成都平原农区地下水中NO3--N含量变化规律研究

采用硝酸根电极法对成都平原温江县天府乡农区田间和水井的地下水NO-3 N含量进行了一年多的连续测定 ,探讨了该农区地下水中NO-3 N的变化规律和氮肥用量的影响。结果表明 :(1)田间地下水NO-3 N含量周年变化规律是冬春枯水季较高 ,且变幅较大 (0 3 6～ 2 62mgL- 1) ,平均值为 2 59mgL- 1;夏秋丰水季较低 ,且变幅较小 (0 84～ 5 48mgL- 1) ,平均值为 1 10mgL- 1。 (2 )前作麦季氮肥施用量 ,对稻季地下水中NO-3 N含量有明显影响 ,当前作施纯氮达 3 75kghm- 2 时 ,稻季地下水NO-3 N含量最高达 3 4 6mgL- 1,其平均值为 17 97mgL- 1,是施纯氮 150kghm- 2 平均值 1 3 0mgL- 1的 13 7倍。 (3 )井水中NO-3 N含量变化幅度为 0 14～ 16 53mgL- 1,3口井水平均值分别为 2 54、3 60、6 52mgL- 1,未超出我国生活饮用水卫生标准 ,但明显高于灌溉水NO-3 N含量的平均值 1 81mgL- 1。 (4)地下水位的高低与井水中NO-3 N含量没有线性关系     

稻田土壤中氮素淋失的研究

本文应用稻田大型原状土柱渗漏计，研究了双季稻田土壤中氮素随渗漏水流淋失的形态、数量、季节性变化以及若干农化因子的影响。明确了稻田中氮素淋失的基本形态是硝态氮（ＮＯ３＾－－Ｎ），估算出双季稻田中氮素淋失总量可接近３０ｋｇＮ／ｈａ，同时肯定了农田施用氮肥对地下水体环境可能的ＮＯ３＾－－Ｎ污染，建议双季稻田中每季水稻的氮肥用量宜控制在１５０ｋｇＮ／ｈａ；本文还证实氮肥用量对氮素淋失有明显影响，不同氮肥品     

Nutrient Retention in a Northern Prairie Marsh (Frank Lake,Alberta) Receiving Municipal and Agro-Industrial Wastewater

Agro-industrial wastewater and municipal sewage wereused to restore Frank Lake, a 1246 ha northernprairie marsh in southern Alberta, Canada, to providewaterfowl habitat and improve water quality. Meanannual inflow wastewater nutrient concentrations were17 mg L^-1 NH₃-N, 30 mg L^-1 NO₃-Nand 11 mg L^-1 SRP. Mean flows greater than 5000 m³ day^-1 loaded the marsh with 23 000 kg of P annually. Summer NH₃-N, NO₃-N andtotal phosphorus (TP) surface water concentrationswere decreased by 76, 87 and 64%, respectively, aswaters flowed through the first basin of the marsh.Winter treatment was less successful, with surfacewater NH₃-N, NO₃-N and TP reductions of46, –26 (export) and 26%, respectively.Short-circuiting of water flow through the marsh andcold seasonal conditions with ice cover caused spatialand temporal variation in marsh treatment. Continuedhigh loadings to the marsh may lead to sediment saturation, eutrophication or phosphorus export from the marsh.     

氮肥形态及配比对菠菜生长和安全品质的影响

【目的】铵态氮肥和硝态氮肥是蔬菜生长过程中经常施用的氮肥种类,氮肥形态及配比对蔬菜生长和安全品质有着重要影响。菠菜是一种叶菜类蔬菜,富含矿质元素、维生素C和维生素E。本文通过施用铵态氮和硝态氮肥,探究氮肥形态及其配比(NH+4-N/NO-3-N)对菠菜生长和安全品质的影响。【方法】采用水培试验,设置5种不同氮素形态配比(NH+4-N/NO-3-N比值分别为100∶0、75∶25、50∶50、25∶75和0∶100)的营养液,定期采集菠菜样品并测定菠菜的生物量、株高、根系长度、硝酸盐和亚硝酸盐、有机酸和氨基酸参数值。【结果】随着NH+4-N/NO-3-N比值从100∶0变化到0∶100,菠菜的生物量、株高、根系长度、硝酸盐和亚硝酸盐累积量以及有机酸含量均呈增加趋势,而氨基酸总量则明显下降;当NH+4-N/NO-3-N比值为0∶100时,菠菜茎叶生物量为6.2g/plant,株高和根系长度分别为16.3 cm和22.5 cm,分别是NH+4-N/NO-3-N比值为100∶0时的6倍、2.2倍和2.0倍,表明菠菜是一种喜硝酸盐氮的蔬菜;当NH+4-N/NO-3-N比值由0∶100变为25∶75时,即在氮肥组合中增加25%的铵态氮肥,此时的硝酸盐和亚硝酸盐含量分别由398.5 mg/kg、1.42 mg/kg降为249.1 mg/kg、0.98mg/kg,降幅为37.5%和8.0%,表明在菠菜生长过程中适当增施铵态氮肥可有效降低硝酸盐和亚硝酸盐在茎叶中的累积;当NH+4-N/NO-3-N比值从100∶0变化到0∶100,对6种有机酸(苹果酸、富马酸、琥珀酸、α-酮戊二酸、柠檬酸和丙酮酸)而言,增加幅度最大的是富马酸,约8.6倍,增加幅度最小的是柠檬酸,约2.5倍,苹果酸则在NH+4-N/NO-3-N=25∶75时达到最大值,为985.3 mg/L;随着NH+4-N比例的减少,菠菜茎叶中的氨基酸总量呈下降趋势,NH+4-N/NO-3-N比值为100∶0、75∶25、50∶50、25∶75和0∶100的氨基酸总量分别为21.80μmol/g、12.92μmol/g、9.20μmol/g、8.30μmol/g和7.50μmol/g,表明菠菜的营养价值降低,这一趋势与上述所研究的指标(株高、根系长度、硝酸盐和亚硝酸盐含量以及有机酸含量)有着明显的区别。【结论】菠菜是一种典型的喜硝态氮类蔬菜,施用硝态氮肥可明显提高菠菜产量,但过高的施用量可导致菠菜安全品质下降。适当增施铵态氮肥可降低硝酸盐和亚硝酸盐在菠菜体内的累积,并有效调节氨基酸和有机酸的代谢。因此,在菠菜种植过程,应该合理地搭配铵态氮肥和硝态氮肥,以便在保证安全性和营养价值的基础上获取最大的生物量。     

太湖地区稻麦高产的氮肥适宜用量及其对地下水的影响

通过田间定位试验与土壤渗漏仪 (Lysimeter)模拟试验 ,研究太湖地区稻麦生产中氮肥过量施用带来氮肥利用率低与环境污染问题 ,探讨本区稻麦高产与减少氮肥淋洗的适宜氮肥用量。初步试验结果表明 ,氮肥适宜用量随着稻麦产量的提高而增加 ,本区两种主要土壤水稻、小麦高产的氮肥适宜用量(以N计 )分别为 2 2 5～ 2 70kghm- 2 与 1 80～ 2 2 5kghm- 2 ;适宜的氮肥用量使单位面积的有效穗数和每穗的结实颖花数均高 ,因而产量高。氮素的淋洗以NO- 3 N为主 ,主要发生在麦季与泡田插秧初期 ,其含量随着施氮量的增加而增加 ,每hm2 施N 2 2 5kg的模拟试验 ,麦季渗漏液的NO- 3 N浓度在 5 4～ 2 1 3mgL- 1,有60 %的样次超过污染标准 (NO- 3 N 1 0mgL- 1) ;田间试验 ,麦季施N量在 2 70～ 31 5kghm- 2 范围内 ,地下水NO- 3 N浓度在 1 9～ 1 1 0mgL- 1,有 2 0 %的样次接近 ,1 0 %的样次超过污染标准。长期NO- 3 N渗漏累积 ,势必对地下水构成潜在威胁。     

Evaluating the Validity of a Nitrate Quick Test in Different Chinese Soils

Because laboratory tests are expensive and time-consuming and may not be available to farmers, soil nitrate quick tests are required for optimal nitrogen management strategies in China to increase nitrogen use effciency and to reduce nitrogen losses. A total of 328 soil samples were collected at different soil depths from 225 sites in China, which covered a wide range of climatic and geographic regions, soil types, croplands and soil textures, to evaluate the suitability of a quick reflectometer test method for analysing soil NO-3-N in a wide range of soil NO-3 concentrations, soil types and cropping systems in China, mainly by comparison of soil NO-3-N assessed by a quick-test method (a reflectometer) and a standard laboratory method, i.e., high-performance liquid chromatography (HPLC). The reflectometer showed excellent agreement with the laboratory HPLC method with regard to soil nitrate contents for all analysed soil samples. The linear regression had slopes of 1 ± 0.08 and intercepts of ±1.38 mg NO-3-N L-1 among different soil types and croplands. Compared with the 1:1 lines, the regression analysis for each soil type showed statistically significant but small differences in slope; the relative difference between the values measured using the two analytical systems varied from -8% to 6%, and there were no differences in intercept except for paddy soil. The reflectometer showed adequate, statistically significant precision in determining soil nitrate contents, and it could therefore be directly used instead of the laboratory methods for soil NO-3-N measurement in China.     

旱作地区长期小麦连作和苜蓿连作土壤剖面的矿质氮研究

对不同施肥条件下23年小麦连作地和苜蓿连作地土壤矿质氮分布和累积进行研究,探讨种植浅根系和深根系植物对硝态氮淋溶的影响。结果表明,不施肥(CK)和单施磷(P)肥,小麦和苜蓿连作地土壤硝态氮主要集中在0—60 cm土层,0—60 cm土层以下硝态氮含量变化稳定并小于2 mg/kg。氮肥、磷肥和有机肥配施(NPM)时,小麦连作地土壤硝态氮累积在20—100 cm和140—320 cm土层,年累积速率可达42.12 kg/(hm2.a);苜蓿连作土壤硝态氮主要集中在0—60 cm土层,仅在200—300 cm土层出现轻微累积,年累积速率仅为1.01 kg/(hm2.a)。在不施肥和单施磷肥下,种植小麦或苜蓿对土壤硝态氮残留量影响不显著,而氮、磷和有机肥配施时,小麦连作地土壤硝态氮残留量迅速增加,并与不施肥、单施磷肥处理有显著差异;苜蓿连作地土壤硝态氮残留量虽有少量增加,但与不施肥、单施磷肥处理无显著差异。不施肥、单施磷肥和氮、磷和有机肥配施,小麦连作、苜蓿连作地土壤剖面铵态氮含量主要在10—20 mg/kg之间波动,在土壤剖面无明显的累积现象,铵态氮残留量受施肥和作物种类的影响不显著。     

不同形态氮素比例对不同小白菜品种生物量和硝酸盐含量的影响

利用NO-3 N∶NH 4 N为 10 0∶0、5 0∶5 0和 0∶10 0三个硝铵配比的营养液对 12个不结球小白菜品种进行水培试验。结果表明 :不同的硝铵配比对不同品种小白菜的生物量、叶绿素SPAD值、硝酸盐积累量等有着显著的影响 ,同一氮源培养下不同的小白菜品种间也表现出显著的差异 ;12个小白菜品种叶绿素SPAD值随营养液中的NH 4 N比例的增加而升高 ,两者间存在着显著的正相关 ;单株生物量除亮白叶 1号和五月慢在全硝培养中生物量较其他两种配比大外 ,其他 10个品种均在 5 0∶5 0硝铵营养液中表现最好 ;供试的 12个小白菜品种中有 9个品种的硝酸盐积累量随着NH 4 N比例的增加而下降 ,表明适当地配施铵态氮较纯硝营养液能获得更好的产量、更高的叶绿素SPAD值和较低的硝酸盐积累量。     

Uptake,transport and assimilation of 15N-nitrate and 15N-ammonium in tea (Camellia sinensis L.) plants

¹⁵N studies were conducted using hydroponically grown tea (Camellia sinensis L.) plants to clarify the characteristics of uptake, transport and assimilation of nitrate and ammonium. From the culture solution containing 50 mg L^-1 N0₃-N and 50 mg L^-1 NH.-N, the uptake of NH₃-N after 24 h was twice as high as that of NO₃-N, while the uptake of N0₃-N from the culture solution containing 90 mg N0₃-N and 10 mg NH₃-N was twice that of NH₄-N. The presence of 0.4 mM Al had no significant effect on the N0₃-N and NH₄-N uptake from the culture solutions containing 50 mg L^-1 N0₃-N and 50 mg L^-1 NH₄-N, 90 mg L^-1 N0₃-N and 10 mg L^-1 NH₄-N or 99 mg L^-1 N0₃-N and 1 mg L^-1 NH₄-N. Transport of N0₃-derived N to young leaves was much more rapid than that of NH₄-derived NO₃ and NH₄-derived N was largely retained in the roots and lower stem. Young and mature shoots separated from the roots absorbed more N0₃-N than intact plants. Nitrate assimilation occurred in both, roots and young as well as mature leaves. Internal cycling of N0₃-derived Nand NH₄-derived N from one root part to another part was not appreciable after 28 h, suggesting that a longer of time is required for cycling in woody plants.     

不同水稻品种根尖吸收NO3-过程中表皮细胞膜电位变化特征

越来越多的结果表明给水稻提供部分硝酸盐营养可促进水稻的氮素总吸收量并明显改善水稻的生长发育。利用微电极技术分别测定了4个水稻品种即农垦57(粳稻)、泗优917(杂粳)、扬稻6号(籼稻)和汕优63(杂籼)幼苗根尖表皮细胞在3种NO3^-浓度(0．1mmol L^-1、1mmol L^-1、10mmol L^-1)处理过程中膜电位的变化特征。结果表明：水稻根系吸收NO3^-引起膜的去极化，去极化到一定程度出现复极化。去极化程度随外界处理液中NO3^-浓度的增加而加强，0．1mmol L^-1 NO3^-处理产生的去极化值平均为7mV，1mmol L^-1 NO3^-处理的平均为11mV，10mmol L^-1 NO3^-处理的平均为21mV；就复极化来说，0．1mmol L^-1 NO3^-处理自动出现复极化，1mmol L^-1 NO3^-处理和处理10mmol L^-1 NO3^-处理只有当除去NO3^-时才出现复极化。就单位时间膜电位变化大小而言，扬稻6号对外界NO3^-较敏感，3种NO3^-浓度引起的去极化值均高于其他3个品种，表现出对NO3^-的吸收能力较强；泗优917和汕优63表现出相似的去极化大小和相似的反应时间，而农垦57对NO3^-相对不敏感，3种NO3^-浓度引起的去极化值均低于其他3个品种，表现出对NO3^-的吸收能力较弱。另外，有部分品种的水稻根在吸收NO3^-以后表现为膜电位先超极化后去极化。上述结果表明用根系对NO3^-响应的细胞膜电位变化来研究水稻的硝酸盐营养是有可行性的。     

蔬菜硝酸盐的还原转化特性研究

利用液体培养试验和15N示踪技术 ,研究了通过改变菜心氮源供应条件 ,降低硝态氮累积过程中硝态氮的还原特性。结果表明 ,营养液中的硝态氮源被其他形态氮源替代后能明显降低菜心的硝态氮含量 ;已累积在菜心体中的硝态氮与改变氮源供应条件后新吸收的硝态氮相比较 ,前者的还原率较小 ,较后者难以被还原。改变氮源供应条件前后累积的硝态氮在菜心各部位的分布上存在差异 ,新吸收的硝态氮易累积在代谢活动较为旺盛的部位。尽管在 2种氮源条件下对新吸收硝态氮的还原率相近 ,但供应硝铵态氮源时原累积硝态氮的还原率较仅供硝态氮源时大。     

氮素形态对巨峰葡萄果实品质的影响

为了探讨氮素形态对巨峰葡萄果实品质性状的影响,设置了尿素T1(酰胺态)、全硝T2(硝铵比为100/0)、混合氮T3、T4、T5(硝铵比为70/30、50/50、30/70)及全铵处理T6(硝铵比为0/100)和清水对照CK,于生长季节进行叶面喷施试验。结果表明,不同处理均提高了果实的营养品质,喷尿素的总糖量、糖酸比最大,其次是混合氮处理,全铵处理最小;果实的Vc含量以混合氮处理较高,全铵处理的最低;果实中花青素的含量顺序为:全硝尿素混合氮全铵CK。果实硝酸盐含量从高到低依次为:全硝混合氮全铵尿素CK;硝态氮促进了果实生长,各处理平均单果重为全硝混合氮全铵尿素CK。综上结果,尿素及适当的硝态氮配比有利于巨峰葡萄果实品质的提高。     

华北山前平原农田土壤硝态氮淋失与调控研究

本文依托中国科学院栾城农业生态系统试验站小麦-玉米一年两熟长期定位试验, 应用土钻取土和土壤溶液取样器取水的方法, 研究了不同农田管理措施下土壤硝态氮的累积变化, 计算了不同氮肥处理通过根系吸收层的硝态氮淋失通量。结果表明, 小麦-玉米生长季土壤硝态氮累积量和淋失量随着施氮量的增加显著增加, 相同氮肥水平下增施磷、钾肥增加了作物的收获氮量, 施磷肥增加的作物收获氮量最高可达123kg·hm^-2·a^-1, 施钾肥增加的作物收获氮量最高为31 kg·hm^-2·a^-1。不同灌溉水平下0~400 cm 土体累积硝态氮随着灌溉量的增加而降低, 控制灌溉(小麦季不灌水, 玉米季灌溉1 水)、非充分灌溉(小麦季灌溉2~3 水, 玉米季按需灌溉)、充分灌溉(小麦季灌溉4~5 水, 玉米季按需灌溉)各处理剖面累积硝态氮量分别为1 698 kg·hm^-2、1148 kg·hm^-2 和961 kg·hm^-2。与非充分灌溉和充分灌溉处理相比, 控制灌溉在100~200 cm 土层硝态氮累积量显著高于其他层次, 2003~2005 年间控制灌溉剖面增加的硝态氮量占施肥总量的23%; 非充分灌溉处理剖面增加的硝态氮量占施肥总量的22%; 充分灌溉处理剖面增加的硝态氮量占施肥总量的47%。免耕措施降低了作物产量, 影响土壤水的运移, 增加了硝态氮的淋失风险。根据作物所需降低氮素投入(N 200 kg·hm^-2·a^-1), 增施磷、钾肥, 控制灌溉量是减少华北山前平原地区硝态氮淋失, 保护地下水的有效措施。     

薄层营养液膜技术(NFT)水培多年生黑麦草对不同富氮废水的净化效果

采用薄层营养液膜技术(NFT)培育多年生黑麦草(Lolium perenne L),以草带为植物滤器净化5种不同配置的富氮废水,废水10 d更换一次.试验结果表明在短期内(2d),TAN、NO-2-N和NO-3-N的去除量均在本身高水平而其他成分低水平的试验组达到最高,4组非离子氨UIA的净化率均高于99%.所有废水的pH值在2 d后均被控制在6.5～8.0.以上述3种氮90%的净化率为目标,废水G3(初始浓度为TAN:40 mg·L-1,NO-2-N:40 mg·L,NO-3-N:10 mg·L-1)和CK(仅在26.77 L自来水中加入18.36 g四水硝酸钙)需2d,废水G4(TAN:40 mg·L-1,NO-2-N:4 mg·L-1,NO-3-N:10 mg·L-1)需4 d,废水G1(TAN:140 mg·L-1,NO-2-N:40 mg·L-1,NO-3-N:80 mg·L-1)、废水G2(TAN:140mg·L-1,NO-2-N:40 mg·L-1,NO-3-N:10 mg·L-1)仅TAN和NO-2-N在6 d内完成.试验结束时G3草净增长最高(169.3 mm),并获得最大干草产量0.205 kg·m-2,G4获得最大鲜草产量1.48 kg·m-2.     

Denitrification Efficiency in Groundwater Adjacent to Ditches within Constructed Riparian Wetlands: Kankakee Watershed,Illinois-Indiana,U.S.A.

Dual isotope evaluations of NO₃ ^- in groundwater adjacentto ditches within constructed riparian wetlands across the Kankakee watershed may assist the determination of denitrificationefficiency. Groundwater sampling indicates that NO₃ ^--N exceeded 10 mg L^-1 in constructed riparian wetlands but not innative wetlands within the riparian zones of the Kankakee basin. Anapparent local empirical threshold for nitrification occurs in groundwater near ditches with less then 1:11 depth to width dimensions within similar hydrogeology. The ¹⁵N and ¹⁸Ocomposition of groundwater nitrate varies widely in these constructed riparian wetlands. Groundwater nitrate associated with broader ditches (e.g. 1:35) most closely matches the denitrification isotope signature of native riparian wetlands in the basin. The geometry of various cut and fill landforms may need evaluation in engineering designs for constructed riparian wetlands to ensure the establishment of local natural groundwaterflow conditions for efficient nitrate attenuation.     

Assessment of Ionic Interferences to Nitrate and Potassium Analyses with Ion-Selective Electrodes

Ion-selective electrodes (ISEs) are simple tools used for rapid measurement of nitrate nitrogen (NO₃-N) and potassium (K) concentrations in plant sap. With the development of best management practices (BMPs), interest exists in using ISEs for soil leachate and soil and fertilizer solutions. Nitrate N and K concentrations in the 0 to 10,000 mg L^–1 ISE working range were measured in diluted solutions of common salts to assess ionic interference of calcium (Ca²⁺), ammonium (NH₄ ⁺), chloride (Cl^–), and sulfate (SO₄ ^2–). The effects of meter (replication) were unexpectedly significant in one out of three ranges for NO₃-N and K (P values of 0.50, 0.72, and 0.01 for NO₃-N and 0.99, 0.01, and 0.74 for K, for the 0–100, 100–1,000 and 1,000–10,000 mg L^–1 ranges, respectively). The responses of calculated NO₃-N and K concentrations to measured NO₃-N and K concentrations were linear, but slopes ranged from 0.85 to 1.54, from 0.24 to 2.72, and from 0.93 to 5.48 for NO₃-N and from 0.80 to 1.01, from 0.71 to 1.39, and from 0.93 to 2.21 for K for the 0–100, 100–1,000, and 1,000–10,000 mg L^–1 measuring ranges, respectively. All slopes were significantly different from zero, and several were significantly different from each other and the 1:1 line. Pairwise slope comparisons conducted with covariance analysis showed that SO₄ ^2– alone interfered with NO₃-N measurements at concentrations ranging from 34 to 171 mg L^–1, which was less than the manufacturer's information, and by its presence in combination with K⁺, NH₄ ⁺, Ca²⁺, and Cl^– within the medium and high concentration ranges. Potassium measurements were not subject to interference from the ions tested for all three concentration ranges. These results highlight the importance of using quality assurance / quality control (QA/QC) samples in the set of unknown samples to detect inacceptable departure from linearity in routine analysis. The increase in measurement variability from one range to the next showed the importance of keeping measurements within a single concentration range by using dilutions. Hence, ISEs may be used for field measurements of NO₃-N and K concentrations in soil leachate as well as soil and nutrient solutions and are therefore a practical BMP tool. However, ISEs should not be used as substitutes for the laboratory methods when official measurements are needed.     

不同铵硝比对菠菜生长、安全和营养品质的影响

通过水培试验,研究了等氮条件下5种不同铵硝比对菠菜生长和品质的影响。结果表明:(1)从铵硝比100∶0到0∶100,菠菜地上部鲜重不断增加,铵硝比为0∶100时,菠菜的鲜重达最大值;但铵硝比25∶75和0∶100两个处理菠菜的干物重没有显著差异(p<0.05)。(2)随着铵硝比的降低,菠菜茎叶中硝酸盐、亚硝酸盐的含量均表现为线性增加;菠菜茎叶中可溶性草酸的含量和营养液中铵硝比之间呈现出二次曲线相关,在铵硝比为25∶75时,菠菜茎叶中草酸含量最低。适当增施铵态氮有利于降低菠菜硝酸盐、亚硝酸盐及草酸的含量。(3)增铵可以提高菠菜Vc含量,铵硝比为50∶50的处理菠菜Vc含量最高;随着铵硝比的下降,菠菜茎叶中可溶性糖的含量逐渐降低,而粗蛋白的含量则以铵硝比25∶75处理最高。     

氮素不同形态配比对菠菜体内游离氨基酸含量和相关酶活性的影响

采用溶液培养试验,研究了氮素不同形态配比对菠菜茎叶中游离氨基酸含量及3种主要氮代谢酶活性的影响。结果表明:1)随着营养液中铵硝比(NH4+-N/NO3--N)的降低,菠菜茎叶中游离氨基酸的总量呈下降趋势。在全硝营养下(NH4+-N/NO3--N=0∶100)下,菠菜茎叶中游离氨基酸的总量只有全铵营养(NH4+-N/NO3--N=100∶0)的34.4%。2)在全铵营养下,菠菜茎叶中游离氨基酸的主要组分是谷氨酰胺、精氨酸和谷氨酸,三者占游离氨基酸总量的百分比依次为39.8%、20.2%和8.9%;在全硝营养下,菠菜茎叶中游离氨基酸以谷氨酸、天冬氨酸和丝氨酸为主,三者占游离氨基酸总量的百分比分别为30.3%1、8.6%和8.5%。3)提高营养液中硝态氮的比例,可以显着提高菠菜茎叶中硝酸还原酶(NR)的活性,同时降低了谷氨酸脱氢酶(GDH)的活性,谷氨酰胺合成酶(GS)活性则呈现先升后降的抛物线状变化规律。4)菠菜茎叶中NR活性与谷胺酰胺含量之间存在着显著负相关关系(r=-0.968)。     

碱性过硫酸钾氧化法测定溶液中全氮含量氧化剂的选择

对碱性过硫酸钾氧化法测定溶液中全氮含量采用的氧化剂进行了比较研究。结果表明,氧化反应过程中溶液的pH值与氧化剂的效果有密切关系;氧化剂中过硫酸钾与NaOH配比合适,有利于溶液中的氮素转化为NO3--N。3％过硫酸钾与0.15mol.L-1NaOH配合是一个适宜的氧化剂,可测定的尿素最大浓度为N,80mgL-1,可定量地回收L-丙氨酸及EDTA溶液所含的氮素,测定的0.5mol.L-1K2SO4土壤浸提液中的全氮与开氏法结果基本一致。     

日光温室番茄灌水量与根层硝态氮淋溶特征及渗漏关系研究

针对蔬菜灌溉水肥渗漏问题,采用田间试验和室内分析相结合,研究了番茄膜下沟灌灌水量与土壤硝态氮的根层外渗漏关系,分析了灌水量与不同根层土壤硝态氮的淋溶和保蓄特征,结果表明:灌溉不施肥条件下灌水量与土壤硝态氮淋溶量和淋溶率、灌溉施肥条件下灌水量与土壤施入硝态氮的保蓄率和渗漏率均呈直线关系;灌溉均会引起浅根层(0—20 cm)硝态氮淋溶,灌溉施肥条件下7.5～15 mm灌水量范围硝态氮积累有一个峰值,而22.5～45 mm范围则有两个峰值;灌水量在7.5～15mm之间,灌溉不施肥条件下根层土壤硝态氮淋溶率为0,灌溉施肥条件下土壤硝态氮渗漏率为0～5.19%;灌水量在22.5～45 mm之间,灌溉不施肥土壤硝态氮淋溶率为5.38%～19.08%,灌溉施肥条件下根层土壤硝态氮渗漏率为21.91%～61.96%。日光温室番茄膜下沟灌能减少肥料淋溶与渗漏的节水灌水量为15 mm。