砂姜黑土玉米秸秆有机碳的矿化特征

 【目的】探讨不同温度（10℃、20℃、30℃）、不同秸秆加入量（秸秆全量和过量）条件下,玉米秸秆还田对土壤有机碳矿化特征及其环境因子的响应机制。【方法】采用室内恒温控湿好气培养试验,对安徽淮北砂姜黑土在不同温度（10℃、20℃、30℃）条件下,设置50 g土样中加秸秆0.3 g（处理Ⅰ）、1.5 g（处理Ⅱ）、3.0 g（处理Ⅲ）及不加秸秆（CK）的处理,进行240 d的矿化培养。【结果】温度对有机碳矿化影响显著,在对照（CK）和秸秆加入量相同的处理中,有机碳的矿化累积量均随温度（10—30℃）升高而增加;温度较低（＜20℃）时,CK、Ⅰ、Ⅱ、Ⅲ各处理的有机碳矿化温度系数（Q10）平均值约为1.229、1.251、1.572、1.399,温度较高（＞20℃）时,CK、Ⅰ、Ⅱ、Ⅲ的Q10平均值约1.006、1.249、1.401、1.374,Q10值在温度较低时大于温度较高时,说明低温条件下,有机碳矿化速率对升温更敏感。同一温度条件下,不同处理秸秆加入量越大,有机碳矿化累积量越高,有机碳矿化的日变化量也越大。本试验中,一级动力学方程能较好地描述了不同处理土壤有机碳的矿化累积动态。土壤有机碳的潜在矿化量（C0）随温度变化不明显,在同一温度条件下,秸秆加入量越大,C0值越大。【结论】一级动力学方程能较好地描述不同处理土壤有机碳的矿化累积动态。不同温度、不同秸秆还田量及温度和秸秆还田量的交互作用,对玉米秸秆矿化过程中土壤有机碳含量的影响均达到显著水平。     

我国红碎茶与斯里兰卡红碎茶比较分析

通过对我国海南通什、云南凤庆、广东英德２号茶和出口拼配红碎茶、斯里兰卡高地、中地和低地红碎茶同年样品的分析,结果表明,我国上述三地的大叶种红碎茶主要品质成分含量及内质化学鉴定分数均高于斯里兰卡红碎茶,仅香气次之。但出口样拼配红碎茶的主要品质成分含量和内质化学鉴定分数均显著低于斯里兰卡红碎茶。文中对我国与斯里兰卡红碎茶品质的差异原因进行了讨论,并建议我国大叶种红碎茶直接并且及时出口。     

投喂卤虫无节幼体条件下黄颡鱼仔稚鱼生长、存活率、摄食力和体成分的变化

试验分析了投喂卤虫无节幼体条件下黄颡鱼(Pseudogrus fulvidraco)仔稚鱼生长、存活率、摄食力和体成分的变化。随着仔稚鱼的生长和发育,摄食率和胃充塞度逐渐加大,体长大于10 mm的仔鱼,摄食率都在93.3%以上,大多数个体胃充塞度都在3～5级。投喂卤虫无节幼体的黄颡鱼仔稚鱼生长较传统育苗方式生长快,存活率高。体内粗养分、氨基酸与脂肪酸含量都发生相应变化。黄颡鱼淀粉酶、蛋白酶与脂肪酶活性均在1日龄时即可检测到,开口期即5日龄时,3种消化酶比活力均达到较高值,15日龄后消化酶比活力又都降低到较低水平。卤虫无节幼体体内营养物质含量丰富,大小适口,是黄颡鱼仔稚鱼开口摄食的优质生物饵料。     

Two pathogens of Greenshell™ mussel larvae, Perna canaliculus: Vibrio splendidus and a V. coralliilyticus/neptunius-like isolate

Bacterial pathogens of Greenshell™ mussel (GSM) larvae can cause batch losses during hatchery production. Twenty-two isolates were screened using a larval bioassay. Two strains were identified as potential pathogens. Phenotypic identification of these strains revealed two non-reactive Gram-negative, oxidase positive rods. Sequencing of the 16S rRNA gene identified Vibrio splendidus and a V. coralliilyticus/neptunius -like isolate as pathogens of GSM larvae, with an ability to cause 83% and 75% larval mortality in vitro , respectively, at a concentration of 10² CFU mL⁻¹. Histopathology indicated that the route of infection was via the digestive system. Using healthy larvae as target hosts, Koch's postulates were confirmed for the two isolates. This is the first report on pathogens of GSM larvae.     

不规则盐度脉冲对许氏平鲉氨氮、磷排泄的影响

在静水系统中,骤然改变水体盐度,形成盐度脉冲;研究许氏平鲉Sebastodes fuscescens(Houttuyn)经历该脉冲后其氨氮、活性磷酸盐排泄的情况。结果表明,盐度改变后,许氏平鲉的氨氮排泄率比正常盐度(30)下呈现出不同程度的升高趋势;当盐度由30降为25和20时,随着体重增加,氨氮排泄率先增大,后又减小;当盐度由30上升为35时,氨氮排泄率随体重增加而呈下降趋势。盐度改变后,许氏平鲉的活性磷酸盐排泄率随体重增大呈先增大后减小的趋势。在同一体重下,盐度由30降至20时,活性磷酸盐的排泄率最大;盐度由30升至35时,磷的排泄率最小。方差分析表明,盐度脉冲对许氏平鲉氨氮排泄率有显著的影响(P<0.05),对活性磷酸盐排泄率的影响不显著(P>0.05)。该研究对于鱼类养殖的水质管理、养殖场的布设等有重要的指导意义。     

Several micronutrients in the rotifer Brachionus sp. may not fulfil the nutritional requirements of marine fish larvae

The current best practice intensive culture of larval Atlantic cod includes feeding rotifers from onset of exogenous feeding until 25–30 days after hatching. These larvae grow considerably slower and develop higher frequencies of deformities than larvae reared in semi‐extensive systems, using copepods as feed. The present study compares the micronutrient concentrations in rotifers with those of copepods, with the aim of identifying nutrients that may be limiting for normal growth and development of cod larvae. An additional criterion used is the nutrient requirements given for fish in general, by NRC (1993) , as nutrient requirements of cod remains to be determined. Rotifers were fed on four different diets, consisting of baker's yeast with cod liver oil (3.3 : 1 dry weight (DW)/v), baker's yeast with Algamac 2000^TM (3.5 : 1 DW), baker's yeast with live algae Chlorella (4.1 : 1 DW), and Culture Selco 3000^TM (CS). CS was a complete commercial diet for rotifers while the other diets are considered as based on raw ingredients. Compared with copepod nutrient levels, rotifers grown on yeast‐based diets supplemented with either cod liver oil, Algamac 2000 or Chlorella were apparently sufficient for covering the requirements in cod larvae for all the B‐vitamins, except thiamine. Rotifers cultured on the CS diet also had sufficient amounts of thiamine. Of the minerals, only calcium and magnesium were sufficient, using this criterion while iron was on the borderline. However, with reference to the requirements given for larger fish ( NRC 1993 ), only thiamine, vitamin A, manganese, selenium and perhaps copper, appear too low in the rotifers cultured without extra micronutrient supplementation. The other nutrients were present at levels intermediate between copepod and fish requirement levels. This study suggests that it is necessary to develop enrichment techniques to produce rotifers with sufficient amounts of all micronutrients. Such techniques will also be important tools for determining which nutrients are present at levels below the actual requirements in cod larvae.     

饵料蛋白能量比对黑鲷幼鱼生长和体成分的影响

取黑鲷(Sparusmacrocephalus)幼鱼960尾,体重(3.39±0.18)g,以鱼粉和豆粕作为蛋白源,鱼油和豆油等比例混合油作为脂肪源,共配制4个蛋白水平(34%、38%、42%、46%),每一蛋白水平设3个脂肪水平(10%、13%、16%),共12种饵料,糖水平保持在16%左右,饵料的蛋白能量比(P/E)在96.76～136.21mg/kcal。黑鲷幼鱼随机分成12组,每组设2重复,实验为期42d。结果表明,对特定生长率(SGR)与饵料系数(FCR)的影响,以较高蛋白组(38%、42%、46%)显著优于低蛋白组(34%)(P<0.05),中、高脂肪组(13%、16%)显著优于低脂肪组(10%)(P<0.05);各组饵料对成活率的影响无显著差异(P>0.05)。当蛋白水平为42%,脂肪水平为16%时,黑鲷幼鱼获得最大特定生长率(3.20)、最高蛋白质效率(2.10)和最小饵料系数(1.14)。全鱼脂肪含量随着饵料中脂肪水平的提高而逐渐升高。在同一饵料蛋白水平内,全鱼蛋白与灰分含量随着饵料脂肪水平的提高呈逐渐升高趋势。经统计分析,饵料中不同蛋白能量比显著影响黑鲷幼鱼生长(P<0.05),饵料中脂肪有明显节约蛋白质的作用(P<0.05)。由生长及体成分的实验结果得出,黑鲷幼鱼的最适饵料蛋白水平为42%,最适蛋白能量比(P/E)为110.37mg/kcal。     

基于厘米级无人机影像的水土保持措施精准识别

基于厘米级高分辨率无人机影像,应用面向对象方法(Object-Based Image Analysis, OBIA)对吉林省伊通县椽子沟流域的横坡改垄、地埂植物带、生态恢复乔木林、生态恢复草地等水土保持措施进行自动精准识别。应用超绿指数(Excess Green Index,ExG)、超红指数(Excess Red Index,ExR)、归一化差异指数(Normalized Difference Index,NDI)等光谱指数,形状的主方向、形状指数等形状特征,均值(Mean)、方差(Variance)、对比度(Contrast)等纹理特征进行措施的特征提取。结果表明:研究区水土保持措施识别的总体精度可达91.24%,Kappa系数为0.87;对垄台、垄沟等线性水土保持措施总体精度可达72.33%,Kappa系数为0.63。基于厘米级无人机影像,应用面向对象方法基本可实现对黑土区水土保持措施的精准识别,也可对垄台垄沟等线性措施进行自动识别,研究结果可为水土保持措施实施范围及完好程度的动态监测提供参考依据。     

地形对黑土区典型坡面侵蚀—沉积空间分布特征的影响

研究地形对黑土区坡面侵蚀-沉积空间分布特征的影响可以为水土保持措施配置提供科学依据。以典型黑土区——黑龙江省宾县东山沟小流域为研究区域,在流域上游、中游和下游各选取2个典型坡面,坡面种植作物均为玉米。典型坡面坡顶、坡上、坡中、坡下和坡脚的平均坡度分别为3.1°,3.0°,4.0°,2.8°,1.2°。利用137Cs示踪技术,分析了坡度、坡长和坡形对坡面侵蚀—沉积空间分布特征的影响。结果表明:研究流域农耕地坡面以侵蚀为主,平均侵蚀速率为448 t km~(~(-2)) a~(~(-1)) ;坡面不同部位土壤侵蚀—沉积分布特征差异明显,坡顶、坡上、坡中和坡下主要表现为侵蚀,平均侵蚀速率分别为819、376、1 000和634 t km~(~(-2)) a~(~(-1)) ,而坡脚表现为明显的沉积,平均沉积速率为~(~(-1)) 382 t km~(~(-2)) a~(~(-1)) 。不同坡形坡面侵蚀-沉积分布存在差异,凸形坡坡面表现为先侵蚀后沉积的分布特征,而复合坡坡面呈现出侵蚀-沉积交错分布特征;坡面土壤侵蚀速率与坡度和坡长均呈极显著的幂函数关系,而坡度对黑土区坡面侵蚀的影响明显大于坡长,反映了即使在长坡缓地形的黑土区坡度对侵蚀的影响仍然有重要作用。因此,在黑土区配置合理的水土保持措施时,应尽量削弱坡度对坡耕地土壤侵蚀的影响。