The Humus Content and Soil Biological Properties as a Function of Organic and Mineral Fertilization

There is a growing recognition for the need to develop sensitive indicators of soil quality that reflect the effects of land management on soil and assist land users in promoting sustainability of agro-ecosystems. Three soil enzymes (dehydrogenase, phosphatase and invertase) microbial biomass as biological variables and soil organic matter content (SOM) were investigated relative to fertilization and soil fertility (estimated by crop yield) at a long-term fertilization trial (Keszthely, Hungary). 0-34.7-69.4-104.1t farmyard manure (FYM) ha m 1 5 yr m 1 and the corresponding amount of mineral fertilizers (NPK) were applied in two different crop rotation systems. There were four straw and/or stalk incorporating treatments in the second crop rotation 'B'. Enzyme activities, microbial biomass and the amount of SOM were generally higher in the fertilized soils than in the unfertilized soils. The type of amendments (mineral, FYM or mixed) had significant effects only on the amount of SOM. The correlations among the biological variables and the crop yield were generally low (r < 0.250. The differences in field management resulted only in the invertase activity.     

The optimal nutrition of maize in the hungarian national long‐term field experimental network

In Hungary, maize is grown on 1 million ha and occupies more than 20% of the arable land. The rich assortment of maize cultivars of different vegetation periods and different responses to nutritional effects, water supply etc. gives the growers the possibility to choose the cultivars suiting best the site characteristics (Jolânkai et al. 1999). Among the cereals maize has the highest genetical potential. To utilize its yield and quality potential, soil types of high nutrient content and regular nutrient supply are required (Gyõrffy, 1979). Both over‐ and under‐fertilization have an unfavourable effect on the yield and quality of maize (Debreczeni, 1985). Crops can be supplied with the appropriate nutrient amounts only with the knowledge of soil characteristics in the different agro‐ecological regions (nutrient content, water supply, soil compactness, pH, nutrient supplying capacity etc.). In Hungary, a network of long‐term field fertilization trials with uniform fertilizer treatments has been maintained at nine experimental sites representing different agro‐ecological regions of the country. This experimental network gives a basis to test the nutrient responses of our main crops and calibrate their optimal nutrient supply (Kismányoky, 1991).     

Level and Timing of Nitrogen Fertilizer Application to Early and Semi-early Potatoes (Solanum tuberosum L.) Grown with Irrigation on Light Soils in Norway

Trials were performed with early and semi-early potatoes to test the effects of nitrogen (N) fertilizer level (0-160 kg N ha^-1) and timing (all at planting versus half then and half either soon after emergence or 3 weeks later). All seven trials with earlies were irrigated as required, whilst different irrigation regimes (moderate versus intensive) were compared in two trials with semi-earlies. No benefit was derived from splitting the N application. Haulm growth and N uptake increased in all cases almost linearly up to the highest N level, but tuber yield did not respond in the same way. The optimum N level was 80 kg N ha^-1 for a yield of 15 Mg ha^-1, rising to 120 kg N ha^-1 for a yield of 40 Mg ha^-1. Tuber quality was lowered by the use of excess N fertilizer, particularly in the case of earlies. The quantity of mineralised N present in the soil after harvest rose sharply with above optimum fertilizer use, and the amount of N present in crop residues also increased. The likely leaching after early potatoes was estimated to be up to 80 kg N ha^-1. The proportion of fertilizer N which was not accounted for in either tuber yield, crop residues or mineral N in soil was 26% in earlies and 38% in semi-earlies.     

Shelf-Life of Spanish Mackerel (Scomberomorus commerson) from Northern Australian Waters

Abstract

The shelf-life of Spanish mackerel caught by line fishing in Northern Australian waters was evaluated. Spiked fish were stored in ice either headed and gutted or left uncut and subjected to sensory, nucleotide, pH, histamine and microbial analysts and the rigor pattern recorded. There was little difference between the two product forms. Rigor in uncut fish lasted for 14 ± 9.8 hours and in headed and gutted fish for 19.6 ± 16.3 hours. Spanish mackerel retained good sensory quality for up to 14 days. The bacterial load reached 105 cfu/g by 18 days. K values were low for most of the storage time, < 40%. Histamine levels did not develop more than 10 mg/kg during storage. The pH of Spanish mackerel did not change much even though bacterial levels become high.     

Comparison of nuclear and capacitance‐based soil water measuring techniques in salt‐affected soils

A field calibration experiment was carried out on salt‐affected clayey soil in Syria, to compare the sensitivity to soil electrical conductivity (ECe), and bulk density (ρ_b) of two instruments for estimating soil moisture: the neutron probe (NP) and the Diviner 2000 capacitance probe (CP). The results showed that the values of the correlation coefficient of the calibration were decreased when the ECe and ρ_b values increased; this decrease was more pronounced for the Diviner 2000, indicating that it was more sensitive to ρ_b and ECe than the NP. When only scaled frequency was used in the fitted equation, the Diviner 2000 in wet soil underestimated soil water content significantly at all depths, but especially in the top layer, by up to 0.09 cm³/cm³ compared with gravimetric determinations. However, in dry soil, the Diviner 2000 overestimated the volumetric water content by up to 0.05 cm³/cm³ in the top 15 cm, and by 0.03 cm³/cm³ at 30‐45 cm depth. The performance of the neutron probe was better overall; using a factory calibration curve no significant differences were observed between NP estimates and the gravimetric values. Including both ρ_b and ECe in the calibration equations improved the fits, although the regression coefficient (R²) for the Diviner 2000 remained low.     

速度赛马粪便微生物种群差异的研究

为筛选提高赛马竞技成绩的有益微生物,试验比较现役纯血速度赛马粪便微生物群落多样性及丰度差异。选择休赛一周的现役纯血马9匹,按比赛成绩分为A(16.8 m/s)、B(16.4 m/s)、C(16.3 m/s)3组。收集新鲜粪便样本,提取粪便样本菌群DNA,对微生物16S rDNA的V3~V4区序列Illumina测序。结果表明,A组与C组粪便微生物菌群之间在纲、种的分类菌群数上差异显著(P<0.05)。LDA效应分析A组马粪微生物标志物种为Bacteria、Firmicutes、Clostridia、Clostridiales、Veillonellaceae、Anaerovibrio,以上微生物标志物种在3组中的相对丰度分布为A组>B组>C组。A组的厌氧弧菌属(Anaerovibrio)、C组的根瘤菌目(Rhizobiales)的LDA效应值显著(P<0.05)。按马粪中微生物丰度,纲、目、科、属中分别有4、3、5、9、14组微生物差异(P<0.05)。研究表明,可以按微生物群落差异筛选出提高赛马成绩的消化道微生物制剂。     

抗菌肽粗提物对肉鸡生长性能、粪便微生物菌群结构及经济效益的影响

为分析抗菌肽粗提物对肉鸡生长性能、粪便微生物菌群结构及经济效益的影响,试验选择体重相近的21日龄白羽肉鸡600只,随机分成4组,每组15个重复,每个重复10只,1组为空白对照组饲喂基础日粮,试验2、3、4组在基础日粮中分别添加1.0%、1.5%、2.0%的抗菌肽粗提物,试验期为21 d。结果表明：（1）试验2、3、4组的平均采食均高于1组（P > 0.05）|试验3、4组的平均日增重较1组比分别提高11.0%、9.4%（P ＜ 0.05）,料重比较1组比分别降低18.5%、15.2% （P ＜ 0.05）|（2）试验3、4组粪便中大肠杆菌的含量较1组分别降低14.3%、18.0%（P ＜ 0.05）,试验3、4组粪便中乳酸杆菌、双歧杆菌的含量较1组比分别提高4.6%、6.7%、14.5%、12.3%（P ＜ 0.05）|（3）试验3、4组每只肉鸡经济效益较1组比分别提高19.3%、17.7%。综上,1.5%抗菌肽粗提物添加可以提高白羽肉鸡生长性能,改善粪便微生物菌群结构,提高其经济效益。 [关键词] 抗菌肽粗提物|白羽肉鸡|生长性能|粪便微生物菌群结构|经济效益     

黄土高原亚高山草地退化对土壤种子库的影响

本试验对黄土高原亚高山草地不同退化程度下土壤种子库的物种组成、种子密度、分布特征以及影响因素进行了研究。结果表明,研究区地上植物有31种,分属于14科、25属;种子库植物有32种,分属于14科、31属;种子库的83.45%都分布于浅层土壤中（0~5 cm）。随着草地退化程度的加重,地上植被和地下种子库中多年生植物的比例减少,种子库密度与丰富度都显著下降（P<0.001）;极度退化样地的地上一年生植物增多,物种组成与地下种子库相似;轻度和中度干扰的样地中,地上植物与种子库的物种的组成具有显著差异（P<0.01）。总之,亚高山草地退化对土壤种子库产生了较大的影响,其中土壤pH与水分是影响种子库密度与丰富度主要的环境因素。极度退化草地种子库密度极低,地上植被靠自然更新很难恢复,需人工辅助。     

黄河源区建植19年人工草地生物结皮CO2通量与叶绿素荧光参数的变化

为了解黄河源人工草地不同类型生物结皮和植被群落CO₂释放和固定的变化特征,并探讨二者的影响因子,本文通过调查黄河源建植19年人工草地不同类型生物结皮CO₂通量和植被土壤特征变化发现：藻和地衣结皮CO₂通量均显著小于苔藓结皮（10.58 μmol·m^-2·s^-1）（P<0.05）;苔藓结皮对应的植被群落CO₂通量（11.55 μmol·m^-2·s^-1）显著低于藻和地衣结皮（P<0.05）;藻和地衣结皮下的土壤CO₂通量显著大于苔藓结皮（约2倍,P<0.05）。苔藓结皮叶绿素初始荧光参数F₀（Minimal Fluorescence）和最大荧光参数F_m（Maximal Fluorescence）均最大;藻和苔藓结皮的PS Ⅱ最大光化学量子产量F_v/F_m（Optimal/Maximal Quantum Yield of PS Ⅱ）均高于地衣结皮。CO₂通量和叶绿素荧光参数的主要影响因子相似,均与禾本科高度、土壤铵态氮含量正相关,与pH负相关。因此,在研究草地碳平衡过程中应充分考虑生物结皮的贡献,同时需注意不同类型的生物结皮的CO₂通量和叶绿素荧光参数的差异变化。     

青藏高原湿草甸土壤氮组分对氮添加浓度的响应

为研究青藏高原湿草甸土壤氮组分对氮添加程度的响应规律,分析氮素大量输入生态系统后可能产生的环境和生态问题,本研究以青藏高原东北边缘碌曲县尕海-则岔国家自然保护区境内的湿草甸土壤为研究对象,设置空白对照(CK,0 g·m^-2)、低浓度(N₅,5 g·m^-2)、中浓度(N₁₀,10 g·m^-2)和高浓度(N₁₅,15 g·m^-2)4种处理,分析不同氮添加下的土壤氮组分含量(铵态氮、硝态氮、可溶性有机氮)的垂直和季节变化。结果表明:不同氮添加处理均能增加土壤氮组分含量,其增加程度依次为N₅＞N₁₀＞N₁₅＞CK;在土壤垂直剖面上,土壤氮组分含量随土层深度增加而降低;在植物生长季内,氮添加处理后的土壤氮组分含量较高值出现在植物生长末期。本研究表明氮添加对青藏高原湿草甸土壤有效氮的增加具有显著促进作用。