蒸发浓缩－CODcr法测定地面水中低浓度COD

对水样蒸发浓缩法用于地面水中低浓度ＣＯＤ的测定进行探讨的实验结果表明，地面水中低浓度ＣＯＤ物质可以在碱性条件下，通过蒸发浓缩处理后，采用重铬酸钾法进行测定，所得结果的精密度和准确度良好．若选择水样浓缩系数为５，则可将重铬酸钾法的最低检测限浓度降低到１０ｍｇ·Ｌ－１，从而使该方法能够适用于地面水水质标准中各类水质ＣＯＤ的监测要求．     

沼液负压蒸发浓缩装置的设计与试验

为了解决沼液浓缩过程中有效成分流失的问题,采用低温负压蒸发浓缩的方法,结合沼液的理化性质,对沼液负压蒸发浓缩装置的主体部分(蒸发罐)和辅助设备(冷凝器、循环液槽、真空泵)分别进行了参数设计计算和设备选型,并在自制20 L负压蒸发浓缩装置上进行了系列试验。试验结果表明:当温度低于80℃时,沼液的有机质含量基本不变,蒸发温度高于80℃之后,有机质含量明显下降,80~100℃的变化率为9.4%;随着温度的升高,氮磷钾含量不断下降,氮含量流失最大,最大变化率为13%。蒸发浓缩后的沼液中有机质和氮磷钾含量随真空度的增大而升高;随着真空度的升高,沼液的蒸发温度逐渐降低,蒸发量不断增大,绝对真空度为0.025 MPa时,最低蒸发温度为67℃,蒸发量最高能达到8 324 m L/(m2·h),蒸发率为28.75%;绝对真空度维持在0.04 MPa到0.05 MPa之间,温度在75~80℃时,蒸发量能达到7 700 m L/(m2·h),蒸发率为26%左右。     

Evaluating the Impact of Combined Application of Biochar and Compost on Hydro-physical Properties of Loamy Sand Soil

ABSTRACT

Biochar, compost and their combination are important organic amendment materials for improving the hydro-physical properties of sandy soils. Series of soil columns experiments were conducted for investigating the application effects of date palm biochar and compost on evaporation, moisture distribution, infiltration, sorptivity (Sp), saturated hydraulic conductivity (K_sat) and water holding capacity (WHC) at application rates of 1%, 2%, 3% and 4% (10, 20, 30 and 40 g kg^?1). The columns were filled manually with air-dried soil with 35 cm depth and the thickness of surface amended layer was 10 cm (T10) and 20 cm (T20) from soil surface at bulk density of 1400 kg m^?3. The results showed that the behavior of soil moisture distribution was influenced by application of biochar, compost and biochar-compost mixture. Moreover, in the amended layer T10, applying biochar at rate of 1%, 2%, 3% and 4% reduced significantly cumulative evaporation by 5.8%, 10.8%, 12.8% and 16.1%, respectively. Meanwhile, the reduction for the biochar-compost mixture at application rates of 1%, 2%, 3% and 4% was 10%, 12.2%, 14.5% and 20%, respectively. In layer T20, applying biochar at rate of 1%, 2%, 3% and 4% reduced cumulative evaporation by 10.24%, 13.0%, 18.3% and 21.5% but this reduction amounted to 18.2%, 21%, 23% and 24% for the biochar-compost mixture, respectively. It was generally observed that the highest application rate (4%) for applied amendments was the most effective impact on Sp, K_sat and WHC compared with other rates.     

Effect of Aquasorb and Organic Compost Amendments on Soil Water Retention and Evaporation with Different Evaporation Potentials and Soil Textures

Abstract

Aquasorb PR3005A, a hydrophilic polymer (a salt copolymer polyacrylamide), and garden waste compost were added to a loamy sand and a loam soil in pots to assess their impact upon soil physical properties at two different evaporation potentials. Compost was mulched and incorporated, the Aquasorb was incorporated, and their effect on temperature and amelioration of soil water content and evaporation was investigated. Mulching with compost reduced evaporation and increased soil temperature. Maize (Zea mays var. single cross 704) was sown in the same pots later, and growth indicator factors (plant height, fresh and dry weight, root weight, and leaf area) were compared. It was concluded that compost mulch application is beneficial to soil water retention whereas compost incorporation did not show these benefits. Compost mulch advances seedling emergence and enhances early growth through hydrologic soil amelioration. High rates of Aquasorb were also beneficial in advancing the emergence and early growth of maize seeded in loamy sand. The hydration capacity of Aquasorb is reduced as the electrolyte concentration and electrical conductivity are increased. Increased electrolyte concentration in soil solution, through drying, may result in gel dehydration and water release at potentials greater than field capacity, which may be lost to drainage. Furthermore, it is concluded that pot experiments with amendments fail to simulate field conditions.     

新疆塔里木盆地蒸发力的研究

本文首先对国内外蒸发力的计算方法进行了较全面的评述，然后利用Ｐｅｎｍａｎ法的修正式计算了塔里木。盆地的蒸发力，最后分析了该地区蒸发力的分布特征。     

Screening Capsicum species of different origins for high temperature tolerance by in vitro pollen germination and pollen tube length

Successful fruit set depends on several reproductive processes including pollen germination and tube growth processes. An experiment was conducted to determine the effects of temperature on pollen germination characteristics and to identify species/genotypic differences in Capsicum using the cumulative temperature response index (CTRI) concept. Pollen was collected from plants of seven genotypes from five Capsicum species, adapted to various parts of the world and grown outdoors in large pots. The pollen was subjected to in vitro temperatures ranging from 15 to 50 °C at 5 °C intervals. Pollen germination and tube lengths were recorded for all species after 24 h of incubation at the respective treatments. Species/genotypes differed significantly for in vitro pollen germination percentage and pollen tube length with mean values of 78% and 734 μm, respectively. The mean cardinal temperatures (T_min, T_opt, and T_max) averaged over genotypes, were 15.2, 30.7, and 41.8 °C for pollen germination and 12.2, 31.2, and 40.4 °C for pollen tube growth. The CTRI of each species/genotype calculated as the sum of eight relative individual stress response values, such as maximum pollen germination, maximum pollen tube length; T_min, T_opt, and T_max temperatures of pollen germination, and pollen tube lengths, identified species tolerance to high temperatures. Capsicum annum cv. Mex Serrano from Mexico was identified as tolerant, C. chacoense cv. 1312 and C. spp. cv. Cobanero from Argentina and Guatemala, respectively as intermediate and C. frutescens cv. Early Spring Giant from China, C. annum cv. Long Green from South Korea, C. spp. cv. NM89C130 and C. pubescens cv. 90002 from Guatemala as sensitive to high temperatures. The tolerant species/genotypes can be used in breeding programs to develop new genotypes that can withstand high temperature conditions both in the present climate and particularly in a future warmer climate.     

蒸发皿蒸发量及主要气象因子变化分析——以桂林灌溉试验站为例

以广西桂林灌溉试验站1980-2003年气象要素实测资料为例,分析蒸发皿蒸发量及主要影响因子的变化特点和规律。采用距平百分率法、滑动平均法和Kendall秩次相关法分析了蒸发量、气温、降雨量、风速、日较差、相对湿度的变化特点。分析结果表明,桂林农田灌溉试验站1980-2003年的蒸发量、降雨量、日较差和相对湿度呈上升趋...     

Estimation of Soil Evaporation During Fallow Seasons to Assess Water Balances for No‐Tillage Crop Rotations

Abstract Estimates of soil evaporation and available soil water of no‐tillage fields under farm conditions are important to assess soil water status at sowing of rainfed grain crops. The objective of this study was to predict stored soil water of no‐tillage fields during the fallow periods following soybean (Glycine max (L.) Merr.) and maize (Zea mays L.) crops by accounting for decreased soil evaporation as a result of the residues left on the soil surface. Three simple phenomenological models were used to simulate stored soil water under field conditions at seven locations in Argentina. Two models calculated decreased soil evaporation based on crop residue mass, and the third assumed a constant fractional decrease in bare soil evaporation. All models gave good estimates of soil water content during the fallow periods following a soybean crop. In cases with large quantities of maize residue, however, the models resulted in more water retention in the soil than observed as a consequence of underprediction of soil evaporation. These results indicate that full benefit of crop residue was not being achieved in these fields, probably due to a failure to finely chop and uniformly distribute the crop material on the soil surface.     

有机-无机复混肥圆盘造粒试验研究

对有机-无机复混肥圆盘造粒进行试验研究，分析了圆盘转速、圆盘倾角、喷头喷孔直径以及水分含量对颗粒成粒率和颗粒抗压强度的影响，确定了有机一无机复混肥圆盘造粒时较适宜的圆盘倾角、圆盘转速和水分含量。     

切沟对沟岸地土壤水分的影响

In order to preliminarily look at rules for soil moisture changes in the bank of the gully and to provide some recommendations for vegetative restoration in gully bank regions in the Loess Plateau, changes of soil moisture with depth and distance to the gully edge and their dynamic changes with time were observed to study the soil water characteristics in the bank of the gully. The results showed that soil water content increased with increasing distance from the gully edge, whereas for the same time period, the closer the distance to the gully wall, the greater the water loss; and that the influential distance of side evaporation decreased as depth increased.