标记停留时间对水稻及其生物质炭的13C和15N丰度的影响

稳定同位素技术是研究土壤元素循环的重要技术手段。本实验研究了同位素标记后的停留时间对水稻地上和地下部分及利用其制备的生物质炭的13C丰度（δ13C）和15N丰度（δ15N）的影响，为深入研究生物质炭对土壤碳、氮过程的影响提供基础。研究以水稻为材料，利用15N-尿素叶面喷施和13C-CO2脉冲标记的方法对水稻进行了15N和13C双标记，15N标记结束后设置4 h、6 h和24 h三个停留时间，将标记后的水稻分为地上和地下部分，分别在300 °C和500 °C下制备成生物质炭，利用同位素质谱仪测定水稻及其生物质炭的δ13C和δ15N。结果表明，随着停留时间的延长，水稻地上部分的δ13C由872‰逐渐降低至578‰，而地下部分的δ13C由226‰逐渐升高至869‰。与δ13C不同，水稻地上部分δ15N呈现先增加后降低的趋势，停留时间6 h时δ15N最大（1764‰），而地下部分的δ15N呈现先降低后增加的趋势。整体而言，与水稻原料相比，生物质炭的δ13C和δ15N分别降低了52.1%和15.9%。而且，生物质炭的δ13C和δ15N均在停留时间为24 h时最高，300 °C生物质炭表现的更加明显。随着停留时间的延长，300 °C生物质炭的热水可提取有机碳的δ13C比残留固体的δ13C降低的比例由4.14%提高到11.0%，而对于500 °C生物质炭则由32.3%降低到18.9%，表明延长停留时间分别降低和提高了300 °C和500 °C生物质炭的13C均匀性。综上所述，本研究发现标记后的停留时间对水稻δ13C和δ15N的影响不同，并且这种影响没有延续至生物质炭，停留时间和制备温度共同影响水稻生物质炭的13C均匀性。     

Microbial activity and hydrolase activities during decomposition of root exudates released by an artificial root surface in Cd-contaminated soils

The aim of this study was to assess the stimulatory effects of different low molecular weight organic compounds commonly present in root exudates on microbial activity and hydrolase activities, and the effects of high Cd concentrations in sandy soils collected from contaminated field plots on the stimulatory effects. Glucose, glutamic acid, citric acid, oxalic acid, or a mixture of all compounds were released by an artificial root surface in a simplified rhizosphere system. The effects were measured at <2 mm (rhizosphere soil layer) and >4 mm (bulk soil layer) distance from the root surface, 7 d after the root exudates release. Results showed that different root exudates were mineralized at different extent and had different stimulatory effects on microbial growth estimated by dsDNA content of soil, and on hydrolase activities, mostly localized in the rhizosphere soil layer. Mineralization of root exudates, microbial growth and stimulation of most of the measured hydrolase activities were drastically reduced by high Cd concentrations in soil.     

化感水稻苗期不同器官水浸提液及根系分泌物对稗草的化感作用

在自然种植条件下研究了强化感水稻品种“P1312777”不同叶期(3～6叶)、不同器官(根、茎、叶)水浸提液对稗草根长的抑制率,比较了不同极性树脂处理后水稻根系分泌物水溶液的抑制率变化。结果表明:在3～6叶期相同水稻器官比较,均以5叶期浸提液抑制率最高;5叶期水稻不同器官比较,以叶的浸提液抑制率最高;土培至6叶期的水稻根系分泌物水溶液的抑制率为47．06％,经极性树脂ADS-21处理后抑制率增强为64．71％,经非极性树脂ADS-5处理后抑制率减弱为26．47％;水培至6叶期的水稻根系分泌物水溶液的抑制率为38．24％,经ADS- 21处理后抑制率增强为58．82％,经ADS-5处理后抑制率减弱为20．59％。因此水稻“P1312777”根系分泌物中化感物质以非(弱)极性物质为主,极性物质减弱了非(弱)极性物质的化感抑草作用。     

根部增氧模式对水稻产量与氮素利用的影响

【目的】根部缺氧是影响水稻生长发育与养分吸收的主要非生物因子之一。为了明确不同增氧模式的作用效果,探明水稻产量和氮素利用效率对根部增氧的响应特征,本试验研究了不同根部增氧模式下水稻生长动态、产量和氮素吸收积累与转运特性。【方法】以深水水稻品种IR45765-3B和水稻品种中浙优1号为材料,试验在顶部用透明塑料膜遮雨的水泥栽培池中进行,试验设施用CaO₂（CaO₂）、微纳气泡水增氧灌溉（MBWI）和干湿交替灌溉（AWD）等三个增氧模式处理及淹水对照（WL）。分别测定了两品种的生长动态、产量和与氮素利用相关的指标。【结果】与淹水对照相比较,根部增氧处理均显著促进IR45765-3B分蘖的发生,增幅为10.7%~33.6%,而中浙优1号茎蘖数仅在CaO₂处理和AWD处理部分调查时期显著高于对照;根部增氧处理显著提高了两品种的干物质积累量,并显著提高两品种水稻产量,增氧处理下IR45765-3B产量较对照分别增加26.3%（CaO₂）、21.8%（MBWI）和10.7%（AWD）,而中浙优1号产量较对照分别增加51.0%（CaO₂）、52.2%（MBWI）和29.68%（AWD）;根部增氧显著增加水稻的氮素吸收与利用,与对照相比较,增氧处理下IR45765-3B和中浙优1号氮肥偏生产力均显著升高;施用CaO₂和MBWI处理水稻氮素转运效率和氮素转运贡献降低,但齐穗期后两品种的氮素吸收量显著增加,齐穗期后IR45765-3B和中浙优1号在CaO₂处理下的氮素吸收量较对照分别增加了73.4%和119.2%,MBWI处理下的氮素吸收量较对照分别增加了128.7%和106.5%。【结论】根部增氧显著促进水稻分蘖发生与成穗,增加水稻干物质积累并显著提高产量;在氮素利用方面,增氧处理下水稻植株对氮素的吸收与积累显著增加,且增氧处理显著促进了水稻对氮素的利用效率;三种增氧模式中CaO₂和MBWI的效果较AWD更明显。     

Gas chromatography–mass spectrometry associated global analysis of rice root exudates under aseptical conditions

Components of rice root exudates were surveyed by gas chromatography–mass spectrometry (GC-MS) and the effect of phosphate (P) starvation was investigated. Rice seedlings were aseptically grown in controlled environments under P-supplied (+P) or P-deficient (–P) conditions. Root exudates were collected from the culture solution 4 and 8 days after treatment (D4 and D8, respectively), which contain the first and second 4-day intervals. The collected solution was lyophilized and then eluted with methanol. In the present study, primary metabolites, such as sugars, amino acids, organic acids and fatty acids, were mainly targeted. After derivatization with methoxyamine hydrochloride and N-methyl-N-trifluoroacetamide, the samples were analyzed by GC-MS. Sugars and various amino acids (such as aspartic acid and l -isoleucine) were mainly detected and the components changed with the growth stage rather than the P content in the culture solution. The relative amount of sugars (such as glucose and fructose) and amino acids (such as aspartic acid and l -isoleucine) decreased in the D8 samples. Of the 78 detected compounds, orthogonal partial least-squares discrimination analysis (O-PLS-DA) showed that four compounds were related to the P content of the nutrient solution and 58 were related to the sampling date (days after treatment). The results suggest that the physiological change during seedling development was unexpectedly large and that the response to the environment was rather small.     

土壤透水状况对水稻根系生长与氮素利用的影响

以"II优7954"为材料,盘栽比较了不同透水性土壤(常规淹水无渗漏、渗漏10mm/d、20mm/d、40mm/d和无水层无渗漏)对水稻根系生长与N素利用的影响,结果表明:水稻植株根系生长与土壤透水性关系较大,适当的土壤水分渗透能促进根系生长,提高N素利用。土壤透水量10mm/d有利于水稻早期根系生长,提高根总量和深层根比例,开花期白根比高,N肥吸收利用率达77.05%,远高于常规淹水无渗漏对照,对水稻产量也有促进作用。土壤透水量超过20mm/d时不利于产量提高及后期水稻根系和植株地上部的生长。适当土壤透水能提高籽粒千粒重,但渗漏率超过20mm/d则千粒重有下降趋势。     

Pedogenic carbonate recrystallization assessed by isotopic labeling: a comparison of 13C and 14C tracers

The C isotopic composition (δ¹³C) of pedogenic carbonates reflects the photosynthetic pathway of the predominant local vegetation because pedogenic (secondary) CaCO₃ is formed in isotopic equilibrium with soil CO₂ released by root and rhizomicrobial respiration. Numerous studies show the importance of pedogenic carbonates as a tool for reconstructing paleoecological conditions in arid and semiarid regions. The methodological resolution of these studies strongly depends on the time scale of pedogenic carbonate formation, which remains unknown. The initial formation rate can be assessed by ¹⁴C labeling of plants grown on loess and subsequent incorporation of ¹⁴C from rhizosphere CO₂ into newly formed carbonate by recrystallization of loess CaCO₃. We tested the feasibility of ¹⁴C and ¹³C tracers for estimating CaCO₃ recrystallization rates by simultaneous ¹⁴C and ¹³C labeling and comparison with literature data. ¹⁴C labeling was more efficient and precise in assessing recrystallization rates than ¹³C labeling. This is connected with higher sensitivity of ¹⁴C liquid scintillation counting when compared with δ¹³C measurement by IRMS. Further, assessment of very low amounts of incorporated tracer is more precise with low background signal (natural abundance), which is true for ¹⁴C, but is rather high for ¹³C. Together, we obtained better reproducibility, higher methodological precision, and better plausibility of recrystallization rates calculated based on ¹⁴C labeling. Periods for complete CaCO₃ recrystallization, extrapolated from rates based on ¹⁴C labeling, ranged from 130 (125–140) to 240 (225–255) y, while it was ≈ 600 (365–1600) y based on the ¹³C approach. In terms of magnitude, data from late‐Holocene soil profiles of known age provide better fit with modeled recrystallization periods based on the ¹⁴C approach.     

水稻氮高效基因型根系分泌物中有机酸和氨基酸的变化特征

采用溶液培养试验,研究水稻氮高效基因型在不同供氮水平下,根系分泌物中有机酸和氨基酸种类及含量的变化情况,并探讨其与氮素利用效率之间的关系。结果表明: 1）水稻氮高效基因型氮积累量随着供氮水平的降低明显下降,而氮素利用效率显著提高; 在供氮水平为20 mg/L时,高效基因型具有较高的氮积累量,且氮素利用效率较低效基因型高42.9%（分蘖期）和21.4%（拔节期）。 2）草酸为高效基因型根系分泌的主要有机酸种类,其分泌量占有机酸总量的80%以上,其次是乙酸和柠檬酸; 有机酸分泌总量和草酸分泌量在分蘖期和拔节期随供氮水平的降低而降低,乙酸和柠檬酸分泌量在拔节期也呈相同趋势; 相同供氮水平下,高效基因型有机酸分泌总量均显著低于低效基因型,且在20 mg/L时差异明显。 3）丙氨酸为高效基因型根系分泌的主要氨基酸种类,其分泌量占氨基酸总量的50%以上,其次是丝氨酸、 谷氨酸、 天冬氨酸、 苯丙氨酸、 甘氨酸和苏氨酸,且氨基酸分泌总量和各组分氨基酸分泌量均随供氮水平的降低而降低; 在低氮水平（10 mg/L和20 mg/L）下,高效基因型氨基酸分泌总量均显著低于低效基因型。4）在分蘖期和拔节期,水稻根系分泌有机酸和氨基酸总量与氮素利用效率均呈显著或极显著负相关,有机酸分泌组分中的草酸和氨基酸分泌组分的天冬氨酸分泌量与氮素利用效率也呈显著或极显著负相关。以上结果表明,低氮条件下水稻氮高效基因型氮效率优势明显,高效基因型氮素利用效率高,有利于体内同化物质的合理分配。     

Effect of root mucilage and modelled root exudates on soil structure

Plant roots release in the rhizosphere diverse organic materials which may have different effects on soil structure. We have evaluated the effect of natural and modelled root‐released materials on soil aggregates and the biodegradation of carbon from roots in the soil. The effects of root mucilage from maize and of a modelled soluble exudate were compared with those of simple compounds (glucose, polygalacturonic acid). For all treatments, soil was amended with 2 g C kg^?1 soil and incubated for 30 days at 25°C. The biodegradation of mucilage was similar to that of polygalacturonic acid, and slower than the decomposition of modelled exudates and glucose. Addition of all substrates increased the stability of aggregates, but the duration of this effect depended on the chemical nature of the material. Compared with the control, the proportion of stable aggregates after 30 days of incubation was multiplied by 3.8 for root mucilage, by 4.2 for modelled soluble exudates, by 2.5 for polygalacturonic acid and by 2.0 for glucose. The different fractions of root exudates in the rhizosphere evidently affected the aggregate stability.     

Microbial communities responsible for the decomposition of rice straw compost in a Japanese rice paddy field determined by phospholipid fatty acid (PLFA) analysis

To identify the microbial communities responsible for the decomposition of rice straw compost in soil during the rice cultivation period, phospholipid fatty acid (PLFA) composition of rice straw compost was determined by periodically sampling the compost from a Japanese rice field under flooded conditions. About 21% of the compost was decomposed within a period of 3 months. The total amount of PLFAs, as an indicator of microbial biomass, was significantly lower under drained conditions than under flooded conditions and was relatively constant during the flooding period. This indicates that the microbial biomass in the compost samples did not increase during the gradual decomposition of rice straw compost under flooded conditions. The proportion of branched-chain PLFAs (biomarker of Grampositive and anaerobic Gram-negative bacteria) slightly decreased during the early period after placement, and increased gradually afterwards. Among the branched-chain PLFAs, i15:0, ail5:0, i16:0 and i17:0 PLFAs predominated and their proportions increased gradually except for i16:0. The proportion of straight mono-unsaturated PLFAs (biomarker of Gramnegative bacteria) was almost constant throughout the period, and 18:1ω9 and 18:1ω7 PLFAs predominated. The proportion of straight poly-unsaturated PLFAs as a biomarker of eukaryotes including fungi was also constant throughout the period, except for a decrease under drained conditions. Straight poly-unsaturated PLFAs consisted mainly of 18:2ω6c PLFA. Therefore, these results suggest that the proportions of Gram-positive and anaerobic Gram-negative bacteria increased during the decomposition of rice straw compost in flooded paddy field. Statistical analyses enabled to divide PLFA patterns of microbiota in the rice straw compost into two groups, one group consisting of rice straw compost samples collected before mid-season drainage and the other of samples collected after mid-season drainage. Small squared distances among samples in cluster analysis indicated that the community structure of microbiota was similar to each other as a whole. These results suggest that the microbial communities changed gradually during the period of placement, and that mid-season drainage may have affected the community structure of microbiota. Principal component analysis of the PLFA composition suggested that the succession of microbiota along with the decomposition in flooded soil was similar between rice straw compost and rice straw and that the changes in the community structure during the decomposition in flooded soil were more conspicuous for rice straw than for rice straw compost.     

放牧与围栏内蒙古针茅草原土壤微生物生物量碳、氮变化及微生物群落结构PLFA分析

以内蒙古贝加尔针茅草原、大针茅草原和克氏针茅草原为研究对象,采用氯仿熏蒸法和磷脂脂肪酸（PLFA）分析方法研究了放牧与围栏条件下内蒙古针茅草原土壤微生物生物量和群落结构特征的变化情况。研究表明放牧与围栏草地土壤微生物生物量和群落结构差异显著。氯仿熏蒸法分析结果表明内蒙古针茅草原土壤微生物生物量碳的含量介于166.6-703.5mg·kg^-1之间,微生物生物量氮含量介于30.34-92.15mg·kg^-1之间,其中贝加尔针茅草原土壤微生物生物量碳、氮最高,大针茅草原次之,克氏针茅草原则最低。放牧条件下,贝加尔针茅草原、大针茅草原土壤微生物生物量碳、氮显著低于围栏草地,克氏针茅草原则无显著变化。PLFA分析结果显示,内蒙古针茅草原土壤微生物群落PLFAs种类、含量丰富,共检测出28种PLFA生物标记磷脂脂肪酸,并且以直链饱和脂肪酸和支链饱和脂肪酸为主,相对含量占总量的2/3左右,其中贝加尔针茅草原土壤微生物含量最丰富,其围栏样地土壤的PLFA含量达到27.3nmol·g-1,大针茅草原和克氏针茅草原依次降低。围栏条件下,各类型草原土壤细菌脂肪酸与总PLFA含量均显著高于放牧草地,真菌脂肪酸含量则因草原类型不同各有差异;放牧导致各类型草原革兰氏阳性细菌PLFAs/革兰氏阴性细菌PLFAs（GPPLFAs/GNPLFAs）比值显著降低,而除了克氏针茅草原,细菌PLFAs/真菌PLFAs比值则显著升高。PLFAs主成分分析表明,放牧和围栏处理对内蒙古针茅草原土壤微生物群落结构产生影响,且围栏处理的影响程度大于放牧处理。经相关分析表明,氯仿熏蒸法和PLFA分析方法之间有很好的一致性,且土壤微生物PLFAs与土壤有机质、全磷、硝态氮显著相关。     

Effects of C and N availability and soil-water potential interactions on N2O evolution and PLFA composition

Mitigation of agricultural N₂O emissions via management requires quantitative information about the regulation of the underlying processes. In this laboratory study, short-term evolution of N₂O from repacked soil was determined using an arable sandy loam soil adjusted to three water potentials (−15, −30 or −100 hPa) that were reached by adjustment of partly air-dried soil with nutrient solutions or water; a water retention curve of repacked soil had been determined prior to the incubation experiment. The amendments included a control treatment receiving water (CTL), and aqueous solutions of carbon in the form of glucose (C), ammonium sulfate (N), or both (CN). Rates of CO₂ and N₂O evolution were followed during 14 days. Soil inorganic N and phospholipid fatty acid (PLFA) composition were analyzed by the end of incubation. Across all nutrient treatments, the soil at the lower moisture content (−100 hPa) showed little or no N₂O evolution irrespective of nutrient treatment. Adding glucose alone reduced N₂O evolution relative to CTL. The addition of N alone had no effect on soil respiration, but significantly increased nitrate accumulation and N₂O evolution. The CN treatment resulted in higher respiration than with C amendment alone, but less N₂O evolution than with N alone, at least at −15 and −30 hPa. Whole-soil PLFA fingerprints at the end of incubation reflected the complex response of gaseous emissions. At −15 hPa growth of Gram negative bacteria, probably including denitrifiers, in the CN treatment was indicated by low cyclopropane-to-precursor ratios. At −100 hPa differentiation of branched-chain fatty acids was taken as evidence for an effect of C amendment on Gram positive bacteria. The highest potential for N₂O evolution was observed at the intermediate soil wetness level; the corresponding gas diffusivities indicated that this parameter may be a better predictor of N₂O emissions than water-filled pore space.     

Metabolic profiling of root exudates of Arabidopsis thaliana

In addition to accumulating biologically active chemicals, plant roots continuously produce and secrete compounds into their immediate rhizosphere. However, the mechanisms that drive and regulate root secretion of secondary metabolites are not fully understood. To enlighten two neglected areas of root biology, root secretion and secondary metabolism, an in vitro system implementing root-specific elicitation over a 48-day time course was developed. After roots of Arabidopsis thaliana had been elicited with salicylic acid, jasmonic acid, chitosan, and two fungal cell wall elicitors, the secondary metabolites subsequently secreted were profiled. High-performance liquid chromatography was used to metabolically profile compounds in the root exudates, and 289 possible secondary metabolites were quantified. The chemical structures of 10 compounds were further characterized by (1)H and (13)C NMR: butanoic acid, trans-cinnamic acid, o-coumaric acid, p-coumaric acid, ferulic acid, p-hydroxybenzamide, methyl p-hydroxybenzoate, 3-indolepropanoic acid, syringic acid, and vanillic acid. Several of these compounds exhibited a wide range of antimicrobial activity against both soil-borne bacteria and fungi at the concentration detected in the root exudates.     

Variation of wheat root exudates under aluminum stress

The wheat (Triticum aestivum L.) cultivar Yangzhou 158 was used as a reference. The wheat root exudates were collected using a hydroponic mode. The changes of the electrolytes, H+, sugar, organic acids, amino acids, and secondary metabolites in wheat root exudates induced by aluminum (Al) were studied. The research results show that Al stress affects wheat root exudation. The secreted electrolytes and sugar increase with the increasing of the external Al3+ concentration. The total amount of secreted amino acids has a specific correlation with the external Al3+ concentration. At first, the amino acids secrete normally, but when Al3+ concentration is over 10 mg.L-1, the amino acid constitution varies obviously. Under Al stress, some original secondary metabolites disappear gradually, and other new secondary metabolites release simultaneously. Increasing the external Al3+ concentration gradually stimulates the exudation of organic acids. The organic acid levels in the wheat root zone increase in response to Al treatments. Active Al ions are accumulated in wheat roots. This Al-dependent variation in wheat root exudates suggests a specific Al-induced response of the wheat.     

根系分泌物在西瓜/旱作水稻间作减轻西瓜枯萎病中的响应

采用盆栽的方法,研究了西瓜/旱作水稻间作对西瓜枯萎病和西瓜根系分泌物中酚酸、氨基酸、有机酸种类和含量的影响。结果表明:与对照相比,接种西瓜专化型尖孢镰刀菌(Fusarium oxysporun f.sp.niveum,FON)显著提高了西瓜根系分泌物中酚酸的含量,增加了酚酸的种类如香豆酸,当西瓜/旱作水稻间作时,大部分酚酸的分泌量降低。在接种FON的条件下,西瓜/旱作水稻间作较单作显著降低西瓜根系分泌物中酚酸含量。与对照相比,接种FON提高了西瓜根系分泌中氨基酸的含量,而在西瓜/旱作水稻间作条件下接种FON时,西瓜根分泌物中氨基酸含量没有变化。与对照相比,接种FON显著提高了西瓜根系分泌有机酸的量,当西瓜/旱作水稻间作时,大部分有机酸分泌量降低。在接种FON的条件下,西瓜/旱作水稻间作较单作降低了西瓜根系分泌物中有机酸含量。总之,接种FON提高了西瓜根系分泌酚酸、氨基酸和有机酸的量,西瓜/旱作水稻间作降低西瓜枯萎病发病率和发病指数,并维持西瓜根系分泌酚酸、氨基酸和有机酸的量不增加,因此,西瓜/旱作水稻间作减轻西瓜枯萎病与西瓜根分泌物的调节有关。     

Soluble root exudates of maize: Influence of potassium supply and rhizosphere microorganisms

Maize was grown for 36 days in solution culture with roots either under axenic conditions or in the presence of rhizosphere organisms. In other experiments with sterile roots the plants were grown with different concentrations of potassium. At the end of the experiments sugars, organic acids and amino acids in the nutrient solutions were determined. Under axenic conditions the exudates consisted of up to 65% sugars, up to 33% organic acids and only up to 2% amino acids. The same substances were detected in non-sterile nutrient solutions. In the presence of microorganisms fructose, arabinose and the predominating glucose decreased to almost one half, while sucrose was not affected. The amounts of organic acids were not changed by microbial growth. The main amino acid, glutamic acid, was nearly doubled by the presence of microorganisms, whereas other amino acids remained unchanged. The lower O₂ content of the nutrient solutions of non-sterile roots suggested microbial decomposition of monosaccharides. In another experiment with roots grown under axenic conditions and with different K treatments low K supply significantly increased the total amounts of sugars, organic acids and amino acids exuded g^?1 root dry matter. As in the previous experiment glucose, fumaric and oxalacetic acid as well as glutamic and aspartic acid dominated in the respective fractions. Again sugars and organic acids represented the major quantity of exudates, while amino acids amounted to less than 2%. In an additional experiment with another cultivar, with nitrate as N source and a 5-day longer growth period, somewhat different results were obtained. In the exudates sugars were found in lower amounts, probably due to a higher growth rate. Under these conditions organic acids were the prevailing root exudates. Unlike sugars and amino acids, their total quantity was not affected by K nutrition, but the proportion of malic acid increased with increasing K supply, while oxalacetic acid dominated at low K nutrition. Similarly the total amount of organic acids within the root was independent of K nutrition. However malic acid content increased with increasing K application, while the likewise dominating citric and oxalacetic acid decreased.     

草莓根系分泌物障碍效应的模拟研究

草莓是一种营养丰富、经济价值较高的水果,但连作障碍使草莓生长发育不良,产量与品质下降,而造成连作障碍的因素种类繁多,极其复杂。本文以“全明星”生根试管苗为材料,应用组织培养技术分析了根系分泌物对草莓生长的影响。结果表明,根系分泌物显著抑制了植株的生长,降低了根系活力、叶片SOD活性和叶绿素含量,而叶片中的MDA含量和细胞质膜相对透性增加,导致草莓抗病性下降。根系分泌物对草莓的不利影响随浓度的增加而增大,表明草莓根系分泌物可能是造成草莓连作障碍的一个重要原因。     

Effects of root exudates and humic substances on weathering kinetics

The effect of complex natural organic ligands on the weathering kinetics of aluminum oxide was investigated in laboratory experiments. A peat-derived humic substance and root exudates obtained from ectomycorrhizal (Picea abies — Hebeloma crustuliniforme) and non-mycorrhizal Norway Spruce trees; and γ-Al₂O₃ were used as a model system. The experimental weathering rates are in accordance with a surface-controlled dissolution mechanism. The effect of the humic material on dissolution rates appears to depend on the degree of protonation of the humic (macro)molecules: we observed dissolution-enhancement or -inhibition at pH 3 and 4, respectively. Ectomycorrhizal exudates proved to be effective weathering agents at pH 4, as opposed to humic material and non-mycorrhizal exudates. Our results suggest that (i) the role of humic materials in mineral weathering and podzolization is different from what is commonly thought, and (ii) mineral weathering rates in the rhizosphere may be higher than in the bulk soil.