油菜菌核病菌的生物学特性研究

在不同温度、不同ｐＨ值的ＰＤＡ平板上培养油菜菌核病菌核和菌丝块,观察菌核萌发的最适温度和菌丝生长的最适温度、最适ｐＨ值,结果表明菌核萌发的最适温度为２４～２８℃,菌丝生长的最适温度为２０～２８℃,３５℃为菌丝的致死温度,菌丝生长的最适ｐＨ值为４.７～８.５。     

鸡油菌菌丝体培养技术研究

[目的]为鸡油菌的驯化和推广提供理论依据。[方法]野外采集鸡油菌,分别配制10种不同pH值和活性碳添加量的培养基对其进行培养,25℃连续培养45d,通过测定不同处理菌丝体的生物量,研究培养基pH值和活性碳添加量对鸡油菌菌丝体生长的影响。[结果]培养基过酸、过碱都会抑制鸡油菌菌丝体生长,培养基pH值为6.0时,鸡油菌菌丝体干重最大,为40.3mg/瓶,增殖倍数为26.85倍;活性碳对鸡油菌菌丝体生长具有明显的促进作用,当培养基中活性碳含量为0.03%时,鸡油菌菌丝体干重最大,为65.7mg/瓶,增殖倍数为43.77倍。[结论]鸡油菌生长的最适培养基pH值为6.0,活性碳添加量为0.03%。     

发酵脱氢产氢过程对微生物铁还原的影响

发酵型微生物是铁还原菌中的主要类群,但其发酵产氢过程对铁还原的作用尚不清楚,为此采用接种水稻土浸提液混合培养的方法对微生物分别利用葡萄糖、丙酮酸盐和乳酸盐为碳源时,Fe（Ⅲ）还原过程中脱氢酶活性变化、培养体系pH、氢气分压及铁还原特征进行分析,探讨了发酵微生物脱氢产氢过程与微生物Fe（Ⅲ）还原的内在关系。结果表明：2种水稻土浸提液中的微生物均能够以葡萄糖为优势碳源进行脱氢、产氢及还原氧化铁,Fe（OH）,可以诱导脱氢酶的产生,利用葡萄糖时脱氢酶活性在厌氧培养的4-6d出现最大峰值,利用丙酮酸盐和乳酸盐时脱氢酶活性出现峰值的时间分别为培养的15d和21-22d,脱氢酶活性出现峰值的时间与最大铁还原速率Vmax显著负相关、与最大反应速率对应的时间zk存在显著正相关关系。脱氢产氢过程中产生的H＋导致培养体系pH的变化是影响铁还原过程的主要原因,培养体系pH与体系氢气分压及Fe（Ⅱ）累积量呈极显著负相关。微生物利用不同碳源产氢时,利用葡萄糖的产氢能力最高,丙酮酸盐次之,乳酸盐最低。Fe（OH）3的加入增加了氢气的消耗量,培养体系氢气分压与Fe（Ⅱ）累积量存在极显著正相关关系。     

Midsummer copper sprays have no effect on ‘delicious’ apple fruit color grade or typiness

Recent reports suggested that multiple midsummer copper (Cu) sprays could improve the proportion of apple fruit (Malus × domestica Borkh.) being packed in the reddest market color grades. We conducted a three‐year field experiment in a low‐Cu orchard with a history of poor fruit coloring. We applied multiple mid‐summer sprays of Cu sulfate and basic Cu sulfate in 1994 and 1995 to ‘Bisbee Delicious’ and ‘Oregon Spur II Delicious’ apple trees. Plant tissue nutrient levels, fruit color grade, and fruit typiness were evaluated in the years of application and the following year. The Cu sprays increased leaf Cu in the years of application; however, leaf Cu in the Cu‐sprayed plots returned to or very near to background concentrations in the year after sprays were terminated. The Cu treatments did not increase the proportion of fruit in the reddest market color grades or influence five fruit typiness indices of either apple cultivar. Although midsummer Cu sprays may not enhance apple fruit red color or typiness, they may be useful for increasing overall tree Cu status, particularly for long‐season cultivars which are harvested too late for postharvest sprays to be effective.     

Changes in soil chemistry associated with the establishment of forest gardens on eroded,acidified grassland soils in Sri Lanka

Topsoil properties were determined in forest gardens established about 20 years ago on eroded grassland soils (abandoned tea lands) in the wet zone of the Sri Lankan highlands. They were compared with adjacent, eroded grasslands (abandoned tea lands) on strongly weathered soils vs soils at earlier stages of pedogenic development in a two-way analysis of variance. Soil pH in forest gardens was, on average, 6.1, nearly one unit higher than in the adjacent grasslands. In the garden soils, the cation exchange capacity (CEC measured at pH 4.8) was nearly double, exchangeable calcium concentrations five times and exchangeable magnesium three times as high as in the grasslands soils. Total soil N content was found to be nearly 40% higher in the gardens. Topsoil gravel contents in the gardens were less than half as high as in the grasslands. The increases in exchangeable bases and N in gardens, relative to grasslands, were attributed to increased nutrient retention and acquisition. Higher retention was partly due to the higher CEC_pH4.8, and probably to reduced erosion and increased, continuous fine root density in the garden topsoils. Higher field CEC in gardens was likely to result from generally higher C contents and from the reversal of acidification, presumably caused by base accumulation and decomposition processes. Our results suggest that forest garden establishment on degraded grasslands can lead to accumulation of mobile nutrients in the topsoil, probably due to increased nutrient retention, subsoil uptake and litter input exceeding nutrient uptake by the standing biomass.     

Changes in chemical and biological properties of a sodic clay subsoil with addition of organic amendments

An experiment was performed to examine the chemical and biological effects on high clay sodic subsoil following the incorporation and incubation with organic amendments. The main treatments consisted of amendments with wheat shoots, lucerne pellets and peat, and these were compared to gypsum addition. Additional treatments were residues of chickpea and canola, chicken manure and sawdust. All materials were finely ground and added to crushed and sieved soil at the rate of 1% by weight. Wheat, canola and chickpea residues and chicken manure resulted in modest reductions in soil sodicity. Carbon and N mineralization were related to the soluble C/total N ratio in the amendment. The initial mineralization of wheat amendment was rapid due to its soluble C content, but then slowed to have the lowest loss, of around one third of added C, of all the plant residues after 174 days. In comparison, lucerne-amended soil increased total N and lost almost half of its C after the 174-day incubation. The canola stubble amendment showed the highest carbon loss, losing 64% of its added C. The addition of gypsum resulted in high soil electrical conductivity which suppressed respiration, compared to the control soil, indicating a detrimental effect on microbial activity due to the high electrolyte concentration in the soil. The peat amendment, with a low-soluble C content, showed a similar respiration rate to the control soil, confirming that a source of soluble C is important for the initiation of rapid biological activity. Soil pH was significantly increased (by 0.6 of a pH unit) with addition of chicken manure, and still remained higher than control soil after 174 days of incubation. Lucerne was the only plant residue to increase soil pH, with the effect being sustained for 56 days. The study demonstrated how some organic amendments can improve chemical fertility and biological activity in high clay sodic subsoil, and at the same time contribute, after 25 weeks incubation, to an increase in carbon content.     

红酵母RS1的高耐铝能力与增厚的细胞壁有关而不来自体外铝离子的螯合作用

Aluminum (Al) is very toxic to many living organisms, including plants, animals and microorganisms. However, despite many studies on Al tolerance in plants, little has been reported concerning these mechanisms in microorganisms. In this study, a red yeast, which could tolerate Al 3+ concentrations as high as 200 mmol L-1 , was isolated from acidic soils, identified as Rhodotorula sp. and designated as RS1. As the medium compositions can greatly affect the responses of microorganisms to Al, two culture mediums, glucose medium (GM) and lysogeny broth medium containing soil extract (S-LBM), were used. During growth of RS1, the pH of medium decreased in GM but increased in S-LBM. These changes in the pH of the media were not induced by Al addition. No or little secretion of organic acids was observed in RS1 growth media. Importantly, the thickness of the cell walls and the ratio of cell wall to biomass of RS1 significantly increased in GM with high Al 3+ concentrations. In the presence of 100 mmol Al L-1 , 78.0% of the total Al of whole cells was present in the thickened cell walls. The Al in cell walls was mostly bound to OH, amide and CO groups of polysaccharides. These results suggest that thickening of the cell wall in response to the high Al 3+ concentrations may play an important role in the high tolerance of RS1 to Al and that pH increase of the medium and chelation of Al ions are not involved in Al tolerance of this organism.     

黑土区高效溶磷真菌筛选及其溶解磷矿粉效果的研究

黑土区高效溶P真菌筛选及其溶解磷矿粉效果的试验结果表明 ,溶P真菌溶P效果高于溶P细菌 ,且其溶P性状稳定。曲霉菌“P39”、“P37”和青霉菌“P6 6”、“P1”溶P效果高于其他供试菌 ,菌株之间溶P活性与培养液pH值和有机酸含量间不存在必然相关性 ,推测不同菌株间溶P活性差异与菌株产生的有机酸种类和数量有关     

采用广义回归神经网络建立酪蛋白乳化性与疏水性关系

为了研究琥珀酰化修饰后酪蛋白乳化性与疏水性关系,该文以琥珀酰化牦牛乳酪蛋白为研究对象,分析了不同酰化程度酪蛋白乳化性及疏水性变化趋势,采用广义回归神经网络建立了牦牛乳酰化酪蛋白乳化性与疏水性关系模型。结果显示,琥珀酰化牦牛乳酪蛋白乳化性和疏水性均与酰化程度、pH值有关,pH值为5以上,随着酰化程度的增加,酪蛋白乳化活性增大;等电点附近,酪蛋白乳化活性较差,等电点之后乳化活性迅速增大。pH值介于2-6时,所有酪蛋白乳化稳定性较强,pH值介于6-11之间时,酪蛋白乳化稳定性差异较小,pH值为12时乳化稳定性有所增加。酪蛋白内荧光与1-苯胺基萘-8-磺酸(1-aniline napthalene-8-sulfonic acid,ANS)外源荧光最大荧光强度和最大发射波长随酰化程度及pH值变化表现出较为复杂的关系。通过广义回归神经网络(generalized-regression-neu-network,GRNN)建立了牦牛乳酪蛋白疏水性参数、pH值、酰化程度与乳化性关系,网络模型对乳化性的预测相对误差小于10%,预测结果良好。研究结果为酪蛋白乳化性研究提供了参考依据。     

单宁酸对不同pH茶园土壤中活性铝形态分布的影响

采集云南省普洱市和江西省南昌县两地典型的茶园土壤,通过添加HCl和Ca(OH)2调节土壤pH,研究不同pH(3.0、3.5、4.0、4.5)茶园土壤添加0.4 mmol·kg 1、2.0 mmol·kg 1、4.0 mmol·kg 1、8.0 mmol·kg 1、12.0 mmol·kg 1单宁酸后,活性铝形态交换态铝(Al3+)、单聚体羟基铝[Al(OH)2+、Al(OH)+2]、酸溶无机铝[Al(OH)03]和腐殖酸铝[Al-HA]的分布特征。结果表明:单宁酸添加量为0~0.4 mmol·kg 1和0~2.0 mmol·kg 1时,江西南昌和云南普洱茶园土壤中交换态铝随土壤pH的增加呈明显下降趋势,而羟基态铝、酸溶无机铝和腐殖酸铝呈逐渐上升趋势;当单宁酸浓度增至2.0 mmol·kg 1以上时,随土壤pH的增加,单宁酸对活性铝释放的抑制作用增强,各形态活性铝含量都较低,且不同pH处理土壤间的差异不显著。0~20 cm土层土壤与20~40 cm土层土壤变化规律大致相似,总体上看,下层土壤活性铝总量高于上层。云南普洱茶园土壤活性铝总量明显高于江西南昌的茶园土壤。相关分析表明,0~20 cm土层土壤中,pH与羟基态铝、腐殖酸铝、土壤酸碱缓冲容量(pHBC)呈正相关(r=0.796,P0.01;r=0.960,P0.01;r=0.852,P0.01);pHBC与交换态铝、羟基态铝呈负相关(r=0.904,P0.01;r=0.645,P0.05),而与腐殖酸铝呈正相关(r=0.795,P0.01)。同时,单宁酸加入浓度为0~0.4 mmol·kg 1时,土壤pH明显上升,之后随着单宁酸加入浓度的增加土壤pH持续下降,土壤pH(YpH)与单宁浓度(CDN)在此阶段基本符合方程:YpH=0.04CDN+3.82(R2=0.95,P0.01)的线性变化趋势,在单宁酸浓度达到8.0~12.0 mmol·kg 1时,土壤pH基本不再变化。