基质和水氮处理对假茉莉水分利用率及生物量的影响

假茉莉(Clerodendrum inerme)是一种重要的半红树植物,是海岛及沿海防护林的重要组成部分,淡水、土壤是海岛植被恢复的重要生态因子。为了总结出最适合假茉莉生长发育的土壤及水肥条件,该文设置了不同基质、浇水频率及氮素处理,对不同处理下假茉莉的生物量及水分利用率进行了研究。结果表明:(1)在不同的基质中,含泥炭的混合基质对于假茉莉生物量的积累具有突出作用,S_4基质(珊瑚砂∶泥炭∶红壤土∶椰糠=12∶2∶3∶3)地下生物量(平方根)为1.66 g,极显著高于不含泥炭的基质,S_1基质(珊瑚砂∶泥炭=3∶2)总生物量(平方根)为4.54 g,极显著高于其他基质。(2)中、低浇水频率下的总生物量分别为4.02、4.23 g,极显著高于高浇水频率下的3.46 g,而不同氮素处理间生物量的差异并不显著,这表明假茉莉在中、低浇水频率,少施氮肥或不施氮肥的条件下仍然能够获得较高的生物量。(3)对于水分利用率而言,原珊瑚砂基质保水性较差,水分利用率较低,而混合基质在中、低浇水频率下水分利用率均有不同显著程度的提高。综上结果显示,假茉莉在含泥炭基质,中、低浇水频率,无氮或低氮条件下能够较好生长。     

不同基质配比对毛桃营养生长的影响

以毛桃幼苗为试材,研究不同基质配比对其无土栽培生长的影响。结果表明,毛桃幼苗栽植于蛭石与珍珠岩按1:1混合的基质中,植株株高、茎粗、生物量均最高,而在粘土与沙土混合基质中生长最差。本试验结果可供开展桃树无土栽培参考。     

AM真菌对煤矿沉陷区不同复合基质上 紫花苜蓿生长和生理特性的影响

该研究采用盆栽试验法,以紫花苜蓿(Medicago sativa)为材料,将煤矸石(CG)、粉煤灰(FA)和沙土(SS)按不同质量配比设置T1(CG∶FA∶SS=75%∶25%∶0%)、T2(CG∶FA∶SS=60%∶25%∶15%)、T3(CG∶FA∶SS=45%∶25%∶30%)、T4(CG∶FA∶SS=30%∶25%∶45%)四组混合基质以模拟,并以T5(CG∶FA∶SS=0%∶0%∶100%)为对照,AM真菌选用摩西斗管囊霉(F.m)和幼套近明球囊霉(C.e),通过单接菌和混合接菌,探索其对紫花苜蓿根系的侵染率、幼苗生长、抗氧化物酶活性和渗透调节物质变化的影响。结果表明:(1)在五组基质上,接种AM真菌显著提高了紫花苜蓿根系的菌根侵染率和菌根依赖性,且基质T4接种F.m+C.e[F.m∶C.e=1∶1(W/W)]的值最大(64.31%和86.24%)。(2)接种AM真菌不同程度提高了紫花苜蓿株高、基径、叶面积和生物量,且混合接菌的效果优于单接菌。(3)基质中填加过量煤矿废弃物抑制了植株根系的生长,接种AM真菌后显著提高了紫花苜蓿总根长、根表面积、根体积,降低了根平均直径。(4)不同接菌处理的紫花苜蓿叶片POD、SOD、CAT活性以及可溶性糖、可溶性蛋白含量总体表现为F.m+C.eC.eF.mnon-AMF,且接种F.m+C.e的增长幅度最大。研究表明煤矿废弃物复合逆境抑制紫花苜蓿的生长,接种AM真菌显著提高了幼苗生长、抗氧化物酶活性和渗透调节物质,提高了植物抗逆性能,且以基质T4接种F.m+C.e的效果最佳。     

洱海底泥特性对七种沉水植物生长的影响

为研究洱海底泥特性对沉水植物生长的影响,采用不同比例洱海底泥与湖岸土壤掺混形成五种基质,并分别移栽苦草、黑藻、微齿眼子菜、马来眼子菜、光叶眼子菜、穿叶眼子菜和狐尾藻,进行为期70d的室外生长实验,结果表明不同基质对几种植物的影响具种间差异。（1）在基质为50%深层底泥+50%湖岸土壤（碳、氮、磷含量分别为31.59、0.334和0.095 mg/g）时,苦草、马来眼子菜和光叶眼子菜的株高最大;基质为100%深层底泥（碳、氮、磷含量分别为37.88、0.803和0.149 mg/g）时,黑藻、微齿眼子菜、穿叶眼子菜和狐尾藻的株高最大;（2）基质为100%深层底泥时,苦草、黑藻、微齿眼子菜、马来眼子菜和光叶眼子菜生物量增加最多且相对生长速率最大;基质为100%浅层底泥（碳、氮、磷含量分别为77.37、5.691和0.136 mg/g）时,穿叶眼子菜生物量增加最多,相对生长速率最大;狐尾藻在基质为50%浅层底泥+50%深层底泥（碳、氮、磷含量分别为49.27、2.005和0.131 mg/g）时生物量增加最多,相对生长速率最大;（3）基质为100%湖岸土壤（碳、氮、磷含量分别为22.06、0.327和0.231 mg/g）时,7种沉水植物均生长缓慢,生物量增加较少。综上所述,中营养底泥（碳、氮、磷含量分别为31.59-49.27、0.334-2.005和0.095-0.131 mg/g）更适合沉水植物生长,底泥中过高或过低营养都不利于沉水植物生长。     

钻井废弃物配合外源有机物质对风沙土理化性质及菠菜生长的影响

采用室内盆栽试验研究水基废弃钻井泥浆、岩屑等钻井废弃物配合腐植酸、木本泥炭等外源有机物质在风沙土中的施用效果,并分析其对菠菜生长的影响,以期为钻井废弃物资源化利用和风沙土改良提供参考。共设3组室内盆栽试验:基础组共4个处理,以风沙土为对照(CK),将风沙土与岩屑按质量比1∶1混合后分别添加0、2%、4%含量水基废弃钻井泥浆(干基);基础组处理分别添加1%腐植酸、1%腐植酸+3%木本泥炭混合物,作为腐植酸组和木本泥炭组。结果表明: 基础组中,与CK相比,施用钻井废弃物显著增加了土壤有机质含量,pH和电导率上升,2%含量水基废弃钻井泥浆显著促进菠菜生长。腐植酸和木本泥炭使土壤pH降低,有机质含量显著增加,电导率上升,腐植酸组株高、总叶面积、鲜重、干重等植物生长指标均高于基础组中对应处理,混合添加腐植酸和木本泥炭后对植物生长促进效果不显著。最佳处理为腐植酸组添加2%含量水基废弃钻井泥浆,土壤有机质含量为13.1 g·kg^-1,播种40 d后菠菜株高、总叶面积、鲜重和干重分别比CK显著增加49.7%、93.4%、83.3%、34.6%。钻井废弃物配合有机物质施用可以显著增加土壤有机质含量,促进菠菜生长,风沙土+岩屑+水基废弃钻井泥浆(2%)+腐植酸(1%)是最佳组合模式。     

施肥对金盏菊生长、开花及养分吸收的影响

研究了氮、磷、钾不同施肥处理对金盏菊（Calendula officinalisL.）生长、开花、干物质积累量及养分吸收的影响。结果表明：推荐施肥[N-P2O5-K2O：（0.4-0.2-0.3）g/kg]能有效促进金盏菊的生长及花朵开放,其中干物质积累量和总花朵数,分别比不施肥处理增加了264.3%和323.1%,比习惯施肥增加了16.0%和25.0%;不施肥、习惯施肥和推荐施肥三者干物质日积累量高峰均出现在移栽后29～35 d,分别为0.15、0.43、0.42 g/d;各处理氮、磷、钾吸收量之间均存在显著差异,推荐施肥处理N、P、K养分累积量分别为0.33、0.04、0.39 g/株,分别是不施肥处理的6.93倍、3.94倍和3.61倍,为习惯施肥的1.49倍、1.35倍和1.24倍,各处理金盏菊对N、P、K养分吸收比例变幅为1∶（0.13～0.24）∶（1.20～2.30）,平均比例为1∶0.17∶1.65。     

不同农林废弃物混合基质对崖柏扦插育苗的影响

为研究不同农林废弃物混合基质对崖柏扦插育苗的影响,筛选可替代草炭、成本低廉的环保型育苗基质,配制草炭+蛭石+珍珠岩(T₁)、食用菌菌渣+蛭石+珍珠岩(T₂)、炭化稻壳+蛭石+珍珠岩(T₃)、食用菌菌渣+炉渣+锯末(T₄)和炭化稻壳+食用菌菌渣+炉渣(T₅)5种混合基质,采用随机区组试验设计,综合评价不同混合基质的优劣。结果表明：T₃容重最低,其次是T₂,二者与其他混合基质差异显著;T₂的非毛管孔隙度显著大于T₁,毛管孔隙度低于T₁,总孔隙度低于T₃;T₂的全氮、全磷、全钾、碱解氮、有效磷、基质含水量和pH最高,且与其他混合基质的大多数化学指标差异显著。不同混合基质的插穗生根率和生长发育指标的隶属函数值表现为T₂>T₃>T₁>T₅     

丛枝菌根真菌对豆科作物生长和生物固氮及磷素吸收的影响

本研究以大豆为材料,采用盆栽和田间试验,探讨丛枝菌根真菌(AMF)对豆科作物生长的影响。盆栽试验设置了接种(+AMF)和不接种(-AMF)丛枝菌根真菌处理,田间试验设置了AMF菌丝非限制与限制处理。盆栽试验结果表明: 接种AMF显著提高了大豆地上部生物量(16.5%)和大豆根瘤数(131.4%),地上部磷含量、磷吸收量、氮含量和氮吸收量也显著增加。田间试验中,AMF菌丝非限制处理下大豆的地上部生物量、根系生物量、根瘤数量分别比限制处理下显著提高了123.6%、61.5%和212.5%,地上部和根系磷吸收量、氮含量、氮吸收量均显著高于限制处理,大豆根际土壤速效氮和有效磷含量也均显著高于限制处理。本研究可为进一步认识豆科作物与AMF的共生关系及田间磷肥高效利用提供理论参考。     

两种配比的控释肥对杭白菊养分吸收和生长效应的影响

利用盆栽试验研究两种不同配比的控释复合肥CRFA（4%树脂包膜,N∶P₂O₅∶K₂O为14∶14∶14）和CRFB（4%树脂包膜,N∶P₂O₅∶K₂O为20∶8∶10）及普通复合肥CCF（N∶P₂O₅∶K₂O为15∶15∶15）对杭白菊营养吸收和生长效应的影响.结果表明：普通复合肥CCF1（每盆6 g氮素用量的CCF）和CCF2（每盆3 g氮素用量的CCF）施入土壤后30 d,土壤中碱解氮、有效磷、有效钾含量分别为163.29和145.26 mg·kg^-1、180.39和163.13 mg·kg^-1、300.08 和213.15 mg·kg^-1,而后迅速下降.控释复合肥养分释放较慢,其土壤碱解氮含量在施肥后缓慢升高,在施肥后60 d达到高峰,此时CRFA1（每盆6 g氮素用量的CRFA）、CRFB1（每盆6 g氮素用量的CRFB）、CRFA2（每盆3 g氮素用量的CRFA）、CRFB2（每盆3 g氮素用量的CRFB）分别为129.51、138.65、118.36、126.31 mg·kg^-1;CRFA1和CRFA2处理土壤有效磷含量与CCF处理变化趋势基本一致,施肥后30 d分别达到169.54和133.46 mg·kg^-1,CRFB1和CRFB2处理在施肥后60 d左右达到释放高峰,含量分别为137.13和84.68 mg·kg^-1,然后缓慢下降.两种不同养分配比的控释复合肥处理植株叶面积、叶面积系数、分枝数、开花率、每株花数、鲜花直径等农艺性状均明显优于等氮素用量的普通复合肥处理,其中CRFB控释效果优于CRFA,其更符合杭白菊对养分的需求,且在本试验条件下,CRFB2处理产量最高.     

短期氮沉降对纳帕海高寒退化疏花早熟禾草甸土壤呼吸干湿季变化的影响

为探究氮沉降增加背景下高寒草甸土壤呼吸干湿季变化及其与环境因子的耦合关系,选择纳帕海典型退化草甸疏花早熟禾群落,设置对照(0 g·m^-2·a^-1)、低氮(5 g·m^-2·a^-1)、中氮(10 g·m^-2·a^-1)和高氮(15 g·m^-2·a^-1)4个水平的氮沉降模拟试验,分析氮沉降引起的地上生物量、植物多样性及土壤理化性质变化对土壤呼吸的影响。结果表明：不同氮沉降处理均显著促进草甸土壤呼吸,干季和湿季土壤呼吸速率相较于对照分别增加了21.9%～53.9%和27.3%～51.2%,且在中氮处理下增幅最大。氮沉降显著提升草甸地上生物量(增幅达52.2%～66.4%);植物多样性随氮添加总体呈降低趋势,湿季最大降幅(13.5%～24.2%)出现在高氮处理。氮沉降显著增加土壤铵态氮、有机质、微生物生物量碳氮、温度和含水率(增幅为14.3%～333.5%),氮沉降显著降低土壤pH(减幅达9.0%～34.6%)。结构方程表明...     

土壤水分对两个冬小麦品种产量和竞争能力的影响

研究了黄土塬区两个旱作冬小麦品种(长武135和平凉40,前者是后者的换代品种)在不同土壤水分条件下竞争能力和产量形成的关系。研究设2种土壤水分条件(土壤含水量为田间最大持水量的75%～80%和40%～45%),采用生态替代法设计了同一播种密度的6个播种比例组合的盆栽试验。低水分单播条件下,长武135具有较高的产量(长武135为27.59g/pot,平凉40为24.91g/pot),而混播条件下平凉40在产量和相对产量上较长武135品种具有明显的竞争优势。高水分条件下,平凉40产量随播种比例的减小下降较快(长武135产量曲线斜率35.468,平凉40为36.237)。平凉40低水分单播时花后干物质积累量较少(长武135为0.67g/pot,平凉40为0.55g/pot),而混播时较多(长武135各比例均值0.58g/pot,平凉40为0.71g/pot),导致了平凉40品种单播时产量较低和混播时产量较高。平凉40地下生物量显著大于长武135(高水分条件下,长武135为10.03g/pot、平凉40为11.51g/pot;低水分条件下二者分别为8.41g/pot和10.69g/pot),且耗水量大(高水分条件下平凉40多耗水2.72kg/pot,低水分条件下多耗0.98kg/pot),而耗水量/地下生物量的比值平凉40低于长武135,从而平凉40品种单位根量消耗的水分低于长武135。总之,在两个生长属性接近的冬小麦品种中,老品种以较大的根系生物量赢得了较高的竞争能力,消耗了较多的水分,而新品种虽然根系生物量较低,耗水量较少,但籽粒产量却较高。亦即,小麦新品种籽粒产量的提高是与根系的减少和对水资源竞争能力的下降相伴随的。     

Effect of inoculum rate on mycorrhizal growth responses in pot-grown onion and clover

Summary White clover and onion plants were grown from seed in pots of sandy loam above pads of mycorrhizal inoculum soil at 0.17–1.40 g/pot (equivalent to 250–2000 kg/ha) and harvested on four occasions. In sterilized soil increasing inoculum rates increased the onset and size of the mycorrhizal growth response of white clover. In unsterilized soil the indigenous mycorrhizal fungi greatly stimulated growth of both clover and onion. Nevertheless, all mycorrhizal inoculum rates further stimulated shoot growth in onion (92% increase over all harvests), while only the highest inoculum rate significantly stimulated clover growth (52% increase).     

可降解螯合剂对镉胁迫下籽粒苋根系形态及生理生化特征的影响

采用盆栽试验研究了可降解螯合剂EDDS和NTA对镉胁迫下籽粒苋(Amaranthus hybridus L.)根系形态及生理生化特征的影响。结果表明:当螯合剂施入10 mg/kg的镉污染土壤后,籽粒苋根系生物量和总长等根系形态指标与对照无显著差异,过氧化物酶(POD)、过氧化氢酶(CAT)活性、谷胱甘肽(GSH)和可溶性蛋白含量显著上升。当螯合剂施入100 mg/kg的镉污染土壤后,籽粒苋根系生物量、总长、表面积、体积及侧根数比对照显著减少了12.30%—23.98%、17.01%—24.90%、41.87%—57.93%、16.46%—32.94%和23.48%—53.35%;EDDS的施入使籽粒苋根系POD、CAT活性、GSH和可溶性蛋白含量显著升高;而NTA施入后,根系中的POD活性比对照降低了4.12%—35.95%,并且CAT活性和可溶性蛋白含量在2 mmol/kg NTA处理下分别显著降低了14.66%—15.79%和26.81%—30.48%;EDDS和NTA施入后,GSH含量比对照显著升高了14.73%—65.65%和28.05%—84.10%。当镉处理浓度分别为10 mg/kg和100 mg/kg时,螯合剂的施入显著增强了籽粒苋根系对镉的吸收,比对照分别增加了40.76%—103.10%和15.03%—49.49%。因此,EDDS和NTA施入镉污染土壤后,通过影响籽粒苋根系形态和生理生化过程以响应重金属镉的胁迫。     

Fine root dynamics and trace gas fluxes in two lowland tropical forest soils

Fine root dynamics have the potential to contribute significantly to ecosystem‐scale biogeochemical cycling, including the production and emission of greenhouse gases. This is particularly true in tropical forests which are often characterized as having large fine root biomass and rapid rates of root production and decomposition. We examined patterns in fine root dynamics on two soil types in a lowland moist Amazonian forest, and determined the effect of root decay on rates of C and N trace gas fluxes. Root production averaged 229 (±35) and 153 (±27) g m^?2 yr^?1 for years 1 and 2 of the study, respectively, and did not vary significantly with soil texture. Root decay was sensitive to soil texture with faster rates in the clay soil (k=?0.96 year^?1) than in the sandy loam soil (k=?0.61 year^?1), leading to greater standing stocks of dead roots in the sandy loam. Rates of nitrous oxide (N₂O) emissions were significantly greater in the clay soil (13±1 ng N cm^?2 h^?1) than in the sandy loam (1.4±0.2 ng N cm^?2 h^?1). Root mortality and decay following trenching doubled rates of N₂O emissions in the clay and tripled them in sandy loam over a 1‐year period. Trenching also increased nitric oxide fluxes, which were greater in the sandy loam than in the clay. We used trenching (clay only) and a mass balance approach to estimate the root contribution to soil respiration. In clay soil root respiration was 264–380 g C m^?2 yr^?1, accounting for 24% to 35% of the total soil CO₂ efflux. Estimates were similar using both approaches. In sandy loam, root respiration rates were slightly higher and more variable (521±206 g C m² yr^?1) and contributed 35% of the total soil respiration. Our results show that soil heterotrophs strongly dominate soil respiration in this forest, regardless of soil texture. Our results also suggest that fine root mortality and decomposition associated with disturbance and land‐use change can contribute significantly to increased rates of nitrogen trace gas emissions.     

福建东山滨海沙地木麻黄林生态系统的能量特征

对福建东山县海岸带红壤性风积沙土与均一性风积沙土木麻黄群落的生物量、生产力、各组分干重热值、去灰分热值及能量分布与结构特征进行了研究.结果表明,红壤性风积沙土木麻黄群落的现存生物量和能量分别为1 681.84 g·m^-2和317 79.31 kJ·m^-2;均一性风积沙土木麻黄群落现存生物量和能量分别为 129.87 g^-1·m^-2和10 71.0kJ·m^-2;红壤性风积沙土的木麻黄群落各组分热值范围为19.84～21.70 kJ·g^-1,各组分能量在群落中所占比例为:干(38.09%)＞枝(19.48%)＞根(17.09%)＞叶(16.86%)＞皮(6.83%)＞枯枝(0.88%)＞果(0.77%),凋落物能量归还量为9 070.47 kJ·m^-2·yr^-1,群落能量的净固定量为31 298.70kJ·m^-2·yr^-1;均一性风积沙土木麻黄群落各组分热值在19.98～21.39kJ·g^-1,其中枯枝热值最高,根最低;各组分能量在群落中所占比例为:干(46.93%)＞根(16.44%)＞枝(13.92%)＞枯枝(12.28%)＞皮(5.87%)＞叶(3.90%)＞果(0.66%),凋落物能量归还量为2 061.77 kJ·m^-2·yr^-1,群落能量净固定量为12 662.82 kJ·m^-2·yr^-1.红壤性风积沙土上的木麻黄群落现存生物量和能量现存量均要高于均一性风积沙土,原因是红壤性风积沙土的沙土层薄(＜20 cm),土壤保水肥的能力要强于沙土层厚(＞100 em)的均一性风积沙土.     

蚯蚓-秸秆及其交互作用对黑麦草修复Cu污染土壤的影响

以高沙土为供试土壤,加入Cu^2＋以模拟成：0,100,200,400mg／kgCu^2＋的Cu污染土壤,设置接种蚯蚓（E）、表施秸秆（M）,同时加入蚯蚓和秸秆（ME）及不加蚯蚓和秸秆的对照（CK）4个处理,并种植黑麦草。研究蚯蚓、秸秆相互作用对黑麦草吸收、富集铜的影响。结果表明：加入秸秆显著提高了蚯蚓的生物量,一定程度上缓解了重金属对蚯蚓的毒害,同时蚯蚓显著提高了秸秆的分解率,较无蚯蚓对照提高了58．11％～77．32％。接种蚯蚓（E,ME）还提高了土壤有效态重金属（DTPA-Cu）含量,秸秆处理（M）则降低了土壤有效态重金属含量。研究还发现,E处理促进了黑麦草地上部生长,而M和ME处理均显著提高了黑麦草地下部的生物量。E和ME处理同时提高了植物地上部和地下部的Cu浓度及Cu吸收量,M处理则只对植物的地下部Cu浓度和Cu吸收量有显著促进作用。总体来看,E处理、M处理及ME处理分别使黑麦草地上部Cu富集系数提高了31．22％～121．07％．2．12％～61．28％和25．56％～132．64％。     

Soil types with different texture affects development of Rhizoctonia root rot of wheat seedlings

The effect of different soil textures, sandy (97.5% sand, 1.6% silt, 0.9% clay), loamy sand (77% sand, 11% silt, 12% clay) and a sandy clay loam (69% sand, 7% silt, 24% clay), on root rot of wheat caused by Rhizoctonia solani Kühn Anastomosis Group (AG) 8 was studied under glasshouse conditions. The reduction in root and shoot biomass following inoculation with AG-8 was greater in sand than in loamy sand or sandy clay loam. Dry root weight of wheat in the sand, loamy sand and sandy clay loam soils infested with AG-8 was 91%, 55% and 28% less than in control uninfested soils. There was greater moisture retention in the loamy sand and sandy clay loam soils as compared to the sand in the upper 10–20 cm. Root penetration resistance was greater in loamy sand and sandy clay loam than in sand. Root growth in the uninfested soil column was faster in the sand than in the loamy sand and sandy clay loam soils, the roots in the sandy soil being thinner than in the other two soils. Radial spread of the pathogen in these soils in seedling trays was twice as fast in the sand in comparison to the loamy sand which in turn was more than twice that in the sandy clay loam soil. There was no evidence that differences among soils in pathogenicity or soil spread of the pathogen was related to their nutrient status. This behaviour may be related to the severity of the disease in fields with sandy soils as compared to those with loam or clay soils. This revised version was published online in June 2006 with corrections to the Cover Date.     

Effects of earthworms on biomass production,nitrogen allocation and nitrogen transfer in wheat-clover intercropping model systems

The effects of earthworms (Lumbricidae) on plant biomass production and N allocation in model intercropping systems of winter wheat and white clover were evaluated in two pot experiments. Wheat and wheat-clover mixtures were grown in a low-organic loam soil, earthworms were added at densities comparable to field population densities and the experiments were terminated 48 and 17 d after earthworm introductions. In both experiments, earthworms significantly increased the biomass and N uptake of wheat while they had generally no effects on clover. As a result, earthworm activity increased the proportion of wheat biomass in the total plant biomass of the mixture. Nitrogen budgets of the experiment lasting 48 d indicated that additional N in the system made available by earthworm activity was primarily taken up by the wheat. Earthworms also affected intra-plant N allocation in wheat which had significantly higher shoot:root N ratios when earthworms were present. When clover was labelled with ¹⁵N in the experiment which lasted 17 d, endogeic earthworms significantly reduced the amounts of ¹⁵N excess transferred from living or decomposing clover roots to accompanying wheat plants. Earthworms assimilated small quantities of ¹⁵N tracer from decomposing clover roots but not from living clover roots. The results of these model experiments suggest that earthworms can affect the balance between intercropped cereals and legumes by altering intra- and inter-plant N allocation. This revised version was published online in June 2006 with corrections to the Cover Date.     

不同质地土壤对花生根系生长、分布和产量的影响

为了探究土壤类型与花生(Arachis hypogaea)根系生长及产量之间的关系, 采用箱栽的方法, 研究了不同质地土壤(砂土、壤土、黏土)对花生根系生长、分布和产量的影响。砂土和壤土中花生根系干物质重各时期均显著高于黏土中, 但生育后期黏土中花生根系干物质重比壤土和砂土下降相对较慢。从不同类型土壤质地根系分布及根系活力来看, 黏土根系主要分布在上层土壤, 但上层土壤根系活力后期下降慢; 砂土有利于花生根系向深层土壤生长, 但上层土壤根系活力后期下降快; 而壤土对花生根系生长和活力时空分布的影响介于黏土和砂土之间。砂土有利于花生荚果的膨大, 且花生荚果干物质积累早而快, 但后期荚果干物质重积累少; 壤土的花生荚果干物质积累中后期多, 黏土则在整个生育期均不利于花生荚果干物质积累。最终荚果产量、籽仁产量和有效果数均表现为壤土最大、砂土次之、黏土最小。研究表明通气性和保肥保水能力居中的壤土更适合花生的根系生长发育及产量的形成。     

Effects of soil compaction and mechanical damage at harvest on growth and biomass production of short rotation coppice willow

The effects of soil compaction and mechanical damage to stools at harvesting on the growth and biomass production of short rotation coppice (SRC) of willow (Salix viminalis L.) were monitored on clay loam (CL) and sandy loam (SL) soils. Moderate compaction, more typical of current harvesting situations did not reduce biomass yields significantly. Even heavy compaction only reduced stem biomass production by about 12% overall; effects were statistically significant only in the first year of the experiment on sandy loam. Heavy compaction increased soil strength and bulk density down to 0.4 m depth and reduced soil available water and root growth locally. Soil loosening treatments designed to alleviate the effects of heavy compaction did not markedly improve the growth of willow on compacted plots. Hence the focus fell on harvesting. Extensive mechanical damage to stools caused a 9% and 21% reduction in stem dry mass on the clay loam and sandy loam soils as a result of fewer stems being produced. The particularly severe effect on the sandy loam soil probably resulted from a combination of dry conditions in the year of treatment, root damage and soil compaction under stools and might have been aggravated by the young age of the plants (1 year) at the time of treatment.