抑制肠道气呼吸大鳞副泥鳅主要呼吸器官的组织病理

为了阐明肠道气呼吸对泥鳅的生理作用,本研究通过抑制大鳞副泥鳅肠道气呼吸,探究其主要呼吸器官的组织病理变化。结果显示,被抑制肠道气呼吸的大鳞副泥鳅通常在1周左右死亡。当被抑制肠道气呼吸的大鳞副泥鳅出现垂死时,采集对照组和实验组的鳃、皮肤、前肠、中肠、后肠以及直肠进行苏木素—伊红(H.E)染色、阿利新蓝—高碘酸雪夫氏(AB-PAS)染色组织切片观察和扫描电镜观察,主要的病理变化:①H.E染色结果显示实验组大鳞副泥鳅鳃丝末端充血,背部皮肤表皮层的毛细血管收缩并减少,且真皮层细胞呈畸形,前肠黏膜褶膨大,后肠浆膜层有血红细胞渗出,后肠、直肠结缔组织显著增厚;②AB-PAS染色结果显示,实验组大鳞副泥鳅鳃、背部皮肤、后肠、直肠组织中嗜酸性空泡细胞均增多,前肠和中肠固有层酸性黏蛋白含量增多,黏膜下层中性黏蛋白含量减少;③扫描电镜结果显示,实验组大鳞副泥鳅鳃丝鳃小片表面皱缩,表皮受损脱落,背部皮肤表面分泌孔增加,中肠内腔表面突起增多,后肠和直肠絮状颗粒增多。研究表明,抑制大鳞副泥鳅肠道气呼吸会引发其主要呼吸器官上皮组织出现黏液细胞增多、血红细胞溢出等病理变化,甚至导致机体死亡,由此可知,肠道气呼吸行为是大鳞副泥鳅的必要生理活动。本研究将为大鳞副泥鳅的健康养殖及幼苗培育提供新的参考。     

不同增氧滴灌方式对蔬菜生长生理指标的影响

为了研究不同增氧方式对盆栽小白菜生长生理指标的影响,以小白菜为供试作物,采用盆栽地下滴灌的方式,以普通地下滴灌作为对照(CK),设置循环曝气(MAI)、双氧水(H₂O₂)、纯氧扩散器曝气(OC)及射流振荡器曝气(FO)4个增氧灌溉处理.结果表明,增氧地下滴灌显著提高了土壤呼吸速率,处理MAI,OC和FO较对照处理分别增大了65.87%,66.79%和111.62%.增氧地下滴灌促进了小白菜的根系生长、光合作用、蒸腾速率和气孔导度,进而提高了小白菜的物质量积累和产量.与对照相比,处理MAI的地下部鲜质量增大了42.03%,地下部干质量增大了79.85%;处理MAI,H₂O₂,OC和FO的光合速率分别增大了868.62%,794.14%,778.67%和650.19%;处理MAI,H₂O₂和OC的气孔导度较CK增大了157.14%,128.57%和85.71%,蒸腾速率增大了55.61%,32.38%和19.58%;处理MAI和H₂O₂的产量分别增大了56.36%和38.72%.综上,增氧地下滴灌可增强小白菜根区的土壤呼吸作用,改善光合作用、蒸腾速率和气孔导度,提高了产量及水分利用效率.其中,循环曝气处理的改善效果最为显著.     

人参皂苷和多糖对肺肠功能影响研究进展

消化和呼吸功能是畜牧养殖过程中面临的两大问题,其会严重影响畜牧业经济效益。作为人参主要功能性成分,人参总皂苷和人参多糖在肺肠功能调节方面具有较好效果。本文总结了近年来人参总皂苷和人参多糖对肺肠功能调节的研究情况,以期为其在畜牧生产应用方面提供参考。     

Rapid salinity changes affect the survival and physiology of a penaeid prawn: Implications of flood events on recruitment to the fishery

Estuaries act as nurseries for many penaeid prawns, but these habitats are highly susceptible to salinity decline through flooding. The rate of salinity decline and duration of exposure to non‐optimal salinity may affect survival and subsequent recruitment of prawns to the fishery. This study aimed to determine the effect of salinity fluctuations observed in local estuaries during flood events using a novel dilution approach. Mortality of juvenile Melicertus plebejus (Hess) was assessed after 24 hr exposure to 24 rates of salinity decline ranging from 0.01% to 20% per hr. After the salinity decline, prawns were held at the final salinities for five days before again assessing mortality as well as aerobic metabolic rate and prawn water content. Salinity decline from 36 to ~0.8 led to 50% mortality, but continued exposure to low salinity for five days increased mortality at this salinity to 99% and shifted the 50% mortality point to salinity ~5. Aerobic metabolic rate and water content data suggested the cause of mortality due to exposure to salinities < 5 was osmoregulatory failure. Rapid salinity declines over 24 hr and sustained low salinity due to flooding could compromise the survival of juvenile prawns, potentially reducing recruitment to the fishery.     

Short-term spatiotemporal variation of soil CO2 emission,temperature, moisture and aeration in sugarcane field reform areas under the influence of precipitation events

Soil CO₂ emission (FCO₂) in agricultural areas results from the interaction of different factors such as climate and soil conditions. Our objective was to investigate the spatiotemporal variation of FCO₂, temperature (T_soil), moisture (M_soil) and air-filled pore space (AFPS), as well as their interactions, during the sugarcane field reform. The study was conducted on a 90 × 90 m sampling grid with 100 points at 10 m spacings. Ten assessments of FCO₂, T_soil and M_soil were carried out at each point over a 28-day period. The greatest mean values of FCO₂ (0.74 g m⁻² hr⁻¹) and M_soil (31.7%) were obtained on Julian day 276, 2013, being associated with precipitation events at the study site. Also, the smallest values of AFPS (19.17%) and T_soil (20.90°C) were observed on the same day. The spatial variability of FCO₂, T_soil, M_soil and AFPS was best described by an adjusted spherical model, although an exponential model better fitted some results. The spatial pattern of all soil attributes showed little temporal persistency, indicating a high complexity for FCO₂ during precipitation. Correlation maps assisted in identifying regions where M_soil and AFPS better controlled the emission process and where T_soil was important. A major challenge for world agriculture is to increase the efficiency of conventional soil management practices. We highlight the importance of the spatial pattern of soil properties that directly influence the CO₂ emission dynamics. Future mitigation actions should involve less intense tillage and ensure homogeneous applications of soil inputs, thereby reducing production costs and the contribution of these activities to CO₂ emissions during the sugarcane field reform.     

富里酸对土壤中DnBP的降解及微生物活性的影响

为探究富里酸对有机污染物DnBP的降解和土壤微生物活性的作用,采用土壤培养试验,研究了FA对土壤中DnBP的降解动力学过程及土壤微生物活性的影响规律。结果表明,FA的添加缩短了DnBP的降解半衰期,FA各处理组的半衰期为对照处理的48.1%~67.7%;FA促进了土壤的基础呼吸,40mg g-1处理组促进作用最强,最大CO2释放量为空白对照组的40.87倍;而过氧化氢酶活性则表现出了低浓度FA(10~20mg g-1)促进,高浓度FA(40~160mg g-1)抑制的变化趋势;FA对土壤脱氢酶活性主要表现为促进作用,40~160mg g-1FA对脱氢酶活性促进作用显著。相关分析结果表明FA用量与土壤中DnBP降解率呈正相关,与过氧化氢酶活性呈极显著负相关,与土壤呼吸强度、脱氢酶活性呈极显著正相关。通径分析结果表明FA用量与土壤中DnBP降解率之间有较强的直接效应,还与土壤呼吸强度、土壤酶之间存在间接效应,从而影响DnBP的降解。     

长期少免耕对中国东北玉米农田土壤呼吸及碳氮变化的影响

在黑土区37年不同耕作模式定位试验田，采用原位法比较常规旋耕灭茬起垄（CT）、旋耕留高茬行间深松-少耕（RT）、免耕（NT）和深翻（PT）4种耕作模式土壤呼吸速率及其与土壤温度和湿度的关系，测定土壤总碳氮、无机氮，微生物碳氮的变化。结果表明，玉米生育期间土壤呼吸呈单峰变化，开花期达最大值，生长季平均呼吸速率依次为RT > NT > CT > PT。4个处理土壤温度与土壤呼吸速率间存在显著指数关系。不同耕作模式0~10 cm土壤温度可解释土壤呼吸速率变异的38.3%~67.9%，温度敏感性系数Q10范围为2.1~5.3；RT和NT处理显著提高0~20 cm土壤碳氮含量；RT处理在0~20 cm土壤中微生物碳含量均高于CT、NT和PT处理。RT处理土壤呼吸对温度响应提高，RT和NT处理显著增加上层土壤总碳氮含量，利于土壤质量提升。     

乙烯处理对树莓果实呼吸速率及乙烯合成代谢的影响

采集不同成熟期(绿果期、白果期、着色期、成熟期、过熟期)"哈瑞太兹"树莓果实,并利用乙烯利及乙烯抑制剂1-MCP处理白果期果实,测定上述果实不同部位(整果、小核果和花托)乙烯生成速率、呼吸速率、ACC合成酶(ACS)和ACC氧化酶(ACO)活性及RiACS1和RiACO1基因相对表达量变化。结果表明,花托是树莓果实中产生乙烯的主要部位,果实食用部分小核果乙烯生成和呼吸速率在果实发育期间变化平稳,同时结合树莓果实采后无后熟、常温贮存后易腐烂的特性,推测树莓应属于非跃变型果实。乙烯利处理促进树莓果实提前着色,整果、小核果和花托乙烯生成速率短时内增加,ABA含量显著增加,提高ACS和ACO酶活性及RiACS1和RiACO1基因转录水平,而1-MCP抑制此过程。乙烯利处理对呼吸速率影响较小,但1-MCP处理显著抑制小核果和花托中的呼吸速率。     

草莓呼吸特性与发酵阈值研究

以红颜草莓为试材,采用密闭系统法,研究了不同温度(0、5、20℃)条件下,草莓包装环境内的气体体积分数变化和草莓的呼吸速率,拟合呼吸速率方程,并确定草莓的发酵阈值、乙醇含量及品质指标的变化。结果表明:密封盒内草莓的米氏模型参数拟合度较高,各方程决定系数(R2)值均在0.9以上。在0、5、20℃环境下,草莓果实的最大呼吸速率分别为5.49、9.09、26.32 mL CO2/(kg·h),最长贮藏时间分别为192、60、16 h,0℃和5℃环境下的发酵阈值比20℃环境下的低;果实的乙醇含量在最长贮藏时间点左右迅速升高;贮藏期间,果实硬度、可溶性固形物和可滴定酸含量呈下降趋势,花色苷含量呈上升趋势。综上所述,各温度下密封盒内草莓的米氏模型参数拟合度较高,低温可以有效地抑制果实的呼吸强度,延缓果实品质的下降,延长其贮藏期。     

High clay content accelerates the decomposition of fresh organic matter in artificial soils

Clay is generally considered an important stabiliser that reduces the rate of decomposition of organic matter (OM) in soils. However, several recent studies have shown trends contradicting this widely held view, emphasising our poor understanding of the mechanisms underlying the clay effects on OM decomposition. Here, an incubation experiment was conducted using artificial soils differing in clay content (0, 5, and 50%) at different temperatures (5, 15, and 25 °C) to determine the effects of clay content, temperature and their interaction on fresh OM decomposition. CO₂ efflux was measured throughout the experiment. Phospholipid fatty acids (PLFAs), enzyme activities, microbial biomass carbon (MBC), and dissolved organic carbon (DOC) were also measured at the end of the pre-incubation and incubation periods in order to follow changes in microbial community structure, functioning, and substrate availability. The results showed that higher clay contents promoted OM decomposition probably by increasing substrate availability and by sustaining a greater microbial biomass, albeit with a different community structure and with higher activities of most of the extracellular enzymes assayed. Higher clay content induced increases in the PLFA contents of all bacterial functional groups relative to fungal PLFA content. However, clay content did not change the temperature sensitivity (Q₁₀) of OM decomposition. The higher substrate availability in the high clay artificial soils sustained more soil microbial biomass, resulting in a different community structure and different functioning. The higher microbial biomass, as well as the changed community structure and functions, accelerated OM decomposition. From these observations, an alternative pathway to understanding the effects of clay on OM decomposition is proposed, in which clay may not only accelerate the decomposition of organic materials in soils but also facilitate the SOM accumulation as microbial products in the long term. Our results highlight the importance of clay content as a control over OM decomposition and greater attention is required to elucidate the underlying mechanisms.