对高校思想政治教育队伍建设的几点思考

高校思想政治教育队伍建设是加强高校思想政治教育的组织保证.文章通过分析高校思想政治教育工作的特点,说明了加强高校思想政治教育队伍建设的必要性.并从加强高校思想政治教育队伍的思想建设、提高思想政治教育队伍的整体素质和加强高校思想政治教育队伍建设的科学研究和管理等三方面阐述了如何建设一支高素质的思想政治教育队伍.     

高职院校混合学生系部思想政治工作讨探

介绍了高职院校混合学生系部学生组成、素质和思想政治状况．分析阐述了混合系部学生思想政治工作情况：四级思想政治工作体系力量均较为薄弱,专职思想政治工作人员热情均不是很高,相关教育教学管理部门配合还不很默契。学生思想政治组织队伍工作也成效不大．提出了有针对性地加强思想政治工作的对策：领导高度重视。创建十项有效工作机制;系部主抓主管,实施教管结合、教导结合、教养结合等“一至万思想政治工作思路”：部门协调一致,齐抓共管,把学生思想政治工作贯穿到教育、教学、管理和服务过程中;“两课”教学与辅导员工作相结合;构建科学合理的高职院校思想政治教育工作教育和评估体系;充分发挥党政社团作用;组建“学生自律委员会”,鼓励学生自我管理、自我教育．参7．     

高职学生思想政治教育的缺失与消弭

随着高职院校的扩招,学生的素质参差不齐,且较之普通高校学生具有自身特点,因此,对他们的思想政治工作要有针对性.然而,目前高职学生的思政工作具有重宣传轻教育、思想政治教育的教育对象调度缺位、思政教育方法低效等缺陷.要提高思想政治教育的实效,就应该营造以人为本的教育环境、设定合理的思想政治教育目标、不断更新高职学生的思想政治教育的内容.     

高校思想政治工作创新浅论

社会进入二十一世纪,时代的发展,教育观念的转变,对高校学生的思想政治工作提出了新的机遇和挑战,新的时期,如何做好高校学生思想政治工作,这是摆在思想政治工作者面前的重要课题。笔者认为,创新,是高校思想政治工作的生命所在,既是时代发展、教育向素质教育转轨的客观要求,也是高校思想政治工作本身发展的内在动力。思想政治工作的创新是整体的,只有从思想政治工作的内容、形式和方法上全面创新,才能适应社会发展和人才成长的需要。     

校园文化建设与大学生思想政治教育之我见

校园文化建设与大学生思想政治教育相互影响、相互促进．深入认识和谐校园文化和大学生思想政治教育的辩证关系,用和谐校园文化推动大学生思想政治教育的发展．本文通过解析和谐校园文化,试图探索一条促进大学生思想政治教育的新途径．参10．     

中国共产党思想政治教育发展历程探索

中国共产党思想政治教育发展历程大致可分为三大时期、六个阶段,从中可看出中国共产党思想政治教育发展中的四次重大历史性转折和贯穿于其中的一条主线.随着时代的发展,中国共产党思想政治教育发展应注意时代化、生活化、大众化、网络化、人性化.     

刍议罗荣桓同志思想政治工作的方法

方法是成功的阶梯,好的方法可以做到事半功倍.罗荣桓同志的一生中,长期从事思想政治教育工作,他在政治工作实践中,创造了务实民主、换位思考、言传身教等方法,无论对革命战争还是和平建设,都做出了巨大的贡献.学习和总结他的思想政治工作的方法,对于加强新时期的思想政治工作,具有重要的现实意义.参6.     

新形势下高职思想政治理论课教学改革的思考

改革高职院校思想政治理论课教学是新形势的要求．在分析了当前高职院校思想政治理论课教学的现状及特点的基础上,就新形势下高职院校思想政治理论课教学改革的背景及思路进行了探讨、参6．     

论高校职工思想政治工作的策略

职工思想政治工作既是一门科学,又是一项社会实践活动,面对新形势下社会生活及职工思想所发生的变化,工会思想政治工作需与之适应,既要继承和发扬优良传统,更要大胆探索新的途径,真正体现工会思想政治工作的预见性、主动性、针对性、实效性,为社会主义现代化建设服务。     

实现新时期思想政治教育改革中的"十大转变"

在改革开放新的历史条件下,重视思想政治工作是党的优良传统和政治优势,也是新时期党的自身建设的重要内容,应当引起人们的高度重视和深入研究.从指导思路、教育观念、内容结构、主客关系、客体心理、组织形式、组织领导、传播载体等方面探讨新时期思想政治教育改革应实现的几个转变.参3.     

Rainwater composition as a function of the cloud type

The influence of the type of clouds that produce precipitation in the rainwater composition was analyzed. Logroño, a remote station in the North of Spain was chosen for the analyses. Results prove that the rainwater composition from Cumulonimbus is different to the composition of the rainwater from the other clouds. In addition, the source of NO₃ ^? and SO₄ ^2? is studied in the different types of clouds. It is shown that the source is the soil except Stratocumulus formed from Cumulus in which the source is the gas‐particle conversion.     

Calculating ecological carrying capacity of shellfish aquaculture using mass-balance modeling: Narragansett Bay, Rhode Island

Increasing growth in the aquaculture industry demands ecosystem-based techniques for management if that growth is to be ecologically sustainable and promote equity among users of the ecosystems in which it occurs. Models of carrying capacity can be used to responsibly limit the growth of aquaculture in increasingly crowded coastal areas. Narragansett Bay, Rhode Island, USA is one such crowded coastal region experiencing a rapid increase in bivalve aquaculture. An ecosystem mass-balance model was used to calculate the ecological carrying capacity of bivalve aquaculture. Cultured oyster biomass is currently at 0.47 t km⁻² and could be increased 625 times without exceeding the ecological carrying capacity of 297 t km⁻². This translates to approximately 38,950 t of harvested cultured oysters annually which is 4 times the total estimated annual harvest of finfish. This potential for growth is due to the high primary productivity and large energy throughput to detritus of this ecosystem. Shellfish aquaculture has potential for continued growth and is unlikely to become food limited due, in part, to the large detritus pool.     

Environmental geochemistry study of arsenic in Western Hunan mining area,P.R. China

The geochemical characteristics of arsenic in the soil of the Western Hunan mining area of P.R. China were systematically studied. The results show that the strata of Western Hunan are rich in arsenic and that Western Hunan is a geochemically abnormal region for arsenic. The experimental study on speciation in the strata also indicates that the speciation of arsenic in the Neoproterozoic-Cambrian strata are mainly easily transferred speciation (exchangeable, carbonate-bound, sulfides-bound), which are approaching or exceed 60%. Arsenic content in the main soil of Western Hunan is in the range of 8.8–22.8 μg g⁻¹, the mean value is 16.1 μg g⁻¹, which is larger than the arsenic background value of Hunan soil. The distribution of rock with high arsenic content or high easily transferred arsenic speciation is consistent with the distribution of high arsenic content soil. In the mining region, part soils and river/brook waters were polluted by mine tailings and mining/smelting waste water. The arsenic content in polluted paddy soils and river/brook water is 46.26–496.19 μg g⁻¹, 0.3–16.5 mgL⁻¹, respectively. The positive abnormality and pollution of arsenic in the soil and water affects the arsenic content of the crop and the inhabitants’ health.     

Influence of temperature on the reproductive potential of Oncholaimus oxyuris (Nematoda: Oncholaimidae)

The large nematode Oncholaimus oxyuris Ditlevsen, 1911 is a dominant predator in a shallow polyhaline brackish-water pond in Belgium. The reproductive potential of this species was calculated as the intrinsic rate of natural increase r=1/D In pN _e , in which D is the generation time, p is the percentage of females, and N _e is the number of eggs per female. The generation time varies between 570 days at 5°C and 101 days at 25°C and is the main factor in the determination of r. The relationship between r and temperature is nearly linear and is given by r=0.0013 T–0.0042. The reproductive potential of O. oxyuris is much lower than would be predicted from body size; this and the dominance of males in the population, is discussed in the light of the evolution of stable predator-prey systems.     

Assimilation of symbiont-derived photosynthates in some solitary and colonial radiolaria

Evidence for host assimilation of ¹⁴C-labeled symbiont photosynthates is presented from laboratory studies of the solitary radiolarian Thalassicolla nucleata and the colonial species Collosphaera huxleyi. The amount of ¹⁴C-labeled product assimilated in the central capsule of T. nucleata is directly related to the amount of ¹⁴C incorporated by the symbionts. In C. huxleyi central capsules, the percentage of ¹⁴C-label occurring in the water-soluble fraction is 38% and in the lipid-soluble fraction is 20%, the remainder being in insoluble products. Within the lipid-soluble fraction, a substantial percentage of the ¹⁴C activity is associated with the triglyceride and wax ester fractions. The significance of these findings is discussed in relation to the possible physiological role of symbionts in sustaining the host and stabilizing the host-symbiont association.     

Uranium Accumulation of Crop Plants Enhanced by Citric Acid

Citric acid was applied to soil to enhance U accumulation in four crop plants. While the highest enhanced U accumulation of aboveground tissues (a.c. 2000 mg kg⁻¹ dry weight) occurred in the leaves of Indian mustard (Brassica juncea), the highest enhanced U accumulation of roots (a.c. 3500 mg kg⁻¹ dry weight) occurred in canola (Brassica napus var. napus). Uranium translocation among tissues of test plants is in the relation of roots>shoots ≅ leaves. The flowers of sunflower (Helianthus annuus) contained similar or higher U concentrations than those found in shoots, but concentrations in seeds are close to zero. In conclusion, Indian mustard is recommended as a potential species for phytoextraction for U-contaminated soil due to its high U accumulation of aboveground biomass (a.c. 2200 μg per plant). There is no evidence that two types of soils cause a significant difference of the enhanced U accumulation (p<0.05). Results, however, indicate that additional citric acid may result in downward U migration that may contaminate groundwater. Speciation of U that is taken up by plants is also discussed in the end.     

Chemical defense of the mint plant, Teucrium marum (Labiatae)

Summary. The mint plant, Teucrium marum (family Labiatae), sometimes called cat thyme, contains two methylcyclopentanoid monoterpenes, dolichodial and teucrein. The former compound is potently anti-insectan. It is repellent to ants (Monomorium pharaonis) and induces preening reflexes in flies (Phormia regina) and cockroaches (Periplaneta americana). Evidence is presented suggesting that dolichodial, which is presumed to be the plant's chief defensive agent, is stored in the tiny epidermal capsules that beset the leaves. It is only when the leaves are injured (and the capsules ruptured) that the leaves become repellent. Teucrein, in contrast, has no anti-insectan potency. It is present predominantly in the leaf buds, unlike dolichodial, which is present mostly in mature leaves. It is argued that teucrein is the storage compound from which dolichodial is generated during leaf development.     

Recycling flows in emergy evaluation: A mathematical paradox?

This paper is a contribution to the emergy evaluation of systems involving recycling or reuse of waste. If waste exergy (its residual usefulness) is not negligible, wastes could serve as input to another process or be recycled. In cases of continuous waste recycle or reuse, what then is the role of emergy? Emergy is carried by matter and its value is shown to be the product of specific energy with mass flow rate and its transformity. This transformity (τ) given as the ratio of the total emergy input and the useful available energy in the product (exergy) is commonly calculated over a specific period of time (usually yearly) which makes transformity a time dependent factor. Assuming a process in which a part of the non-renewable input is an output (waste) from a previous system, for the waste to be reused, an emergy investment is needed. The transformity of the reused or recycled material should be calculated based on the pathway of the reused material at a certain time (T) which results in a specific transformity value (τ). In case of a second recycle of the same material that had undergone the previous recycle, the material pathway has a new time (T + T₁) which results in a transformity value (τ₁). Recycling flows as in the case of feedback is a dynamic process and as such the process introduces its own time period depending on its pathway which has to be considered in emergy evaluations. Through the inspiration of previous emergy studies, authors have tried to develop formulae which could be used in such cases of continuous recycling of material in this paper. The developed approach is then applied to a case study to give the reader a better understanding of the concept. As a result, a ‘factor’ is introduced which could be included on emergy evaluation tables to account for subsequent transformity changes in multiple recycling. This factor can be used to solve the difficulties in evaluating aggregated systems, serve as a correction factor to up-level such models keeping the correct evaluation and also solve problems of memory loss in emergy evaluation. The discussion deals with the questions; is it a pure mathematical paradox in the rules of emergy? Is it consistent with previous work? What were the previous solutions to avoid the cumulative problem in a reuse? What are the consequences?     

Modeling compensated root water and nutrient uptake

Plant root water and nutrient uptake is one of the most important processes in subsurface unsaturated flow and transport modeling, as root uptake controls actual plant evapotranspiration, water recharge and nutrient leaching to the groundwater, and exerts a major influence on predictions of global climate models. In general, unsaturated models describe root uptake relatively simple. For example, root water uptake is mostly uncompensated and nutrient uptake is simulated assuming that all uptake is passive, through the water uptake pathway only. We present a new compensated root water and nutrient uptake model, implemented in HYDRUS. The so-called root adaptability factor represents a threshold value above which reduced root water or nutrient uptake in water- or nutrient-stressed parts of the root zone is fully compensated for by increased uptake in other soil regions that are less stressed. Using a critical value of the water stress index, water uptake compensation is proportional to the water stress response function. Total root nutrient uptake is determined from the total of active and passive nutrient uptake. The partitioning between passive and active uptake is controlled by the a priori defined concentration value c_max. Passive nutrient uptake is simulated by multiplying root water uptake with the dissolved nutrient concentration, for soil solution concentration values below c_max. Passive nutrient uptake is thus zero when c_max is equal to zero. As the active nutrient uptake is obtained from the difference between plant nutrient demand and passive nutrient uptake (using Michaelis–Menten kinetics), the presented model thus implies that reduced passive nutrient uptake is compensated for by active nutrient uptake. In addition, the proposed root uptake model includes compensation for active nutrient uptake, in a similar way as used for root water uptake. The proposed root water and nutrient uptake model is demonstrated by several hypothetical examples, for plants supplied by water due to capillary rise from groundwater and surface drip irrigation.