Phosphorus enrichment from point to catchment scale following fire in eucalypt forests

Erosion studies at multiple scales have shown selectivity in particle transport and delivery can be inferred from nutrient enrichment. Most studies reveal the enrichment ratio (ER) of phosphorus on sediment is high, demonstrating the deposition of coarser particles over the transport pathway. Experimental work on burnt landscapes often takes place at the hillslope plot scale (1–10 m²) by necessity, with inferences made on system sediment and nutrient responses from small areas. Scale effects on generation and delivery need to be considered in such cases. In a study in wet eucalypt forests burnt by wildfire, phosphorus concentration on mineral sediment and organic material at the point (0.01 m²), plot (1–10 m²) and catchment (10⁶ m²) was used to estimate ERs over two scales. The data revealed ERs of 1.5 from point to plot and 2 from plot to catchment. These ratios are relatively low compared with other studies. We suggest the principal reason is short transport pathways which act to decrease deposition, due to the spatial heterogeneity of post-burn soil hydraulic properties. The association of total phosphorus with mineral material was slightly higher than with organic matter. The study suggests that using plot scale hillslope experiments to infer sediment and nutrient loss after wildfire would have overestimated losses by around 100%.     

应用发光细菌法检测饲用抗生素单一及联合毒性的研究

以HgCl2为毒性参照,以等毒性配比法研究了饲用盐酸金霉素、吉他霉素、盐霉素和黄霉素对发光细菌的单一及联合毒性。结果表明:盐酸金霉素、吉他霉素、盐霉素、黄霉素对明亮发光杆菌的急性毒性EC50分别为9.21、146.13、4.24 mg/L和134.68 mg/L,发光细菌的相对发光强度(RLU)随着抗生素浓度的提高而降低,并分别在2~16、25~200、1~8 mg/L和25~200 mg/L范围内呈良好线性关系;多元饲用抗生素对发光细菌具有联合毒性的作用,吉他霉素与盐酸金霉素、盐霉素和黄霉素3种抗生素的二元组合对发光细菌的联合毒性表现为较强的协同作用,而盐酸金霉素、盐霉素和黄霉素两两分别组合对发光细菌的联合毒性表现为拮抗作用;三元及四元抗生素混合体系对发光细菌的联合毒性均表现为拮抗作用。     

采用新电导率指标分析土壤盐分变化规律

土壤电导率(Electrical conductivity,EC)是限制植物和微生物活性的阈值,影响到土壤养分和污染物的转化、存在状态及有效性[1],反映了在一定水分条件下土壤盐分的实际状况,且包含了土壤水分含量及离子组成等丰富信息[2]。在一定浓度范围内,土壤溶液含盐量与电导率呈正相关,溶解的盐类越多,溶液电导率就越大,故可根据溶液电导率的大小,间接地测量土壤含盐量[3-5]。     

施用生物黑炭对新疆灰漠土肥力与玉米生长的影响

通过田间小区对比试验,研究生物黑炭作为改良剂与堆肥等其他生物质改良剂相比对新疆低产土壤——灰漠土的改良和玉米增产的效果。结果表明,施入20t·hm^-2和40t·hm^-2的生物黑炭,能显著提高土壤有机质含量,与基础土壤相比,提高了22．77％和49．80％,明显高于秸秆还田、羊粪和腐植酸有机肥等对土壤有机质的提升效果。施用生物黑炭提高了玉米单穗重、千粒重、产量以及生物量,降低了玉米的根冠比,促进玉米根系生长,而追施氮肥对玉米产量的影响差异不显著。因此,施用生物黑炭能够大幅度提高土壤有机质含量,对灰漠土土壤质量和作物产量以及农艺性状的提高具有重要作用。     

内蒙古乌梁素海入湖水质超标风险率分析

以内蒙古乌梁素海入流水体为研究对象,考虑湖泊水质的随机性和灰色不确定性,以灰色概率统计理论为基础,引入灰色-随机风险率方法,通过计算并分析2006年、2007年和2008年入湖断面各水质参数存在的超标风险性,反映不同水质参数的污染强度和污染历时的变化过程。结果表明,入湖水体总氮总磷浓度超标风险率呈现逐年上升的趋势;总氮浓度超过Ⅴ类标准值的上限风险率达96.4%,下限风险率达87.7%;总磷浓度超过Ⅴ类标准值的上限风险率达96.2%,下限风险率达86.9%;BOD5浓度超过Ⅴ类标准值的平均风险率达55%;COD浓度超过Ⅴ类标准值的平均风险率达85%。乌梁素海入湖水体污染程度已十分严重,源头水污染防治已刻不容缓。     

延迟荧光光谱F730/F685与植物耐热性的关系

为研究延迟荧光光谱特性与植物耐热性的关系,该文以3种不同品种的植物为研究对象,分析了温度胁迫下样品延迟荧光发射光谱曲线的变化情况,研究了各样品延迟荧光光谱中685 nm附近峰值（标记为F685）与730 nm附近峰值（标记为F730）的光谱峰值比F730/F685的温度响应曲线,并与叶绿素荧光参数的温度变化趋势进行对照,探讨了温度拐点出现的原因及变化趋势。试验结果证实延迟荧光发射光谱F730/F685温度响应曲线的变化真实地反应了植物在高温胁迫下光系统的光合功能,有效地体现了样品间对高温逆境响应的差异,且温度响应曲线的拐点及其变化特性可能会是一种鉴定植物耐热性的有效指标。     

Quantifying aggregate stability of a clay soil under annual forage crops

This study explored the influence of 10 annual forage legumes belonging to the Lathyrus and Vicia genera on wet aggregate stability (WAS) and dispersion ratio (DR) indices of a clay soil. Five Lathyrus and five Vicia species were sown in autumn. Seed‐to‐seed and row‐to‐row distance was maintained at 5 cm and 20 cm, respectively. The experiment was planned in a randomized block design with three replications. After 90 d following seed harvest, soil cores were collected from two depths (0–15, 15–30 cm) in each plot and WAS and DR were determined. Annual forage legumes increased WAS of the soil but decreased the DR index. The WAS and DR values were affected at level of p < 0.001 by genus, species, and soil depth. Values of WAS and DR of the control plots without plant on the average were found to be 44.5% and 9.3% for 0–15 cm, and 41.2% and 10.1% for 15–30 cm, respectively. For 0–15 cm depth, the highest WAS (77.7%) and the lowest DR (6.4%) values were found in L. sphaericus L. (wild) plots. For 15–30 cm depth, the highest WAS value (62.6%) was obtained in L. annuus L. (wild) plots and the lowest DR value (6.7%) was in L. sativus L. (Gurbuz‐2001) plots.     

不同钠吸附比的咸水结冰融水入渗后滨海盐土的水盐分布

在室内利用相同矿化度(10 g·L^-1)、不同钠吸附比(5、10 和30)的咸水进行咸水结冰融水模拟试验、结冰融水入渗和咸水直接入渗的土柱试验, 以淡水处理为对照, 分析不同钠吸附比咸水结冰融水入渗下滨海盐土水盐分布特征。结果表明: 咸水冰融化过程中, 融出水的矿化度和钠吸附比均呈由高到低的变化趋势。咸水结冰融水入渗速度和入渗深度均快于和深于淡水。咸水钠吸附比越小, 结冰融水入渗速率越快、深度越深。水盐分布也表现为低钠吸附比咸水结冰处理的表层土壤含水量较低, 水分向深层迁移, 这种水分分布也使盐分向深层运移, 表现为表层土壤含盐量低, 深层土壤含盐量大。土层含水量低钠吸附比咸水处理高于高钠吸附比处理, 10~45 cm 土层则表现出相反的趋势; 表层土含盐量低钠吸附比处理高于高钠吸附比处理, 且咸水处理下土壤脱盐的深度大于淡水处理。钠吸附比5 的咸水结冰处理, 0~10 cm 土壤平均含水量和含盐量分别为30.3%和1.1 g·kg^-1, 显著低于其他处理。为比较咸水结冰灌溉和咸水直接灌溉的效果, 室内利用含盐量为10 g·L^-1、钠吸附比10 的咸水进行直接入渗的土柱(土壤含盐量为21.3 g·kg^-1)模拟试验, 结果表明: 与咸水直接入渗处理相比, 咸水结冰融水处理盐分淋洗效果更好, 该处理0~25 cm土层平均土壤含盐量为2.9 g·kg^-1, 显著低于咸水直接入渗的10.6 g·kg^-1。     

稻田CH4产生途径研究进展

H2/CO2还原和乙酸（CH3COOH）发酵是稻田CH4产生的主要途径。碳同位素示踪技术、添加甲烷产生途径抑制剂和稳定性碳同位素方法是稻田CH4产生途径的主要研究方法。本文综述了这三种研究方法及研究结果,并指出了今后的研究重点：加强我国有关稻田CH4产生途径的研究;对比分析三种研究方法,查明研究结果存在差异的原因;加强同位素分馏系数a(CO2/CH4)和e(ac/CH4)以及碳同位素组成δ13CH4和δ13CH4(CO2/H2)的研究     

A GIS-based comparative study of frequency ratio, analytical hierarchy process, bivariate statistics and logistics regression methods for landslide susceptibility mapping in Trabzon, NE Turkey

Over the last few decades, many researchers have produced landslide susceptibility maps using different techniques including the probability method (frequency ratio), the analytical hierarchy process (AHP), bivariate, multivariate, logistics regression, fuzzy logic and artificial neural network In addition, a number of parameters such as lithology, slope, aspect, land cover, elevation, distance to stream, drainage density, distance to lineament, seismicity, and distance to road are recommended to analyze the mechanism of landslides. The data quality is a very important issue in landslide studies, and more accurate results will be achieved if the data is adequate, appropriate and drawn from a wide range of parameters. The aim of this study was to evaluate the susceptibility of the occurrence of landslides in Trabzon province, situated in north east Turkey. This was achieved using the following five methods the frequency ratio model, AHP, the statistical index (Wi), weighting factor (Wf) methods, and the logistics regression model, incorporating a Geographical Information System (GIS) and remote sensing techniques. In Trabzon province there has been an increasing occurrence of landslides triggered by rainfall. These landslides have resulted in death, significant injury, damage to property and local infrastructure and threat of further landslides continues. In order to reduce the effects of this phenomenon, it is necessary to scientifically assess the area susceptible to landslide. To achieve this, landslide susceptible areas were mapped the landslide occurrence parameters were analyzed using five different methods. The results of the five analyses were confirmed using the landslide activity map containing 50 active landslide zones. Then the methods giving more accurate results were determined. The validation process showed that the Wf method is better in prediction than the frequency ratio model, AHP, the statistical index (Wi), and logistics regression model.