L-肉碱强化卤虫对鲤鱼开口苗脂肪酸组成和C/N比率的影响

【目的】研究L-肉碱强化卤虫对鲤鱼开口苗脂肪酸组成和C/N比率的影响,为鲤鱼开口苗的饲养提供参考。【方法】分别用质量浓度为0(对照),1,100,1 000 mg/L的L-肉碱强化卤虫无节幼体(Artemiasp.)12和24h,然后投喂给鲤鱼(Cyprinus carpio)开口苗,21 d后测定鱼苗的脂肪酸组成和C/N比率。【结果】投喂L-肉碱强化12 h的卤虫时,1 mg/L L-肉碱处理组鲤鱼开口苗的∑C14-24脂肪酸含量、饱和脂肪酸含量和单不饱和脂肪酸含量较对照组显著降低(P<0.05);1 000 mg/L L-肉碱处理组鲤鱼开口苗的单不饱和脂肪酸含量较对照组显著升高(P<0.05);L-肉碱对鲤鱼开口苗的多不饱和脂肪酸含量、∑n-3+∑n-6和∑DHA+EPA含量均无显著影响(P>0.05);1 000mg/L L-肉碱处理组鲤鱼开口苗的C/N比率显著低于对照组和1 mg/L L-肉碱处理组(P<0.05)。投喂L-肉碱强化24 h的卤虫时,1和100 mg/L L-肉碱处理组鲤鱼开口苗的∑C14-24脂肪酸和饱和脂肪酸含量较对照组显著降低(P<0.05),但2组之间差异不显著(P>0.05);1 000 mg/L L-肉碱处理组鲤鱼开口苗的∑C14-24脂肪酸和饱和脂肪酸含量较对照组显著升高(P<0.05);1 mg/L L-肉碱处理组鲤鱼开口苗的单不饱和脂肪酸含量较其他3组显著降低(P<0.05),多不饱和脂肪酸、∑n-3+∑n-6和∑DHA+EPA含量与对照组差异不显著(P>0.05);100 mg/L和1 000 mg/L L-肉碱处理组鲤鱼开口苗的多不饱和脂肪酸、∑n-3+∑n-6和∑DHA+EP A含量较对照组显著升高(P<0.05),且2组之间差异显著(P<0.05);1,100 mg/L L-肉碱处理组鲤鱼开口苗的C/N比率较对照组和1 000 mg/L L-肉碱处理组显著降低(P<0.05)。【结论】本试验条件下,以质量浓度100 mg/L L-肉碱强化卤虫24 h后再投喂鲤鱼开口苗,可显著改善鲤鱼开口苗的脂肪酸组成和C/N比率。     

黄土高原不同封育年限草地土壤与植物根系的生态化学计量特征

黄土高原特别是干草原地区植被演替的研究比较薄弱。当前植物生态化学计量学的研究主要集中在植物叶片方面,对根系的研究较少。选取宁夏云雾山草原植被不同封育年限的土壤和植物样品,以生态化学计量学原理为基础,测定并分析了土壤与根系的碳(C)、氮(N)、磷(P)及其生态化学计量比与相互关系。结果表明:(1)随着封育年限的增加,土壤容重逐渐减小,土壤有机碳和全氮变异性较大,全磷变异性较小,且封育初期土壤有机碳和全氮含量先降后升,至封育20、30年,保持相对平稳。0~20 cm土层土壤的碳氮比(C∶N)、碳磷比(C∶P)、氮磷比(N∶P)分别为9.04~9.63、19.62~32.27、2.14~3.37,20~40 cm土层土壤的分别为8.68~9.22、15.74~26.32、1.80~3.03。土壤有机碳与全氮、全磷之间存在极显著的正相关。(2)植物根系C、N、P含量变化范围分别为357.6~381.4 g kg-1、7.35~8.18 g kg-1、0.54~0.70 g kg-1;根系中的C元素含量随封育年限的增加逐渐升高,N、P元素含量均小于全球平均值。根系C∶N随着封育年限的增加变异性较大,C∶P、N∶P随着封育年限的增加变异性较小。(3)植物根系的C∶N∶P化学计量特征受土壤的影响调控大于其自身,且土壤磷含量对植物根系C∶N∶P生态化学计量特征影响的显著性(p0.01)大于土壤氮含量(p0.05)。此外,该地区封禁后,草地生产力易受到土壤N含量的限制。     

秸秆还田对灌溉玉米田土壤反硝化及N2O排放的影响

运用乙炔抑制技术研究了不同施氮水平下秸秆还田对灌溉玉米田土壤反硝化反应和氧化亚氮(N2O)排放的影响。结果表明,土壤反硝化速率及N2O的排放受氮肥施用、秸秆处理方式及其交互作用的显著影响。与秸秆燃烧相比,不施氮或低施氮水平时,秸秆还田可刺激培养初期反硝化反应速率及N2O排放,增加培养期间N2O平均排放通量;高施氮水平时,秸秆还田可降低反硝化反应速率及反硝化过程中的N2O排放。秸秆还田可降低反硝化中N2O/N2的比例。     

荔枝树体N素分布及累积特点

采用整株枝解法,在采果后把9a生成年妃子笑和黑叶、3a生幼年妃子笑荔枝的根、木质部、皮部、叶、复叶柄5个器官分成14～16个部位,测定各个部位各个器官的N含量。结果表明,1)N在不同器官和不同部位含量是不同的。N含量在叶片最高,在根颈、主茎木质部、主根含量较低;在同级枝根中,皮部N含量显著高于木质部;荔枝枝干和根系,随着其粗度增加,其N含量基本上呈下降趋势,但成年树下降幅度比幼年树的大。2)成龄妃子笑与黑叶各部位各器官N含量没有显著差异,但成年树叶、复叶柄、末级侧枝皮部、木质部N含量高于幼年树相应部位相应器官N含量。3)荔枝N素累积在叶片最多,其次为枝干,根系N累积量较少,末级侧枝N素累积量占整株树N素累积量50%以上。     

Mineralization of carbon and nitrogen from fresh and anaerobically stored sheep manure in soils of different texture

A sandy loam soil was mixed with three different amounts of quartz sand and incubated with (¹⁵NH₄)₂SO₄ (60 g N g^-1 soil) and fresh or anaerobically stored sheep manure (60 g g^-1 soil). The mineralization-immobilization of N and the mineralization of C were studied during 84 days of incubation at 20°C. After 7 days, the amount of unlabelled inorganic N in the manure-treated soils was 6–10 g N g^-1 soil higher than in soils amended with only (¹⁵NH₄)₂SO₄. However, due to immobilization of labelled inorganic N, the resulting net mineralization of N from manure was insignificant or slightly negative in the three soil-sand mixtures (100% soil+0% quartz sand; 50% soil+50% quartz sand; 25% soil+75% quartz sand). After 84 days, the cumulative CO₂ evolution and the net mineralization of N from the fresh manure were highest in the soil-sand mixutre with the lowest clay content (4% clay); 28% fo the manure C and 18% of the manure N were net mineralized. There was no significant difference between the soil-sand mixtures containing 8% and 16% clay, in which 24% of the manure C and -1% to 4% of the manure N were net mineralized. The higher net mineralization of N in the soil-sand mixture with the lowest clay content was probably caused by a higher remineralization of immobilized N in this soil-sand mixture. Anaerobic storage of the manure reduced the CO₂ evolution rates from the manure C in the three soil-sand mixtures during the initial weeks of decomposition. However, there was no effect of storage on net mineralization of N at the end of the incubation period. Hence, there was no apparent relationship between net mineralization of manure N and C.     

黄鳝体内新棘衣棘头虫的种群生态学研究

通过野外取样调查研究 ,揭示了新棘衣棘头虫种群生态学的一些特点。结果表明 ,新棘衣棘头虫寄生在黄鳝的肠道内 ,多集中于前肠 ;其感染率和感染强度都有随宿主体长的增加而逐渐增加的趋势 ;种群的平均丰度随宿主体长的增加呈指数增加 ,其回归方程为M =7.6× 10 -9L3 .3 83 0 ;随着黄鳝体长的增加 ,棘头虫种群在宿主中的频率分布的尾不断增长 ,即感染较多棘头虫的黄鳝所占比例增加 ;棘头虫种群在宿主不同体长组的分布类型为聚集分布 ,且聚集强度随棘头虫的种群平均丰度增加而增加。     

Seasonal effects of liming,irrigation, and acid precipitation on microbial biomass N in a spruce (Picea abies L.) forest soil

Summary Seasonal effects of liming, irrigation, and acid precipitation on microbial biomass N and some physicochemical properties of different topsoil horizons in a spruce forest (Picea abies L.) were measured throughout one growing season. The highest biomass N was recorded in autumn and spring in the upper soil horizons, while the lowest values were obtained in summer and in deeper horizons. The clearest differences between the different soil treatments were apparent in autumn and in the upper horizons. Liming increased the microbial biomass N from 1.7% of the total N content to 6.8% (Olf₁ layer) and from 1% to 2% of the total N content in the Of₂ layer. The main inorganic-N fraction in the deeper horizons was NO _inf3 ^sup- . An increase in cation exchange capacity was observed down to the Oh layer, while soil pH was only slightly higher in the Olf₁ and Of₂ layers after liming. The effects of irrigation were less marked. The microbial biomass N increased from 1.7% of total N to 4.8% in the Olf₁ layer and from 1% to 2% of total N in the Of₂ layer. In the Olf₁ layer an increase in C mineralization was observed. Acid precipitation decreased the microbial biomass N in the upper horizons from 4.8% of total N to 1.8% in the Olf₁ layer and from 2% to 0.5% in the Of₂ layer. No significant changes in soil pH were observed, but the decrease in cation exchange capacity may result in a decrease in the proton buffering capacity in the near future.     

亚硝酸盐添加对土壤硝化和反硝化基因转录活性及N2O排放的影响

设施菜田土壤氧化亚氮（N2O）脉冲式排放期间通常伴随着亚硝酸盐（NO2-）的大量积累,为揭示NO2-对设施菜田土壤N2O排放的影响机制,以两种典型蔬菜种植区土壤（碱性土壤/酸性土壤）为研究对象,通过室内培养试验,对比厌氧和好氧培养条件下添加NO2-后两种土壤无机氮转化与N2O、氮气（N2）和二氧化碳（CO2）等气体排放,以及氨氧化单加氧酶α亚基调控基因（amoA）、亚硝酸盐还原酶调控基因（nirK和 nirS,统称nir）和N2O还原酶调控基因（nosZ）的丰度和转录情况。结果显示：受pH等环境因素影响,土壤中NO2-含量并不一定与N2O排放之间存在相关性,但添加NO2-的处理显著增加了两种土壤的N2O排放量和N2O/(N2O+N2)指数（IN2O）（P<0.05）。碱性土壤中,60 mg?kg-1外源NO2-对土壤CO2排放无明显抑制作用,厌氧培养条件下nirK基因、好氧培养条件下amoA和nirS基因均出现了添加NO2-后转录拷贝数显著高于空白处理的现象,而nosZ基因无此现象。酸性土壤中,amoA转录活性整体较低,好氧空白处理时nirS基因转录拷贝数随培养时间的延长而增加（P<0.05）;60 mg?kg-1外源NO2-明显降低了酸性土壤的CO2排放量、相关基因的丰度及转录拷贝数。上述结果显示,土壤中积累的NO2-会通过诱导nir基因转录与N2O还原酶竞争电子和抑制N2O还原酶活性等途径,增加土壤的IN2O,影响有氧条件下N2O的排放途径,研究结果将为探索设施菜田土壤氮素高效利用和N2O减排提供科学依据。     

无氮肥投入条件下黑麦生长过程中土壤酸解氮的消长动态

取沙、壤、粘3种质地的潮土，采用盆栽试验，应用Bremmner法测定黑麦不同生育时期土壤酸解氮及各组分氮含量。结果表明，3种质地的土壤氮素主要以酸解氮为主，占土壤全氮的70％以上，在酸解氮中，氨基酸氮和酸解未知态氮为主要成分，其次为氨态氮，最低为氨基糖态氮。黑麦生长过程中，在无氮肥投入条件下，酸解氮及各组分氮处在动态变化中，而且变化趋势相似，3种质地的氨基酸氮和酸 未知态氮相对变化率较氨态氮和氨基糖态氮大，说明质地不能改变酸解氮及各组分氮的变化趋势，但可以改变其变化程度；同样水平的全氮量，而质地不同的土壤供应速效氮的能力是沙土＞壤土＞粘土，但在无氮肥投入情况下，土壤氮素数量和质量都有所下降。     

氮气介质环境中热处理樟子松木材主要性能的变化

以氮气为介质,采用160℃、180℃、200℃ 3种不同温度,2、4、6 h 3种不同时间分别对樟子松木材进行热处理改性,分析热处理前后樟子松材色、尺寸稳定性及力学性能的变化规律,并采用FTIR及XRD手段分析了其变化机理。结果表明,樟子松木材色差随热处理温度和时间增大而增大,而明度随热处理温度和时间增大逐渐降低,处理材红绿色品指数a^*值和黄蓝色品指数b^*值均大于未处理材。樟子松木材平衡含水率随热处理温度和时间的增大逐渐减小,ASE和吸湿滞后现象随温度的增大逐渐增大。樟子松木材的顺纹抗压强度、抗弯弹性模量及抗弯强度随热处理强度的增加呈现先增大后降低的趋势,但在200℃下对这3个力学性能指标影响均不显著。热处理温度对樟子松材色及尺寸稳定性影响均极显著,热处理时间对樟子松木材明度、黄蓝色品指数b^*、色差、平衡含水率和体积湿胀率影响均极显著。研究结果为高品质樟子松热处理木材的生产提供科学依据。