Fungicide and cultivar affect post-anthesis patterns of nitrogen uptake, remobilization and utilization efficiency in wheat

Three successive field experiments (2000/01-2002/03) assessed the effect of wheat cultivar (Consort.. Hereward and Shamrock) and fungicide (epoxiconazole and azoxystrobin) applied at and after flag leaf emergence on the nitrogen in the above-ground crop (Total N) and grain (Grain N), net nitrogen remobilization from non-grain tissues (Remobilized N). grain dry matter (Grain Dill), and nitrogen utilization efficiency (NUtE(g) = Grain DM/Total N). Ordinary logistic curves were fitted to the accumulation of Grain N, Grain DM and Remobilized N against thermal time after anthesis and used to simultaneously derive fits for Total N and NUtE(g). When disease was controlled, Consort achieved the greatest Grain DM, Total N, Grain N and NUtEg; in each case due mostly to longer durations, rather than quicker rates, of accumulation. Fungicide application increased final Grain Dill.. Grant N, Total N and Remobilized N, also mostly through effects on duration rather than rate of accumulation. Completely senesced leaf laminas retained less nitrogen when fungicide had been applied compared with leaf laminas previously infected severely with brown rust (Puccinia recondita) and Septoria tritici, or with just S. tritici. Late movement of nitrogen out of fungicide-treated laminas contributed to extended duration of both nitrogen remobilization and grain N filling, and meant that increases in NUtE(g) could occur without simultaneous reductions in grain N concentration.

The effects of triazole and strobilurin fungicide programmes on nitrogen uptake, partitioning, remobilization and grain N accumulation in winter wheat cultivars

Field experiments were conducted over 3 years to assess the effect of a triazole fungicide programme, and additions of strobilurin fungicides to it, on nitrogen uptake, accumulation and partitioning in a range of winter wheat cultivars. Commensurate with delayed senescence, fungicide programmes, particularly when including strobilurins, improved grain yield through improvements in both crop biomass and harvest index, although the relationship with green area duration of the flag leaf (GFLAD) depended on year and in some cases, cultivar. In all years fungicide treatments significantly increased the amount of nitrogen in the above-ground biomass, the amount of nitrogen in the grain and the nitrogen harvest index. All these effects could be linearly related to the fungicide effect on GFLAD. These relationships occasionally interacted with cultivar but there was no evidence that fungicide mode of action affected the relationship between GFLAD and yield of nitrogen in the grain. Fungicide treatments significantly reduced the amount of soil mineral N at harvest and when severe disease had been controlled, the net remobilization of N from the vegetation to the grain after anthesis. Fungicide maintained the filling of grain with both dry matter and nitrogen. The proportionate accumulation of nitrogen in the grain was later than that of dry matter and this difference was greater when fungicide had been applied. Effects of fungicide on grain protein concentration and its relationship with GFLAD were inconsistent over year and cultivar. There were several instances where grain protein concentration was unaffected despite large (1(.)5 t/ha) increases in grain yield following fungicide use. Dilution of grain protein concentration following fungicide use, when it did occur, was small compared with what would be predicted by adoption of other yield increasing techniques such as the selection of high yielding cultivars (based on currently available cultivars) or by growing wheat in favourable climates.

The Ni-Cu-PGE sulfide ores of the komatiite-hosted Fortaleza de Minas deposit, Brazil: Evidence of hydrothermal remobilization

The Fortaleza de Minas Ni-Cu-PGE sulfide deposit is hosted by Archean komatiitic rocks of the Morro do Ferro greenstone belt, near the southwestern margin of the Sa (aFrancisco) over tildeo Francisco craton, Minas Gerais state, Brazil. The deposit contains 6 million tonnes of ore with an average grade of 2.2 wt% Ni, 0.4% Cu, 0.05% Co and 1.2 ppm PGE+Au, and comprises (i) a main orebody, which is metamorphosed, deformed and transposed along a regional shear zone, consisting mainly of disseminated, brecciated and stringer sulfide ores that are interpreted to be of early magmatic origin, and (ii) PGE-rich discordant veins that are hosted in N-S- and NE-SW-trending late faults that cross-cut the main orebody. The discordant PGE-rich ore (up to 4 ppm total PGE) is characterized by thin, discontinuous and irregular veins and lenses of massive sulfides hosted by serpentinite and talc schist, and is relatively undeformed if compared with the early types of ore. It is composed mainly of pyrrhotite, pentlandite, chalcopyrite, magnetite, carbonates, and amphiboles, with minor cobaltite-gersdorffite, sphalerite, ilmenite, and quartz, and rarely maucherite (Ni11Asg), tellurides and platinum-group minerals (PGM). Omeeite, irarsite, sperrylite, and Ni-bearing merenskyite are the main PGM, followed by minor amounts of testibiopalladite and an unknown phase containing Ru, Te, and As. The PGM occur either included in, or at the margins of, sulfides, sulfarsenides, silicates and oxides, or filling fractures in pyrrhotite, pentlandite, and chalcopyrite, suggesting that they started to precipitate with these minerals and continued to precipitate after the sulfides were formed. The mantle-normalized metal distribution of the two samples of discordant veins shows distinct patterns: one richer in Ni-Pd-Ir-Rh-Ru-Os and another with higher amounts of Cu-Pt-Bi. Both are strongly depleted in Cr if compared with the metamorphosed magmatic ore of this deposit, which follows the general Kambalda-type magmatic trend. on the basis of structural, mineralogical and geochemical evidence, we propose that the PGE-rich discordant ore may have formed by remobilization of metals from the deformed, metamorphosed magmatic orebody (which shows a depleted pattern in these elements) by reduced (pyrrhotite - pentlandite - pyrite are stable), neutral to alkaline and carbonic fluids (carbonate-stable). The PGE may have been transported as bisulfide complexes, and precipitated as tellurides (mainly Pd) and arsenides (Pt, Rh, Ru, Os, Ir) in the late N-S and NE-SW-trending faults owing to a decrease in the activity of S caused by the precipitation of sulfides in the veins.

Nitrogen metabolism and remobilization during senescence

Senescence is a highly organized and well‐regulated process. As much as 75% of total cellular nitrogen may be located in mesophyll chloroplasts of C3‐plants. Proteolysis of chloroplast proteins begins in an early phase of senescence and the liberated amino acids can be exported to growing parts of the plant (e.g. maturing fruits). Rubisco and other stromal enzymes can be degraded in isolated chloroplasts, implying the involvement of plastidial peptide hydrolases. Whether or not ATP is required and if stromal proteins are modified (e.g. by reactive oxygen species) prior to their degradation are questions still under debate. Several proteins, in particular cysteine proteases, have been demonstrated to be specifically expressed during senescence. Their contribution to the general degradation of chloroplast proteins is unclear. The accumulation in intact cells of peptide fragments and inhibitor studies suggest that multiple degradation pathways may exist for stromal proteins and that vacuolar endopeptidases might also be involved under certain conditions. The breakdown of chlorophyll‐binding proteins associated with the thylakoid membrane is less well investigated. The degradation of these proteins requires the simultaneous catabolism of chlorophylls. The breakdown of chlorophylls has been elucidated during the last decade. Interestingly, nitrogen present in chlorophyll is not exported from senescencing leaves, but remains within the cells in the form of linear tetrapyrrolic catabolites that accumulate in the vacuole. The degradation pathways for chlorophylls and chloroplast proteins are partially interconnected.

Environmental effects of thermal and radioactive discharges from nuclear power plants in the boreal brackish-water conditions of the northern Baltic Sea

During recent decades, thermal and radioactive discharges from nuclear power plants into the aquatic environment have become the subject of lively debate as an ecological concern. The target of this thesis was to summarize the large quantity of results obtained in extensive monitoring programmes and studies carried out in recipient sea areas off the Finnish nuclear power plants at Loviisa and Olkiluoto during more than four decades. The Loviisa NPP is located on the coast of the Gulf of Finland and Olkiluoto NPP on that of the Bothnian Sea. The state of the Gulf of Finland is clearly more eutrophic; the nutrient concentrations in the surface water are about 1½ 2 times higher at Loviisa than at Olkiluoto, and the total phosphorus concentrations still increased in both areas (even doubled at Loviisa) between the early 1970s and 2000. Thus, it is a challenge to distinguish the local effects of thermal discharges from the general eutrophication process of the Gulf of Finland. The salinity is generally low in the brackish-water conditions of the northern Baltic Sea, being however about 1 higher at Olkiluoto than at Loviisa (the salinity of surface water varying at the latter from near to 0 in early spring to 4 6 in late autumn). Thus, many marine and fresh-water organisms live in the Loviisa area close to their limit of existence, which makes the biota sensitive to any additional stress. The characteristics of the discharge areas of the two sites differ from each other in many respects: the discharge area at Loviisa is a semi-enclosed bay in the inner archipelago, where the exchange of water is limited, while the discharge area at Olkiluoto is more open, and the exchange of water with the open Bothnian Sea is more effective. The effects of the cooling water discharged from the power plants on the temperatures in the sea were most obvious in winter. The formation of a permanent ice cover in the discharge areas has been delayed in early winter, and the break-up of the ice occurs earlier in spring. The prolonging of the growing season and the disturbance of the overwintering time, in conditions where the biota has adjusted to a distinct rest period in winter, have been the most significant biological effects of the thermal pollution. The soft-bottom macrofauna at Loviisa has deteriorated to the point of almost total extinction at many sampling stations during the past 40 years. A similar decline has been reported for the whole eastern Gulf of Finland. However, the local eutrophication process seems to have contributed into the decline of the zoobenthos in the discharge area at Loviisa. Thermal discharges have increased the production of organic matter, which again has led to more organic bottom deposits. These have in turn increased the tendency of the isolated deeps to a depletion of oxygen, and this has further caused strong remobilization of phosphorus from the bottom sediments. Phytoplankton primary production and primary production capacity doubled in the whole area between the late 1960s and the late 1990s, but started to decrease a little at the beginning of this century. The focus of the production shifted from spring to mid- and late summer. The general rise in the level of primary production was mainly due to the increase in nutrient concentrations over the whole Gulf of Finland, but the thermal discharge contributed to a stronger increase of production in the discharge area compared to that in the intake area. The eutrophication of littoral vegetation in the discharge area has been the most obvious, unambiguous and significant biological effect of the heated water. Myriophyllum spicatum, Potamogeton perfoliatus and Potamogeton pectinatus, and vigorous growths of numerous filamentous algae as their epiphytes have strongly increased in the vicinity of the cooling water outlet, where they have formed dense populations in the littoral zone in late summer. However, the strongest increase of phytobenthos has extended only to a distance of about 1 km from the outlet, i.e., the changes in vegetation have been largest in those areas that remain ice-free in winter. Similar trends were also discernible at Olkiluoto, but to a clearly smaller extent, which was due to the definitely weaker level of background eutrophy and nutrient concentrations in the Bothnian Sea, and the differing local hydrographical and biological factors prevailing in the Olkiluoto area. The level of primary production has also increased at Olkiluoto, but has remained at a clearly lower level than at Loviisa. In spite of the analogous changes observed in the macrozoobenthos, the benthic fauna has remained strong and diversified in the Olkiluoto area. Small amounts of local discharge nuclides were regularly detected in environmental samples taken from the discharge areas: tritium in seawater samples, and activation products, such as 60Co, 58Co, 54Mn, 110mAg, 51Cr, in suspended particulate matter, bottom sediments and in several indicator organisms (e.g., periphyton and Fucus vesiculosus) that effectively accumulate radioactive substances from the medium. The tritium discharges and the consequent detection frequency and concentrations of tritium in seawater were higher at Loviisa, but the concentrations of the activation products were higher at Olkiluoto, where traces of local discharge nuclides were also observed over a clearly wider area, due to the better exchange of water than at Loviisa, where local discharge nuclides were only detected outside Hästholmsfjärden Bay quite rarely and in smaller amounts. At the farthest, an insignificant trace amount (0.2 Bq kg-1 d.w.) of 60Co originating from Olkiluoto was detected in Fucus at a distance of 137 km from the power plant. Discharge nuclides from the local nuclear power plants were almost exclusively detected at the lower trophic levels of the ecosystems. Traces of local discharge nuclides were very seldom detected in fish, and even then only in very low quantities. As a consequence of the reduced discharges, the concentrations of local discharge nuclides in the environment have decreased noticeably in recent years at both Loviisa and Olkiluoto. Although the concentrations in environmental samples, and above all, the discharge data, are presented as seemingly large numbers, the radiation doses caused by them to the population and to the biota are very low, practically insignificant. The effects of the thermal discharges have been more significant, at least to the wildlife in the discharge areas of the cooling water, although the area of impact has been relatively small. The results show that the nutrient level and the exchange of water in the discharge area of a nuclear power plant are of crucial importance.

Petrogênese das rochas máficas alcalinas do litoral entre São Sebastião (SP) e Parati (RJ)

Lamprófiros e diabásios alcalinos afloram no litoral dos estados de São Paulo e Rio de Janeiro e integram o Enxame de Diques da Serra do Mar (EDSM). Essas rochas ocorrem sob a forma de diques e intrudem o Orógeno Ribeira, de idade Neoproterozóica/Cambro-Ordoviciana, inserindo-se no contexto geodinâmico de abertura do Oceano Atlântico Sul durante o Cretáceo Superior. Essas intrusões são subverticais e orientam-se preferencialmente a NE-SW, seguindo a estruturação das rochas encaixantes. Os lamprófiros são classificados como monchiquitos e camptonitos e exibem, respectivamente, textura hipocristalina e holocristalina. Apresentam também textura panidiomórfica, fenocristais de clinopiroxênio e olivina, imersos em matriz formada essencialmente por esses mesmos minerais, além de biotita, kaersutita e minerais opacos. O camptonito apresenta ainda plagioclásio na matriz. Os diabásios alcalinos são hipocristalinos a holocristalinos, equigranulares a inequigranulares, com fenocristais de olivina e/ou clinopiroxênio e/ou plagioclásio, em uma matriz composta essencialmente por esses minerais. As rochas estudadas caracterizam séries alcalinas miaskíticas, com os lamprófiros sendo tanto sódicos, potássicos e ultrapotássicos e os diabásios alcalinos como predominantemente sódicos. Modelagens petrogenéticas envolvendo possíveis processos evolutivos mostram que é improvável que os lamprófiros sejam cogenéticos por processos evolutivos envolvendo tanto cristalização fracionada, com ou sem assimilação concomitante, quanto hibridização. O mesmo ocorre para os diabásios alcalinos. A discriminação de fontes mantélicas foi feita com base nos teores de elementos traços de amostras representativas de líquidos parentais e indica que esse magmatismo alcalino está relacionado a fontes lherzolíticas com fusão parcial na zona de estabilidade do espinélio, isto é, a poucas profundidades. Os dados litogeoquímicos e isotópicos do sistema Sr-Nd das rochas estudadas sugerem tanto o envolvimento de fontes férteis, associadas ao manto sublitosférico, quanto de fontes enriquecidas, relacionadas ao manto litosférico subcontinental. Modelagens de mistura binária revelam que a petrogênese dos lamprófiros e diabásios alcalinos envolveu uma grande participação de um componente fértil misturado com contribuições menores de um componente enriquecido. Idades TDM (760-557 Ma) obtidas sugerem remobilização do manto litosférico no Neoproterozóico, talvez relacionadas à subducção da Placa São Francisco preteritamente à colisão do Orógeno Ribeira. Altas razões CaO/Al2O3 para os líquidos lamprofíricos menos evoluídos, altos teores de Zr, correlações negativas Zr/Hf e Ti/Eu e associação com carbonatitos indicam condições metassomáticas de alto CO2/H2O. Em escala local, modelos geodinâmicos baseados na astenosfera não isotérmica parecem mais aplicáveis. No entanto, modelos geodinâmicos baseados na astenosfera isotérmica (com o envolvimento de plumas) parecem mais indicados num contexto regional, considerando-se outras províncias alcalinas contemporâneas e correlatas.

Contribution à l'étude des modifications hydro-sédimentaires consécutives à la réouverture artificielle de l'embouchure du Comoé à Grand-Bassam

The Bassam artificial inlet was opened (in September 22, 1987) in order to revacuate offshore invasive aquatic plants. This has considerably modified the hydro-sedimentary environment of the lagoonal domain at Grand-Bassam. Tidal currents effect has confered the lagoonal waters an estuarine feature, the saline intrusion (25-35%o) increased beyond the Moossou bridges up to the confluence of the Comoe river. This has led to a cleaning of the river lower course and above all to the bottoms of the lagoon, which were previously confined. The remobilization of mud (from lagoonal bottoms around Bouet Island) evacuated offshore, has exposed lagoonal and oceanic sandy features. This new system remains fragile, with the seasonal (low river-flow) clogging.

Influência do Complexo Vulcânico de Abrolhos na evolução tectono-sedimentar da porção centro-sul da bacia do Espírito Santo

A busca por novas acumulações de hidrocarbonetos necessita de esforços exploratórios contínuos, gerando novas possibilidades e modelos geológicos e diminuindo os riscos associados à atividade exploratória. O interesse no entendimento da formação de armadilhas, migração e reservatórios de hidrocarbonetos, associado à halocinese motivou a realização deste trabalho. Apresenta-se como principal objetivo deste trabalho a caracterização e a descrição da evolução halocinética na porção centro-sul da bacia do Espírito Santo. Dados de poços, sísmicos e gravimetria foram utilizados com o intuito de gerar uma interpretação geológica integrada, possibilitando entender à influência do Complexo Vulcânico de Abrolhos (CVA) na evolução tectonossedimentar da área, por meio da técnica de restauração de seção geológica. Na área estudada, ocorreu uma intensa atividade halocinética, já a partir do Albiano, em resposta a distensão causada pela subsidência da bacia e a abertura do Atlântico Sul. Durante o Neocretáceo, cunhas clásticas do Rio Doce adentraram na bacia provocando um novo pulso halocinético, resultando num aumento da taxa de sedimentação nas mini-bacias. Em outras regiões esta progradação causou a migração da camada-mãe de sal para porções distais da bacia, acarretando uma deficiência no suprimento de sal. Isto ocasionou o colapso de alguns diápiros associados a uma quiescência tectônica na área. A principal fase tectônica na área ocorreu no Eoterciário, época em que ocorre a implantação do CVA, formando estilos estruturais característicos de terrenos compressivos, com falhas de empurrão, popups, dobras e gotas de sal. Esta nova configuração tectônica na área mudou os eixos dos principais depocentros, que passaram a ser controlados pelos altos estruturais gerados pela tectônica compressiva, e pelos seus baixos relativos, que passaram a receber os sedimentos sin-tectônicos. (As associações destas características de remobilização tectonossedimentar formou uma nova compartimentação, a saber: a) Zona de translação; b) Zona dobrada e c) Zona de Cavalgamento com falhas de empurrão . Esta nova configuração tectônica tem sua formação diretamente relacionada à implantação do CVA.

水稻灌浆期籽粒与 胚乳发育的蛋白质组学分析

籽粒的灌浆是将光合器官合成的有机物贮存在籽粒中的过程。这一过程直接决定了籽粒的产量及品质。先前研究表明灌浆籽粒中贮存物质的累积是各种代谢活动和细胞学过程协同作用的结果，但灌浆的分子机制目前还不是非常清楚。水稻是研究籽粒灌浆的优良模式材料，不仅因为它是世界上最重要的淀粉食物来源，更重要的是其全基因组的测序完成为分子机制的研究带来极大的便利。我们对发育水稻籽粒的观察表明在开花后6 天，籽粒就已完成了胚的分化和胚乳的细胞化；此后籽粒经历了一个显著的细胞增大过程，并在开花后12 天左右达到成熟籽粒的大小；而籽粒的灌浆过程起始于开花后6 天，这个过程一直持续到开花后20 天。因此，我们将开花后6 天到20 天的籽粒分为8 个连续的发育阶段进行动态的蛋白质组分析，396个蛋白点的表达在灌浆过程中发生了两倍以上变化。质谱鉴定得到的345 个差异表达的蛋白划分为10 个不同的功能类别。其中新陈代谢类（45%）和蛋白合成/终点（destination）类（20%）两个功能类别中就包括了大多数的差异表达蛋白，预示着这两类蛋白在籽粒发育中的重要性。蛋白功能群的表达分析显示与淀粉合成和乙醇发酵相关的蛋白在发育过程中大幅度的上调，而与碳代谢中心过程（糖酵解和三羧酸循环）相关蛋白呈现明显的下调趋势。大多数的功能类或（亚类）也呈现出下调的表达趋势，如细胞生长/分裂类，蛋白合成类，水解类，信号传导类和转录类。蛋白表达分析的结果表明蛋白的表达随籽粒的发育发生了显著的变化，这些变化与籽粒在不同阶段的发育和代谢过程密切相关并协调一致，是细胞从生长分裂过渡到以淀粉合成为中心的物质基础。同时也说明代谢重点由中心碳代谢向乙醇发酵的转变对于籽粒的发育和淀粉的合成与累积具有重要意义。 籽粒发育的研究表明在长到成熟籽粒大小后（开花后12 天），籽粒的代谢集中到淀粉累积途径上，一直持续到进入脱水期（18 天），绝大多数淀粉合成相关蛋白在这期间到达表达的顶点。为了解淀粉累积关键时期淀粉合成关键部位（胚乳）的发育规律，我们进一步应用DIGE 技术对这一淀粉累积关键时期（灌浆中后期，开花后12 到18 天）的蛋白表达特性进行分析。细胞学的观察发现胚乳在灌浆后期先后经历了过氧化氢的爆发、半透明胚乳的形成以及胚乳细胞死亡事件。相应的DIGE 分析显示有321 个蛋白点在胚乳的后期发育中发生了显著的表达变化。细胞学的观察结合DIGE 分析显示胚乳的后期发育是一个典型的衰老过程：细胞结构的崩溃；氧化自由基的爆发；脱水干燥；蛋白、脂类和DNA 由同化作用向异化作用的代谢转化。与代谢转化相伴随的细胞营养的重新分配是胚乳后期发育的一个显著过程。DIGE分析全面展示了参与营养重新分配相关蛋白在后期发育中的表达变化，为细胞学中观察到的有机物向淀粉的转化提供了清晰的蛋白水平的证据支持。在鉴定的差异表达蛋白中有2/3 的蛋白是已知的对氧化电位变化敏感的蛋白，表明由H2O2 爆发形成的氧化压力将引起氧化还原调控从而对胚乳的后期发育进行全面的影响。而其中与碳元素代谢相关的代谢途径中尤其富含氧化还原电位敏感的蛋白，表明后期的营养重新分配以及淀粉的累积受到氧化还原电位的紧密调控。另一方面，H2O2 的爆发激发了胚乳中的抗氧化体系。由抗氧化蛋白（如thioredoxin、抗坏血酸和超氧化物歧化酶等）、氧化还原敏感蛋白、代谢中间产物以及glyoxalase 构成的抗氧化体系在胚乳后期发育中协同作用调节氧化还原电位的变化，从而控制胚乳细胞衰老的节奏。另外，我们发现与RraA 相关的转录本的调控在胚乳发育末期急剧上调，在调控的代谢途径、调控时间以及调控的部位与氧化还原调控相重叠，并且支持RraA 活动有利于胚乳细胞对氧化压力的适应。所有这些结果表明内生的过氧化氢（或氧化自由基）在胚乳的后期发育和淀粉累积中起到核心的调控作用。

土壤干旱对小麦茎秆贮藏物质积累与再转运的影响

在防雨池栽条件下,以小麦旱地品种长武134(抗旱性强)和水地品种(抗旱性弱)为试材,研究干旱对不同抗旱性小麦茎秆及其组成节间花后干物质积累、转运及其对籽粒产量贡献率的影响。结果表明,干旱降低了主茎及其各组成节间干物质的积累量、主茎穗粒重积累量及其灌浆中后期的积累速率,长武134(除其它茎)降低幅度均小于陕253;干旱条件下茎秆贮藏物质的转运并未对籽粒产量产生补偿效应,干旱降低主茎穗粒重积累量与其它茎贮藏物质转运量和转运率较低有密切关系;抗旱性强的小麦品种其它茎的转运量、转运率降低幅度均大于抗旱性弱的小麦品种,从而导致其主茎贮藏物质转运对籽粒产量的贡献率显著降低。

干旱对不同抗旱性冬小麦旗叶光合及主茎干物质转运的影响

以冬小麦品种长武134(抗旱性强)和陕253(抗旱性弱)为材料,研究干旱对旗叶净光合速率和叶绿素含量、主茎及其组成节间花前积累干物质的转运及其对穗粒重贡献的影响。结果表明,干旱条件下长武134主茎穗粒重降幅小于陕253;干旱缩短了小麦花后旗叶光合速率高值持续期(PAD)和叶绿素含量缓降期(RSP),长武134受影响程度较小。长武134除穗下节外,其余各节间及茎杆干物质转运量及对籽粒贡献率降幅均大于陕253;干旱提高了陕253穗下节和倒二节干物质转运率,降低了倒三节和下部节干物质转运率,茎杆干物质转运率无明显变化;长武134除穗下节外其余各节间及茎杆干物质转运率均明显低于对照,而且距离穗部越远的节位降低幅度越大。上述结果表明,干旱条件下不同节位干物质转运能力变化与距离穗远近有关,花前茎杆干物质转运并不能补偿籽粒产量的损失,花后旗叶光合功能期延长是小麦抗旱高产的主要原因。

Effects of a stay-green mutation on plant nitrogen relations in Lolium perenne during N starvation and after defoliation

Macduff, J. H., Humphreys, M. O., Thomas, Howard (2002). Effects of a stay-green mutation on plant nitrogen relations in Lolium perenne during N starvation and after defoliation. Annals of Botany, 89 (1), 11-21. Sponsorship: BBSRC RAE2008

Modification of nitrogen remobilisation, grain fill and leaf senescence in maize (Zea mays L.) by transposon insertional mutagenensis in a protease gene

Donnison, I. S., Gay, A. P., Thomas, Howard, Edwards, K. J., Edwards, D., James, C. L., Thomas, A. M., Ougham, H. J. (2007). Modification of nitrogen remobilization, grain fill and leaf senescence in maize (Zea mays) by transposon insertional mutagenensis in a protease gene. New Phytologist, 173 (3), 481-494. Sponsorship: BBSRC RAE2008

Characterisation of virus transport and attenuation in epikarst using short pulse and prolonged injection multi-tracer testing

Attenuation processes controlling virus fate and transport in the vadose zone of karstified systems can strongly influence groundwater quality. This research compares the breakthrough of two bacteriophage tracers (H40/1 and T7), with contrasting properties, at subsurface monitoring points following application onto an overlying composite sequence of thin organic soil and weathered limestone (epikarst). Short pulse multi-tracer test results revealed that T7 (Source concentration, Co=1.8x106pfu/mL) and H40/1(Co=5.9x106pfu/mL) could reach sampling points 10m below ground less than 30 minutes after tracer application. Contrasting deposition rates, determined from simulated tracer responses, reflected the potential of the ground to differentially attenuate viruses. Prolonged application of both T7 (Co=2.3x104pfu/mL) and H40/1 (Co=1.3x105pfu/mL) over a five hour period during a subsequent test, in which ionic strength levels observed at monitoring points rose consistently, corresponded to a rapid rise in T7 levels, followed by a gradual decline before the end of tracer injection; this reflected reaction-limited deposition in the system. T7’s response contrasted with that of H40/1, whose concentration remained constant over a three hour period before declining dramatically prior to the end of tracer injection. Subsequent application of lower ionic strength tracer-free flush water generated a rapid rise in H40/1 levels and a more gradual release of T7. Results highlight the benefits of employing prolonged injection multi-tracer tests for identifying processes not apparent from conventional short pulse tests. Study findings demonstrate that despite rapid transport rates, the epikarst is capable of physicochemical filtration of viruses and their remobilization, depending on virus type and hydrochemical conditions.