基于MODISNDVI的锡林郭勒草原近10年的时空动态

利用MODIS数据计算得到的归一化差值植被指数(NDVI), 对内蒙古自治区锡林郭勒草原不同类型草地近10年(2003－2012)生长季(4－10月)植被状况时空特征和变化情况进行研究。结果表明, 锡林郭勒草原NDVI总体表现为由东北向西南递减的规律, 空间差异2005年最大, 2007年最小, 且不同年度间相同类型草原空间变化基本一致。全区整体年际间变化表现为2012年最大, 2003年次之;沙地草原和荒漠草原在2005年变化最小, 波动主要在2004－2006年;草甸草原和典型草原则在2007年变化最小, 波动主要在2007－2009年。空间变异分析显示, 2003－2012年沙地草原变异系数(CV)小于0.1, 属非常稳定型, 草甸草原、典型草原和荒漠草原的CV值依次增大, 但都介于0.1～0.2, 属于稳定型。说明近10年来锡林郭勒草原状况较为稳定。通过对区域主要气象要素与NDVI间关系的分析, 得到NDVI主要受降水影响, 二者之间存在显著正相关关系, 相关系数高达0.83;日照时数与NDVI间存在相反的变化趋势;而平均气温与NDVI没有明显关系。     

Air oxidation of S(IV) in cloud-water samples

Aerobic oxidation of S(IV) was investigated in cloud-water samples collected at Great Dun Fell,U.K., as part of a wider project into cloud-water chemistry. The rate was found to be first-order in S(IV) concentration, and the reaction rate constant. k_S(IV), was found to vary from 10^–5 to 10^–3 s^–1. The rate constant was highly correlated with H⁺ concentration (pH 3.5 to 6.5) and Fe concentration (<0.02 to=">^–6 mol dm^–3). The aerobic oxidation of S(IV) does not contribute significantly to SO₂ oxidation in clouds at Great Dun Fell, however, the reaction may be of consequence in clouds and fogs at polluted or urban sites with elevated trace metal concentrations. Also, this reaction may be responsible for the oxidation of S(IV) in cloud-water samples during storage.     

Changes in herbage chemical composition due to proportion of species in alfalfa‐orchardgrass mixtures

Abstract

Legumes and grasses are widely grown in mixtures throughout the United States and Canada. This study was conducted to determine the changes in chemical composition of herbage that occur as proportion of legume and grass change in the mixture. Composition of mixtures of alfalfa (Medicago sativa L.) and orchardgrass (Dactylis glomerata L.) were studied after their herbage had been mixed by weight into seven different proportions: 100% alfalfa ‐ 0% orchardgrass, 80% ‐ 20%, 65% ‐ 35%, 50% ‐ 50%, 35% ‐ 65%, 20% ‐ 80%, and 0% ‐ 100%, respectively. The forages were grown in rows of pure alfalfa or pure orchardgrass spaced 45 cm apart on fertilized Dodge silt loam (Typic Hapludalf). Alfalfa was at late bud and orchardgrass was a few days from the appearance of the first anthers when harvested on May 29, 1975. Four replications of each of the mixtures were prepared, and the mixtures were made after tissues had been ground to 40‐mesh size.

No significant differences among mixtures were found for S, Cu, total nonstructural carbohydrates (TNC), or in vitro digestible dry matter (IVDDM). Concentrations of N, P, Ca, Mg, Na, Al, Ba, Fe, Sr, B, Zn, starch, and acid‐detergent lignin (ADL) were highest in pure alfalfa herbage and significantly decreased in concentration as amount of orchardgrass in the mixture increased. In direct contrast, concentrations of K, Mn, total sugars, fructosan, cell wall constituents (CWC), cellulose, hemicellulose, and acid detergent fiber (ADF) were lowest in pure alfalfa herbage and significantly increased in concentration as amount of orchardgrass in the mixture increased. These data show that an increase in amount of orchardgrass in a mixture with alfalfa reduced the concentrations of most herbage constituents important to animal nutrition and increased the fibrous constituents.     

特大暴雨下油松林根系对土壤元素迁移的影响

根际是元素由土壤进入植物体的主要界面,降水对根际土壤元素的迁移有显著影响。本文用原状土柱淋滤实验装置及大型挖掘剖面壁法,定量分析了特大暴雨下不同深度土层油松林根系影响土壤元素的稳定输出通量的剖面特征,旨在探索黄土区林木根系对土壤养分生物有效性的提高途径。研究结果表明,特大降雨条件下,油松林地的元素随土层深度增加呈明显的递减规律,在农地土壤剖面中变异不明显。油松林地元素稳定输出通量的平均值显著大于无根系土壤。油松林030.cm土壤剖面中的元素输出通量占总剖面元素输出通量的96.32%;油松林根系对常量元素K、Na、Mg、Ca、有益元素Si、微量营养元素Mn有明显稳定强化作用的土层深度范围为030cm,对有益元素Al和微量元素Cu、Fe有明显稳定强化作用的土层深度范围为045.cm。     

基于地理探测器的寻乌县土壤微量元素影响因子分析

为了对江西省赣州市寻乌县土壤硼(B)、硒(Se)、锰(Mn)、铜(Cu)4种微量元素的空间分布特征进行探究,同时分析影响其分布的因子,基于寻乌县2018年采集的572个表层土壤(0～20 cm)样点数据,采用描述性统计分析、相关性分析、地统计分析、地理探测器等方法进行分析.结果 表明,根据《土地质量地球化学评价规范》划...     

Response of Yield and Some Physiological Traits of Groundnut (Arachis hypogaea L.) to Topping Height and Application Methods of Zn and Ca Nano-Chelates

Groundnut is an annual legume and important oilseed crop in the world. In order to evaluate the influence of the topping height and application methods of Zinc (Zn) and Calcium (Ca) nano-chelates on quantitative and qualitative characteristics of groundnut, these experiments were carried out during the 2016–2017 cropping seasons on groundnut in Iran. Both foliar and in soil applications of Zn and Ca nano-chelates improved groundnut yield. Foliar application of Zn nano-chelate in combination with topping the main stem 20 cm above the ground produced the highest 100-seed weight (82.19 g), seed yield per unit area (2722.5 kg.h^?1), harvest index (57.53%), biological yield (6540.00 kg.h^?1), oil yield (1486.76 kg.h^?1), protein yield (742.66 kg.h^?1), seed Zn content (12.08 ppm) and Ca content (35.86 ppm). The application of Zn nano-chelate had different positive influences on vegetative and reproductive growth of groundnut plants. Generally, optimizing of the nutritional status in groundnut plants with Ca and Zn supplements is recommended to enhance the quantitative and qualitative yield of groundnut.     

Assessing biogas digestate,pot ale,wood ash and rockdust as soil amendments: effects on soil chemistry and microbial community composition

Applying by-products as soil amendments to agricultural systems is growing in popularity. We aimed to assess the efficacy of some contemporary by-products to provide nutrients to crops as well as the potential harm of adding toxic elements to the environment. Four different by-products widely available in Northern Europe were tested for their effects on two nutrient-poor agricultural soils in terms of increasing available macro- and micro-nutrients as well as toxic elements. Assessing soil microbial community as a sensitive tool for evaluating soil quality was conducted with the focus on microbial activity, carbon metabolism and on Rhizobium/Agrobacterium. Wood ash increased pH and Ca_EDTA, K_EDTA and Mg_EDTA in the soils. The only increase in EDTA-extractable micronutrients in the soils was observed by applying pot ale, increasing Cu. None of the amendments increased the availability of Pb and Cd in the soils. Soils amended with the by-products thus remained similar to the unamended control but were quite different from fully mineral fertilised soils. There were no detectable adverse effects on the physiological and genetic profiles of microbial communities. The by-products were moderately beneficial and did not change the soil microbial community as much as the fully fertilised treatment with mineral fertilisers. Changes in the microbial community profiles were probably due to direct effects on microbes limited by K, Ca and N as opposed to indirect effects on plant growth. This is potentially significant in understanding how to improve impoverished and marginal soils as microbial activity affects many other ecosystem functions.     

铵硝营养对水稻氮效率和矿质养分吸收的影响

NH_4~+和NO_3~–是对植物有效的两种主要无机氮源。水稻一般被认为是偏好NH_4~+的植物,但是在NO_3~–条件下,水稻也能良好地生长。大多数关于水稻铵硝营养的报道是在pH 6.0左右的水培条件下开展的,但是对于酸性条件下水稻铵硝营养研究很少。随着土壤酸化的加重及一些边际酸性土壤被用作水稻种植,研究酸性条件下水稻的铵硝营养具有重要意义。本文采用水培试验,在pH 5.0的条件下,通过添加和不添加pH缓冲剂MES(2-(N-吗啡啉)乙磺酸),研究了NH_4~+和NO_3~–对水稻生长、氮效率和矿质养分(N、P、K、Ca、Mg、Fe、Zn、Cu、Mn)吸收的影响。结果表明,在不添加MES的条件下,水稻地上部生长(株高、叶绿素含量、干重)在NH_4~+和NO_3~–之间没有显著差异,而添加MES后,NH_4~+处理的水稻地上部生长优于NO_3~–。不管是否添加MES,NO_3~–处理的水稻地下部生长(根长、根表面积和根物质量)优于NH_4~+。水稻含氮量和氮利用效率在不同NH_4~+和NO_3~–处理之间没有显著差异,但是NH_4~+处理的水稻氮吸收效率高于NO_3~–。与NO_3~–相比,NH_4~+增加了水稻地上部P和Fe含量,而降低了水稻地上部Ca、Mg、Zn、Cu和Mn含量,对K含量影响较小。上述结果表明,NH_4~+有利于改善水稻地上部生长,提高氮吸收效率、地上部P和Fe含量,而NO_3~–则有利于水稻发根,提高地上部Ca、Mg、Zn、Cu和Mn含量。     

不同品种肉鸡屠宰性能、胸肌肉品质和成分测定及分析

研究旨在探讨中国自主研究培育的白羽肉鸡和爱拔益加AA在屠宰性能、肌肉品质和组成成分之间差异。以‘wod’系列白羽肉鸡和爱拔益加AA为素材,测定7周龄时各个品种的屠宰性能、胸肌肉品质以及胸肌中风味前体物质、矿物元素、微生素等成分含量,分析比较不同品种间的差异变化。结果表明：wod168和wod178的屠体率、全净膛率和胸肌率均极显著低于wod188和AA(P<0.01),翅膀率极显著高于后两者(P<0.01)。wod168的胸肌肌肉pH和嫩度极显著小于AA(P<0.01),肉色的L值和b值显著高于AA(P<0.05)。wod168胸肌肌肉氨基酸总量、矿物元素总量和粗蛋白含量均高于其他三个品种,肌内脂肪和胆固醇含量低于其他品种。wod168产肉性能不及其他品种,但其胸肌肌肉肉品质更佳,更符合消费者对优质肉品质的需求。     

江西省土壤可溶态稀土元素含量和分布规律的研究

对江西 1 1种母质发育的有代表性的水稻土、旱作地、自然土壤 ,61个剖面 ,4 1 2个土样的可溶态稀土元素分析测定 ,统计结果表明 :江西土壤稀土元素的强度因素处于较高水平 ,平均值为 1 9 0mg/kg ,有 4 2 80 %的样点处于丰富级 ;有由南向北 ,由东向西逐渐降低的趋势 .其含量最高的地区是赣南由花岗岩、泥质岩、第四纪红粘土、酸性紫色土、碳质岩类风化物等母质发育的土壤 ,较低的为赣西北由石英岩 ,第三纪红砂岩、石灰岩、下蜀系黄土等母质发育的土壤 ;在土壤剖面分布中 ,旱作地表层低于底层 ,水稻土表层有生物富集作用高于底层 ;影响土壤中可溶态稀土元素含量的主要因子有 :成土母质 ,气候条件 (温度 ,降水量 ) ,土壤 pH ,土壤质地和耕作类型