南京典型利用方式土壤中球囊霉素含量及剖面分布特征

采用Brad-ford染色法研究了南京市5种典型利用方式土壤不同土层中(0~10、10~20、20~40 cm)球囊霉素的含量。结果表明:土壤中总球囊霉素含量为1.96~3.12 mg/g,占土壤有机碳的12.5%~29.0%,所占比例随土壤有机碳含量的增加而降低。林地和草地土壤中球囊霉素和有机碳的含量均高于3种耕作土壤(水稻田、茶园土和菜园土)。随着土层深度(0~40 cm)的增加,5种不同利用方式土壤中总球囊霉素和有机碳的含量均减小;与其他土层相比,0~10 cm土层总球囊霉素和有机碳含量均最大。耕作土壤中易提取球囊霉素更易于向总球囊霉素转化。发现5种土地利用方式下土壤中总球囊霉素含量与土壤有机碳含量极显著正相关,与土壤p H显著负相关;易提取球囊霉素与土壤有机碳含量极显著负相关。总球囊霉素和易提取球囊霉素可作为评价土壤丛枝菌根真菌活性和土壤质量的重要指标。     

不同施肥处理对球囊霉素土壤蛋白含量的影响

球囊霉素是丛枝菌根真菌分泌的一种疏水性蛋白,通过研究不同施肥处理对棕壤中Bradford反应性球囊霉素土壤蛋白(GRSP)含量的影响以及GRSP与土壤有机碳之间的关系表明:不同施肥处理显著影响土壤中GRSP的含量,无机肥、有机肥以及有机-无机肥配施均显著增加农田土壤总GRSP(T-GRSP)和易提取GRSP(EE-GRSP)的含量,以有机-无机肥配施效果最好。与CK和单施NPK处理比较,有机肥施用提高土壤T-GRSP在土壤有机质(SOM)中的比例,表明有机肥促进GRSP在土壤有机质中的累积,提高GRSP对土壤有机质的贡献。同时,不同施肥处理GRSP含量与土壤有机碳(SOC)含量呈极显著相关关系。     

球囊霉素在土壤团聚体中的分布特征及影响因素的Meta分析

为充分认识球囊霉素在维持土壤有机碳平衡和土壤团聚体稳定性中的重要作用,建立改善土壤结构 和提升土壤质量的管理策略,通过收集整理近些年来已发表的19篇文献中的332组数据,定量分析球囊霉素在不同粒径土壤团聚体中的分布特征,系统解析其影响因素,并比较了不同土地利用方式下球囊霉素在土壤团聚体中的分配差异。结果表明：无论是总球囊霉素还是易提取球囊霉素,在大团聚体（>2 000 μm）和小团聚体（2 000~250 μm）中的质量百分比（分别约占30%）均显著高于微团聚体（250~53 μm）和黏粉粒级微团聚体（<53 μm）（分别约占15%）。易提取球囊霉素占总球囊霉素的比例在粉黏粒级微团聚体（<53 μm）中更低,约为20%,其他粒径均在30%以上。球囊霉素中碳占土壤有机碳的比例在各团聚体中无显著差异,不同粒径团聚体中易提取球囊霉素约占有机碳的2%左右,而总球囊霉素约占有机碳的8%左右。大于250 μm团聚体中球囊霉素随温度和降水的增加而增加,而随着pH的增加而降低。在小于250 μm团聚体中未发现显著相关性,但发现球囊霉素随土壤有机碳增加而增加,呈显著正相关。通过比较不同利用方式的土壤,本研究还发现林地土壤各粒径团聚体中的球囊霉素均不低于耕地和草地土壤,这说明林地土壤较其他类型土壤更有利于球囊霉素的积累。     

球囊霉素及其在土壤生态系统中的作用

球囊霉素(Glomalin)是一种在土壤中大量存在的、由丛枝菌根真菌(Arbuscular mycorrhizal fungi, AMF)产生的具有良好热稳性的特殊糖蛋白。球囊霉素因其在促进土壤团聚体形成,保持团聚体稳定性,增加土壤有机碳库,提高植物抗逆能力以及降低重金属在土壤中的毒性等方面的作用备受人们关注。目前由于提取方法的原因,人们一般将球囊霉素的命名改为球囊霉素相关土壤蛋白(Glomalin related soil protein, GRSP)。随着研究的不断深入,人们对GRSP在生态系统中的作用展开了广泛的研究。GRSP对土壤颗粒有较强的胶结作用,其胶结能力为其他胶结物质的3～10倍;作为有机碳库的重要组成部分对土壤有机碳的贡献率为6.98%～31.3%,并且在土壤中周转时间较长为6～42年;GRSP还可以螯合不同的重金属,减少它们在土壤中的毒害作用以及降低潜在毒性。但想要更为深入的了解GRSP在生态系统中的作用需要对其结构进行进一步的了解、提取测定方法进行进一步的优化。本文重点总结了国内外研究中GRSP对土壤团聚体、土壤有机碳库的作用,GRSP研究中存在的主要问题以及未来...     

钼污染对丛枝菌根和球囊霉素的影响

丛枝菌根作为地球上最广泛的共生体,在各种逆境环境中发挥着重要作用.基于不同钼污染程度的钼矿区,分析了钼污染对丛枝菌根真菌侵染、繁殖及其分泌球囊霉素能力的影响.结果 表明,在4个不同钼污染级别的土壤中,丛枝菌根真菌与植物共生关系的形成未受到钼污染的影响,平均菌根侵染频度为50.64％.洛阳钼矿区土壤的平均孢子密度为19....     

土地利用方式对酸性红壤丛枝菌根真菌群落的影响

为了研究土地利用方式对酸性红壤丛枝菌根真菌(arbuscular mycorrhizal fungi, AMF)群落的影响,调查了酸性红壤4种土地利用方式(草地、玉米、花生和大豆)下非根际和根际土壤AMF群落多样性和组成结构。结果表明：土地利用方式显著影响了AMF群落优势属球囊霉属(Glomus)和巨孢囊霉属(Paraglomus)的相对丰度,但是根际作用影响不明显。土地利用方式而非根际作用显著影响了AMF群落香农指数和物种丰富度,其中大豆地表现出最低的香农指数和物种丰富度。土地利用方式和根际作用都显著影响AMF群落组成结构,但是土地利用方式的作用强度明显高于根际作用。球囊霉属主要解释了不同土地利用方式之间的AMF群落组成差异。土壤p H是影响土壤AMF群落结构的最关键因子。因此,土地利用方式比根际作用表现出对酸性红壤AMF群落更大的影响,展现了土地利用变化在影响土壤AMF群落方面的重要作用。     

接种丛枝菌根真菌的种植紫花苜蓿土壤中球囊霉素含量与去除的关系

以菲和芘为多环芳烃（PAHs）代表物,以紫花苜蓿（Medicago sativa L.）为宿主植物,选用幼套球囊霉（Glomus etunicatum, Ge）、摩西球囊霉（Glomus mosseae,Gm）和层状球囊霉（Glomus lamellosum,Gla）3种丛枝菌根真菌（AMF）,研究了接种AMF下土壤中AMF菌丝密度、球囊霉素含量与PAHs去除率的关系。35~75 d,接种Ge、Gm、Gla处理的土壤中菌丝密度、总球囊霉素含量、易提取球囊霉素含量均随时间延长而显著增大,与不接种对照相比,75 d时接种Ge、Gm、Gla处理的土壤中易提取球囊霉素含量提高了48.58%、55.99%和50.23%,总球囊霉素含量则提高了38.75%、50.95%和46.12%。接种AMF促进了土壤中菲和芘的去除,随着时间（35~75 d）延长,接种Ge、Gm、Gla处理的土壤中菲去除率分别高达83.4%~92.7%、82.1%~93.8%、86.9%~93.4%,芘去除率达42.2%~63.5%、43.7%~69.2%、44.6%~66.4%。接种Ge、Gm和Gla处理土壤中AMF菌丝密度、总球囊霉素含量均与土壤中菲和芘的去除率之间存在极显著正相关关系,表明接种AMF提高了土壤中AMF菌丝密度和总球囊霉素含量,并促进了土壤中PAHs的去除。研究结果为阐明丛枝菌根修复PAHs污染土壤的规律及机理提供了依据。     

AM真菌对桑树根围土壤团聚体的影响机制

为揭示丛枝菌根 (Arbuscular mycorrhizal,AM)真菌对植桑土壤的影响及机制,采用盆栽试验研究接种摩西管柄囊霉 (Funneliformis mosseae,Fm)和根内根生囊霉 (Rhizophagus intraradices,Ri)对土壤有机碳(Soil organic carbon, SOC)、球囊霉素相关土壤蛋白 (Glomalin related soil protein, GRSP)及团聚体组成与稳定性的影响。结果表明：⑴ 接种Ri显著增加土壤大团聚体百分比,并提高平均质量直径 (Mean weight diameter, MWD)和几何平均直径 (Geometric mean diameter, GMD)、显著降低团聚体破坏率 (Percentage of aggregate destruction, PAD)。⑵ 接种Fm和Ri均显著增加微团聚体SOC含量,接种Fm显著降低大团聚体总GRSP含量,而接种Ri却显著增加大团聚体和微团聚体总GRSP含量及易提取GRSP含量。⑶ 接种AM真菌对整体SOC的效应为负,土壤总GRSP对SOC占比在25.5%~76.5%之间,土壤易提取GRSP对SOC占比在4.87%~5.93%之间,且Ri的接种效应高于Fm。⑷ 总GRSP、易提取GRSP和SOC对团聚体组成表现均为正向显著影响,其中易提取GRSP是主要驱动因子,而总GRSP是土壤团聚体稳定性的主要影响因子。综上,AM真菌作用下桑树根围土壤团聚体得以改善并趋于稳定,Ri的接种效应明显大于Fm;土壤团聚体的形成主要依赖易提取GRSP,而其稳定性主要受总GRSP影响。     

丛枝菌根真菌对红三叶草利用不同有机磷源的研究

以红三叶草为材料 ,利用三室隔网培养方法 ,施用不同有机磷源 :植酸钠 (Na -Phytate)、核糖核酸 (RNA)和卵磷脂 (Lecithin) ,研究接种菌根真菌Glmous versiforme对土壤及外加有机磷源的利用效率 ,另设无机磷及不施磷作为对照。结果表明 ,接种菌根真菌能明显增加植株干物重、含磷量和吸磷总量。与各有机磷处理相比 ,无机磷处理前期的生长效应较好 ,施用有机磷各处理在不同生长时期均明显促进了植株生长 ,但不同有机磷源之间没有显著差异。在植株吸磷量上 ,植株生长 7周以前 ,磷酸二氢钾处理高于其它处理 ,而植株生长 10周时 ,植酸钠处理高于磷酸二氢钾处理。接种菌根处理由于丛枝菌根活化了土壤有机磷 ,到植株生长 10周时其吸收有机磷的量已占吸磷总量的 76 .7%。     

接种AMF对海绵结构重构土层的玉米根系分布及水分利用特征的影响

[目的] 露天煤矿区生态脆弱,水资源短缺,利用微生物复垦已成为矿区生态重建的研究热点。探究露天矿排土场重构土层海绵生态结构条件下接种丛枝菌根真菌(arbuscular mycorrhiza fungi,AMF)对玉米根系生长及水分利用特征的影响,为矿区生态农业建设提供科学依据。[方法] 在室内布设土柱模拟试验,设置裸土柱(CK)、玉米不接菌(NM)和玉米接菌(AM)3个处理,采用氢氧稳定同位素示踪技术研究玉米根系水分利用特征。[结果] ①接种AMF处理促进了玉米根系的生长,改变了玉米根系分布。AM处理玉米的总根长、总根表面积、总根体积和根尖数分别比NM处理高19.3 %,14.8 %,9.1 %和34.0 %,AM处理小于0.3 mm的细根及大于0.7 mm的粗根比例分别比NM处理高3.2 %和3.5 %。②AMF改变了玉米的水分利用特征,AM处理玉米利用的水分来源于0-20 cm土层的比例较NM处理提升5.5 %。③AM处理土柱0-20 cm土层含水率显著低于NM处理,饱和黏土层含水率:CK处理>NM处理>AM处理。AMF提升了玉米根系吸收水分的能力,影响黏土层中水分的释出。[结论] 在矿区排土场海绵结构重构土层上接种AMF能促进玉米根系发育,改善水分利用策略,使其充分利用海绵结构中涵水层保蓄的水分。     

Differential decomposition of arbuscular mycorrhizal fungal hyphae and glomalin

Arbuscular mycorrhizal fungi (AMF) are obligate symbionts of most higher plants. In addition to being a major component of soil microbial biomass, AMF hyphae produce glomalin, a recalcitrant glycoproteinaceous substance highly correlated with soil aggregate water stability. This study addresses the lack of knowledge concerning the decomposition of hyphae and glomalin. We used an experimental design that exploited the lack of saprobic capabilities of AMF hyphae by incubating field soil samples in the dark, and hence in the absence of plant or AMF hyphal growth. In 150 days, hyphal length decreased 60%, while glomalin, quantified by the Bradford protein assay, declined only 25%. Immuno-reactive glomalin decreased 46%. This study serves as a proof-of-concept for further examination of factors that influence decomposition of AMF hyphae using similar experimental designs.     

Losses of glomalin-related soil protein under prolonged arable cropping: A chronosequence study in sandy soils of the South African Highveld

Residues of arbuscular mycorrhizal fungi (AMF) may be important for agroecosystem functioning due to their ability to promote soil aggregation, especially in coarse textured soils with little biomass input and low capacity to conserve soil organic matter (SOM). Our aim was to assess the fate of AMF residues with prolonged arable cropping in coarse textured soils in a subtropical savannah assuming that glomalin-related soil protein (GRSP), especially the MAb32B11-immunoreactive fraction, mainly constitutes material of AMF origin. In three agroecosystems on the South African Highveld, surface soils were sampled. The former grassland soils had a history of up to 98 yr of cropping. We measured four GRSP fractions: Bradford-reactive soil protein (BRSP) and immunoreactive soil protein (IRSP), and easily extractable fractions of both. The primary grassland sites exhibited generally low contents of SOM and low GRSP contents. Prolonged arable land use of former grassland soils reduced the content of GRSP further. The decline could be described with a mono-exponential function with rate constants ranging from 0.04 to 0.41 yr⁻¹. Depending on the GRSP fraction, steady-state conditions were reached after 11-92 yr on a level of 39-69% of the initial contents. We conclude that even though GRSP fractions had the same hypothesized origin, they comprised pools with different stability or replacement rate. Easily extractable IRSP was lost most rapidly. In contrast to carbon, nitrogen and microbial residue dynamics, GRSP contents were not reduced below a certain steady-state level, despite potentially negative management effects on AMF, such as tillage, inclusion of fallows into crop rotation and fertilization with inorganic phosphorus. The steady-state GRSP contents coincided with low, but steady agroecosystem yields under the given cropping management.     

有机管理对不同土地利用方式下土壤质量的影响

许多研究发现有机管理可以改善农田土壤质量,但是否不同土地利用方式下都存在此结论尚未明确。为探究有机管理对不同土地利用方式土壤质量的影响,本研究基于一个多土地利用方式的有机管理农场及其附近常规管理农田进行土壤质量调查,对比不同管理措施及大棚菜地、果园、露天菜地、农田边界、稻田田埂5种土地利用方式下农田土壤质量的差异,并对不同管理措施下农田土壤养分含量、重金属含量、动物数量共计20个指标进行方差分析和主成分分析。研究发现虽然总体上(综合5种土地利用方式的均值)有机管理的土壤pH显著高于常规农田;但针对一种土地利用方式,只有露天菜地和农田边界的土壤pH显著提高。总体上有机管理下土壤全磷、全钾、有效磷含量显著降低,但露天菜地土壤有机质和全氮含量均显著高于常规管理农田。有机管理在总体上显著降低了土壤Cr、Cu、Ni、Zn含量;但针对一种土地利用方式,只显著降低了大棚菜地土壤Cr、Ni、Zn含量,果园和稻田田埂土壤Cu含量,露天菜地和农田边界土壤Zn含量。有机管理虽然总体上均显著增加了土壤中蜘蛛目、倍足纲、步甲、蚯蚓的数量;但针对一种土地利用方式,只显著增加了露天菜地地表蜘蛛目、倍足纲、步甲,稻田田埂地表步甲、土壤蚯蚓以及果园倍足纲数量。主成分分析结果表明,不同管理方式下土壤质量差异明显,有机管理下蜘蛛目、倍足纲、步甲和蚯蚓等土壤动物较多,土壤pH较高,土壤P含量较低,重金属Cu、Pb、Zn、Cr含量较低,但并非在所有土地利用方式下都成立。由此可见,有机管理虽然总体上可以改善土壤质量,但受具体管理措施、人为投入品数量和有机种植时间等因素影响,并非在所有土地利用方式下效果都显著,且在不同土地利用方式下显著改善的指标也各不相同,因此需要针对不同土地利用方式和不同指标采取针对性的改善措施。     

Characterization of glomalin as a hyphal wall component of arbuscular mycorrhizal fungi

Arbuscular mycorrhizal fungi (AMF) produce a protein, glomalin, quantified operationally in soils as glomalin-related soil protein (GRSP). GRSP concentrations in soil can range as high as several mg g⁻¹ soil, and GRSP is highly positively correlated with aggregate water stability. Given that AMF are obligate biotrophs (i.e. depending on host cells for their C supply), it is difficult to explain why apparently large amounts of glomalin would be produced and secreted actively into the soil, since the carbon could not be directly recaptured by the mycelium (and benefits to the AMF via increased soil structure would be diffuse and indirect). This apparent contradiction could be resolved by learning more about the pathway of delivery of glomalin into soil; namely, does this occur via secretion, or is glomalin tightly bound in the fungal walls and only released after hyphae are being degraded by the soil microbial community? In order to address this question, we grew the AMF Glomus intraradices in in vitro cultures and studied the release of glomalin from the mycelium and the accumulation of glomalin in the culture medium. Numerous protein-solubilizing treatments to release glomalin from the fungal mycelium were unsuccessful (including detergents, acid, base, solvents, and chaotropic agents), and the degree of harshness required to release the compound (autoclaving, enzymatic digestion) is consistent with the hypothesis that glomalin is tightly bound in hyphal and spore walls. Further, about 80% of glomalin (by weight) produced by the fungus was contained in hyphae and spores compared to that released into the culture medium, strongly suggesting that glomalin arrives mainly in soil via release from hyphae, and not primarily through secretion. These results point research on functions of glomalin and GRSP in a new direction, focusing on the contributions this protein makes to the living mycelium, rather than its role once it is released into the soil.     

省域土壤有机碳空间分布的主控因子——土壤类型与土地利用比较

基于河北省第二次全国土壤普查数据,运用方差分析和回归分析对比了河北省土壤类型和一级土地利用类型对0～20 cm深土壤有机碳空间分布的影响,探讨了省域土壤有机碳空间分布的主控因子。研究结果表明,土壤类型和土地利用是河北省表层土壤有机碳密度空间分布的重要影响因子。其中土壤类型对土壤有机碳密度空间分布的影响与土壤分类级别相关,土壤分类级别越低,对土壤有机碳密度空间变异的反映能力越大。与土壤类型相比,土地利用对表层土壤有机碳密度空间分异的解释能力要大于土类,但小于亚类和土属。为此,在省域尺度对土壤有机碳密度进行区域预测和估算时应将土地利用和土壤类型结合起来作为土壤有机碳空间分布的主控因子,优先考虑土地利用后,在相同土地利用类型内再尽量以低级土壤分类进行空间预测或估算。     

The combined effects of earthworms and arbuscular mycorrhizal fungi on microbial biomass and enzyme activities in a calcareous soil spiked with cadmium

Earthworms and arbuscular mycorrhizal fungi (AMF) are known to independently affect soil microbial and biochemical properties, in particular soil microbial biomass (SMB) and enzymes. However, less information is available about their interactive effects, particularly in soils contaminated with heavy metals such as cadmium (Cd). The amount of soil microbial biomass C (MBC), the rate of soil respiration (SRR) and the activities of urease and alkaline phosphatase (ALP) were measured in a calcareous soil artificially spiked with Cd (10 and 20 mg Cd kg⁻¹), inoculated with earthworm (Lumbricus rubellus L.), and AMF (Glomus intraradices and Glomus mosseae species) under maize (Zea mays L.) crop for 60 days. Results showed that the quantity of MBC, SRR and enzyme activities decreased with increasing Cd levels as a result of the elevated exchangeable Cd concentration. Earthworm addition increased soil exchangeable Cd levels, while AMF and their interaction with earthworms had no influence on this fraction of Cd. Earthworm activity resulted in no change in soil MBC, while inoculation with both AMF species significantly enhanced soil MBC contents. However, the presence of earthworms lowered soil MBC when inoculated with G. mosseae fungi, showing an interaction between the two organisms. Soil enzyme activities and SRR values tended to increase considerably with the inoculation of both earthworms and AMF. Nevertheless, earthworm activity did not affect ALP activity when inoculated with G. mosseae fungi, while the presence of earthworm enhanced urease activity only with G. intraradices species. The increases in enzyme activities and SRR were better ascribed to changes in soil organic carbon (OC), MBC and dissolved organic carbon (DOC) contents. In summary, results demonstrated that the influence of earthworms alone on Cd availability is more important than that of AMF in Cd-polluted soils; and that the interaction effects between these organisms on soil microorganism are much more important than on Cd availability. Thus, the presence of both earthworms and AMF could alleviate Cd effects on soil microbial life.