Nutritional significance of amino acids,vitamins and minerals as nutraceuticals in poultry production and health – a comprehensive review     

Mahmoud Alagawany  Shaaban S. Elnesr  Mayada R. Farag  Ruchi Tiwari  Mohd. Iqbal Yatoo  Kumaragurubaran Karthik  Izabela Michalak  Kuldeep Dhama 《The Veterinary quarterly》2021,41(1):1

Nutraceuticals have gained immense importance in poultry science recently considering the nutritional and beneficial health effects of their constituents. Besides providing nutritional requirements to birds, nutraceuticals have beneficial pharmacological effects, for example, they help in establishing normal physiological health status, prevent diseases and thereby improve production performance. Nutraceuticals include amino acids, vitamins, minerals, enzymes, etc. which are important for preventing oxidative stress, regulating the immune response and maintaining normal physiological, biochemical and homeostatic mechanisms. Nutraceuticals help in supplying nutrients in balanced amounts for supporting the optimal growth performance in modern poultry flocks, and as a dietary supplement can reduce the use of antibiotics. The application of antibiotic growth enhancers in poultry leads to the propagation of antibiotic-resistant microbes and drug residues; therefore, they have been restricted in many countries. Thus, there is a demand for natural feed additives that lead to the same growth enhancement without affecting the health. Nutraceuticals substances have an essential role in the development of the animals’ normal physiological functions and in protecting them against infectious diseases. In this review, the uses of amino acids, vitamins and minerals as well as their mode of action in growth promotion and elevation of immune system are discussed.  相似文献   

不同养殖模式翘嘴鲌肌肉营养品质比较   总被引：1，自引：0，他引：1  

丁德明  陈杏华  伍远安  陈虎  刘丽  何志刚 《中国饲料》2021,(1):89-95

为评价池塘与大湖不同养殖模式翘嘴鲌(Culter alburnus)肌肉营养品质差异,试验分析了商品翘嘴鲌肌肉常规营养成分、氨基酸、脂肪酸、矿物元素含量等营养指标。结果表明:大湖翘嘴鲌肌肉水分含量显著低于池塘翘嘴鲌(P<0.05),粗蛋白质含量高于池塘翘嘴鲌,差异不显著(P>0.05)。池塘与大湖翘嘴鲌肌肉,除了赖氨酸和组氨酸以外(P<0.05),绝大部分氨基酸含量均无显著性差异(P>0.05)。大湖翘嘴鲌肌肉的总氨基酸、必需氨基酸和鲜味氨基酸含量分别较池塘翘嘴鲌高出2.72%、2.87%和2.50%。根据氨基酸评分(AAS)和化学评分(CS)结果,池塘与大湖翘嘴鲌肌肉中第一限制性氨基酸均为蛋氨酸+胱氨酸,赖氨酸相对含量最高,必需氨基酸指数(EAAI)分别为68.81和69.62。池塘翘嘴鲌的棕榈油酸(C16:1)含量显著高于大湖翘嘴鲌(P<0.05),而大湖翘嘴鲌肌肉的单不饱和脂肪酸(MUFAs)、高不饱和脂肪酸(HUFAs)、必需脂肪酸(EFA)、EPA+DHA含量则高于池塘翘嘴鲌(P>0.05)。试验检测了池塘与大湖翘嘴鲌肌肉11种矿物元素,其中镁有显著差异(P<0.05),重金属元素(铬、镉、铅)含量均在限量范围以内。综上所述,大湖养殖翘嘴鲌营养品质优于池塘养殖。  相似文献   

Desiccation and cracking behaviour of clay layer from slurry state under wetting-drying cycles   总被引：3，自引：0，他引：3  

Chao-Sheng Tang  Yu-Jun Cui 《Geoderma》2011,166(1):111-118

Laboratory tests were conducted to investigate the effect of wetting-drying (W-D) cycles on the initiation and evolution of cracks in clay layer. Four identical slurry specimens were prepared and subjected to five subsequent W-D cycles. The water evaporation, surface cracks evolution and structure evolution during the W-D cycles were monitored. The effect of W-D cycles on the geometric characteristics of crack patterns was analyzed by image processing. The results show that the desiccation and cracking behaviour was significantly affected by the applied W-D cycles: the measured cracking water content θ_c, surface crack ratio R_sc and final thickness h_f of the specimen increased significantly in the first three W-D cycles and then tended to reach equilibrium; the formed crack patterns after the second W-D cycle were more irregular than that after the first W-D cycle; the increase of surface cracks was accompanied by the decrease of pore volume shrinkage during drying. In addition, it was found that the applied W-D cycles resulted in significant rearrangement of specimen structure: the initially homogeneous and non-aggregated structure was converted to a clear aggregated-structure with obvious inter-aggregate pores after the second W-D cycle; the specimen volume generally increased with increasing cycles due to the aggregation and increased porosity. The image analysis results show that the geometric characteristics of crack pattern were significantly influenced by the W-D cycles, but this influence was reduced after the third cycle. This is consistent with the observations over the experiment, and indicates that the image processing can be used for quantitatively analyzing the W-D cycle dependence of clay desiccation cracking behaviour.  相似文献   

水耕人为土磁性矿物的生成转化机制研究回顾与展望   总被引：2，自引：0，他引：2  

韩光中  黄来明  李山泉  陈留美 《土壤学报》2017,54(2):309-318

随着环境问题的日益突出,人为活动对土壤的影响越来越深刻,需加强对"人为作用"的研究以便解释现代土壤磁性的过程和变化。水耕人为土在发育过程中人为作用的方式多种多样,明确其磁性矿物的生成和转化机制及其影响因素有利于理解人为活动对现代土壤磁性的作用。但目前水耕人为土磁学研究还比较零散,缺乏系统性,已有研究结果有待深入梳理。本文对已有的相关研究报道,包括水耕人为土磁性参数的演变特征、磁性矿物的生成转化机制以及对成土因素的响应等进行综合评述。最后,对当前研究的不足和存在问题进行总结,并对研究方向进行了展望,以期有助于环境磁学的发展。  相似文献   

适宜无机盐及浓度抑制麦胚脂肪酶存在时油水界面张力     

陈中伟  孙俊  王力坤  吴其飞  徐斌 《农业工程学报》2017,33(15):308-314

为了探明无机盐稳定化脂肪酶的潜在机理,该文以小麦胚芽脂肪酶为研究对象,基于界面酶学的分析方法,研究添加浓度介于1.0×10-9~1.0×10-2 mol/L的Na~+、K+、Ca~(2+)、Mg~(2+)的氯化物对小麦胚芽脂肪酶存在的油-水界面特性的影响。结果表明,当小麦胚芽脂肪酶体系浓度为1.7×10-6 mol/L时,一价金属中Na~+更有利于抑制油-水界面的表面张力(P0.05),对麦胚脂肪酶存在时的油水界面特性影响也较大;二价金属离子Ca~(2+)对界面张力的影响趋势与一价离子不同,在高浓度时反而增加界面张力;当油水界面上存在脂肪酶的催化底物(三油酸甘油酯)和产物(油酸)时,添加浓度分别为10-6、10-6、10-4和10-9mol/L的Na~+、K~+、Ca~(2+)、Mg~(2+)均可一定程度上降低油水界面张力,从而降低麦胚脂肪酶的作用效果,三油酸甘油酯存在时Mg~(2+)的作用效果最明显(P0.05),油酸存在时Na+的作用效果最明显(P0.05)。综上,无机盐金属离子主要通过影响麦胚脂肪酶在油水界面的聚集行为及底物结构状态起到钝化麦胚脂肪酶的作用,该结果可为麦胚脂肪酶存在时界面的活性调控及麦胚的稳定化处理提供参考。  相似文献   

九宫山土壤剖面中黏土矿物的组成特征     

刘智杰  董雪  张志毅  黄丽 《土壤》2017,49(4):795-802

以湖北省九宫山的4种垂直地带性土壤为对象,研究其剖面层次的黏土矿物组合和铁、铝氧化物的特征,揭示山地土壤中黏土矿物的变化特点。结果表明,随海拔升高,土壤中黏土矿物类型从以高岭石为主,逐渐变为以14.0?矿物、伊利石及三水铝石为主,有从1︰1型向2︰1型矿物过渡的趋势;不同层次的土壤中黏土矿物类型和相对含量变化明显;土壤随垂直高程的升高,其中游离态铁、铝减小,非晶形和络合态铁、铝增加,各种形态铁、铝氧化物的总量也增加。  相似文献   

热带地区时间序列土壤中伊利石类矿物的演化——P.Barré假设在热带地区土壤中也存在吗?     

杨艳芳  李德成  胡锋  Bruce Velde  张甘霖  杨金玲 《土壤学报》2010,47(1):13-18

P.Barré等认为温带地区自然土壤中,由于植物根系将下层土壤中的钾和硅向上搬运,减缓了上层土壤中伊利石类矿物(混层伊利石/蒙皂石+伊利石)脱钾和脱硅过程,致使其长时间地存在较多的伊利石类矿物。本文旨在了解热带地区土壤中这一假设是否也存在,以海南琼北地区发育于由不同年代火山喷发形成的玄武岩所构成的时间序列土壤(1×104a,(9.0±2.0)×104a,(14.6±0.9)×104a,64×104a,(133±18)×104a,(181±8)×104a)为对象,利用X-射线衍射(XRD)技术分析了其黏土矿物的变化情况,结合土壤钾、硅、活性硅的分析结果,发现伊利石类矿物仅存在于(133±18)×104a以前的土壤中,表层土壤中钾和硅的含量高于下层的土壤,活性硅含量随成土年龄而降低。为此,我们认为:P.Barré假设在热带土壤形成发育过程中,在具有一定的生物复钾和复硅条件下,在成土初期也会存在,但最终会由于土壤强烈的脱钾和脱硅作用而逐步消失。  相似文献   

土壤粒度和磁化率特征对绰墩古水稻土成因的指示     

李学林  李福春  杨梅  代静玉  陈国岩  杨用钊 《土壤》2019,51(6):1226-1231

本文研究了绰墩农业遗址P-02原状土剖面的粒度分布,定量分析了土壤黏粒的矿物组成,测定了土壤/沉积物及其各粒级组分(黏粒、粉砂粒、细砂粒和粗砂粒)的磁化率。结果表明：在0 ~ 30 cm和134 ~ 154 cm两层段,黏粒含量从下向上有降低的趋势,这可能预示着长期的水耕作业造成黏粒从表层向亚表层移动;在148 ~ 200 cm层段,土壤磁化率从下向上有降低的趋势,可能说明该处存在长期淹水的状况。总之,黏粒含量和质量磁化率数据说明长江下游地区的先民在马家浜文化时期已开始采用“水溽”方式进行水稻的栽培。  相似文献   

铁氧化物-硅酸盐复合物的形成、性质及其对砷的固定     

杨忠兰  曾希柏  孙本华  苏世鸣  王亚男  张楠  张洋  吴翠霞 《农业现代化研究》2021,42(2):294-301

铁氧化物与硅酸盐矿物是土壤中最重要、最活跃的固相组分,它们之间的交互作用直接影响土壤物理化学特性,可有效地调控土壤(类)重金属的迁移、转化。本文以铁氧化物和硅酸盐矿物胶结过程中的一些表观特征变化为出发点,从宏观、表观到微观综述了二者交互作用的界面特性和机理、交互作用前后对土壤砷的固定与释放机制等内容。本文阐明层状硅酸盐与铁氧化物通过多种化学作用而发生表面复合,其中静电作用是作用力之一,带负电荷的硅酸盐与带正电荷的铁氧化物在静电引力的作用下迅速结合,在胶体表面双电层上形成二元团聚体;形成的二元团聚体可改变土壤矿物的表面积和孔性结构、表面电化学特性和物理性质。同时,铁氧化物-硅酸盐复合物表面的活性基团可以通过内层络合共氧的方式将土壤中AsO_4~(2-)络合,形成单核或双核表面络合物而固定砷。复合物对AsO_4~(2-)的吸附能力介于铁氧化物和硅酸盐矿物之间,并更接近铁氧化物的表面吸附特性。本文旨在为土壤砷的原位固定提供理论支撑。  相似文献   

中国福建省土壤的主要粘土矿物     

WANG Guo  ZHANG Wei-Ming  ZHOU Xin-Dun 《土壤圈》1996,6(1):47-56

The clay minerals of more than 200 soil samples collected from various sites of Fujian Province were studied by the X-ray diffraction method and transmission electron microscopy to study their distribution and evolution.Montmorillonite was found in coastal solonchak,paddy soils derived from marine deposit,lacustrine deposit and river deposit,and some lateritic red soil,red soil and yellow soil with a low weathering degree.Chlorite existed mainly in coastal solonchak and paddy soil developed from marine deposit.1.4nm intergradient mineral appeared frequently in yellow soil,red soil and lateritic red soil.The content of 1.4nm intergradient mineral increased with the decrease of weathering degree from lateritic red soil to red soil to yellow soil.Hydrous micas were more in coastal solonchak,paddy soils derived from marine deposit,lacustrine deposit and river deposit.and puple soil from purple shale than in other soils.Kaolinte was the most important clay mineral in the soils iun this province.The higher the soil weathering degree,the more the kaolinite existed.From yellow soil to red soil to lateritic red soil,kaolinite increased gradually,Kaolinite was the predominant clay mineral accompanied by few other minerals in typical lateritic red soil. Tubular halloysite was a widespread clay mineral in soils of Fujian Province with varying quantities.The soil derived from the paent rocks rich in feldspar contained more tubular halloysite.Spheroidal halloysite was found in a red soil and a paddy soil developed from olivine basalt gibbsite in the soils in this district was largely“primary gibbsite” which formed in the early weathering stage.Gibbsite decreased with the increase of weathering degree from yellow soil to red soil to lateritic red soil.Goethite also decreased in the same sequence while hematite increased.  相似文献