不同水肥处理对夏玉米田土壤微生物特性的影响

以氮高效率型玉米品种(ZN99)为试验材料,研究了不同水肥处理对夏玉米田土壤微生物特性的影响.采用裂区设计,主区为灌水处理,设置了2个灌溉水平(玉米全生育期内灌水526和263 mm);副区为施肥处理,设置了3种肥料类型(无机肥U、有机肥M、有机无机混施UM)和2个施氮水平(N 100和200 kg·hm-2).结果表明:灌水量影响了肥料对土壤微生物生物量(碳、氮)和微生物多样性的调控,施有机肥只有在充足灌水条件下才能显著提高土壤微生物生物量碳(14.3%~33.6%)、微生物生物量氮(1.8~2.3倍)和丰富度.适量灌水、增施有机肥或有机无机配施可增加土壤中具有固氮能力的厚壁菌、γ-变形菌或α-变形菌的种类和相对数量.同一施氮量下,有机肥与无机肥对产量的影响差异不显著.从可持续生产角度考虑,适量灌水条件下,增施有机肥更有利于土壤微生物生物量及多样性的提高,增强土壤水肥供应能力.     

15N交叉标记有机与无机肥料氮的转化与残留

有机无机肥配施能够培肥土壤,改善土壤氮素供给,但目前有机无机肥配施主要集中在化肥氮的研究,忽略秸秆氮对化肥氮转化的影响。为了解秸秆还田对不同氮源转化和残留的影响,采用¹⁵N对尿素和水稻秸秆进行交叉标记,在两种不同肥力水稻土 (粘土矿物类型为1 ∶ 1型红黄泥和2 ∶ 1型紫潮泥) 进行水稻盆栽试验。设置对照(CK),单施尿素(¹⁵NU)、标记尿素与稻草配施(¹⁵NU-S) 和标记稻草与尿素配施(¹⁵NS-U)4个处理。结果表明,水稻吸收的氮素60%以上来自土壤氮,土壤氮素肥力相对较低的红黄泥较之紫潮泥对肥料氮的依赖更强;水稻生长期间微生物同化的尿素氮占标记底物的百分数红黄泥为1.8%-8.3%,紫潮泥为1.8%-19.2%;微生物同化的秸杆氮占标记底物的百分数红黄泥为1.7%-5.0%,紫潮泥为2.0%-6.2%。而粘土矿物固持的尿素氮占标记底物的百分数,红黄泥为0.3%-2.1%,紫潮泥为3.5%-18.7%;粘土矿物固持的秸杆氮红黄泥为0.2%-0.9%,紫潮泥为1.7%-5.0%。水稻成熟期尿素氮的残留率,红黄泥¹⁵NU处理、¹⁵NU+S分别为14.5%和17.0%,紫潮泥分别为16.9%和17.1%。秸秆氮的残留率分别为红黄泥38.8%、紫潮泥41.5%;有机无机肥配施提高了微生物同化化肥氮的能力,降低了粘土矿物晶格固持化肥氮的水平。有机无机配施提高了化肥氮利用率同时,提高了有机形态氮残留,降低了无机形态氮(矿质氮+固定态铵)的残留。     

长期施肥黄土旱塬农田土壤-微生物-植物系统碳氮磷生态化学计量特征

探讨长期不同施肥制度对农田土壤、植物生态系统的碳(C)、氮(N)、磷(P)含量及其生态化学计量比的影响,可为揭示该系统能量平衡和养分循环,实现农业生态系统元素平衡及可持续发展提供参考意义。以位于黄土高原半干旱地区的长武国家黄土高原农业生态实验站长期施肥试验为研究对象,选取不施肥(CK)、单施氮肥(N)、单施磷肥(P)、施氮磷肥(NP)、单施有机肥(M)、氮肥配施有机肥(NM)、磷肥配施有机肥(PM)、氮磷肥配施有机肥(NPM)8个处理,分析了黄土旱塬典型农田土壤-微生物-植物生态系统中C、N、P含量及其生态化学计量变化规律。研究结果表明:1)长期单施有机肥和化肥配施有机肥处理可显著提高土壤和有机质C、N、P含量。2)氮、磷肥的输入显著降低了土壤和小麦C∶N、N∶P,施P显著降低了有机态C∶P和小麦C∶P;有机肥配施对微生物生物量和小麦C∶N∶P的影响更为明显。3)长期有机肥配施条件下土壤养分和小麦化学计量比存在较强的相关关系。微生物生物量碳与有机C、N、P呈显著正相关,土壤微生物生物量氮与土壤N、P总量呈显著正相关,微生物生物量磷与土壤C、N、P总量含量呈显著负相关;植株碳含量与微生物...     

有机无机肥配施对旱地冬小麦产量和硝态氮残留淋失的影响

针对渭北旱塬氮肥施用不合理的问题,通过不同氮肥用量(0、75、150、225、300 kg N·hm^-2)与有机肥(30 t·hm^-2)配施,明确渭北旱塬麦田配施有机肥条件下合理的氮肥用量以及配施有机肥的减氮增产作用和对硝态氮残留淋失的影响.结果表明: 与单施化肥处理相比,有机无机肥配施可以在减少27.1%的氮肥用量情况下,提高14.7%的小麦籽粒产量,其中,施氮量150 kg·hm^-2配施有机肥处理的产量最高;有机无机肥配施可以促进小麦籽粒氮素吸收,氮肥利用率提高20.2%,尤其当氮肥用量为150 kg·hm^-2时,氮肥利用率达到最高值(42.0%);配施有机肥还能减少氮肥当季残留量和小麦生育期硝态氮向深层土壤淋溶,降低夏闲期淋失层硝态氮的淋失比例,当施氮量低于115 kg·hm^-2时,配施有机肥可以降低夏闲期硝态氮淋失量.基于本研究,推荐渭北旱塬在配施有机肥30 t·hm^-2的基础上,氮肥用量150 kg·hm^-2左右可实现小麦高产,提高氮肥利用率,防止氮肥过量残留.     

秸秆生物有机肥的施用对土壤供氮能力的影响

通过盆栽试验研究了秸秆生物有机肥的施用对土壤供氮能力的影响。结果表明,与原始秸秆相比,秸秆生物有以与尿素配合施用能明显提高土壤生物量碳,氮的含量,增幅约为3－4倍;土壤微生物量氮与土壤的供氮能力关系非常密切,前期发生强烈的微生物增殖过程,则中后期必会发生无机氮释放过程,这对作物的生长发育极为重要。同时提高了肥料氮利用率,揭示了秸秆生物有机肥配施无机氮肥改善土壤供氮能力的机理。     

有机无机肥分次配施对嘎啦苹果生长、15N-尿素吸收利用及损失的影响

以15年生嘎啦苹果/平邑甜茶为试材,采用¹⁵N同位素示踪技术,研究有机无机肥分次配施对嘎啦苹果/平邑甜茶生长、¹⁵N-尿素吸收利用及损失的影响.结果表明: 与不施有机肥相比,有机无机肥配施显著提高了植株根冠比、叶绿素含量、单株叶片总氮量和单果质量,且有机无机肥分次配施的效果要优于有机无机肥一次性配施.有机无机肥配施提高了各器官对氮的吸收征调能力(Ndff值),其中有机无机肥分次配施的效果更显著;而不同施肥处理各器官的Ndff值均表现为果实最高,其次是叶片、一年生枝、细根、粗根和多年生枝,中心干最低.有机无机肥分次配施植株总氮量和¹⁵N肥料利用率分别为395.39 g和28.4%,显著高于有机无机肥一次性配施处理(342.77 g和21.1%)和不施有机肥处理(296.41 g和14.6%),而¹⁵N损失率为51.3%,显著低于有机无机肥一次性配施处理(57.5%)和不施有机肥处理(60.6%).     

有机无机肥分次配施对嘎啦苹果生长、15N-尿素吸收利用及损失的影响

以15年生嘎啦苹果/平邑甜茶为试材,采用¹⁵N同位素示踪技术,研究有机无机肥分次配施对嘎啦苹果/平邑甜茶生长、¹⁵N-尿素吸收利用及损失的影响.结果表明: 与不施有机肥相比,有机无机肥配施显著提高了植株根冠比、叶绿素含量、单株叶片总氮量和单果质量,且有机无机肥分次配施的效果要优于有机无机肥一次性配施.有机无机肥配施提高了各器官对氮的吸收征调能力(Ndff值),其中有机无机肥分次配施的效果更显著;而不同施肥处理各器官的Ndff值均表现为果实最高,其次是叶片、一年生枝、细根、粗根和多年生枝,中心干最低.有机无机肥分次配施植株总氮量和¹⁵N肥料利用率分别为395.39 g和28.4%,显著高于有机无机肥一次性配施处理(342.77 g和21.1%)和不施有机肥处理(296.41 g和14.6%),而¹⁵N损失率为51.3%,显著低于有机无机肥一次性配施处理(57.5%)和不施有机肥处理(60.6%).     

长期施用有机物料下黑土氮素有效性及其与作物产量的关系

利用长期定位施肥试验,于2011年采样研究长期施用不同有机物料(秸秆、有机肥)对东北黑土氮素有效性的影响,并分析氮供应与作物生物量及产量的关系.结果表明:化肥配施有机肥、化肥配施低量秸秆均可显著提高黑土农田土壤无机氮和硝态氮含量,进而提高作物产量;尽管化肥配施高量秸秆提高了土壤氮矿化速率,但可能由于硝态氮淋溶或者其他形式的氮素损失或转化,与化肥配施低量秸秆处理相比,化肥配施高量秸秆下土壤无机氮量并没有增加.可见,适量施用有机物料对提高土壤氮素有效性、提高作物产量及保护环境具有重要意义.     

不同有机无机肥配施比例对红壤旱地花生产量、土壤速效养分和生物学性质的影响

大田条件下,研究了不同有机无机配施比例对红壤花生旱地可培养微生物数量、土壤主要酶活性、土壤速效养分及花生产量的影响。结果表明:(1)有机肥配施花生产量显著高于其他处理,有机肥比例为40%时,荚果产量、籽仁产量、单株结果数及百粒重效果增加最明显,分别较常规施肥提高20.14%、26.92%、27.87%和7.08%;(2)有机肥配施可以显著提高土壤速效养分含量,40%有机肥在花生生育期结束后能显著提高土壤碱解氮、有效磷、速效钾含量,与常规施肥相比,分别增加了17.89%、22.96%、12.57%;(3)土壤中细菌、真菌、放线菌数量随着有机肥配施比例增高而增加;40%有机肥配施比常规施肥处理的细菌、真菌、放线菌数量全生育期平均值分别提高:71.62%、40.42%、43.94%。(4)施肥可以显著提高土壤脲酶、酸性磷酸酶、蔗糖转化酶活性,其中有机无机中量配施(40%有机肥)、高量配施(60%、80%有机肥)显著高于其他处理,低量有机肥配施(20%有机肥)接近于常规施肥水平。综上表明,在等量N、P、K养分条件下,配施40%猪粪N更有利于红壤地区土壤肥力及产量的改善。     

氮硅添加对青藏高原高寒草甸土壤氮矿化的影响

为了解全球气候变化背景下氮沉降对土壤氮矿化的影响及硅添加对土壤氮矿化的促进作用, 该试验设置不同浓度的氮肥单独添加(0、20、40、60 g·m ^-2, 分别为对照CK、N20、N40、N60)以及与硅肥配施(硅酸4 g·m ^-2, Si4), 测定不同处理下0-20、20-40、40-60 cm土层土壤硝态氮含量、铵态氮含量、净硝化速率、净氨化速率以及净矿化速率。结果显示: (1)单独添加氮肥, 各土层土壤硝态氮和铵态氮含量均随处理浓度的增加而增加, 0-20 cm土层N20、N40、N60处理下土壤硝态氮和铵态氮分别较CK增加63.48%、126.04%、247.03%和80.66%、152.52%、244.56%; 随着土层深度增加, 土壤硝态氮、铵态氮含量均有下降, 20-40、40-60 cm土层较0-20 cm土层硝态氮含量分别平均减少53.90%、76.05%, 铵态氮含量分别平均减少48.62%、68.23%。(2)土壤净硝化速率、净氨化速率及净矿化速率随着氮肥浓度增加均呈上升趋势。相同氮肥添加浓度下, 土壤净硝化速率、净氨化速率和净矿化速率随着土层深度增加逐渐下降(除CK外)。(3)与单独添加氮肥比较, 氮硅肥配施, 土壤氮含量有显著提高, 在0-20 cm土层硝态氮和铵态氮较CK分别增加98.78%、192.62%、330.16%和99.96%、195.82%、306.32%, 20-40、40-60 cm土层也有类似趋势。同时, 氮硅配施促进了土壤氮矿化行为, 在0-20 cm土层, N60Si4处理下的土壤净硝化速率、净氨化速率较单独施氮时分别增加35.88%、27.41%。以上结果表明, 与单独氮肥添加相比, 氮硅配施不但能提高土壤氮含量, 而且能促进土壤氮的矿化作用, 对大气氮沉降有一定的缓解作用。     

土壤动物与N素循环及对N沉降的响应

以主要的生态过程之一——N循环为对象,论述了土壤动物不仅对凋落物的分解有重要影响,而且在N素矿化和植物对N的吸收过程中也起着重要作用。同时,日益严重的全球变化问题之一——N沉降对土壤动物的多样性及其在生态系统中的功能构成了极大的威胁。另还对土壤动物与N循环研究的方法、土壤动物在N循环过程中的作用机制、热带地区的需求及N沉降下土壤动物的响应作了探讨,并提出,开展大尺度的专类研究及长期定位研究成为下一步研究的需要。     

Electron transport-linked nitrous oxide synthesis and reduction by Paracoccusdenitrificans monitored with an electrode

The nitrous oxide reductase activity of $\text{Paracoccus}\text{denitrificans}$ can be conveniently measured using an electrochemical method for determining N₂O. Introduction of this procedure has shown that (i) N₂O reductase activity is reversibly inhibited by oxygen; (ii) antimycin strongly inhibits electron flow to N₂O and that the inhibition is bypassed by tetramethyl-p-phenylenediamine; (iii) ascorbate plus tetramethyl-p-phenylenediamine, presumably by donating electrons to cytochrome c, is an effective reductant for nitrous oxide reductase; (iv) in the presence of the nitrous oxide reductase inhibitor, acetylene, N₂O is promptly produced from nitrite, consistent with the product of nitrite reductase being N₂O.     

Yield and crop parameters of wetland rice as influenced by soil and fertilizer nitrogen

Summary The behavior of soil N, fertilizer N and plant N was studied in a greenhouse experiment with 2 plant densities of rice (IR 36) under flooded conditions. Increasing plant density from 25 hills m² to 50 hills m² increased tiller number and panicle number but had no influence on grain yield. The yield of grain was linearly related to N content of the above ground dry matter at harvest (r²=.96) and thus the effect of manipulating the N supply on yield was directly related to N uptake.Mixing of (NH₄)₂SO₄ with the soil volume before transplanting resulted in increases in N in the aboveground dry matter equal to 87% of the applied N. When (NH₄)₂SO₄ was broadcast into the flood water at 4 stages of growth beginning 25 DAT, the corresponding increase was 77% of the applied N. When (NH₄)₂SO₄ was split between shallow mixing before transplanting and a broadcast application of 32 DAT, the corresponding increase was 42%. Thus several applications of fertilizer N increased grain production per unit of applied N.Inorganic N extractable by KCl was a useful but not an infailible guide to the behavior of the soil and fertilizer inorganic N.     

Allometry and morphometrics of clypeal membrane size and shape in Nicrophorus (Coleoptera: Silphidae)

Contests between same‐sex opponents over resources necessary for reproduction, as well interactions used to discern mate quality, often involve exaggerated traits wherein large individuals have disproportionately larger traits. This positive allometric scaling of weapons or signals facilitates communication during social interactions by accentuating body size differences between individuals. Typically, males carry these exaggerated traits, as males must compete over limited female gametes. However, in Nicrophorus beetles both males and females engage in physical contests over the vertebrate carcasses they need to provision and raise offspring. Male and female Nicrophorus beetles have extended clypeal membranes directly above their mandibles, which could serve as signals. We investigated the scaling relationships between clypeal membrane size and shape and body size for five species of North American burying beetle to determine whether clypeal membranes contain exaggerated body size information. We found that clypeal membranes for both sexes of all species scaled positively with body size (slope > 1). Three of the five species also displayed sexual dimorphism in aspects of clypeal membrane size and shape allometry despite lack of dimorphism in body size. In two dimorphic species, small male clypeal membranes were statistically indistinguishable from the female form. We conclude that colored clypeal membranes in Nicrophorus beetles do contain exaggerated body size information. Observed patterns of dimorphism suggest that males sometimes experience stronger selection on marking size and shape, which might be explained by life history differences among species.     

EUF-N fractions in different soils during a vegetation period in pot and field experiments

Summary Mobilization of soil-borne N, N fertilization and N removal by crops influence EUF-NO₃-N contents as well as EUF-N_org contents in the course of a vegetation period. N mobilization alone (no N fertilization) increases the EUF-N_org contents only temporarily (mainly in May and July), while in December they are almost the same as in March (Table 1). The EUF-NO₃ contents, on the contrary, increase during the vegetation period, so that an increment in NO₃ is registered in unplanted pots in December. This increment is larger the higher the EUF-N_org contents are in March (Table 2).N fertilization increases the contents of both EUF-N_org and EUF-NO₃, so that there is an increment in EUF-N_org as well as EUF-NO₃ in December (Table 2). This finding also applies to field experiments under fallow (Figs. 4 and 5). However, in contrast to the pot experiment, the EUF-N contents in the field experiment were only temporarily increased by N mobilization alone. This means that N immobilization had taken place which had not been observed in the pot experiment under stable moisture conditions (Fig. 4 and Table 1).A close correlation between hot-water-soluble N contents and EUF-N_org is found only under uniform management conditions (uniform N-fertilizer rates). Depending on the time of sampling different regression equations are, however, obtained because of changes in EUF-N_org due to N mobilization, whereas the hot-water-soluble N contents hardly show any variations during the vegetation period (Fig. 6 and Table 3).     

冬玉米对氮肥的吸收利用和需求

在不同施氮量下 ,研究了冬玉米对氮肥的吸收利用 ,结果表明 :(1 )冬玉米地上各部分中氮的累积随着用氮量的增加而增加 ,花丝期前的吸收量均多于后期 ,但高氮区的前期吸氮比大于低氮区 ;(2 )营养体氮的转移率随施氮量的增加而降低 ,但绝对量依然是高氮处理大于低氮处理 ,其中雄穗的转移率最高 ,叶的转移量最大 ;(3 )氮肥利用率随施氮量的增加而提高 ,但氮的生产力下降。根据试验结果 ,在肥力好的土地上种植冬玉米以 1 80～ 2 70 kg N/hm2比较适宜     

Distribution and remobilization of symbiotically fixed nitrogen in soybean (Glycine max)

Partitioning of nitrogen by soybeans ( Glycine max L. Merr. cv. Hodgson) grown in natural conditions was studied by successive exposures of root systems to ¹⁵N₂ and periodical measurements of ¹⁵N distribution. Nitrogen derived from the atmosphere was mainly found in the aerial parts of the plants, and the stage of development exerted a strong influence on the initial ¹⁵N distribution (measured one week after incorporation). Until day 69 after sowing, leaf blades contained 47 to 57% of the fixed N. After that, reproductive structures attracted increasing proportions, 10 to 60% between days 69 and 92. Around day 82, stems and petioles stored up to 30% of the newly fixed N. During pod development and pod filling and until maturity, fixed N was remobilized from vegetative tissues and pod walls to seeds. These transfers first concerned the newly incorporated N, but at maturity 80 to 90% of the total was recovered in the seeds. The high mobility of N originating from the atmosphere as compared to that coming from the soil (vegetative tissues exported only 50% of their total N) seems to indicate that fixed N was at least partially integrated in a special pool. This was certainly the case at the later stage of N₂ fixation, when a large portion of fixed N accumulated in the stems and petioles, probably in the form of storage compounds such as ureides for later transfer to the developing seeds. Further research is needed in order to investigate the nature and role of this pool in the nitrogen nutrition of soybeans.     

Localization of Cu and heme a on cytochrome c oxidase polypeptides.

After mild dissociation of cytochrome $\text{c}$ oxidase protomers, and polyacrylamide gel electrophoresis, copper was found predominantly in polypeptides of Bands V (m.w. 12,100) and VII (m.w. 3,400), and heme a predominantly in polypeptides of Bands I (m.w. 35,300) and II (m.w. 21,000). Some copper was found in Band II – III, and heme a in Band V.     

Transformations in soil and availability to plants of15N applied as inorganic fertilizer and legume residues

Summary A pot experiment was conducted to study the transformations of organic and inorganic N in soil and its availability to maize plants. Inorganic N was in the form of¹⁵N labelled ammonium sulphate (As) and¹⁵N labelledSesbania aculeata (Sa), a legume, was used as organic N source. Plants utilized 20% of the N applied as As; presence of Sa reduced the uptake to 14%. Only 5% of the Sa-N was taken up by the plants and As had no effect on the availability of N from Sa. Losses of N from As were found to be 40% which were reduced to 20% in presence of Sa. Losses of N were also observed from Sa which increased in the presence of As. Application of As had no effect on the availability of soil or Sa-N. However, more As-N was transported into microbial biomass and humus components in the presence of Sa.Plants derived almost equal amounts of N from different sourcesi.e., soil, Sa and As. However, more As-N was transported into the shoots whereas the major portion of nitrogen in the roots was derived from Sa.