为探讨桑树(Morus alba L.)应对锑(Antimony,Sb)胁迫的响应机制以及对锑污染的累积修复效果,采用土培法,以2年生桑树幼苗为实验材料,设置Sb3+(50、100、200、300 mg·kg-1),Sb5+(100、200、400、600 mg·kg-1)和Sb3++Sb5+(25+50...为探讨桑树(Morus alba L.)应对锑(Antimony,Sb)胁迫的响应机制以及对锑污染的累积修复效果,采用土培法,以2年生桑树幼苗为实验材料,设置Sb3+(50、100、200、300 mg·kg-1),Sb5+(100、200、400、600 mg·kg-1)和Sb3++Sb5+(25+50、50+100、100+200、150+300 mg·kg-1)12个浓度,研究不同价态、不同浓度锑处理对桑叶叶绿素含量、超氧化物歧化酶(SOD)、过氧化氢酶(CAT)、丙二醛(MDA)含量、谷胱甘肽(GSH)含量的影响,测定桑树各部位锑含量并计算富集转运系数。结果显示,单一和复合锑胁迫都会抑制桑叶的叶绿素合成,对于SOD和CAT活性,各处理都呈现出低浓度促进,高浓度抑制的现象,锑胁迫下MDA含量较对照组有显著增加,各个锑处理的富集系数均小于对照组。研究表明,单一Sb3+胁迫下桑树中锑分布为根>枝>茎>叶,Sb3+、Sb5+复合胁迫下桑树锑分布为根>茎>叶>枝,锑污染程度的增加抑制了桑树根向桑叶运输锑的能力,减小了桑树的富集能力。展开更多
The spatial and temporal variations of some important near-surface climate parameters and extreme climate events in North China during 1961-2010 are analyzed by using 94 meteorological stations' data in the study ...The spatial and temporal variations of some important near-surface climate parameters and extreme climate events in North China during 1961-2010 are analyzed by using 94 meteorological stations' data in the study area. Results show that the annual mean surface air temperature in North China increased at the rate of 0.36°C per decade, higher than the national average in the same period. Increasing was particularly significant since the mid-1980s, with maximum increase in the middle and northeastern parts of Inner Mongolia. Increasing rate of the annual mean minimum temperature is much higher than that of the maximum temperature, which results in the decrease of the annual mean diurnal temperature range. Noticeable decrease is also observed in the frequency of cold wave. Annual precipitation shows a slight decreasing trend, with more pronounced decrease in southern Shanxi and eastern Hebei provinces, which is mainly represented as decreasing in contribution rates of rainstorm and heavy storm in flood-season (May to September). During 1961-2010, North China is characterized by a noticeable reduction in annual extreme precipitation, and an increase in high-temperature days over most parts, as well as more frequent droughts. There are remarkable reductions in annual sunshine duration and mean wind speed, associated with the most significant reduction of mean wind speed in mid- western and eastern parts of Inner Mongolia. Meanwhile, North China has experienced a noticeable decrease/increase in annual mean sanddust/haze days during the study period. However, there is no significant trend in fog days, except a pronounced decrease since the 1990s.展开更多
基金supported by the Climate Change Special Foundation of China Meteorological Administration(No. CCSF2010-1)
文摘The spatial and temporal variations of some important near-surface climate parameters and extreme climate events in North China during 1961-2010 are analyzed by using 94 meteorological stations' data in the study area. Results show that the annual mean surface air temperature in North China increased at the rate of 0.36°C per decade, higher than the national average in the same period. Increasing was particularly significant since the mid-1980s, with maximum increase in the middle and northeastern parts of Inner Mongolia. Increasing rate of the annual mean minimum temperature is much higher than that of the maximum temperature, which results in the decrease of the annual mean diurnal temperature range. Noticeable decrease is also observed in the frequency of cold wave. Annual precipitation shows a slight decreasing trend, with more pronounced decrease in southern Shanxi and eastern Hebei provinces, which is mainly represented as decreasing in contribution rates of rainstorm and heavy storm in flood-season (May to September). During 1961-2010, North China is characterized by a noticeable reduction in annual extreme precipitation, and an increase in high-temperature days over most parts, as well as more frequent droughts. There are remarkable reductions in annual sunshine duration and mean wind speed, associated with the most significant reduction of mean wind speed in mid- western and eastern parts of Inner Mongolia. Meanwhile, North China has experienced a noticeable decrease/increase in annual mean sanddust/haze days during the study period. However, there is no significant trend in fog days, except a pronounced decrease since the 1990s.
