2℃低温下冬小麦幼苗质膜Ca~(2 )-ATPase的活性变化

用氯化铈 (CeCl3 )沉淀的电镜细胞化学方法 ,对常温下及 2℃低温处理后的冬小麦 (TriticumaestiviumL .)幼苗质膜Ca2 ATPase活性进行定位 .结果显示 :(1)常温下生长的冬小麦幼苗 ,质膜上有部分Ca2 ATPase活性反应 .(2 )冬小麦幼苗经 2℃低温处理 1h ,质膜上Ca2 ATPase活性增加 .处理 3h ,活性进一步加强 .2℃下处理 12h ,有强的酶活性反应 .处理 2 4h后 ,活性反应达到最强 .2℃处理 3d ,Ca2 ATPase活性有所下降 ,但仍高于CK .细胞结构完整 .据结果推测 ,质膜Ca2 ATPase活性受细胞内Ca2 浓度反馈调节 .图 1参 10     

[CO2]和温度增加的相互作用对植物生长的影响

ＣＯ2 和温度是影响植物生长、发育和功能的两个关键因子 .在过去一个世纪中 ,[ＣＯ2 ]从 2 80 μｍｏｌ/ｍｏｌ增加到 36 0μｍｏｌ/ｍｏｌ且每年增长速率为 1～ 5 μｍｏｌ/ｍｏｌ,到 2 0世纪末达到更高的浓度[1] .最近的模型预测表明 ,到 2 10 0年 ,全球表面温度可能会增加 1～ 4 .5℃ [2 \〗.ＣＯ2 是光合作用的底物 ,而且还是初级代谢过程 (气孔反应和光合作用 )、光合同化物分配和生长的调节者 .温度几乎影响植物所有的生物学过程 .因此 ,在全球气候变化要素中 ,大气 [ＣＯ2 ]和温度升高对植物的生理过程和生物量及产量具有极为重要的…     

生活垃圾堆肥工艺条件及其反应动力学研究

为了改善堆肥微环境 ,提高生活垃圾堆肥速率 ,研究堆肥工艺条件及其反应动力学是非常必要的。通过控制堆肥工艺条件 ,如初始温度、含水率、C/N比及堆料颗粒大小 ,研究生活垃圾堆肥过程中生物、化学及物理因素的变化。试验结果表明 ,生活垃圾堆肥反应符合一级反应动力学 ;合理控制堆肥初始反应条件 ,能明显提高堆肥效率。     

不同混凝剂处理低温低浊水

针对低温低浊水处理难度大的问题进行了一系列的混凝实验,实验结果表明,随着混凝剂投加量的增加,剩余浊度呈现先降低后升高的趋势,单独使用HPAC时,剩余浊度在投加量为14 mg/L时达到最低(2.39 NTU)。pH值对余铝含量具有重要的影响,3种铝系混凝剂均在pH=7.0时余铝含量达到最低。AlCl3对水中有机物的去除率较其他3种混凝剂低。絮体形成与破碎受搅拌强度的影响很大,当破碎强度增加到50 r/min,使用PACl、HPAC、FeCl3作混凝剂时絮体粒径下降不明显,当破碎强度增加到100 r/min时,絮体粒径有明显的下降。破碎结束后,絮体粒径有所恢复,但是并不能增长到破碎前的粒径。PACl、HPAC以及FeCl3形成的絮体的沉降性较好,上覆水浊度下降较快,经过3 h的沉降后,剩余浊度分别达到1.82、1.44和0.97 NTU。     

碳氮比对低温投加介体生物反硝化脱氮的影响

污水的生物脱氮效果受低温抑制,投加氧化还原介体有利于反硝化过程。采用规格相同的序批式反应器,使用人工配制硝酸盐废水和经过驯化的活性污泥,考察了不同碳源浓度(碳氮比)对低温(10 ℃)投加氧化还原介体1, 2-萘醌-4-磺酸(NQS)污水生物反硝化脱氮过程的影响。结果表明：当碳源浓度(以COD计)为150~400 mg·L⁻¹ (碳氮比为1.8~4.7)时,脱氮效率随碳氮比的升高而升高;当碳源浓度为400~550 mg·L⁻¹ (碳氮比为4.7~6.5)时,脱氮效率随着碳氮比的升高而降低;当碳源浓度为400 mg·L⁻¹ (碳氮比为4.7)左右时效果最好,总氮去除率最高为64.7%。对于脱氮速率,介体强化脱氮速率随着碳氮比的升高而升高。同时,探讨了投加介体污水生物反硝化脱氮的机理,发现投加介体降低了体系的氧化还原电位(ORP),有利于反硝化脱氮反应的进行。     

污泥的粘度与浓度、温度三者关系式的实验推导

通过融合污泥粘度与污泥浓度关系式、污泥粘度与温度关系式,得到一个新的关系式:污泥粘度与污泥浓度、温度的关系式,并通过实验数据拟合出各项参数,拟合效果比较理想.得出的污泥粘度与污泥浓度、温度的关系式对了解污泥的粘度变化非常有帮助,同时,该关系式也将为污泥处理、处置方案的制定提供参考依据.     

典型进口再生塑料颗粒中重金属溶出特性及其影响因素

为了解我国进口再生塑料颗粒中重金属溶出特性,以某检测机构的5种再生塑料颗粒PP、PE、PS、PET和ABS为研究对象,研究不同温度、不同接触时间和不同模拟液等条件下,再生塑料颗粒中重金属溶出特性。结果表明,在25、40、70 ℃这3种温度下,PP、PE、PET和ABS再生塑料颗粒中重金属铬、铅、锰、镉、汞和铜的溶出量随着温度的升高而增加,PS中重金属浓度随温度升高变化不大;随着接触时间的增长,样品中的6种重金属Cr、Pb、Mn、Cu、Cd、Hg溶出量增长趋势由快至慢,5种再生塑料颗粒中重金属Cr的溶出浓度最高;PE、PS、PET和ABS再生塑料颗粒在4种模拟液中重金属溶出量大小整体呈现出：50%乙酸>3%乙酸>10%乙醇>95%乙醇,但PP再生塑料颗粒中重金属Cu在3%乙酸中的溶出量比10%乙醇中的多。本研究结果可为建立塑料接触材料及制品中重金属溶出量的标准方法提供依据。     

INVESTIGATION OF TURBIDITY MAXIMUM IN A MESOTIDAL ESTUARY,TAIWAN1

ABSTRACT: To comprehend the distributions of salinity, temperature, and suspended sediment in the Danshuei River estuary in Taiwan, monthly field surveys were conducted in 2003. These included several high and low slackwater surveys and intensive surveys. The results show that the Danshuei River estuary is predominately a partially mixed estuary. The highest concentration of suspended sediment is typically observed at the Chung‐Hsin Bridge, the most upstream sampling station. The suspended sediment concentration exhibits a general decreasing trend in the downstream direction. It may be concluded that the sediments mostly come from the upstream reach. A locally high concentration of suspended sediment is found at the Kuan‐Du station because of the local deep channel bathymetry and two‐layered estuarine circulation. A vertical two‐dimensional hydrodynamic and sediment transport model is applied to investigate the tidally averaged salinity distribution, residual circulation, and suspended sediment concentration. The modeling results reveal that, under the Q₇₅ flow condition (i.e., low flow), a turbidity maximum occurs at the Kuan‐Du station due to the strong estuarine circulation. The model simulation with a much higher river flow condition results in a weaker residual circulation and weaker turbidity maximum.     

STREAM TEMPERATURE ESTIMATION FROM AIR TEMPERATURE1

ABSTRACT: Air temperatures are sometimes used as substitutes for stream temperatures. To examine the errors associated with this procedure, linear relationships between stream temperatures, T, and air temperatures, T_a, recorded for 11 streams in the central U.S. (Mississippi River basin) were analyzed. Weather stations were an average 42 miles (range 0 to 144 miles) from the rivers. The general equations, T_w= 5.0 + 0.75 T_a and T_w= 2.9 + 0.86 T_a with temperatures in °C, were derived for daily and weekly water temperatures, respectively, for the 11 streams studied. The simulations had a standard deviation between measurements and predictions of 2.7°C (daily) and 2.1°C (weekly). Equations derived for each specific stream individually gave lower standard deviations, i.e., 2.1°C and 1.4°C, respectively. Small, shallow streams had smaller deviations than large, deep rivers. The measured water temperatures follow the air temperatures closely with some time lag. time lags ranged from hours to days, increasing with stream depth. Taking into account these time lags improved the daily temperature predictions slightly. Periods of ice cover were excluded from the analysis.     

The Volta Lake and Declining Rainfall and Streamflows in the Volta River Basin

This paper looks at the rainfall and streamflow patterns over two distinct time periods, i.e., 1950–1970 and 1971–1991 within the two most prominent catchments in the Volta river system – White Volta and the Oti basins. The first period (1950–1970) represents relatively vegetated catchments and low population whilst the latter (1971–1990) represents intense land use practices resulting from increased population that have severely degraded the environment. These two catchments are among the most significant contributors to the Volta lake. The Volta lake, which was formed between 1962 and 1966 in Ghana and created primarily for hydroelectric power generation, will probably be one of the greatest man-made lakes for a long time. It produces 912MW of electricity at its maximum operating capacity. Recently, there have been declines in the lake levels resulting most probably from inadequate rainfall and/or runoff from the river catchments that feed the lake. Comparisons of runoffs for the two time periods show reductions in mean streamflows of 32.5% at Saboba on the Oti and 23.1% at Nawuni on the White Volta.