土壤腐殖质化学性质的影响

Chemical characteristics of humic substances in soils with different mineralogical characteristics and under different utilization paterns in Zhangpu,Fujian Province,together with two pairs of cultivated soils in North China Plain were studied by chemical analysis,visible and IR spectroscopy and ^13C NMR spectrometry.For soils in Zhanpu the HA/FA ratio and both the aromaticity and the degree of humification of HA were higher in soils with montmorillonite as the predominant clay mineral than in those with kaolinite as the predominant clay mineral,provided these soils were under the same utilization pattern.While for each pair of soils with similar mineralogical characteristics the HA/FA ratio was higher and the C/H ratio and the contnet of carboxyl group of HA were lower in paddy soil than in upland soil.Among the upland soils(or paddy soils)studied the Ha/FA ratio of soil in Zhangpu with kaolinite as the predominant clay mineral was the lowest,and that of soil in Zhangpu with montmorillonite as the predominant clay mineral was the highest .the lowest.and that of soil in Zhangpu with montmorillonite as the predominant clay mineral was the highest It was concluded that the presence of montmorillonite favored the fromation and maturation of humic acid.     

Chemical Composition of Ten Blackcurrant (Ribes nigrum L.) Cultivars

Abstract

Ten blackcurrant cultivars were evaluated for some quality components. On average, the sugar content was 9.0%, of which fructose made up 45%, glucose 40% and sucrose 15%. Soluble solids were 15.4% as an average for the ten cultivars in three years. The acid content was 5.1% of fresh weight, 88% was citric acid and 12% malic acid. The ascorbic acid content varied from 67 mg per 100 g fresh fruit in Hedda, to 204 mg per 100 g in Blackdown. Except for Hedda and Øjebyn, which both had low values of ascorbic acid and colour properties, the quality components of the cultivars were found to be within an acceptable range.     

不同来源腐殖酸的组成和性质的研究

本研究从三种有机物料草炭、褐煤、风化煤中提取腐殖酸,对其组成和性质进行了测定,同时对胡敏酸进行酒精沉淀分级。研究结果表明:褐煤胡敏酸氧化度和芳香度最高,其次为风化煤胡敏酸,最后是草炭胡敏酸;风化煤富里酸的氧化度和芳香度最高,其次为褐煤富里酸和草炭富里酸。胡敏酸各级分的回收率均随着级分数的升高而增加。回收率以风化煤胡敏酸最高,依次为褐煤胡敏酸、草炭胡敏酸。     

Plant defence inducers rapidly influence the diversity of bacterial communities in a potting mix

Plant hormones and their functional analogues are used in agriculture to combat plant diseases and pests. These chemicals are generally targeted at shoots, but soils inevitably receive a dose during application. In this study, we used 16S rRNA gene amplicon pyrosequencing to determine whether the diversity of bacterial communities in a potting mix (referred here as ‘model soil’) is influenced by exposure to salicylic acid (SA), methyl jasmonate (MeJA), ethylene (ET) and abscisic acid (ABA). The number of operational taxonomic units (OTUs; richness) and Simpson's Diversity Index values (evenness) associated with each sample was not influenced by the hormone treatments, but changes in community composition were observed. Relative to the control, all hormones more than doubled the abundance of a Limnobacter population, ABA led to a four-fold increase in a Cellvibrio population, ET led to a c. 70% decrease in an Algoriphagus population, and MeJA and ABA applications halved the abundance of a Massilia population. These changes may influence plant productivity.