不同管理方式下橡胶林土壤氮动态特征

对西双版纳割胶、未割胶条件下橡胶林种植带土壤及其保护带土壤氮素动态变化特征进行了研究,并比较了不同保护带种植方式(距瓣豆绿肥覆盖与野生杂草覆盖)对土壤氮素动态的影响。结果表明,橡胶林种植带土壤全氮、碱解氮和硝态氮含量低于保护带。橡胶林土壤全氮、碱解氮、铵态氮、硝态氮均呈现明显的动态变化,种植距瓣豆绿肥覆盖与野生杂草生长覆盖的橡胶林土壤氮变化趋势一致。土壤全氮随时间逐渐下降,碱解氮含量先升后降,铵态氮和硝态氮含量变化幅度较大。橡胶林土壤全氮和碱解氮含量呈现表层(0～20cm)>中层(20～40cm)>底层(40～60cm)的趋势,且未割胶处理全氮和碱解氮含量>割胶处理,而保护带为距瓣豆绿肥覆盖的割胶橡胶林>杂草生长覆盖的橡胶林。距瓣豆绿肥覆盖的保护带土壤硝态氮含量高于杂草生长覆盖。碱解氮与铵态氮含量呈显著的负相关、与硝态氮呈显著正相关。割胶橡胶林土壤氮养分含量最低。橡胶林土壤种植豆科距瓣豆绿肥能够改善土壤氮素肥力。     

长期施肥及撂荒对土壤氮素矿化特性及外源硝态氮转化的影响

以黄土高原南部17年长期定位试验不同处理土壤为研究对象,研究了不同肥料处理及撂荒条件下土壤氮素矿化特性、灭菌与不灭菌条件下不同肥力土壤对施入外源硝态氮转化的影响.结果表明：氮磷钾化肥和有机肥配施（MNPK）及长期撂荒处理显著提高了土壤有机质和全氮含量以及土壤氮素矿化量和矿化率;氮磷钾化肥（NPK）处理虽然提高了土壤无机氮含量,但对土壤有机质、全氮、土壤氮素矿化量和矿化率的影响相对较小.高温高压灭菌显著增加了土壤铵态氮含量,但对不同处理土壤硝态氮含量无明显影响;在灭菌土壤培养过程中,土壤铵态氮含量呈显著增加趋势.同一土壤类型,不论灭菌与否,培养过程中施入土壤的硝态氮含量保持相对稳定,说明在本研究培养条件下,生物因素和非生物因素对外源硝态氮在土壤中的转化无明显影响.     

陈山红心杉根际土壤有机碳、氮含量及根际效应

陈山红心杉(Cunninghania lanceolata)是江西特有树种,获国家地理标志保护。目前关于其植物—土壤关系的研究较少。以不同林龄(5、10、20和40a)陈山红心杉为对象,研究了其根际和非根际土壤有机碳、氮含量和根际效应。结果表明:根际pH略小于非根际,有机碳和氮素总体上大于非根际。随林龄的增加,根际和非根际土壤有机碳和氮含量先降后增;有机碳、全氮和有机氮的根际效应先增后降;铵态氮、硝态氮和无机氮的根际效应先降后趋于平缓;pH和碱解氮的根际效应变化平缓。氮含量对根际和非根际土壤pH和有机碳的影响为全氮无机氮碱解氮;碱解氮和全氮的根际效应分别对pH和有机碳根际效应影响最大。随着林龄的增加,硝态氮的比重高于铵态氮,应注意反硝化作用可能造成的氮素流失,同时林地土壤养分下降,在10 a前后应注意林地有机质和氮素的补充,以防地力衰退。     

菜园土壤微生物生态特征与土壤理化性质的关系

对广州白云区64个菜园土壤样本的研究表明,微生物碳与土壤全氮、碱解氮、有效钾、阳离子交换量和有机质,微生物氮与土壤全氮、全磷、阳离子交换量及有机质,土壤基础呼吸与土壤全氮、碱解氮、全钾、阳离子交换量及有机质,AWCD值与全氮及有机质含量,以及Shannon多样性指数与全氮和阳离子交换量均呈显著正相关关系.较低的碱解氮含量使土壤微生物碳、土壤基础呼吸和呼吸商的值升高,过高的碱解氮则使呼吸商下降;过高的土壤有效磷降低微生物碳、微生物氮和微生物呼吸商.有效磷/碱解氮比值过高降低了土壤微生物碳、微生物氮、微生物碳氮比及土壤基础呼吸.土壤微生物生态特征与土壤理化性质关系密切,有效养分过高及养分比例不适当对土壤微生物均存在不利影响.     

双氰胺单次配施和连续配施的土壤氮素形态和蔬菜硝酸盐累积变化

采用田间试验研究了双氰胺(dicyandiamide,缩写DCD)单次配施和连续配施的土壤氮素形态和蔬菜硝酸盐累积变化。结果表明,与单施化肥相比,DCD单次配施的长期叶菜甘蓝生长过程中土壤铵态氮含量增幅为21.3%—339.4%,土壤硝态氮和菜体硝酸盐含量降幅分别为5.4%—80.2%和4.4%—58.3%;短期叶菜空心菜收获时土壤铵态氮含量增加了299.4%,土壤硝态氮和菜体硝酸盐含量分别降低了26.2%和31.7%。DCD连续配施的"甘蓝-菠菜-空心菜-萝卜-大白菜"种植体系中,土壤铵态氮、硝态氮和菜体硝酸盐含量均呈累积的趋势,配施DCD的土壤铵态氮含量从略高于化肥处理(44.0%)发展到极显著高于化肥处理(392.5%,P<0.01),土壤硝态氮含量从极显著低于化肥处理(-68.2%,P<0.01)发展到显著高于化肥处理(146.6%,P<0.05),菜体硝酸盐含量从显著低于化肥处理(-30.2%,P<0.05)发展到极显著高于化肥处理(40.4%,P<0.01)。由此可见,DCD单次配施可显著降低菜体硝酸盐含量,而连续配施DCD的土壤能维持一定量的铵态氮水平,这些盈余的铵态氮会进一步转化为硝态氮残留在土壤中,并可能产生蔬菜硝酸盐累积的风险。     

藏东南色季拉山沟壑区土壤氮素空间分布特征

以西藏东南部色季拉山海拔3950—4350 m为研究区,采用30×50 m网格采样法,以地统计学半变异函数为工具,研究了色季拉山森林生态系统沟谷与坡面上土壤氮素空间变异特征及模型。结果表明:土壤全氮、硝态氮和铵态氮含量均表现为0—10 cm10—20 cm,两个层次上空间变异性表现为全氮和铵态氮0—10 cm10—20 cm,而硝态氮表现为10—20 cm0—10cm;不同海拔高度土壤氮含量表现为随着海拔高度的升高而增加,但这种海拔梯度效应并未达显著水平(P0.05);沟谷区土壤氮含量高于坡面,这可能与植被残体在沟谷区的堆积分解促进氮循环有关;土壤全氮、铵态氮和硝态氮均具有中等程度的空间依赖性,其中土壤全氮空间变异符合指数模型,块金值/基台值为50%;土壤铵态氮和硝态氮含量空间变异分布均符合高斯模型,块金值/基台值分别为70.91%和37.45%;该区域土壤全氮、铵态氮和硝态氮含量空间依赖性表现为:硝态氮全氮铵态氮,即土壤硝态氮更易受到空间结构因素的影响,而铵态氮含量空间变化则主要受随机因素的影响。     

不同氮素形态及其配比对紫苏品质及矿质元素累积的影响

以紫苏幼苗为试验材料,通过营养液盆栽试验,在等氮条件下设置6种不同氮素形态[NH4+-N、NO3--N、CO(NH2)2]及其配比处理,测定其采收期前硝酸盐和亚硝酸盐含量的变化以及营养成分和药用成分的含量,探讨不同氮素形态及其配比对紫苏叶片硝酸盐和亚硝酸盐含量的动态变化、营养成分、矿质元素和次生代谢产物含量的影响,为生产中合理施用氮肥提供理论基础。结果表明,(1)紫苏叶片中的硝酸盐和亚硝酸盐含量随栽培时间的增加而不断累积,在采收前,叶片硝酸盐含量在全铵处理下最低,亚硝酸盐含量在铵硝比(NH4+-N/NO3--N)为25∶75时最低。(2)紫苏叶片中的可溶性糖、淀粉含量在全硝态氮处理下最高,而其游离氨基酸和维生素C含量在酰胺态氮处理时达到最大值;紫苏叶片中P、K、Ca累积量在铵硝比为50∶50时最高,Zn、Fe、Mn元素的含量在全铵态氮处理下最高,而Mg元素含量在全硝态氮处理下含量最高。(3)紫苏叶片中的总黄酮含量、挥发油含量以及迷迭香酸含量均随着铵硝比的增加呈现先升高后降低的趋势,并在铵硝比为25∶75时最高;紫苏叶片中花色苷相对含量在酰胺态处理下达到最大值。研究表明,在紫苏的栽培生产中,铵硝比为25∶75更有利提高其药用品质和营养品质,并且能降低其亚硝酸盐含量。     

氮素形态对樱桃番茄果实发育中氮代谢的影响

以樱桃番茄为材料,采用基质 营养液共培养的方法,研究了全硝态氮(NO₃^-）、铵态氮和硝态氮配施（75%NO₃^-∶25%NH₄⁺）及全铵态氮（NH₄⁺）营养对樱桃番茄果实氮代谢及硝酸还原酶（NR）和谷氨酰胺合成酶（GS）基因表达的影响.结果表明： 铵态氮和硝态氮配施处理下樱桃番茄的单果质量比全硝态氮处理略有增加,且果实中NH₄⁺、总氨基酸、氮含量和氮素累积量均显著高于全硝态氮处理;全硝态氮及铵态氮和硝态氮配施处理下果实NR活性及其基因表达没有明显差异,但都显著高于全铵态氮处理;铵态氮和硝态氮配施处理下果实GS活性都高于全硝态氮处理.不同形态氮素及配施处理下,同工酶GS1（胞质型GS）和GS2（叶绿体型GS）的表达与GS的活性不一致,说明氮素对GS活性的影响主要发生在转录后水平.     

川西亚高山-高山森林土壤养分动态及其对季节性冻融的响应

为深入了解川西亚高山-高山森林冬季生态学过程,于2008年11月—2009年10月,在土壤冻结初期、冻结期和融化期及植被生长季节,研究了不同海拔(3582 m、3298 m和3023 m)岷江冷杉林土壤养分动态及其对季节性冻融的响应。3个海拔森林土壤冬季具有较高养分含量,且随土壤冻融过程不断变化。土壤有机层可溶性碳和氮、铵态氮、硝态氮含量在冻结初期显著增加后快速降低,并随融化过程迅速增加后再次降低,而土壤可溶性碳和氮、硝态氮含量在冻结期变化不明显,铵态氮显著增加。矿质土壤层可溶性碳和氮、铵态氮含量也在冻结初期显著增加后降低,而土壤可溶性氮、铵态氮和硝态氮在冻结期显著增加,并在融化期经历一个明显的含量高峰。海拔和土层的交互作用显著影响土壤可溶性碳和硝态氮含量,土壤养分含量与土壤温度的相关性随海拔差异而不同。这表明季节性冻融期是土壤生态过程的重要时期,土壤冻融格局显著影响川西亚高山-高山森林土壤养分动态。     

不同典型地带性土壤氮素分布特征及其影响因素

在野外取样的基础上,研究中国不同典型地带性土壤各形态氮素分布特征及其影响因素.结果表明: 垂直地带性土壤中0.5 mol·L^-1 K₂SO₄提取的提取态总氮、提取态有机氮、吸附氨基酸随取样点海拔的增加而显著增加,且提取态总氮、提取态有机氮和吸附氨基酸平均值都大于水平地带性土壤;水平地带性土壤各形态氮含量随土壤类型的不同而差异显著.土壤吸附氨基酸含量是游离氨基酸的5倍,占提取态有机氮百分比为21.1%,表明吸附氨基酸可能作为土壤有机氮库的一种重要存在形态.相关分析结果表明,垂直地带性土壤中提取态总氮、提取态有机氮、铵态氮、氨基酸态氮均与有机质、全氮呈显著正相关(r=0.57～0.93,P<0.05),但与pH、硝态氮呈显著负相关(r=-0.37～-0.91,P<0.05);水平地带性土壤pH与提取态总氮、硝态氮、有机质、全氮、碱解氮及盐基离子(K⁺、Ca²⁺、Mg²⁺)呈显著正相关(r=0.36～0.85,P<0.05),与铵态氮、氨基酸态氮呈显著负相关(r=-0.39～-0.81,P<0.05).     

济南地区日光温室土壤养分的分布状况和累积规律

对济南地区不同种植年限日光温室内外及不同蔬菜作物的土壤养分差异和频数分布进行比较,分析了日光温室土壤养分随种植年限的累积特征,并对不同蔬菜温室土壤养分与种植年限进行曲线拟合,研究了引起土壤盐渍化和酸化的原因.结果表明:济南地区日光温室土壤碱解氮、速效磷、速效钾、有机质、电导率显著高于棚外土壤,增幅分别为135.3％、475.2％、290.1％、97.7％、188.7％,pH值较棚外土壤降低0.31;各土壤养分的频数分布曲线均呈正态分布.不同蔬菜温室土壤养分含量各有差别,其中,碱解氮和电导率为番茄＞甜椒＞黄瓜,有机质和pH为黄瓜＞甜椒＞番茄,速效磷为黄瓜＞番茄＞甜椒,速效钾为番茄＞黄瓜＞甜椒.日光温室土壤有酸化的趋势,但不明显.温室土壤盐渍化程度加重主要由碱解氮和速效钾的累积所致.pH的降低与碱解氮的累积关系密切.日光温室各土壤养分随种植年限的累积规律基本一致,1～2年为养分的快速累积期,3～4年的累积速率变缓,以后处于一个稳定水平,整体上表现为土壤系统的动态平衡.除pH的累积为负向外,其他均为正向累积.不同蔬菜温室土壤养分与种植年限呈极显著相关,且可用2次或3次曲线进行拟合.     

Assimilation of [N]Nitrate and [N]Nitrite in Leaves of Five Plant Species under Light and Dark Conditions

Light dependency of nitrate and nitrite assimilation to reduced-N in leaves remains a controversial issue in the literature. With the objective of resolving this controversy, the light requirement for nitrate and nitrite assimilation was investigated in several plant species. Dark and light assimilation of [¹⁵N]nitrate and [¹⁵N]nitrite to ammonium and amino-N was determined with leaves of wheat, corn, soybean, sunflower, and tobacco. In dark aerobic conditions, assimilation of [¹⁵N]nitrate as a percentage of the light rate was 16 to 34% for wheat, 9 to 16% for tobacco, 26% for corn, 35 to 76% for soybean, and 55 to 63% for sunflower. In dark aerobic conditions, assimilation of [¹⁵N]nitrite as a percentage of the light rate was 11% for wheat, 7% for tobacco, 13% for corn, 28 to 36% for soybeans, and 12% for sunflower. It is concluded that variation among plant species in the light requirement for nitrate and nitrite assimilation explains some of the contradictory results in the literature, but additional explanations must be sought to fully resolve the controversy.

In dark anaerobic conditions, the assimilation of [¹⁵N]nitrate to ammonium and amino-N in leaves of wheat, corn, and soybean was 43 to 58% of the dark aerobic rate while dark anaerobic assimilation of [¹⁵N]nitrite for the same species was 31 to 41% of the dark aerobic rate. In contrast, accumulation of nitrite in leaves of the same species in the dark was 2.5-to 20-fold higher under anaerobic than aerobic conditions. Therefore, dark assimilation of nitrite cannot alone account for the absence of nitrite accumulation in the in vivo nitrate reductase assay under aerobic conditions. Oxygen apparently inhibits nitrate reduction in the dark even in leaves of plant species that exhibit a relatively high dark rate of [¹⁵N]nitrite assimilation.

     

湖南烟区土壤交换性钙、镁含量及对烤烟品质的影响

分析了湖南烟区主要土壤类型交换性钙、镁元素含量状况及其对烟叶品质的影响,结果表明:(1)土壤交换性钙、镁含量在不同土壤类型间存在显著性差异,交换性钙含量平均为8.87cmol/kg,以红壤含量最高;交换性镁含量平均为1.16cmol/kg,以黄棕壤含量最高;交换性钙镁比值大小依次为:红壤(11.74)>水稻土(10.25)>黄壤(6.84)>黄棕壤(6.14),在烟叶实际生产中,应重视镁肥在红壤和水稻土中的施用;(2)烟叶钙含量偏高(21.93g/kg±4.37g/kg),烟叶镁含量偏低(2.52g/kg±1.26g/kg),两者均存在广泛的变异性;(3)整体来看,烟叶钙含量随土壤中交换性钙含量的升高和镁含量的降低而显著升高;烟叶镁含量随土壤交换性镁含量的升高而升高,与土壤交换性钙含量的相关性不显著;(4)典型相关分析表明,土壤中交换性镁含量的降低可能引起烟叶钾含量的提高,从而使得烟叶钾素和镁素含量达到较好的平衡;(5)土壤交换性钙、镁含量与烟叶其它化学成分指标的相关分析表明,土壤交换性钙有利于烟株对硼和氯素的吸收,对氮、锌和锰素的吸收则有显著的抑制作用;而土壤交换性镁有利于烟叶总糖、硼素和锰素的积累,对氮、磷、铁和锌素的吸收具有显著的抑制作用。     

氮肥形态和用量对藏东南地区烤烟产量和质量的影响

在藏东南地区进行了氮肥用量和形态对烟产量与质量影响的田间试验。结果表明,在施N量0－150kg·hm^-2范围内,施N量与烘烤后烟叶产量、产值、氧化钾及总N含量呈显著或极显著正相关,与上中等烟比例、还原糖含量则呈显著负相关,糖／碳比显著下降,氮肥用量75kg·hm^-2时,产量、质量最佳。无机氮肥对烟产量与质量的效应极显著优于有机氮肥。铵态氮、硝态氮、硝铵态氮肥处理间除上中等烟比例,其它各项指标仅略有差异,但均极显著优于酰胺态氮肥。铵态氮对烤烟产量与质量的影响略优于硝态氮,主要在于烟株吸收和同化过程的差异。     

桂北丰水梨园土壤养分与叶片营养的相关性分析

选取桂北地区有生理异常现象发生的丰水梨园,以成年结果树为研究对象,通过检测年生长周期内梨树叶片矿质营养元素、土壤养分的含量,分析不同时期梨树叶片营养元素和土壤养分含量及其动态变化规律,探讨年生长季内叶片营养与土壤养分之间的相关关系。结果表明:(1)在生长季节内,丰水梨叶片中N、P、K含量丰富;营养元素含量随时间的变化幅度均为P最大,N、K较小,但均未达到显著水平(P>0.05)。(2)梨园土壤中有机质、水解性N含量丰富,有效P、速效K含量普遍偏高;年生长周期内土壤速效N、P、K含量随时间的推移变化较大,均达显著水平(P<0.05),而有机质含量则相对稳定。(3)梨树叶片N含量与土壤有机质、水解性N、有效P、速效K含量呈显著正相关关系(P<0.05);叶片P和K含量与土壤水解性N含量分别呈显著负相关和正相关关系(P<0.05),而与土壤有机质、有效P、速效K相关关系不明显。     

Interaction of sulfur and nitrogen nutrition in tobacco (Nicotiana tabacum) plants: significance of nitrogen source and root nitrate reductase

Abstract: The significance of root nitrate reductase for sulfur assimilation was studied in tobacco (Nicotiana tabacum) plants. For this purpose, uptake, assimilation, and long-distance transport of sulfur were compared between wild-type tobacco and transformants lacking root nitrate reductase, cultivated either with nitrate or with ammonium nitrate. A recently developed empirical model of plant internal nitrogen cycling was adapted to sulfur and applied to characterise whole plant sulfur relations in wild-type tobacco and the transformant. Both transformation and nitrogen nutrition strongly affected sulfur pools and sulfur fluxes. Transformation decreased the rate of sulfate uptake in nitrate-grown plants and root sulfate and total sulfur contents in root biomass, irrespective of N nutrition. Nevertheless, glutathione levels were enhanced in the roots of transformed plants. This may be a consequence of enhanced APR activity in the leaves that also resulted in enhanced organic sulfur content in the leaves of the tranformants. The lack of nitrate reductase in the roots in the transformants caused regulatory changes in sulfur metabolism that resembled those observed under nitrogen deficiency. Nitrate nutrition reduced total sulfur content and all the major fractions analysed in the leaves, but not in the roots, compared to ammonium nitrate supply. The enhanced organic sulfur and glutathione levels in ammonium nitrate-fed plants corresponded well to elevated APR activity. But foliar sulfate contents also increased due to decreased re-allocation of sulfate into the phloem of ammonium nitrate-fed plants. Further studies will elucidate whether this decrease is achieved by downregulation of a specific sulfate transporter in vascular tissues.     

The effect of sodium chlorate and nitrapyrin on the nitrification mediated nitrosation process in soils

Summary The influence of total nitrification to nitrate or partial nitrification to nitrite on the soil organic nitrogen status was examined. NH ₄ ⁺ –¹⁵N was added to the soil in the absence and the presence of NaClO₃, respectively nitrapyrin. The first chemical inhibits only nitrate formation, the second inhibits total nitrification. The accumulation of nitrite nitrogen in the soil at levels up to 5 mg kg^–1 increased the loss of nitrogen. Yet, it did not increase the binding of mineral nitrogen into soil organic matter, relative to the control soil. The data suggest that the biochemistry of the nitrite formation process, rather than the levels of nitrite ions formed, are of primary importance in the role of nitrification mediated nitrosation of soil organic matter.     

Diurnal changes in nitrogen assimilation of tobacco roots.

To gain an insight into the diurnal changes of nitrogen assimilation in roots the in vitro activities of cytosolic and plasma membrane-bound nitrate reductase (EC 1.6.6.1), nitrite reductase (EC 1.7.7.1) and cytosolic and plastidic glutamine synthetase (EC 6.3.1.2) were studied. Simultaneously, changes in the contents of total protein, nitrate, nitrite, and ammonium were followed. Roots of intact tobacco plants (Nicotiana tabacum cv. Samsun) were extracted every 3 h during a diurnal cycle. Nitrate reductase, nitrite reductase and glutamine synthetase were active throughout the day-night cycle. Two temporarily distinct peaks of nitrate reductase were detected: during the day a peak of soluble nitrate reductase in the cytosol, in the dark phase a peak of plasma membrane-bound nitrate reductase in the apoplast. The total activities of nitrate reduction were similar by day and night. High activities of nitrite reductase prevented the accumulation of toxic amounts of nitrite throughout the entire diurnal cycle. The resulting ammonium was assimilated by cytosolic glutamine synthetase whose two activity peaks, one in the light period and one in the dark, closely followed those of nitrate reductase. The contribution of plastidic glutamine synthetase was negligible. These results strongly indicate that nitrate assimilation in roots takes place at similar rates day and night and is thus differently regulated from that in leaves.     

Effect of tree species and soil properties on nutrient immobilization in the forest floor

To investigate the effect of tree species and soil properties on organic matter accumulation and associated nutrients, an area-based sampling of the forest floor was carried out in a 28 years old species trial including Norway spruce, Douglas fir, beech, and common oak at two sites, a poor and sandy soil, and a fertile loamy soil.The accumulation of C, N and P in the forest floor was significantly higher at the sandy site than at the loamy site under all species. At the loamy site, oak was characterized by lesser accumulation of C, N and P than the other species. Remarkably, the C/N-ratios showed no substantial differences, whereas the C/P-ratios were significantly higher at the sandy site for all species. pH was significantly lower at the sandy site for all species, and among the species, pH was lower in the conifer forest floors than in the broadleave forest floors. The concentration of ammonium, nitrate and phosphate in the soil solution was much higher at the loamy site under all species showing a stronger microbial activity. It is therefore hypothesized that the differences in accumulation rates were, at least partly, caused by differences in the mineralization regimes. Strong root infiltration in the forest floors at the sandy site compared to almost none at the loamy site, is probably responsible for the differences in mineralization rate due to competition between the organic matter decomposers and the tree-roots/mycorrhiza for nutrients.