Numerical experiments for the impacts of temperature and precipitation variation on the growth and development of winter wheat

The growth process of winter wheat was simulated by CERES-wheat model assuming the daily temperature increase -1, 0,1, 2℃ and daily precipitation increase -20, -10, -5, 0, 5, 10, and 20 percent, respectively. The case study site is Zhenjiang City of Jiangsu Province in the east China. Simulation results show that the impacts of temperature variation on winter wheat is stronger than that of precipitation. Climate warming would speed development rate and shorten phonological period. In general, the adverse effect of climate change on grain yield is greater than that of its beneficial effect, especially when the climate becoming cooler and dryer. The increase of temperature and decrease of precipitation would reduce the plant extractablc soil water content.     

小麦中T-2毒素酶联免疫吸附测定法(ELISA)

T-2毒素是某些植物致病菌的次生代谢产物,尤其是由镰刀菌(Fusarium sp)引致的麦类、玉米等作物的赤霉病,菌体在一定条件下能产生大量的该类毒素.T-2毒素对人畜的毒性很大,同时,还与某些癌症的发病率有密切的关系.T-2毒素的检测方法,常用的有薄层层析法,气相、液相色谱法以及气-质联用等,这些方法,有的精确度     

二氧化硫对作物游离氨基酸浓度的作用

观察了四种作物接触二氧化硫后游离氨基酸,特别是十种昆虫必需氨基酸含量的变化.二氧化硫引起油菜、大豆和小麦叶片中昆虫必需氨基酸浓度明显增加,非必需氨基酸中,增加或减少趋势不一.玉米没有这种反应.二氧化硫熏气的大豆上叶螨生长繁殖快于对照.讨论了植物中氨基酸浓度的增加和大气污染诱发虫害加剧的关系.     

Differences of cadmium absorption and accumulation in selected vegetable crops

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紫外线辐射对小麦和燕麦竞争性平衡的影响--小麦和燕麦生物量结构与冠层结构

在模拟１５％臭氧层减薄条件下讨论了紫外线辐射增强对大田中小麦和燕麦在单独种植与混合种植时的生物量结构和冠层结构的影响。紫外辐射使两物种的生物量减少，使节间缩短，叶片着生高度下降，但使根冠比和单株有效穗数增加。两物种在单种和混种时对紫外辐射的反应有所不同，种间竞争有时加强紫外辐射的影响，但有时则又能抵消其作用。紫外辐射使竞争性平衡向有利于小麦的方向发展，这一改变可以部分地由两物种的生物量及冠层结构对     

Contribution of winter fluxes to the annual CH4, CO2 and N2O emissions from freshwater marshes in the Sanjiang Plain

Introduction C arbon dioxide, m ethane and nitrous oxide play im portant roles in the radiation balance of the earth contributing to the greenhouse effect (Rodhe, 1990). N 2O also takes part in the destruction of stratospheric ozone (W ang, 1999). N atura…     

Secondary effect of SO_2 pollution: enhanced growth of the army worm, Mythimna separata (Walker)

Effects of SO2 pollution on growth of the army worm, Mythimna separata, were investigated by rearing the larvae for 12 days on the wheat plants being exposed to SO2 levels ranged from 50 to 200 ppb in the field open-top fumigation devices. Larval period shortened while their mean relative growth rate (MRGR) increased as SO2 dose elevated. Similar experiment with the insect on the artificial diet excluded the possibility that SO2 pollution directly stimulated growth of the army worm.The patterns of change in amino acid hydrolysates in the host foliage suggested that contents of methionine, and perhaps, arginine in food material exposed to unpolluted air were at such levels that they could only support sub-optimum growth of the insect, and SO2 pollution increased concentrations of these limiting amino acids, resulting in better performance of the larvae.     

Secondary effect of SO2 pollution: enhanced growth of the army worm, Mythimna separata (Walker)

Effects of SO₂ pollution on growth of the army worm, Mythimna separata, were investigated by rearing the larvae for 12 days on the wheat plants being exposed to SO₂ levels ranged from 50 to 200 ppb in the field open-top fumigation devices. Larval period shortened while their mean relative growth rate (MRGR) increased as SO₂ dose elevated. Similar experiment with the insect on the artificial diet excluded the possibility that SO₂ pollution directly stimulated growth of the army worm.The patterns of change in amino acid hydrolysates in the host foliage suggested that contents of methionine, and perhaps, arginine in food material exposed to unpolluted air were at such levels that they could only support sub-optimum growth of the insect, and SO₂ pollution increased concentrations of these limiting amino acids, resulting in better performance of the larvae.     

Phosphorus Losses to Water from Lowland Rice Fields under Rice–Wheat Double Cropping System in the Tai Lake Region

To assess P losses to surface water by runoff during the rice season and by drainage flow during the winter wheat season, serial field trials were conducted in different types of paddy soils in the Tai Lake Region (TLR) during 2000 and 2001. Four P application rates were set as 0 (CK), 30, 150, and 300 kg P/hm² for flooded rice trials and 0 (CK), 20, 80, 160 kg P/hm² for winter wheat trials respectively. Field experiments were done in two locations with a plot size of 30 m² and four replications in a randomized complete block design. A simplified lysimeter was installed for each plot to collect all the runoff or drainage flow from each event. Total P (TP) losses to surface water during rice season by runoff flow from four treatments were 150 (CK), 220 (T30), 395 (T150), 670 (T300) g P/hm² in year 2000, and 298, 440, 1828, 3744 g P/hm² in year 2001 respectively in Wuxi station, here the soil is permeable paddy soil derived from loam clay deposit. While the losses were 102, 140, 210, 270 in year 2000, and 128, 165, 359, 589 g P/hm² in year 2001 respectively in Changshu station, here the soil is waterlogged paddy soil derived from silt loam deposit. During the winter wheat season, total P lost from the fields by drainage flow in the four treatments were 253 (CK), 382 (T20), 580 (T89), 818 (T160) g P/hm² in year 2000–2001, and 573.3, 709.4, 1123.2, 1552.4 g P/hm² in year 2001–2002 at the Wuxi station. While these were 395.6, 539.1, 1356.8, 1972.1 g P/hm² in year 2000–2001, and 811.5, 1184.6, 3001.2, 5333.1 g P/hm² in year 2001–2002 at the Changshu station. Results revealed that P fertilizer application rates significantly affected the TP concentrations and TP loads in runoff during the rice season, and by drainage flow during the winter wheat season. Both TP loads were significantly increased as the P application rate increases. The data indicate that TP losses to surface water were much higher during the winter wheat season than during the rice season in two tested sites. The data also reveal that the annual precipitation and evaporation rate affected the soil P losses to surface water significantly. Year 2000 was relatively dried with higher evaporation thus P losses to water by both runoff and drainage flow were less than in year 2001 which was a relatively wet year with lower evaporation. Results indicate that texture, structure of the soil profile, and field construction (with or without ridge and deep drains) affected soil P losses to surface water dramatically. Annual possible TP lost to water at the application rate of 50 kg P/hm² year tested in TLR were estimated from 97 to 185 tones P from permeable paddy soils and 109–218 tones P from waterlogged paddy soils. There was no significant difference of TP lost between the CK and the T50 treatments in both stations, which indicate that there is no more TP lost in field of normal P fertilizer application rate than in control field of no P fertilized. Much higher TP lost in runoff or drainage flow from those other P application rates treatments than from the T50 treatment, which suggest that P losses to surface water would be greatly increasing in the time when higher available P accumulation in plough layer soil in this region.     

浅层咸水灌溉对冬小麦和土壤安全性的研究

主要研究利用浅层地下咸水灌溉冬小麦及土壤的安全性。试验采取3因素多水平组合设计,利用2.5~6.0g·L-1不同矿化度咸水对冬小麦进行灌溉。试验结果表明:冬小麦产量与咸水矿化度呈负相关关系r=-0.8542、r=-0.8457,与咸水灌溉量呈正相关关系r=0.7487、r=0.7401。利用小于4.0g·L-1咸水灌溉对土壤具有一定的脱盐作用,咸水矿化度为6.0g·L-1时土壤中的盐分积累达到85.5%。矿化度5.0g·L-1以上的咸水不宜直接灌溉农田,需经淡水与咸水调配后,矿化度在4.0g·L-1以下方可灌溉农田。