8种棕榈植物幼苗耐盐性的比较分析

摘要：将加那利海枣(Phoenix canariensis)、棍棒椰子(Hyophorbe verschaffeltii)、三角椰子（Dypsis decaryi）、国王椰子（Ravenea rivularis）、飓风椰子（Dictyosperma album）、大王椰子（Roystonea regia）、红棕榈（Latania lontanoides）和狐尾椰子(Wodyetia bifurcata)8种棕榈植物幼苗培养在不同含盐量的土壤中,研究了土壤盐度与棕榈植物幼苗株高生长、植株各部分生物量的关系,确定棕榈植物幼苗生长的土壤盐度的适宜值、临界值和极限值。根据植物生长量和土壤盐度的关系曲线,可以分成3种类型：低盐促进类型（三角椰子和棍棒椰子）、直线负相关类型（国王椰子、加那利海枣和飓风椰子）和低盐敏感类型（狐尾椰子、红棕榈和大王椰子）。8种棕榈植物幼苗耐盐性依次为：加那利海枣>棍棒椰子>三角椰子>国王椰子>飓风椰子>大王椰子>红棕榈>狐尾椰子。     

Deficit irrigation based on drought tolerance and root signalling in potatoes and tomatoes

Agriculture is a big consumer of fresh water in competition with other sectors of the society. Within the EU-project SAFIR new water-saving irrigation strategies were developed based on pot, semi-field and field experiments with potatoes (Solanum tuberosum L.), fresh tomatoes (Lycopersicon esculentum Mill.) and processing tomatoes as model plants. From the pot and semi-field experiments an ABA production model was developed for potatoes to optimize the ABA signalling; this was obtained by modelling the optimal level of soil drying for ABA production before re-irrigation in a crop growth model. The field irrigation guidelines were developed under temperate (Denmark), Mediterranean (Greece, Italy) and continental (Serbia, China) climatic conditions during summer. The field investigations on processing tomatoes were undertaken only in the Po valley (North Italy) on fine, textured soil. The investigations from several studies showed that gradual soil drying imposed by deficit irrigation (DI) or partial root zone drying irrigation (PRD) induced hydraulic and chemical signals from the root system resulting in partial stomatal closure, an increase in photosynthetic water use efficiency, and a slight reduction in top vegetative growth. Further PRD increased N-mineralization significantly beyond that from DI, causing a stay-green effect late in the growing season. In field potato and tomato experiments the water-saving irrigation strategies DI and PRD were able to save about 20-30% of the water used in fully irrigated plants. PRD increased marketable yield in potatoes significantly by 15% due to improved tuber size distribution. PRD increased antioxidant content significantly by approximately 10% in both potatoes and fresh tomatoes. Under a high temperature regime, full irrigation (FI) should be undertaken, as was clear from field observations in tomatoes. For tomatoes full irrigation should be undertaken for cooling effects when the night/day average temperature >26.5 °C or when air temperature >40 °C to avoid flower-dropping. The temperature threshold for potatoes is not clear. From three-year field drip irrigation experiments we found that under the establishment phase, both potatoes and tomatoes should be fully irrigated; however, during the later phases deficit irrigation might be applied as outlined below without causing significant yield reduction:

•

Potatoes

°

After the end of tuber initiation, DI or PRD is applied at 70% of FI. During the last 14 days of the growth period, DI or PRD is applied at 50% of FI.

•

Fresh tomatoes

°

From the moment the 1st truce is developed, DI is applied at 85-80% of FI for two weeks. In the middle period, DI or PRD is applied at 70% of FI. During the last 14 days of the growth period, DI or PRD is applied at 50% of FI.

•

Processing tomatoes

°

From transplanting to fruit setting at 4th-5th cluster, the PRD and DI threshold for re-irrigation is when the plant-available soil water content (ASWC) equals 0.7 (soil water potential, Ψ_soil = −90 kPa). During the late fruit development/ripening stage, 10% of red fruits, the threshold for re-irrigation for DI is when ASWC = 0.5 (Ψ_soil = −185 kPa) and for PRD when ASWC (dry side) = 0.4 (Ψ_{soil, dry side} = −270 kPa).

The findings during the SAFIR project might be used as a framework for implementing water-saving deficit irrigation under different local soil and climatic conditions.     

Glomus-wetland rice mycorrhizas influenced by nursery inoculation techniques under high fertility soil conditions

 We investigated the effect of nursery inoculation techniques on mycorrhizal colonization and sporulation, growth responses, and nutrient (N and P) uptake to determine the suitable nursey inoculation method of wetland rice (Oryza sativa L.) under high-fertility soil conditions. Seedlings were produced in dry-nursery (DN, watered to 60% of –0.03 MPa) and wet-nursery (WN, 3–5 cm water from the soil surface) conditions with or without arbuscular mycorrhizal fungal (Glomus spp.) inoculation. Soil was γ-ray sterilized before use in this experiment. Mycorrhizal fungal colonization was 56% in DN and 23% in WN plants at 6 weeks of growth. The arbuscular mycorrhizal fungal colonization was significantly higher in plants of DN origin than in WN plants after transplantation to the pots, irrespective of growing stages. Mycorrhizal colonization was significantly decreased to 28% in DN plants and to 25% in WN plants at harvest. The grain yield was significantly influenced by nursery conditions. N and P acquisition of wetland rice plants inoculated with Glomus spp. was significantly greater than that of non-inoculated plants at maturity, especially in those originating from DN conditions. P translocation from shoots to grain was accelerated by mycorrhizas. Received: 6 April 1997     

植物对水分胁迫的分子响应及其遗传改良研究进展

植物对水分胁迫适应性的生理机理已相继在水稻、小麦、玉米、高梁等作物中得以报道。然而，有关这些性状的遗传控制及其在与逆境下作物生产的关系却了解甚少，由此阻碍了抗性遗传改良的进展。随着基因定位、基因组图谱、基因转移等分子生物学技术的发展，对植物抗逆性状进行分子剖析成为可能。本文综述了主要禾谷类作物对水分胁迫的抗性生理及遗传研究上的最新进展，讨论了植物抗性遗传改良的发展前景。     

Methane emission from two Indian soils planted with different rice cultivars

In a greenhouse study, methane emissions were measured from two diverse Indian rice-growing soils planted to five rice cultivars under similar water regimes, fertilizer applications and environmental conditions. Significant variations were observed in methane emitted from soils growing different cultivars. Total methane emission varied between 8.04 and 20.92gm^–2 from IARI soil (Inceptisol) and between 1.47 and 10.91gm^–2 from Raipur soil (Vertisol) planted to rice. In all the cultivars, emissions from IARI soil were higher than from Raipur soil. The first methane flux peak was noticed during the reproductive phase and the second peak coincided with the grain-ripening stage of the rice cultivars. Received: July 7, 1996     

Evolution of dinitrogen and nitrous oxide from the soil to the atmosphere through rice plants

Summary It is commonly assumed that a large fraction of fertilizer N applied to a rice (Oryza sativa L.) field is lost from the soil-water-plant system as a result of denitrification. Direct evidence to support this view, however, is limited. The few direct field, denitrification gas measurements that have been made indicate less N loss than that determined by ¹⁵N balance after the growing season. One explanation for this discrepancy is that the N₂ produced during denitrification in a flooded soil remains trapped in the soil system and does not evolve to the atmosphere until the soil dries or is otherwise disturbed. It seems likely, however, that N₂ produced in the soil uses the rice plants as a conduit to the atmosphere, as does methane. Methane evolution from a rice field has been demonstrated to occur almost exclusively through the rice plants themselves. A field study in Cuttack, India, and a greenhouse study in Fort Collins, Colorado, were conducted to determine the influence of rice plants on the transport of N₂ and N₂O from the soil to the atmosphere. In these studies, plots were fertilized with 75 or 99 atom % ¹⁵N-urea and ¹⁵N techniques were used to monitor the daily evolution of N₂ and N₂O. At weekly intervals the amount of N₂+N₂O trapped in the flooded soil and the total-N and fertilized-N content of the soil and plants were measured in the greenhouse plots. Direct measurement of N₂+N₂O emission from field and greenhouse plots indicated that the young rice plant facilitates the efflux of N₂ and N₂O from the soil to the atmosphere. Little N gas was trapped in the rice-planted soils while large quantities were trapped in the unplanted soils. N losses due to denitrification accounted for only up to 10% of the loss of added N in planted soils in the field or greenhouse. The major losses of fertilizer N from both the field and greenhouse soils appear to have been the result of NH₃ volatilization.     

Frog communities and wetland condition: relationships with grazing by domestic livestock along an Australian floodplain river

Frogs are in decline worldwide, and are known to be sensitive indicators of environmental change. Floodplains of the Murray-Darling Basin in southeastern Australia have been altered in many ways by livestock grazing, by the introduction of exotic fish, and by changes to flooding regimes. These changes have led to declines in wetland condition and hence to the availability of habitat for wetland frogs. This study examined relationships between frogs, wetland condition and livestock grazing intensity at 26 wetlands on the floodplain of the Murrumbidgee River. Frog communities, species richness, and some individual species of frogs declined with increased grazing intensity. Wetland condition also declined with increased grazing intensity, particularly the aquatic vegetation and water quality components. There were clear relationships between frog communities and wetland condition, with several taxa responding to aquatic and fringing vegetation components of wetland condition. Thus, grazing intensity appeared to influence frog communities through changes in wetland habitat quality, particularly the vegetation. Reduced stocking rates may result in improved wetland condition and more diverse frog communities. River management to provide natural seasonal inundation of floodplain wetlands may also enhance wetland condition, frog activity and reproductive success.     

华北平原冬小麦田问蒸散与棵问蒸发的变化规律研究

试验研究冬小麦田间蒸散和棵间蒸发变化规律及其影响因子结果表明 ,播种～返青期冬小麦棵间蒸发占蒸散比例 (E ET)最大 ,抽穗～灌浆期最小。整个生长期间棵间蒸发占蒸散量 31 .4 % ,棵间蒸发占蒸散比例 (E ET)与冬小麦叶面积指数 (LAI)有一定关系 ,E ET =0 .36 93× (LAI) - 0 .74 93(R2 =0 .82 36 )。     

三江平原典型湿地土壤中硫的分布特征

本文以三江平原的三种典型类型湿地:小叶樟(Calamagrostisangustifolia)草甸、毛果苔草(Carexlasiocarpa)沼泽、乌拉苔草(Carexmeyeriana)沼泽为研究对象,对其土壤中硫的含量在水平及垂直变化方面进行分析。研究在自然环境下硫的分布特征。经过试验分析和数据处理,得出以下结论:总硫、水溶性硫、吸附性硫、盐酸可溶性硫、盐酸挥发性硫、有机硫含量均为小叶樟草甸<乌拉苔草沼泽<毛果苔草沼泽;别拉洪河、挠力河、鸭绿河、浓江是三江平原四条有代表性的沼泽性河流,流域土壤中的硫素含量为挠力河>鸭绿河>浓江>别拉洪河;在土壤层次上,具有明显的规律性:除盐酸挥发性硫以外,其余各硫组分自上而下含量呈递减趋势;在湿地土壤各形态硫中,有机硫是土壤总硫的主体,盐酸挥发性硫含量最低。总硫与有机硫相关性最显著,达极显著正相关(P=0.01),水溶性硫与盐酸可溶性硫的相关性最差。影响湿地土壤中硫素含量的因素为土壤有机质、土壤pH值、物理粘粒及氧化-还原条件。     

低温胁迫下三七一年生紫、绿地上茎植株抗氧化能力的研究

旨在探究三七地上茎积累花色苷对其抗寒性的效应。研究了冰水模拟低温胁迫下三七一年生紫、绿地上茎植株叶片可溶性蛋白质和丙二醛(MDA)含量及抗氧化酶比活力。结果表明,在冰水模拟低温胁迫下,紫、绿地上茎植株叶片的可溶性蛋白质含量和过氧化氢酶(CAT)比活力及绿地上茎植株叶片的MDA含量均上升,紫、绿茎植株叶片的过氧化物酶(POD)和超氧化物歧化酶(SOD)比活力及紫茎植株叶片的MDA含量均下降,且紫茎叶片可溶性蛋白质含量和CAT比活力的升幅及绿茎叶片POD和SOD比活力的降幅均更大;在冰水处理结束时,紫茎植株叶片的可溶性蛋白质含量、POD和SOD的比活力均高于绿茎的,但CAT比活力和MDA含量略低于绿茎的。但是,紫、绿茎植株叶片的可溶性蛋白质和MDA含量及抗氧化酶比活力的差异均未达到显著水平。因此,三七地上茎积累花色苷利于其抗寒。