运用多隔层根箱研究黑麦草根际微域中芘的降解

采用多隔层根箱,通过尼龙撩网插片的控制,实现根室土(S0)、离根室0～2 mm(S1)、2～4 mm(S2)、4～6 mm(S3)及>6 mm(S4)各室层土壤的分离采集,测定各室层土壤可提取态芘含量、土壤微生物生物量碳、土壤基础呼吸强度、微生物熵、代谢熵、脱氢酶和多酚氧化酶活性。结果表明:种植黑麦草处理的各室层内土壤可提取态芘含量存在显著的不同,可提取态芘含量在各室层的大小顺序为S4>S3>S0>S2>S1;各室层土壤微生物生物量碳、土壤基础呼吸强度、微生物熵、代谢熵、脱氢酶和多酚氧化酶活性表现出与可提取态芘含量变化相反的趋势。未种植黑麦草处理的各室层土壤可提取态芘含量、土壤微生物生物量碳、土壤基础呼吸强度、微生物熵、代谢熵、脱氢酶和多酚氧化酶活性没有差异。种植黑麦草处理各室层土壤可提取态芘含量与土壤微生物生物量碳、土壤基础呼吸强度、微生物熵、代谢熵、脱氢酶活性和多酚氧化酶活性之间均存在显著的负相关性(p<0.05)。主成分分析结果表明种植黑麦草处理土壤微生物活性在各室层间发生了明显的变化。     

玉米幼苗对芘污染土壤微生物活性及多样性的影响

通过盆栽土培试验研究了玉米幼苗生长期间对芘污染土壤微生物活性及多样性的影响。结果表明,玉米加快了土壤中芘的降解,提高了芘在土壤中的降解速率。试验期间,根际土中可提取态芘含量显著低于非根际土,根际土微生物生物量碳、微生物熵、多酚氧化酶和脱氢酶活性均高于非根际土,代谢熵低于非根际土。脂肪酸（FAME）分析结果表明,与非根际土相比,芘污染玉米根际土微生物群落结构发生了显著的变化,主要表现在真菌特征脂肪酸以及真菌/细菌的比值显著升高,细菌和GN^-细菌特征脂肪酸显著降低,且这种效应随着培养时间的推移在P〈0.01水平显著。根际土和非根际土中丛枝菌根真菌、GN^＋细菌和放线菌特征脂肪酸差异随着培养时间的延长逐渐加大,45 d时其差异均在P〈0.05水平显著。     

丛枝菌根真菌菌丝对土壤微生物群落结构及 多氯联苯降解的影响

以摩西球囊霉(Glomus mosseae)为供试菌种,在光照培养箱内利用分室根箱研究丛枝菌根真菌菌丝对多氯联苯(polychlorinated biphenyls,PCBs)污染土壤的修复效应及其机理。试验设置接种丛枝菌根真菌的处理以及不接种的对照,选用美国南瓜(Cucurbita pepo L.)为供试植物,在南瓜生长40天后将接种菌根真菌处理的菌丝室土壤从尼龙网向外水平分为4层取样,测定PCBs及磷脂脂肪酸含量。结果表明:菌丝可以穿越尼龙网影响菌丝室土壤,且距离尼龙网越远菌丝量越低;菌丝显著促进了土壤微生物量(P0.05),并改变了不同土层土壤微生物群落结构;接种菌根真菌处理各土层PCBs降解率为35.67%~57.39%,均显著高于对照的17.31%,相关分析结果表明土壤三氯、四氯联苯以及PCBs总量与菌丝量呈极显著负相关(P0.01);菌丝际土壤微生物量,特别是细菌生物量与土壤三氯联苯含量呈显著负相关(P0.05)。可见,菌丝通过影响菌丝际土壤微生物群落结构及生物量,促进三氯及四氯联苯降解,从而提高土壤PCBs修复效率。     

福建海岸沙地5种防护林土壤微生物群落特征

[目的]探明福建海岸沙地不同防护林对土壤微生物群落的影响及机制,为海岸带防护林森林质量提升提供科学依据。[方法]选择5种主要防护林为对象,分别为次生林、木麻黄(Casuarina equisetifolia)人工林、湿地松(Pinus elliottii)人工林、厚荚相思(Acacia crassicarpa)人工林和尾巨桉(Eucalyptus urophylla×E.grandis)人工林,采用磷脂脂肪酸法(Phospholipids fatty acid, PLFA)比较了不同防护林的土壤微生物群落结构。[结果](1)海岸沙地不同防护林土壤中共检测到18种PLFA生物标记,在尾巨桉和次生林中种类最多,湿地松和厚荚相思人工林最少。(2)土壤总磷脂脂肪酸、革兰氏阳性细菌和革兰氏阴性细菌含量均表现为尾巨桉和次生林较高,厚荚相思和木麻黄人工林较低,土壤真菌含量为尾巨桉林最高,丛枝菌根菌含量为次生林最高,真菌和丛枝菌根菌含量在其他防护林间无显著差异。(3)次生林的土壤微生物多样性和均匀度均高于4种人工林。(4)土壤pH、细根碳氮含量为土壤微生物群落的主要影响因子,其次为土壤全氮和硝态氮含量...     

改变凋落物和根系输入对米槠天然林土壤微生物群落的影响

伴随气候变化下亚热带地区米槠天然林净初级生产力变化,凋落物以及植物根系输入亦会发生改变,这将显著影响土壤微生物群落。于2019年7月在设置7年的米槠天然林植物残体添加和去除试验（the detritus input and removal treatments,DIRT）样地采集不同处理（对照、去除地上凋落物、去除地下根系、无凋落物输入、添加双倍地上凋落物）的2个土层土壤（0—10,10—20 cm）,测定微生物磷脂脂肪酸（phospholipid fatty acid,PLFA）含量,计算各微生物群落比值以及多样性,进一步揭示凋落物和植物根系输入对亚热带米槠天然林土壤微生物群落组成和多样性的影响。结果表明：（1）不同处理下0—10 cm土层微生物磷脂脂肪酸含量约为10—20 cm土层的2倍;（2）地上凋落物变化均使得革兰氏阳性菌、阴性菌及放线菌等细菌含量出现不同程度的下降,但不会对丛枝菌根等真菌含量产生影响,而去除根系处理显著降低丛枝菌根真菌含量;（3）微生物群落Shannon-wiener、Simpson多样性指数不受凋落物输入的影响,凋落物去除降低表层土壤微生物群落的Margalef丰富度,提高Pielou均匀度,表明0—10 cm土层微生物群落含量与分布状况受凋落物输入变化影响较大;（4）地下植物根系存在可提高真菌（如丛枝菌根真菌）含量,而地上凋落物输入主要改变细菌丰度以及群落结构。可溶性有机碳以及矿质氮是影响不同处理土壤微生物群落组成和多样性的主要因素。可见,凋落物和根系输入通过土壤理化性质的变化而影响了微生物群落,研究结果可为全面认识植物、土壤与微生物间的相互作用对森林生产力的影响提供科学依据。     

丛枝菌根对芘污染土壤修复及植物吸收的影响

采用温室盆栽试验方法,研究了两种丛枝菌根真菌Glomus mosseae和 Glomus etunicatum对三叶草(Trifolium subterraneum L.)和辣椒（Capsicum annuum L.）修复芘污染土壤的影响。供试土样中芘初始浓度为0 ~ 75.18 mg/kg。结果表明,接种AMF可促进供试植物对土壤中芘的吸收,并且显著提高三叶草根的芘含量、根系富集系数、根和茎叶的芘积累量,但对辣椒根和茎叶芘含量、根系富集系数的影响不显著,这主要与植物的菌根侵染率和“菌根依赖度”不同有关。接种AMF土壤中芘的削减率高于普通植物修复,但植物吸收积累对修复的贡献率小于0.2%;因此推测,AM作用下良好的根际环境对土壤微生物数量和活性的提高、进而对土壤中芘降解的促进可能是菌根修复的主要机理。     

保护性耕作对黑土微生物群落的影响

耕作方式通过影响土壤微生物群落而影响土壤生态系统过程。本研究以传统耕作玉米连作处理为对照,通过测定土壤微生物量碳及磷脂脂肪酸含量,分析了保护性耕作(包括免耕玉米连作和免耕大豆-玉米轮作)对黑土微生物群落的影响。结果表明,保护性耕作可显著增加土壤表层(0～5cm)全碳、全氮、水溶性有机碳、碱解氮和微生物量碳(P0.05),为微生物代谢提供了丰富的资源。同时,保护性耕作显著提高了土壤表层(0～5cm)总脂肪酸量、真菌和细菌生物量(P0.05),提高了土壤的真菌/细菌值,有利于农田土壤生态系统的稳定性。研究结果对于探讨保护性耕作的内在机制具有重要意义。     

长期种植毛竹林土壤丛枝菌根真菌群落演变趋势

为揭示长期种植毛竹林土壤丛枝菌根(Arbuscular mycorrhizae,AM)真菌群落演变特征,通过磷脂脂肪酸(Phospholipid fatty acid,PLFA)和Illumina Miseq测序平台研究了AM真菌生物量及群落结构的演变趋势。结果表明,长期种植毛竹林土壤养分含量总体呈下降趋势,球囊霉素相关土壤蛋白(Glomalin-related soil protein,GRSP)含量及AM真菌生物量也显著降低(p0.05),其中易提取态球囊霉素相关土壤蛋白(Easily extractable glomalin-related soil protein,EE-GRSP)含量与有机质、碱解氮、速效钾显著正相关(p0.05),而AM真菌菌丝生物量(16:1ω5 PLFA)与碱解氮极显著正相关(p0.01)。长期种植毛竹林显著降低了土壤2~0.25 mm大团聚体比例(p0.05),且与AM真菌菌丝生物量极显著正相关(p0.01)。测序结果表明,毛竹林土壤AM真菌以球囊霉属(Glomus)为优势种群,其次为无梗囊霉属(Acaulospora),长期种植毛竹后土壤球囊霉属相对丰度显著增加而无梗囊霉属显著降低(p0.05)。非度量多维尺度转换排序(Non-metric multidimensional scaling,NMDS)分析显示,对照马尾松林与不同种植年限毛竹林土壤AM真菌群落显著区分(p=0.001),土壤含水量(p=0.005)、碱解氮(p=0.001)、有效磷(p=0.014)对AM真菌群落结构变异具有重要贡献。长期种植毛竹显著降低了AM真菌生物量、球囊霉素相关土壤蛋白含量以及2~0.25 mm大团聚体比例,并改变了AM真菌群落结构,不利于土壤碳固存和维持生态系统稳定。     

林分改变驱动的优势菌根真菌类型变化影响土壤有机碳积累

马尾松林（Pinus massoniana Lamb.）是典型的外生菌根（Ectomycorrhiza, ECM）优势林，但是近年来受到松材线虫病的影响，生态服务功能下降，逐渐被丛枝菌根（Arbuscular mycorrhiza, AM）占优势的阔叶林所替代，但亚热带地区马尾松林转变为阔叶林过程中，优势菌根类型的改变对土壤有机碳积累的影响仍不清楚。以建德市马尾松林和阔叶林为研究对象，通过高效液相色谱和中性脂肪酸、磷脂脂肪酸等技术，测定优势菌根真菌生物量、球囊霉素相关土壤蛋白（GRSP）含量以及土壤胞外酶活性和微生物群落特征。结果表明：AM真菌占优势的阔叶林（AMD）取代ECM真菌占优势的马尾松林（ECMD），土壤有机碳显著提高了36.81%，微生物碳利用效率（CUE）显著提高了53.85%，AM真菌生物量提高了25.57%，ECM真菌生物量下降45.04%，并且ECM真菌占优势的马尾松林受到更严重的氮限制。磷脂脂肪酸分析显示，相比于AM真菌占优势的阔叶林，ECM真菌占优势的马尾松林革兰氏阳性细菌（G+）以及革兰氏阳性与阴性细菌之比（G+/G-）分别显著下降了21.47%和6.46%。冗余分析（Redundancy analysis, RDA）结果表明，AM真菌占优势和ECM真菌占优势的森林之间土壤微生物群落结构存在显著差异（P<0.05），其中AM真菌生物量和土壤有机碳与微生物群落结构变异显著相关。GRSP含量下降以及不同类型菌根真菌招募微生物类群不同是导致ECM真菌占优势森林土壤有机碳下降的重要原因。因此，亚热带地区马尾松林被阔叶林替代后增加森林土壤有机碳含量，提高森林碳汇功能。     

蚯蚓与菌根提高玉米生长和氮磷吸收的互补效应

【目的】蚯蚓和丛枝菌根真菌处于不同的营养级,但在促进植物生长和提高土壤肥力等方面却都发挥着积极作用。研究蚯蚓菌根互作及其对玉米吸收土壤中的氮、磷养分的影响,可为提升土壤生物肥力及促进农业的可持续发展提供理论依据。【方法】本研究采用田间盆栽方式,以玉米为供试作物,研究蚯蚓(Eisenia fetida)与丛枝菌根真菌(Glomus intraradices)互作及其对玉米养分吸收的影响。试验设置P 25和175 mg/kg两个水平。每个磷水平进行接种与不接种菌根真菌以及添加与不添加蚯蚓,共8个处理。调查了玉米生长、养分吸收以及真菌浸染和土壤养分的有效性。【结果】两个磷水平下,蚯蚓和菌根在增加玉米地上部和根系生物量方面有显著正交互作用(P0.05)。接种菌根真菌的各处理显著增加了玉米的侵染率及泡囊丰度、根内菌丝丰度等菌根指标。同时添加蚯蚓和接种菌根真菌的处理(AM+E)显著提高了菌根的侵染率、菌丝密度、丛枝丰度和根内菌丝丰度但是泡囊丰度有所下降。两种磷水平下,AM+E处理玉米地上部和地下部含氮量和含磷量均显著高于其他三个处理。在低磷条件下,地上部氮磷总量的增加分别是添加蚯蚓和接菌的作用;而地下部磷总量的增加主要是菌根真菌的作用。在高磷条件下,单加蚯蚓显著增加玉米氮磷的总量,而接种菌根真菌对玉米氮磷吸收的影响未达显著性水平。在高磷条件下,单加蚯蚓的处理显著提高玉米地上地下部生物量(P0.05),而单接菌的处理效应不显著,蚯蚓菌根互作通过提高土壤微生物量碳、氮实现对玉米生长和养分吸收的调控。在低磷条件下,单接菌显著提高了玉米的生物量(P0.05),单加蚯蚓的处理具有增加玉米生物量的趋势。菌根真菌主要促进玉米对磷的吸收,蚯蚓主要矿化秸秆和土壤中的氮磷养分增加土壤养分的有效性,蚯蚓菌根互作促进了玉米根系对土壤养分的吸收并形成氮磷互补效应。【结论】无论在高磷还是低磷水平下,蚯蚓菌根相互作用都提高了玉米地上地下部生物量、氮磷吸收量同时提高了土壤微生物量碳、氮。蚯蚓菌根相互作用对植物生长的影响取决于土壤养分条件。在高磷条件下(氮相对不足),蚯蚓菌根互作通过调控土壤微生物量碳、氮调控玉米生长和养分吸收。低磷条件下,菌根主要发挥解磷作用,蚯蚓主要矿化秸秆和土壤中的氮素,蚯蚓和菌根互补调控土壤中氮、磷,从而促进植物的生长和养分吸收。     

Effects of humic acid on remediation of the nutritional deficiency of gerbera in hydroponic culture

Information is scant on the effect of humic acid (HA) on physiological, antioxidant and photosynthesis attributes of gerbera plants undergoing nutrient deficiency in culture solution. Gerbera plants cv. Malibu were grown in a factorial experiment based on a completely randomized design with 3 replications, using 3 different nutrient solutions [complete nutrient solution (NSc), 25% NSc (NS1), and 50% NSc (NS2)] treated with 2 levels of humic acid [0 (HA0) and 500 mg/l (HA1)].The interaction effect of HA and NS showed that HA improved the flower number in NSc, the transpiration in NS1+HA1, photosynthesis rate in NSc+HA1, stomatal conductance (gs) in NS2, mesophyll conductance of leaves in all NS levels and photosynthetic water use efficiency in NSc+HA1. The interaction effect of nutrient solution and HA on antioxidant activity was inconclusive, malondialdehyde content was the highest in NS2 and the lowest in NS1+HA1. The peroxidase activity increased in complete nutrient solution with and without HA and there were no differences among other treatments. Superoxide dismutase activity increased in NS1 and complete nutrient solution with HA and reached the highest in NSc. Humic acid was more effective in nutrient uptake, i.e., nitrogen, phosphorus, potassium, calcium, zinc, and iron (N, P, K, Ca, Zn, and Fe) in complete nutrient solution compared to NS1 and NS2. Conclusively, humic acid can compensate the nutrient deficiency stress of the culture solution in regards to protein synthesis, photosynthesis attributes regardless of the nutrient uptake of gerbera.     

Predicting the Classes and Distribution of Salt-Affected Soils in Northwest Libya

Sodicity and salinity can adversely affect soil structure and are common constraints to plant growth in arid regions. Current remote sensing techniques cannot distinguish between the various classes of salt-affected soils. Field and laboratory measurements of salt-affected soils are time-consuming and expensive. Mapping of the salt-affected soils can be used in soil conservation planning to identify regions with different degrees of limitations. There is a need to use existing field and laboratory measurements to create maps of classes of salt-affected soils. The objectives of this study are to classify salt-affected soils, use existing field data to interpolate and validate geospatial predictions of the classes of salt-affected soils using Geographic Information Systems (GIS), and create maps showing the different classes and distribution of salt-affected soils. The classification framework for salt-affected soils is based on electrical conductivity (ECe), soil pH and the sodium adsorption ratio (SAR), and provides four degrees of limitations to salt-affected soils: slight (normal soils), moderate (saline soils), severe (sodic soils), and extreme (saline-sodic soils). Spatial interpolation of the field data from northwestern Libya was verified by cross-validation, and maps of the salt-affected soils in the region were created. The majority of soils in this region of Libya are normal (slight degree of limitation). Twenty percent of the topsoil is saline-sodic (extreme degree of limitation). Land use recommendations and rehabilitation strategies can be developed from such maps of salt-affected soil classes. The methodology followed in this study can be applied to other arid regions around the world, particularly in developing countries where budgetary constraints limit detailed field and laboratory measurements of sodicity and salinity.     

黑龙江农田土壤壬基酚及其短链聚氧乙烯醚残留调查

对黑龙江土壤样品中的壬基酚(NP)、壬基酚一氧乙烯醚(NP1EO)和壬基酚二氧乙烯醚(NP2EO)的残留状况开展研究。结果表明,NP、NP1EO和NP2EO均有不同程度的检出,检出率在68.46%~95.38%之间;NP、NP1EO和NP2EO的浓度分别为ND~156.8μg kg-1、ND~15.70μg kg-1和ND~13.63μg kg-1,均值分别为22.02μg kg-1、4.04μg kg-1和2.15μg kg-1;进一步分析,已检出的样品中,NP在0~10μg kg-1的比重最大,NP1EO在4~6μg kg-1比重最大,NP2EO在1~2μg kg-1比重最大。NP的残留水平高于NP1EO和NP2EO,说明NP相对较难降解,更易在土壤中累积。     

有限性灌溉对设施草莓产量及水分利用效率的影响

在日光温室环境及盆栽条件下,通过与全灌(FI)比较,研究了亏缺灌溉(DI)及分根交替灌溉(PRD)对草莓产量和灌水利用效率(IWUE)的影响.试验从开花期开始到果实成熟期结束.共分5个处理,全灌(FI);分根灌溉PRD分2个处理水平,即PRD1和PRD2;限制灌溉DI也分两个处理水平,即D11和D12.与F1处理相比,DI1和DI2处理的叶水势和气孔导度明显偏低,单株叶面积、鲜果重、平均单果重也显著低于FI处理.但水分利用效率却比FI处理的高(分别高15.8%和29.3%);PRD1处理的叶水势与FI处理的相当.且高于其它处理,而气孔导度比FI,DI1和D12处理的明显降低,与PRD2处理的相近.PRD1处理的鲜果重、平均单果重与FI处理的相当,比DI1,DI2和PRD2处理的显著提高;与FI处理相比,DI1,DI2,PRD1和PRD2处理分别节水31.5%,50.0%,31.5%和50.0%,水分利用效率分别提高了15.8%,29.3%,44.4%和84.4%,从草莓产量和水分利用效率各指标可以看出,PRD1处理比DI1,DI2和PRD2处理表现出明显的优势,其综合效益最佳.     

Effects of residue coverage on the characteristics of soil carbon pools in orchards

The effects of organic waste coverage on the quality of soil carbon (C) pools in orchards remain unclear. In this study, we performed a 3-year experiment in an 8-year-old Fuji apple orchard to investigate the effects of inter-row weed growing/inner-row pruning residue coverage (PRC), weed coverage (WC), and inter-row weed growing/inner-row non-coverage (used as a control) on the contents of soil water, available nitrogen, phosphorus, and potassium, organic C components, glomalin-related soil protein (GRSP), soil microbial biomass C, and the number of microorganisms at different soil depths. PRC increased the percentage of readily oxidizable C (ROC), whereas WC improved the percentage of soil humin (HM). Thus, PRC enhanced SOC activity, whereas WC promoted SOC stability. Moreover, soil water, available nitrogen, phosphorus, and potassium contents increased in WC in 0–20-cm soil depths as compared to that in PRC, and the correlation between total GRSP (T-GRSP) and HM (r = 0.92) was higher than that between T-GRSP and ROC (r = 0.79). Therefore, T-GRSP is important in HM formation and maintaining stability of C pools. Overall, these results improve our understanding of the positive effect of organic waste coverage on soil internal C cycling and energy flow within an orchard ecosystem.     

Phosphorous accumulation and distribution of two ecotypes of Pilea sinofasciata grown in phosphorous-enriched soils

Water eutrophication and poultry manure require an efficacious remediation technology to decrease phosphorous (P) concentration. In this study, the P phytoremediation potential of a mining (ME) and nonmining ecotype (NME) of Pilea sinofasciata were analyzed by pot experiments employing different concentrations of P treatments (CK, P100, P200, P400, P800 and P1600) in tested soil. Growth, P accumulation and P-relevant enzyme activities of P. sinofasciata in ME and NME were assessed after 10 weeks’ plantation. The results showed that there was no significant difference between the shoot biomass of the ME and NME. Higher P concentration and accumulation were observed in the ME than NME for all treatments. Stem P concentration of the ME were 117%, 189%, 152%, 153%, 140% and 139% higher than the NME, and leaf P concentration were 122%, 146%, 138%, 144%, 137% and 113%. Maximum P uptake and phytoextraction was observed at P400 for the ME of P. sinofasciata. Elevated activities of acid phosphatase and phytase in roots were examined in P-enriched soil, and the ME presented higher activities compared with the NME. The results in this paper provide a theoretical basis for the use of ME of P. sinofasciata for phosphorus accumulators and suggest that ME of P. sinofasciata is a promising species for the excess P phytoextraction of P-enriched soils.     

溶解性有机质对镉在蔬菜中累积的影响

在赤红土中施用溶解性有机质（ＤＯＭ）——稻秆ＤＯＭ（稻秆发酵液中的有机质）后，生长在该土壤上的蔬菜体内镉含量，较不施稻秆ＤＯＭ的显著增加，加重了对蔬菜的危害程度     

羟基萘酚蓝在伪狂犬病病毒环介导等温扩增检测方法中的应用

伪狂犬病毒(Pseudorabies virus,PRV)传统诊断方法具有程序繁琐、周期长、成本高、特异性差等缺点,本实验建立了敏感、特异的PRV的环介导等温扩增(loop-mediated isothermal amplification,LAMP)检测方法,并在此基础上应用金属离子指示剂羟基萘酚蓝(hydroxy naphthol blue,HNB)进行反应结果判定.实验选取保守性较高的gB基因(glycoprotein B,糖蛋白gB)筛选引物,确定反应体系后,可在45 min内完成检测.LAMP方法特异性与PCR方法一致,敏感性是PCR方法的100倍,最低能够检测10个拷贝的目的基因.在HNB的应用试验中,发现LAMP反应体系中,HNB浓度为150 μmol/L时,阴阳性的颜色对比明显且反应的敏感性最高,可用于LAMP扩增产物的判断.临床样本的检测结果表明,PCR方法和LAMP方法的检出率一致.因此,本研究中所建立的LAMP方法是一种高度特异敏感的,可替代PCR方法的检测技术.     

四种常规方法提取伊利石有效钾的机制比较

采用化学分析、X射线衍射、中红外光声光谱以及原子力显微镜的方法,比较了0.2 mol L~(-1)四苯硼钠法、1 mol L~(-1)沸硝酸法、2 mol L~(-1)冷硝酸法和2 mol L~(-1)热盐酸法浸提伊利石中有效钾的机制。结果表明,四苯硼钠法浸提时,伊利石中钾素释放量达到全钾量的59.5%,且基本均通过层间交换反应予以释放,结构离子铁、铝和硅释放量极低;采用三种酸溶液浸提时,其钾素释放量仅占全钾量的1.53%~2.46%,通过层间交换反应释放的钾量占释放量的比例为88.4%~94.0%。四苯硼钠浸提时伊利石层间距扩大,产生次生过渡矿物,并形成富硅表层,但在伊利石表面无溶蚀特征;三种酸溶液浸提时伊利石结构无改变,但其结晶度降低,且表面有明显的溶蚀特征。因此,土壤矿物层间钾是作物可利用有效钾的主要来源,三种酸溶液浸提方法一方面低估了有效钾容量,另一方面提取了一部分不能为植物所利用的结构态钾,不适宜于用来评价伊利石及土壤有效钾库容量。     

Effects of nitrification inhibitors on denitrification of nitrate in soil

Summary The influence of 28 nitrification inhibitors on denitrification of nitrate in soil was studied by determining the effects of different amounts of each inhibitor on the amounts of nitrate lost and the amounts of nitrite, N₂O and N₂ produced when soil samples were incubated anaerobically after treatment with nitrate or with nitrate and mannitol. The inhibitors used included nitrapyrin (N-Serve), etridiazole (Dwell), potassium azide, 2-amino-4-chloro-6-methylpyrimidine (AM), sulfathiazole (ST), 4-amino-1,2,4-triazole(ATC),2,4-diamino-6-trichloromethyl-s-triazine (CL-1580), potassium ethylxanthate, guanylthiourea (ASU), 4-nitrobenzotrichloride, 4-mesylbenzotrichloride, sodium thiocarbonate (STC), phenylmercuric acetate (PMA), and dicyandiamide (DCD).Only one of the nitrification inhibitors studied (potassium azide) retarded denitrification when applied at the rate of 10 g g^–1 soil, and only two (potassium azide and 2,4-diamino-6-trichloromethyl-s-triazine) inhibited denitrification when applied at the rate of 50 g g^–1 soil. The other inhibitors either had no appreciable effect on denitrification, or enhanced denitrification, when applied at the rate of 10 or 50 g g^–1 soil, enhancement being most marked with 3-mercapto-1,2,4-triazole. Seven of the inhibitors (potassium azide, sulfathiazole, potassium ethylxanthate, sodium isopropylxanthate, 4-nitrobenzotrichloride, sodium thiocarbonate, and phenylmercuric acetate) retarded denitrification when applied at the rate of 50 g g^–1 soil to soil that had been amended with mannitol to promote microbial activity.Reports that nitrapyrin (N-Serve) and etridiazole (Dwell) inhibit denitrification when applied at rates as low as 0.5 g g^–1 soil could not be confirmed. No inhibition of denitrification was observed when these compounds were applied at the rate of 10 g g^–1 soil, and enhancement of denitrification was observed when they were applied at the rate of 50 or 100 g g^–1 soil.