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91.
本文所介绍的基于GPS接收机的车辆运行记录仪主要是利用单片机对GPS接收机所接收到的数据进行存储记录,借此来对一段时间内车辆的运行轨迹进行跟踪、记录。当需要查看数据时,可利用串行口与上位机进行通信。本文介绍了实现此功能的硬件电路图、相关的控制软件以及试验数据。  相似文献   
92.
    
Changes in the metabolic pattern of proline-14C were examined in barley seedlings germinated at the low temperature of 2°C (LT) and compared with those germinated at 25°C (HT). In the LT shoots. proline-14C incorporation was higher in the cationic fraction and lower in the acid-neutral fraction than that of HT, respectively. More proline-14C of LT was converted to other amino acids, especially to acidic amino acids in free amino acid state, than was the HT proline-14C which had a comparatively wide distribution.

In the LT protein fractions. more proline-14C was incorporated into the cytoplasmic protein than into the cell wall protein. On the contrary, the radioactivity of the lIT cell wall increased more distinctively. proline-14C in the two proteins of LT was a little less converted to other amino acids than in those of HT. A little higher radioactivity was found in the aspartate and glutamate of the LT protein hydrolysates. The hydroxyproline which is closely related with proline had a little lower level of radioactivity in the LT cell wall.  相似文献   
93.
94.
以维生素c为对照,采用DPPH法研究紫茎泽兰叶和茎醇提物的抗氧化活性,并计算它们的Ic20。结果表明:1.6mg/mL紫茎泽兰叶和茎的醇提物有很好的清除能力,清除率均达到80%以上,相当于0.10mg/mL维生素C的清除率;紫茎泽兰叶和茎的Ic50为0.3.0.7mg/mL,维生素c为0.04mg/mL。说明紫茎泽兰叶的清除能力强于茎,紫茎泽兰清除自由基的能力为维生素c的1/10。总之,紫茎泽兰具有较强的抗氧化活性。  相似文献   
95.
Relatively little is known about soil organic carbon (SOC) dynamics in montane ecosystems of the semi-arid western U.S. or the stability of current SOC pools under future climate change scenarios. We measured the distribution and quality of SOC in a mosaic of rangeland-forest vegetation types that occurs under similar climatic conditions on non-calcareous soils at Utah State University's T.W. Daniel Experimental Forest in northern Utah: the forest types were aspen [Populus tremuloides] and conifer (mixture of fir [Abies lasiocarpa] and spruce [Picea engelmannii]); the rangeland types were sagebrush steppe [Artemisia tridentata], grass-forb meadow, and a meadow-conifer ecotone. Total SOC was calculated from OC concentrations, estimates of bulk density by texture and rock-free soil volume in five pedons. The SOC quality was expressed in terms of leaching potential and decomposability. Amount and aromaticity of water-soluble organic carbon (DOC) was determined by water extraction and specific ultra violet absorbance at 254 nm (SUVA) of leached DOC. Decomposability of SOC and DOC was derived from laboratory incubation of soil samples and water extracts, respectively.

Although there was little difference in total SOC between soils sampled under different vegetation types, vertical distribution, and quality of SOC appeared to be influenced by vegetation. Forest soils had a distinct O horizon and higher SOC concentration in near-surface mineral horizons that declined sharply with depth. Rangeland soils lacked O horizons and SOC concentration declined more gradually. Quality of SOC under rangelands was more uniform with depth and SOC was less soluble and less decomposable (i.e., more stable) than under forests. However, DOC in grass-forb meadow soils was less aromatic and more bioavailable, likely promoting C retention through cycling. The SOC in forest soils was notably more leachable and decomposable, especially near the soil surface, with stability increasing with soil depth. Across the entire dataset, there was a weak inverse relationship between the decomposability and the aromaticity of DOC. Our data indicate that despite similar SOC pools, vegetation type may affect SOC retention capacity under future climate projections by influencing potential SOC losses via leaching and decomposition.  相似文献   

96.
楸树的初代培养研究   总被引:2,自引:0,他引:2  
以楸树的4个品种(类型)(圆基长果楸、豫楸1号、豫楸2号和梓树)为材料进行组织培养研究,试验结果表明:(1)通过豫楸1号和圆基长果楸在MS、1/2MS、N6、WPM、B55种基本培养基上的诱导率和启动时间确定了该实验的最佳培养基为N6,其诱导率达80%,接种后2 d即启动。(2)外植体的消毒方式采用75%的酒精和0.1%HgC l2双步消毒,4个品种(类型)中豫楸2号的成活率最高,污染率最小。而不同品种(类型)最适消毒时间分别为:圆基长果楸5 min、豫楸1号8 min、豫楸2号7 min、梓树9.5 min。(3)大田栽培的圆基长果楸的污染率是温室栽培下的4~6倍,而成活率仅为温室栽培下的1/4,温室栽培的材料更适于进行组织培养。(4)豫楸1号在30 d内的污染率动态变化表明,外植体在接种7 d后出现污染,而主要污染发生在接种后的第14 d和第21 d。  相似文献   
97.
    
In forest soils where a large fraction of total phosphorus (P) is in organic forms, soil micro-organisms play a major role in the P cycle and plant availability since they mediate organic P transformations. However, the correct assessment of organic P mineralization is usually a challenging task because mineralized P is rapidly sorbed and most mineralization fluxes are very weak. The objectives of the present work were to quantify in five forest Spodosols at soil depths of 0-15 cm net mineralization of total organic P and the resulting increase in plant available inorganic P and to verify whether net or gross P mineralization could be estimated using the C or N mineralization rates. Net mineralization of total organic P was derived from the net changes in microbial P and gross mineralization of P in dead soil organic matter. We studied very low P-sorbing soils enabling us to use lower extractants to assess the change in total inorganic P as a result of gross mineralization of P in dead soil organic matter. In addition, to enable detection of gross mineralization of P in dead soil organic matter, a long-term incubation (517 days) experiment was carried out. At the beginning of the experiment, total P contents of the soils were very low (19-51 μg g−1) and were essentially present as organic P (17-44 μg g−1, 85-91%) or microbial P (6-14 μg g−1; 24-39%). Conversely, the initial contents of inorganic P were low (2-7 μg g−1; 9-15%). The net changes in the pool size of microbial P during the 517 days of incubation (4-8 μg g−1) and the amounts of P resulting from gross mineralization of dead soil organic matter (0.001-0.018 μg g−1 day−1; 0.4-9.5 μg g−1 for the entire incubation period) were considerable compared to the initial amounts of organic P and also when compared to the initial diffusive iP fraction (<0.3 μg g−1). Diffusive iP corresponds to the phosphate ions that can be transferred from the solid constituents to the soil solution under a gradient of concentration. Net mineralization of organic P induced an important increase in iP in soil solution (0.6-10 μg g−1; 600-5000% increase) and lower increases in diffusive iP fractions (0.3-5 μg g−1; 300-2000% increase), soil solid constituents having an extremely low reactivity relative to iP. Therefore, soil micro-organisms and organic P transformations play a major role in the bioavailability of P in these forest soils. In our study, the dead soil organic matter was defined as a recalcitrant organic fraction. Probably because gross mineralization of P from this recalcitrant organic fraction was mainly driven by the micro-organisms’ needs for energy, the rates of gross mineralization of C, N and P in the recalcitrant organic fraction were similar. Indirect estimation of gross mineralization of P in dead soil organic matter using the gross C mineralization rate seems thus an alternative method for the studied soils. However, additional studies are needed to verify this alternative method in other soils. No relationships were found between microbial P release and microbial C and N releases.  相似文献   
98.
孟鹏 《中国农学通报》2012,28(30):289-295
优化超临界CO2萃取柠檬苦素的工艺条件,为金柑籽中柠檬苦素的开发提供理化依据。采用单因素试验研究夹带剂、夹带剂浓度、萃取温度、萃取时间、萃取压力和二氧化碳流量对柠檬苦素提取率的影响,在单因素试验的基础上,采用响应面分析法建立了二次多项式数学模型,并分析模型的有效性与各因素间的交互作用。在萃取压力为33 MPa,萃取温度为50℃,萃取时间为2.5 h的条件下,柠檬苦素提取率达3.98 g/kg。在最佳条件下得到实验结果与模型预测值吻合,说明所建立的模型是切实可行的。超临界CO2萃取技术的运用,有利于柠檬苦素提取的工业化推广和应用。  相似文献   
99.
100.
This study compared soil physical, chemical, and biological characteristics between natural grassland and recently abandoned rice fields in order to identify those variables that might explain the observed increase of Camponotus punctulatus anthills in abandoned rice paddy fields from Northern Argentina. Mainly due to a reduction of macropores and mesopores, overall porosity decreased by around 6% and bulk density was about 7% greater, in the 0- to 10- and 10- to 20-cm layers of the abandoned rice fields. Carbon and nitrogen content from organic matter increased (29% and 41% respectively for the 0- to 20-cm horizon) during cultivation but decreased (38% and 24%) 2 years after the last rice harvest. Forty percent of natural grassland-organic matter and 30% of abandoned rice-organic matter mineralized in less than 2 years. There was a different community structure between the abandoned rice fields and the undisturbed natural grassland and only a 20.6% (i.e. only 19 species from a total of 92) overlap in species composition. The abundance of macrofauna was greater in abandoned rice fields (2,208 individuals m–2) in comparison to natural grasslands (288 ind m–2) due to higher densities of small earthworms and Camponotus punctulatus ants; however, the Shannon index showed lower values in comparison to natural grasslands. Earthworms and C. punctulatus in the abandoned rice fields showed a change in their 13C signature indicating a switch in diet from natural grassland organic matter (C4) to organic matter from rice (C3). Our results indicate that the effects of rice cultivation practices did not seem to produce any physical or trophic limitations to recolonization by the macrofauna. It seems that changes in overall soil conditions have favored a change in the construction behavior of C. punctulatus which, in combination with population increases, could explain the explosion in number of anthills.  相似文献   
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