珠江三角洲典型地区蔬菜硝酸盐与亚硝酸盐污染评价

研究了珠江三角洲典型地区中山市大型蔬菜生产基地中9种蔬菜30个样品中硝酸盐与亚硝酸盐的污染现状,初步摸清了蔬菜中硝酸盐及亚硝酸盐的污染状况。并以WHO/FAO规定的日允许摄入量换算得到的标准评价了其主要蔬菜品种的硝酸盐污染状况。结果表明:在被调查的蔬菜中,硝酸盐含量由高到低依次为菜心→白菜>芥菜→空心菜→生菜→瓜果类,菜心、芥菜和白菜为严重污染,生菜与空心菜为重污染,瓜果类蔬菜为轻污染;亚硝酸盐含量普遍较低,均未超标。因而有必要采取有效的污染防治措施控制该地区蔬菜中的硝酸盐污染状况。     

低镉铅菜心品种田间试验研究

华南地区不少农田土壤受到Cd/Pb污染,为了得到可以应用的低积累Cd/Pb的菜心(Brassica parachinensis L.)品种,在广东省2个典型重金属污染农田,包括代表有色金属矿区的韶关市翁源县和珠江三角洲的广州市白云区,分别于2017年和2018年开展大田试验,种植了3个已经筛选的品种(2个低Cd品种LGL、YL702和1个高Cd品种ZCCX)和3个当地菜心品种(翁源CCXW、CJ60、TL60;白云CCXW、CXSH、CL80),测定作物产量和食用部位重金属含量。结果表明,本研究所选用的菜心品种茎叶Cd含量在轻微污染土壤上(Cd质量分数介于0.3—0.6mg·kg-1)均能符合国家食品卫生标准(0.2 mg·kg-1)。翁源试验区土壤为酸性,菜心对Cd的富集系数较高,变化于0.4—0.6之间;对Pb的富集系数相对较小,变化于0.000 5—0.000 9之间。在翁源试验区Pb重度污染土壤条件下种植的4个菜心品种,其茎叶Pb含量超过国家食品卫生标准(0.3 mg·kg-1),只有LGL和TL60品种符合食品卫生标准,为新筛选出的低积累Pb的品种,然而TL60产量低。白云区的试验土壤为弱酸性,菜心对Cd的富集系数变化于0.07—0.22之间,对Pb的富集系数变化于0.000 3—0.000 7之间,并核实了LGL为较高产低积累Cd、Pb的菜心品种。不同品种的菜心茎叶富集重金属的能力还受生长期长度和成熟期类型的影响,值得进一步试验研究。     

广州市蔬菜地重金属剂量对蔬菜富集重金属的影响--以菜心为例

调查并分析了广州市蔬菜地土壤和菜心中主要重金属元素质量分数，通过多元统计分析建立了菜心中某一重金属元素和土壤中元素的数学回归模型。结果表明，Cd更易在菜心体内造成累积；总体上菜心中重金属质量分数与其在土壤中的质量分数有一定的相关性，菜心中Pb、As的积累分别取决于土壤中Pb、As的质量分数，土壤中Pb和As还分别促进了菜心对Cr、Hg的吸收，Pb对菜心中Cd的累积表现为协同作用；土壤重金属质量分数临界值可为今后无污染蔬菜的生产提供参考依据。     

盐生杜氏藻对硝酸盐的转运特性

盐生杜氏藻(Dunaliella salina)是已知最耐盐的真核光合生物,硝酸盐作为盐生杜氏藻氮源的主要来源,影响盐生杜氏藻的生长代谢,研究盐生杜氏藻对硝酸盐的转运吸收状况,可为生长于高盐、低盐环境中作物吸收氮的研究提供理论基础.以水杨酸法测定硝酸盐浓度,设计相关实验,结果发现盐生杜氏藻在低浓度的硝酸盐(0.2mmol/L)溶液中对硝酸盐有吸收,吸收效率随硝酸盐浓度的增大而提高;当盐浓度为2mol/L时其硝酸盐吸收效率最高,说明一定的盐浓度能诱导盐生杜氏藻对硝酸盐的吸收;经(NH_4)~+预处理过的盐生杜氏藻,在相同硝酸盐浓度下培养时其硝酸盐吸收效率比未经(NH_4)~+预处理的低.实验结果提示盐生杜氏藻存在高亲和性的硝酸盐转运蛋白.图6参17     

土壤中常见离子在紫外区的吸收特性──Ⅱ.高浓度离子溶液与低浓度混合

探讨不同离子浓度与不同无机溶液的混合对紫外光吸收的影响,结果表明,盐酸盐在较高浓度下吸收值迅速增大,吸收峰向红区移动,而硫酸盐在远紫区有一定程度的吸收,KH2PO4与NH4F接近无吸收。多数情况下,无机溶液对紫外光的吸收主要决定于阴离子类型,而与阳离子无关.不同类型溶液的混合基本不改变溶液的吸收特性,硝酸盐在低浓度下对紫外的吸收极为稳定,基本不受共存离子的干扰。0.01mol/LCuSO4与2mol/LKCI吸收峰与硝酸盐吸收峰重叠,但饱和CaSO4与硝酸盐吸收峰不重叠。     

保护地番茄养分利用及土壤氮素淋失

在施用不同复合肥料的条件下,对保护地蔬菜蕃茄对N、P、K养分的吸收利用及保护地条件下土壤的硝酸盐淋洗进行了研究,结果表明,复合肥的品种及施肥水平对番茄的产量影响不大,与CK相比番茄果实增产12．．7％－18．4％;复合肥N、P养分的当季利用率不足10％,而K素的当季利用率也不超出25％,传统的大水漫灌条件,蔬菜保护地土壤硝酸盐的淋洗状态相当严重,并有可能造成地下水的硝酸盐污染,长期过量施肥及大小漫灌等措施是造成土壤养分累积、硝酸盐淋洗严重、肥料利用率低的根本原因,图2表3参11     

两种菠菜累积硝酸盐特性差异的研究

水培试验结果表明,日本超能菠菜生长后期的生长量较大,硝酸盐累积量较低,氮素吸收量较少,可以肯定其优良性;在生长后期供给等量硝、铵态氮的条件下,日本超能菠菜吸收硝态氮较少,还原硝酸盐的相对能力又较高,因而累积硝酸盐较宁夏圆叶菠菜低;在仅供给铵态氮源的条件下,日本超能菠菜还原硝酸盐能力较小,可能与其易于吸收和利用铵态氮源有关。     

镉对不同硝酸盐累积型小白菜及根际土壤氮素转化的影响

镉污染是农业生态和农产品安全的重大威胁。采用盆栽方法,对比分析硝酸盐高、低累积型品种的小白菜Brassica chinens(前者为品种H,抗病矮脚黄;后者为品种L,金夏时青梗菜)对镉污染的响应,探究不同镉水平对小白菜-土壤系统氮素吸收和转化效应,以期为城郊蔬菜的安全生产提供依据。结果表明,在土壤镉质量分数为0~0.5 mg·kg-1时,小白菜生长不受影响,品种间氮素累积量为品种H品种L。随着镉质量分数的增加,2个品种小白菜生物量均显著降低,品种H单株鲜质量最大降幅达20%,表现更为敏感。镉质量分数高于0.5 mg·kg-1时,显著降低了品种H的氮素吸收和利用,而对低累积品种影响不显著。2个品种小白菜体内硝酸盐含量均在较低的镉质量分数(0.5~1.0 mg·kg-1)处理下有所降低,而当镉质量分数达5.0 mg·kg-1时有所增加,同样是品种H表现更为敏感。随着镉污染水平的增加,小白菜体内镉积累量显著增加,其中品种H在镉质量分数达5.0 mg·kg-1时,累积速率明显降低。通过一元二次模型拟合镉和土壤无机氮质量分数可以得出,镉质量分数为7.1 mg·kg-1时,2个品种小白菜土壤无机氮质量分数均达到最高,分别为34.83和23.73 mg·kg-1。不同品种小白菜在镉污染水平较低时,均具有一定的抗性,而随着镉含量的增加,不同品种对镉毒害响应不同。因此,城郊土壤不同镉污染区域小白菜的种植可依据其品种特性进行选择,从而为蔬菜的生长和土壤的改良提供保障。     

水分和氮素供应对菠菜硝酸盐累积和钾素吸收的影响

研究了水分和氮素供应对露地秋菠菜的硝酸盐累积和钾、氮吸收的影响。结果表明：与传统的水氮管理措施相比，采用水分平衡法和氮素专家系统进行的水氮供应并没有造成作物减产，但对钾、氮元素的吸收却有明显的影响，同氮素吸收相比，作物对钾素的吸收数量更高；并且作物对钾、氮的吸收比例随氮素供应水平的增加而降低，试验还动态监测了菠菜最新展开叶的叶柄汁液中的硝酸盐和K^ 浓度在一天内的变化情况。结果表明，不同水氮处理的菠菜叶柄汁液的硝酸盐浓度在白天均没有发生显著变化；叶柄汁液中的K^ 浓度和NO3^-／K^ 的浓度比在白天受氮素供应水平的影响很大，供氮量高，K^ 浓度和NO3^-／K^ 浓度比的变化也大，但受灌水量影响不大。图3表2参17。     

土壤栽培和无土栽培菜心中内生细菌比较及分离鉴定

菜心(Brassica parachinensis)是华南地区的一种特色蔬菜.为探究无土栽培和土壤栽培菜心内生细菌的差异,以这两种栽培方式的菜心为材料,分离内生细菌.根据插入序列指纹图谱(IS-PCR)结果进行聚类,对代表性菌株的16S rRNA基因序列进行系统发育分析,并将菌株加入无土栽培营养液中,收获后测定菜心的的相对叶绿素含量(SPAD)和可溶性糖含量.结果显示,从两种菜心中共分离到31株内生细菌,IS-PCR结果将其聚为9个类群,16S rRNA基因鉴定其分别属于Bacillus sp.(芽孢杆菌属)、Rhizobium sp.(根瘤菌属)、Microbacterium sp.(微杆菌属)、Leifsonia sp.(雷夫松氏菌属)、Sphingomonassp.(鞘氨醇单胞菌属)、Alcaligenessp.(产碱菌属)和Agrobacteriumsp.(农杆菌属).土壤栽培菜心中可培养细菌数目多于无土栽培菜心,且土壤栽培菜心中内生细菌的碳代谢更多样化.生理生化实验显示,部分菌株能分泌生长素和铁载体.加入土壤栽培菜心中分离得到的菌株SCG14和SCG0802后,无土栽培菜心的相对叶绿素含量和可溶性糖含量比对照显著提高.本研究表明无土栽培和土壤栽培的菜心中的内生细菌在种类、数目、分布部位和碳源利用能力上有差异;此外,分离得到的菌株能提高无土栽培菜心的相对叶绿素以及可溶性糖含量,有开发为微生物制剂的潜力.(图4表6参35)     

黑麦草在模拟人工湿地中对奶牛场污水高浓度氮的吸收转化

以土壤为基质,黑麦草(Lolium multiflorm)为植被,通过模拟间歇性人工湿地净化系统处理不同质量浓度的奶牛场污水试验,研究黑麦草对高质量浓度畜牧场污水中氮的吸收转化效果.结果表明,黑麦草在间歇性进水的污水质量浓度高达TN(816.8±125.1) mg·L~(-1),NH_4~+-N(443.6±97.9) mg·L~(-1),NO_3~--N(141.5±51.7) mg·L~(-1)都能较好的适应,生长良好.在不同浓度处理的净化系统中,水力停留时间为8d的条件下,NH_4~+-N的去除率为75.9%～88.3%;NO_3~--N的去除率平均为69.3%;TN的去除率74.5%～83.1%.该试验黑麦草对污水中氮的吸收转化在系统对氮净化中的贡献率平均为20.03%.     

Interactions between nitrate and ammonium uptake: variation with growth rate,nitrogen source and species

The interaction between nitrate and ammonium uptake was examined as a function of preconditioning growth rate and nitrogen source by adding nitrate, ammonium, or both to nitrogen-sufficient,-deficient, and-starvedSkeletonema costatum (Grev.) Cleve and nitrogen-deficientChaetoceros debilis Cleve. By simultaneously measuring the internal accumulation of intermediates of nitrogen assimilation and the rates of nitrogen assimilation, the metabolic control of nitrogen uptake could be assessed. After the simultaneous addition of nitrate and ammonium to culture, both nitrate and ammonium uptake rates were decreased in comparison with the rates observed when each was added alone, although nitrate uptake was usually decreased more than ammonium uptake. Since both nitrate and ammonium uptake rates vary with time, preconditioning growth conditions, nitrogen sources present, and species, it was necessary to use several different indices to quantify inhibition. In general, ammonium inhibition of nitrate uptake inS. costatum was greatest in cultures preconditioned to ammonium and those at low growth rates, whereas ammonium uptake was inhibited most in cultures preconditioned to nitrate. In nitrogen-deficientC. debilis, nitrate uptake was more inhibited by ammonium, but uptake returned to normal rates more quickly than inS. costatum, whereas inhibition of ammonium uptake was similar. These results explain why the interaction between nitrate and ammonium uptake in the field can be so variable. Inhibition of uptake is not controlled by internal ammonium or total amino acids, nor is it related to the inability to reduce nitrate. Instead, inhibition must be determined in part by the external concentration of nitrogen compounds and in part by some intermediate(s) of nitrogen assimilation present inside the cell.Bigelow Laboratory Contribution No. 82022     

Response of marine phytoplankton to nitrogen deficiency: Decreased nitrate uptake vs enhanced ammonium uptake

The uptake of nitrate and ammonium was measured separately in uni-algal, nitrogen-deficient cultures of four species of marine phytoplankton. Nitrogen-deficient phytoplankton took up ammonium at initial rates which greatly exceeded those measured for nitrogen-sufficient phytoplankton. However, nitrate uptake by nitrogendeficient cultures was generally much slower than either nitrate or ammonium uptake by nitrogen-sufficient cultures or ammonium uptake by nitrogen-deficient cultures. Considerable species differences were observed in the degree to which nitrogen deficiency increased ammonium uptake or decreased nitrate uptake. Loss of ability to take up nitrate, but enhanced ability to take up ammonium, as a result of nitrogen deficiency may be an adaptation to the different mechanisms by which nitrate and ammonium are supplied to the euphotic zone. In areas with an intermittent supply of nitrogen, changes in the ability of some species to take up nitrogen as a result of nitrogen starvation will influence species composition and complicate interpretations of measurements of nitrogen uptake.Contribution no. 1249 from the Department of Oceanography, University of Washington, and contribution no. 82006 from the Bigelow Laboratory for Ocean Sciences     

The rapid response of the marine diatom Skeletonema costatum to changes in external and internal nutrient concentration

A nitrogen-deficient batch culture of the marine diatom Skeletonema costatum, when resupplied with a mixture of nitrate and ammonium, showed an initial enhanced nitrate uptake rate leading to a large internal concentration (pool) of nitrate. Following this initial nitrate uptake event, nitrate uptake ceased, and nitrate assimilation was inhibited until the ammonium present was used. At this point, nitrate uptake resumed and nitrate assimilation began. No internal ammonium pool was observed during nitrate utilization, but a large nitrate pool remained throughout the utilization of external nitrate. The internal nitrate pool decreased rapidly after exhaustion of nitrate from the culture medium, but growth of cellular particulate nitrogen continued for about 24 h. A mathematical simulation model was developed from these data. The model cell consisted of a nitrate pool, ammonium pool, dissolved organic nitrogen pool, and particulate nitrogen. It was found that simple Michaelis-Menten functions for uptake and assimilation gave inadequate fit to the data. Michaelis-Menten functions were modified by inclusion of inhibitory and stimulatory feedback from the internal pools to more accurately represent the observed nutrient utilization.     

准好氧填埋渗滤液中氮转化机理

依据准好氧填埋的原理构建了填埋试验装置,在填埋装置各个层次设计采样装置.定期采集渗滤液进行分析,测定各个层次区域渗滤液中氨氮、硝态氮、亚硝态氮和总氮的质量浓度,分析各形态氮之间的变化规律与相关性,初步探讨氮转化的机理.结果表明,准好氧填埋上层区域中,渗滤液的氨氮与硝态氮质量浓度变化相关性极显著;中层和下层区域由于处于兼氧和厌氧状态,硝化作用较弱,渗滤液中氨氮与硝态氮质量浓度变化相关性不显著.上层渗滤液中氨氮与总氮相关性不显著,中层和下层氨氮与总氮相关性极显著,表明中层和下层区域中,渗滤液的氨氮质量浓度变化是导致总氮含量变化的主要贡献因素.     

The kinetics and possible significance of nitrate uptake by several algal-invertebrate symbioses

Nitrification in the coral reef community at Lizard Island, Great Barrier Reef, Australia, elevated the nitrate concentration to above that of the nearby open ocean water. Reef corals and a zooxanthellae-bearing foraminiferan were shown to take up nitrate from nitrate-enriched seawater; a lag period was absent, indicating that the responsible enzymes did not require induction. The relationship of nitrate uptake to seawater nitrate concentration could be described by a hyperbola with a non-zero intercept on the abscissa. Corals are opportunistic in acquiring nitrogen; in addition to gaining particulate nitrogen from ingested food, they acquire dissolved nitrogen in the form of nitrate, ammonia and urea.     

铜绿微囊藻、四尾栅藻和小环藻竞争实验培养基的选择

改变培养基的氮源形态和碳源浓度,研究铜绿微囊藻、小环藻和四尾栅藻的单藻增长行为,筛选适宜的培养基作为混藻竞争实验的共培养基。研究表明,铜绿微囊藻和四尾栅藻在氨氮培养基中的最大生物量K和最大比增长速率r均不及以硝态氮为氮源的培养基;添加高浓度HCO3-(NaHCO3 1.410 mmol/L)能够提高铜绿微囊藻和四尾栅藻藻细胞对氨氮的吸收能力;较低碳源浓度(NaCO3 0.0943 mmol/L)的培养基中,四尾栅藻的初始比增长速率及生物量远高于铜绿微囊藻,但其最大比增长速率r低于铜绿微囊藻,在实验的第10天左右铜绿微囊藻的生物量超过四尾栅藻;小环藻不能在较高浓度碳源(NaHCO3 1.504 mmol/L)下存活;铜绿微囊藻、四尾栅藻与小环藻均可在以氨氮(HA)或硝态氮(HN)为氮源的培养基中单独培养并达到实验所需生物量,因此,HN和HA可以作为实验室内这三种藻共培养适宜的培养基,为今后研究藻类种间资源竞争机制提供实验依据。     

有机肥对土壤NO3--N累积的影响

长期定位试验和调查取样的结果表明,土壤中NO3--N的累积量随有机肥施用量的增加而增加,过量施用有机肥会引起2 m以下深层次土壤中NO3--N的大量累积。当有机肥和无机肥配合施用时,土壤中NO3--N的累积量随总施N量的增加而增加。有机肥对土壤NO3--N累积的影响和对地下水的潜在威胁不容忽视。     

水肥耦合效应对保护地土壤硝态氮运移的影响

采用二次回归正交旋转组合设计,研究了水肥耦合效应对保护地土壤硝态氮运移的影响。结果表明,0—20cm土层硝态氮含量主要受灌水和施氮的影响,且灌水影响程度大于施氮,灌水与0—20cm土层硝态氮含量呈负相关,而与施氮呈正相关。20—40cm土层和40—60cm土层硝态氮也主要受灌水和施氮的影响,但施氮影响程度大于灌水。灌水和施氮对0—20cm土层硝态氮含量影响有相互拮抗作用。施磷对3个层次土壤硝态氮含量影响都很小。