Modelled and measured ratio of PAR to global radiation under cloudless skies

The ratio between photosynthetic photon flux density (PPFD) and solar broadband irradiance depends on the spectral structure of radiation. Therefore, at the Earth surface, this ratio depends on atmospheric conditions and solar height. Specifically, for cloudless skies, and based on results from a spectral radiative transfer model, a parameterised model is presented here in order to obtain the ratio between PPFD and global irradiance from meteorological routine measurements. The two main input variables of the model are air mass and an estimation of precipitable water column. Modelled values are compared to measurements taken at Girona (NE Iberian Peninsula). A correction to measurements is developed to take into account the non-cosine response of the instruments. Agreement between measurements and model is significantly better than merely considering a constant value of the ratio between PPFD and global broadband irradiance.     

常压列管式灭菌器研究

以对流换热理论为依据,对常压列管式灭菌器的结构、传热方式、换热系的计算及其设计进行了讨论和研究。这种灭菌器中的传热热阻主要发生在列管内壁与被加热物料之间的对流中。对牛奶等含水率大于85％的流体食品物料,其部分热物性参数可参照水的相应参数的变化规律推断计算。对其它物性参数可视其随温度或其它条件变化规律推算,以便在灭菌温度下物料物性参数未知的条件下进行有关的换热计算。其结果用经验数据和实验分别进行验算和验证是可靠、可行的,可在有关食品物料的热计算中推广应用。     

利用WRF模拟兰州城市边界层

利用WRF中尺度模式对兰州城市边界层进行了模拟,结果表明,WRF在兰州地区模拟效果较好,可用于研究山谷城市的大气边界层情况。     

Climate Change and CO2 Effects on Productivity of Danish Agricultural Systems

SUMMARY

Scenarios of climate change for Denmark suggest increases in annual mean temperature of 1 to 4°C by the end of the 21st century with an associated increase in rainfall of approximately 10%. The climatic warming and the associated increase in atmospheric CO₂ concentration will increase the productivity of agricultural crops. The increase may be slightly higher for indeterminate species, such as grass and other fodder crops, compared with cereals and other determinate species, where the duration of growth depends on temperature and daylength. The full benefits of the climatic warming requires adaptation in crop management, which at the individual crop level means changes in sowing dates, i.e., later sowings for winter cereals and earlier sowings for spring cereals. Some crop substitution will probably occur. On dairy farms more cereals will be grown due to higher productivity of the grasslands, which frees up some land for grain production. On sandy loam and loam soils spring cereals may become slightly more favorable and winter cereals slightly less favorable.     

2006～2012年武陵山区黔江区域大气污染物变化分析及防治对策

利用黔江区环境空气的监测资料,采用空气综合污染指数、Daniel趋势检验方法等评价和分析方法,研究了2006～2012年环境空气质量状况及变化趋势.结果表明,SO2 、NO2和PM10年均浓度分别为0.019 ～0.060、0.004 ～0.022、0.063 ～0.089 mg/m3,均达到国家二级标准限制要求.环境空气综合污染指数为1.08 ～2.14,属于轻度污染,主要污染物为SO2和PM10.2006～2012年环境空气质量年际变化趋势表明,NO2浓度随年份变化呈增长趋势.根据黔江区环境空气质量状况,分析了污染成因,并提出了污染防治对策.     

大气干湿沉降向城市系统输入重金属元素通量特征研究——以沈阳市为例

[目的]探讨大气干湿沉降向城市系统输入重金属元素通量特征.[方法]根据沈阳市不同行政区采样点重金属元素沉降通量,分析沈阳市不同行政区重金属大气干湿沉降污染的空间分布特征.[结果]在不同的采样点,大气干湿沉降中元素的年沉降通量差异较大,但其在沈阳市不同行政区分布规律大致相同.Cd、Pb、Hg的年沉降通量在各地区的分布分别表现为：铁西区＞皇姑区＞沈河区＞和平区＞大东区＞东陵（浑南）区＞于洪区,铁西区＞沈河区＞皇姑区＞和平区＞东陵区＞于洪区＞大东区＞浑南区,铁西区＞沈河区＞皇姑区＞和平区＞大东（东陵）区＞于洪（浑南）区.大气降尘污染的空间分布与污染源地域分布具有一致性,即工业区＞商业区或交通区＞文化区＞居民区＞郊区.[结论]该研究为大气干湿沉降污染的控制与治理提供了理论参考.     

重庆主城区空气降尘中重金属的特点及其在表层土壤中的累积量研究

探索不同功能区空气降尘中重金属通量特征并对其进行污染评价,对于了解空气降尘输入对土壤中重金属累积影响具有重要意义。对重庆主城的居住区(JZ)、文教区(WJ)、商业区(SY)、郊区(JQ)、交通区(JT)和工业-居住混合区(GJ)逐月进行空气降尘通量和Cr、Ni、Cd、Pb含量的测定。结果表明,工业–居住混合区的空气降尘通量平均值最高,文教区的最低。6类功能区秋季的降尘量相对较低。Cd、Cr、Ni和Pb的平均降尘量在不同功能区分布存在差异。空气降尘中4种重金属元素的平均含量为:Cd 2.14 mg/kg、Cr 66.36 mg/kg、Ni 27.69 mg/kg、Pb 98.33 mg/kg。6类功能区降尘中Cd、Cr、Ni和Pb 4种重金属含量一般冬季较高。地积累指数法的分析表明降尘中Cd污染最严重。经推算,以空气降尘的方式向土壤中输入的重金属,使重庆主城区土壤中Cd、Cr、Ni和Pb等4种重金属元素的浓度在累积100a后仍将低于《土壤环境质量标准》中的二级标准。土壤中重金属元素增加速度最快为Cd,其次为Pb和Cr,Ni的增长为负值。     

江西红壤地区农田生态系统大气氮沉降通量的研究

2004年12月至2005年11月在江西鹰潭中国科学院红壤生态实验站进行了为期1a的大气氮沉降的外场观测试验。本文对观测得到的数据资料进行分析,定量给出了农田生态系统大气氮化物浓度和氮沉降通量。结果表明,鹰潭地区农田下垫面大气中NH3、NOx和ON(有机氮)的平均浓度分别为24.6、3.54、7.2μgm-3。气溶胶中铵盐、硝酸盐、ON的平均浓度分别为4.16、4.64、0.92μgm-3。降水中NH4+离子、NO3-离子、ON的平均浓度分别为0.89、0.73、0.26mgL-1。全年大气氮沉降总量为N6.26gm-2,其中干沉降为N3.19gm-2,占总沉降量的51%;湿沉降为N3.07gm-2,占总沉降量的49%。无机氮沉降为N5.47gm-2,占总沉降量的87.4%;有机氮沉降为N0.79gm-2,占总沉降量的12.6%。与草地、森林、湖泊等其他下垫面相比,江西红壤地区农田下垫面大气氮沉降量相对较大,对农田生态系统氮素平衡将产生重要影响。     

大气沉降对我国土壤中污染分布及元素循环的影响

大气沉降是污染物进入土壤的重要途径,也是土壤中污染物的主要来源。同时,大气沉降和土壤元素循环息息相关。本文综述了大气沉降对我国土壤中污染物分布以及元素循环的影响。结果表明,重金属沉降依赖于长期的干湿混合沉降,有机污染物沉降依赖于干沉降,氮硫磷等元素的沉降依赖于湿沉降。同时,季风和人为活动会影响大气污染物的迁移和沉降。本文的结论为污染物大气沉降的防控和土壤污染治理提供了思路。     

Response of protozoan and microbial communities in various coniferous forest soils after transfer to forests with different levels of atmospheric pollution

During recent decades, forest ecosystems have been exposed to high levels of atmospheric pollution, and it has been argued that this affects the composition and activity of decomposer communities and, subsequently, ecosystem functioning. To investigate the effects of atmospheric pollution on protozoa and microflora, a new experimental design was used. Undisturbed soil columns, originating from six coniferous forests across Europe and representing different stages of soil acidification, were transferred to two Scots pine forests (Fontainebleau and Wekerom) with different levels of N and S deposition (NH₄ ⁺-N=4.90 and 42.50?kg ha^–1 year^–1; SO₄ ^–S=10.90 and 30.40?kg ha^–1 year^–1, respectively). The number of protozoa, microbial biomass C and microbial activity were estimated in the organic layer (Of) of the transferred soils at the two host sites after 21 months of incubation. The experiment aimed at answering two questions: (1) Do changes in environmental conditions, studied by transferring soils from one site to another, affect protozoa and microbial communities and, if so, (2) how important are changes in both N and S deposition in explaining the effects of soil transfer on protozoa and microbial communities? The interaction between protozoa and microbial communities was addressed with regard to these changes in environmental conditions. No effect of enhanced N or S deposition on protozoan numbers and microbial biomass C, basal respiration and caloric quotient was revealed. Reciprocal transfer of various soil columns resulted in lower abundance and activity of protozoa and microbes. This reduction could not be explained by differences in N and S deposition, but by differences in microclimate and adaptation. In some cases, protozoa correlated with pH, C/N ratio, P and S content and leached mineral N.