水稻适雨灌溉对稻田CH_4和N_2O排放的影响

采用静态暗箱-气相色谱法,观测分析了水稻适雨灌溉和常规灌溉2种模式下稻田CH_4和N_2O的季节排放情况,评估了水稻适雨灌溉对稻田CH_4和N_2O排放的影响。结果表明,适雨灌溉稻田CH_4、N_2O排放峰值分别出现在分蘖期和拔节孕穗期,整个生育期CH_4、N_2O平均排放通量分别为16.77 mg/(m~2·h)、6.64μg/(m~2·h),适雨灌溉稻田CH_4、N_2O排放量较常规灌溉显著下降(p0.05),分别下降了74.47%和67.06%。水稻适雨灌溉通过合理利用雨水资源,减少灌溉次数及灌水量,显著降低了稻田CH_4和N_2O的排放。     

Al2O3含量对烧结初始液流动行为的影响

在铁矿粉烧结过程中,初始液相流动行为是烧结矿固结效果的重要影响因素。采用微型烧结法,探讨了Al2O3含量对初始液相流动行为的影响,并通过对初始液相微观结构的解析,揭示了Al2O3含量对初始液相气孔分布和结构的影响规律。实验结果表明,初始液相的流动性指数随着Al2O3含量提高而降低。水淬试样的XRD实验结果结果证实,Al2O3含量的增加提高了复合铁酸钙的稳定性,降低了初始液相的流动能力。此外,初始液相流动性亦会对气孔性质产生影响。高Al2O3初始液相中气孔结构不规则程度提高,且小于50 μm气孔数目也随之增多。     

利用籼粳交探讨水稻株高和抽穗期的遗传基础

广亲和基因的发现,克服了籼粳交杂种不育的矛盾,但杂种后代株高过高、抽穗期延迟等问题仍然限制着籼粳亚种间杂种优势的利用。本试验利用一个籼粳交(珍汕97/武育粳2号)双单倍体群体(doublehaploidpopulation,DH系)及其分别与两亲本回交构建的两个回交群体,考查了株高和抽穗期的遗传,将三个群体的表型值和两个回交群体的中亲优势值进行了数量性状位点(quantitativetraitlocus,QTL)检测及效应分析,并对结果进行了比较。2个性状在3个相关群体中一共检测到了21个主效QTL和10个上位性QTL,主效QTL的数目和贡献率都比上位性QTL大,而且,在10个上位性QTL中,发生在2个主效QTL间的互作有3个,主效QTL与背景位点间的互作有6个,2个互补位点间的互作仅有1个,进一步说明了主效QTL在株高和抽穗期遗传中的重要作用。比较加性和非加性QTL的作用,发现加性效应、显性效应和上位性效应是籼粳亚种间杂种株高和生育期变化的共同遗传基础。     

土壤水分状况和质地对稻田N2O 排放的影响

１９９４年中国科学院封丘生态试验站通过小区试验研究了土壤质地和水分状况对稻田Ｎ２Ｏ排放的影响。结果表明稻田Ｎ２Ｏ排放主要受土壤水分状况的影响,淹水状态下,Ｎ２Ｏ排放很少,水分落于期间Ｎ２Ｏ排放量占水稻生长期Ｎ２Ｏ排放总量的８７．５０％～９８．６５％。土壤质地显影响稻田平均Ｎ２Ｏ排放通量,砂质土壤排放的Ｎ２Ｏ显或极显高于壤质和粘质土壤,水稻生长期砂质、壤质及粘质土壤的平均Ｎ２Ｏ排放通量分别为１３７．６３、８７．５４和６３．６μｇＮ２Ｏ－Ｎ／ｍ＾２．ｈ。     

浅谈推算和预测宏观尺度土壤N_2O释放量的方法

土壤是N2 O的最主要释放源 .本文综述了根据局部地区土壤N2 O释放观察结果 ,推算和预测宏观尺度土壤甚至全球土壤N2 O释放通量变化和年释放量的方法 ,评述了各类方法的优缺点 ;并着重讨论了释放过程机理模型的应用 .     

不同秸秆还田模式与氮肥施用量对土壤N2O排放的影响

以山东省桓台县为试验地点,分析在高产条件下,不同秸秆还田模式和氮肥施用量对农田N2O排放的影响.试验结果表明,氮肥施用量与秸秆还田模式都是影响土壤N2O排放的重要因素;小麦秸秆还田可以大大降低土壤N2O的排放,施用有机粪肥是影响N2O排放的另一重要因素.     

Transitioning from standard to minimum tillage: Trade-offs between soil organic matter stabilization, nitrous oxide emissions, and N availability in irrigated cropping systems

Few studies address nutrient cycling during the transition period (e.g., 1–4 years following conversion) from standard to some form of conservation tillage. This study compares the influence of minimum versus standard tillage on changes in soil nitrogen (N) stabilization, nitrous oxide (N₂O) emissions, short-term N cycling, and crop N use efficiency 1 year after tillage conversion in conventional (i.e., synthetic fertilizer-N only), low-input (i.e., alternating annual synthetic fertilizer- and cover crop-N), and organic (i.e., manure- and cover crop-N) irrigated, maize–tomato systems in California. To understand the mechanisms governing N cycling in these systems, we traced ¹⁵N-labeled fertilizer/cover crop into the maize grain, whole soil, and three soil fractions: macroaggregates (>250 μm), microaggregates (53–250 μm) and silt-and-clay (<53 μm). We found a cropping system effect on soil N_new (i.e., N derived from ¹⁵N-fertilizer or -¹⁵N-cover crop), with 173 kg N_new ha⁻¹ in the conventional system compared to 71.6 and 69.2 kg N_new ha⁻¹ in the low-input and organic systems, respectively. In the conventional system, more N_new was found in the microaggregate and silt-and-clay fractions, whereas, the N_new of the organic and low-input systems resided mainly in the macroaggregates. Even though no effect of tillage was found on soil aggregation, the minimum tillage systems showed greater soil fraction-N_new than the standard tillage systems, suggesting greater potential for N stabilization under minimum tillage. Grain-N_new was also higher in the minimum versus standard tillage systems. Nevertheless, minimum tillage led to the greatest N₂O emissions (39.5 g N₂O–N ha⁻¹ day⁻¹) from the conventional cropping system, where N turnover was already the fastest among the cropping systems. In contrast, minimum tillage combined with the low-input system (which received the least N ha⁻¹) produced intermediate N₂O emissions, soil N stabilization, and crop N use efficiency. Although total soil N did not change after 1 year of conversion from standard to minimum tillage, our use of stable isotopes permitted the early detection of interactive effects between tillage regimes and cropping systems that determine the trade-offs among N stabilization, N₂O emissions, and N availability.     

陆地生态系统N_2O排放源研究进展

N2O是一种痕量气体,不仅能产生温室效应,而且对臭氧同温层有严重的破坏作用。随着人类活动的加剧,大气中N2O浓度每年以0.2%～0.3%的速度增加,N2O排放问题引起了人们的广泛关注。目前,对大气N2O排放的源与汇还缺乏全面认识,N2O在大气中增加量的40%～50%尚不知来源。综述了陆地生态系统N2O排放的自然源和人为源,分析了N2O排放的影响因素,并对今后N2O的研究提出了展望。     

施肥对稻田N2O排放的影响

肥料施用是影响稻田N20排放的重要因素之一。以国内外相关文献为基础,综述了肥料的种类、施用量、施用方式和施用时间对稻田N2O排放的影响,指出了有待研究的内容：加强对土壤N2O排放机理的研究;进一步研究肥料施用对稻田N2O排放的影响;进一步研究施肥管理措施对稻田温室气体（CH4和N2O）排放的交互影响,寻求科学合理、切实可行的减排措施。     

冬小麦-夏玉米轮作条件下氮素反硝化损失研究

  在北京潮土上研究了冬小麦-夏玉米轮作体系下土壤氮素反硝化损失。结果表明，不同氮肥用量处理，土壤氮素反硝化损失量为4.71～9.67 kg·ha-1。夏玉米生育期是反硝化损失的关键时期。氮肥施用后的1～2周是氮素反硝化损失的最剧烈阶段。土壤N2O的生成、排放与反硝化作用有相似的规律性，N2O可能大部分来自于硝化作用。