水稻光合同化碳在土壤中的矿化和转化动态

作物光合碳是"大气-植物-土壤"碳循环的重要组成部分,是农田土壤有机碳的重要来源,然而其在土壤碳库中的矿化和转化动态尚不清楚.应用室内模拟培养实验,研究水稻收获后输入土壤的光合同化碳在土壤碳库中的矿化及其转化特征.结果表明,100 d的培养期内,原有有机碳的平均矿化速率在4.44~17.8μg·(g·d)-1之间,而光合碳(新碳)的矿化速率则在0.15~1.51μg·(g·d)-1之间.光合同化碳的输入对土壤活性碳库(DOC、MBC)的转化产生显著影响,在培养期内,14C-DOC的转化量为1.89~5.32 mg·kg-1,转化速率的变化幅度为0.18~0.34 mg·(kg·d)-1,原有DOC则在61.13~90.65 mg·kg-1,减少幅度为4.10~5.48 mg·(kg·d)-1;14C-MBC和原有MBC的转化量分别为10.92~44.11 mg·kg-1和463.31~1 153.46mg·kg-1,转化速率变化幅度分别为0.80~2.87 mg·(kg·d)-1和41.60~74.46 mg·(kg·d)-1,说明水稻光合碳的输入对MBC的周转要大于DOC的周转.而且,与原有有机碳相比,输入的"新碳"易被微生物矿化分解,100 d的培养期内,有13.5%~20.2%的新碳被矿化分解,而仅2.2%~3.7%的原有有机碳被矿化分解,光合同化碳的输入对维持稻田土壤的碳汇功能具有重要作用.     

变温环境对典型石灰土有机碳矿化的影响

采用野外采样和室内培养试验,研究了不同土地利用类型(林地和旱地)下的石灰土表层土壤有机碳(SOC)矿化对变温环境的响应.两种供试土样分别采自贵州省普定县天龙山区域的典型林地和旱地的0~10 cm表层.在培养试验中,依据积温相同的原则,设置变温(范围:15~25℃,变温间隔12 h)和恒温(20℃)两个温度处理,培养时间为56 d.在整个培养期内,旱地石灰土变温处理的SOC累积矿化量(63.32 mg·kg-1)虽略低于恒温处理(63.96 mg·kg-1),但两者之间差异不显著,而森林石灰土变温处理的SOC累积矿化量(169.46 mg·kg-1)则显著低于恒温处理(209.52 mg·kg-1)(P<0.05),这表明不同土地利用类型的石灰土SOC矿化对变温环境的响应不同.受植被和土地利用类型的影响,森林石灰土和旱地石灰土表层的SOC含量和组成差异显著,这可能是导致其SOC矿化对变温环境响应差异的重要原因.另外,各温度处理中,土壤可溶性有机碳(DOC)含量与SOC日均矿化量之间均呈极显著正相关(P<0.01),表明制约土壤DOC生成是温度影响土壤有机碳矿化的一个重要途径.在培养过程中,土壤微生物量碳含量不能有效反映恒温和变温下的SOC矿化差异,结合矿化动力学分析可知,同恒温相比,变温虽然不能通过改变微生物数量来影响SOC矿化,但能通过改变微生物群落的总体活性来影响SOC矿化过程.     

微生物脱臭研究应用进展

随着恶臭气体污染成为环境污染的重大问题,对恶臭气体的控制和治理逐渐兴起。文章论述了用微生物法治理恶臭气体污染的基本原理,国内外研究现状以及主要工艺的类型和特点。讨论微生物法的主要影响因素,总结其存在的问题,并对发展趋势做了介绍。     

城市河道水质恢复技术及发展趋势

在分析城市河道水体污染现状和污染源的基础上,介绍了物理、化学、生物生态等城市河道水质恢复技术,分析了不同技术的优缺点及适用性,并预测了城市河道水体恢复技术的发展趋势。     

Topsoil organic carbon mineralization and CO2 evolution of three paddy soils from South China and the temperature dependence

Carbon mineralization and its response to climatic warming have been receiving global attention for the last decade. Although the virtual influence of temperature effect is still in great debate, little is known on the mineralization of organic carbon （SOC） of paddy soils of China under warming. SOC mineralization of three major types of China＇s paddy soils is studied through laboratory incubation for 114 d under soil moisture regime of 70% water holding capacity at 20℃ and 25℃ respectively. The carbon that mineralized as CO2 evolved was measured every day in the first 32 d and every two days in the following days. Carbon mineralized during the 114 d incubation ranged from 3.51 to 9.22 mg CO2-C/gC at 20℃ and from 4.24 to 11.35 mg CO2-C/gC at 25℃ respectively; and a mineralizable C pool in the range of 0.24 to 0.59 gC/kg, varying with different soils. The whole course of C mineralization in the 114 d incubation could be divided into three stages of varying rates, representing the three subpools of the total mineralizable C： very actively mineralized C at 1-23 d, actively tnineralized C at 24--74 d and a slowly mineralized pool with low and more or less stabilized C mineralization rate at 75-114 d. The calculated Q10 values ranged from 1.0 to 2.4, varying with the soil types and N status. Neither the total SOC pool nor the labile C pool could account for the total mineralization potential of the soils studied, despite a well correlation of labile C with the shortly and actively mineralized C, which were shown in sensitive response to soil warming. However, the portion of microbial C pool and the soil C/N ratio controlled the C mineralization and the temperature dependence. Therefore, C sequestration may not result in an increase of C mineralization proportionally. The relative control of C bioavailability and microbial metabolic activity on C mineralization with respect to stabilization of sequestered C in the paddy soils of China is to be further studied.     

Nitrogen cycling of atmosphere-plant-soil system in the typical Calamagrostis angustifolia wetland in the Sanjiang Plain, Northeast China

The nitrogen (N) distribution and cycling of atmosphere-plant-soil system in the typical meadow Calamagrostis angustifolia wetland (TMCW) and marsh meadow Calamagrostis angustifolia wetland (MMCW) in the Sanjiang plain were studied by a compartment model. The results showed that the N wet deposition amount was 0.757 gN/(m2·a), and total inorganic N (TIN) was the main body (0.640 gN/(m2·a)). The ammonia volatilization amounts of TMCW and MMCW soils in growing season were 0.635 and 0.687 gN/m2, and the denitrification gaseous lost amounts were 0.617 and 0.405 gN/m2, respectively. In plant subsystem, the N was mainly stored in root and litter. Soil organic N was the main N storage of the two plant-soil systems and the proportions of it were 93.98% and 92.16%, respectively. The calculation results of N turnovers among compartments of TMCW and MMCW showed that the uptake amounts of root were 23.02 and 28.18 gN/(m2·a) and the values of aboveground were 11.31 and 6.08 gN/(m2·a), the re-translocation amounts from aboveground to root were 5.96 and 2.70 gN/(m2·a), the translocation amounts from aboveground living body to litter were 5.35 and 3.38 gN/(m2·a), the translocation amounts from litter to soil were larger than 1.55 and 3.01 gN/(m2·a), the translocation amounts from root to soil were 14.90 and 13.17 gN/(m2·a), and the soil (0-15cm) N net mineralization amounts were 1.94 and 0.55 gN/(m2·a), respectively. The study of N balance indicated that the two plant-soil systems might be situated in the status of lacking N, and the status might induce the degradation of C. angustifolia wetland.     

17 β-estradiol mineralization in human waste products and soil in the presence and the absence of antimicrobials

Natural steroidal estrogens, such as 17 β-estradiol (E2), as well as antimicrobials such as doxycycline and norfloxacin, are excreted by humans and hence detected in sewage sludge and biosolid. The disposal of human waste products on agricultural land results in estrogens and antibiotics being detected as mixtures in soils. The objective of this study was to examine microbial respiration and E2 mineralization in sewage sludge, biosolid, and soil in the presence and the absence of doxycycline and norfloxacin. The antimicrobials were applied to the media either alone or in combination at total rates of 4 and 40 mg kg^?1, with the 4 mg kg^?1 rate being an environmentally relevant concentration. The calculated time that half of the applied E2 was mineralized ranged from 294 to 418 days in sewage sludge, from 721 to 869 days in soil, and from 2,258 to 14,146 days in biosolid. E2 mineralization followed first-order and the presence of antimicrobials had no significant effect on mineralization half-lives, except for some antimicrobial applications to the human waste products. At 189 day, total E2 mineralization was significantly greater in sewage sludge (38 ±0.7%) > soil (23 ±0.7%) > biosolid (3 ±0.7%), while total respiration was significantly greater in biosolid (1,258 mg CO₂) > sewage sludge (253 mg CO₂) ≥ soil (131 mg CO₂). Strong sorption of E2 to the organic fraction in biosolid may have resulted in reduced E2 mineralization despite the high microbial activity in this media. Total E2 mineralization at 189 day was not significantly influenced by the presence of doxycycline and/or norfloxacin in the media. Antimicrobial additions also did not significantly influence total respiration in media, except that total CO₂ respiration at 189 day was significantly greater for biosolid with 40 mg kg^?1 doxycycline added, relative to biosolid without antimicrobials. We conclude that it is unlikely for doxycycline and norfloxacin, or their mixtures, to have a significant effect on E2 mineralization in human waste products and soil. However, the potential for E2 to be persistent in biosolids, with and without the presence of antimicrobials, is posing a challenge for biosolid disposal to agricultural lands.     

“全面放开二孩”政策对中国人口出生率的冲击与趋势探讨

从"单独二孩"政策到"全面放开二孩"政策,政府针对中国人口现实情况不断做出符合社会需求的政策调整,尽管有可能缓解长期以来计划生育政策导致的适龄劳动力短缺及"未富先老"等社会问题,但人口政策调整的长期效果却有待验证。为此,本文运用灰色预测模型和Leslis模型等方法,对"全面放开二孩"生育政策背景下中国未来人口出生率的冲击和波动趋势作出预测,并对"全面放开二孩"政策所带来的对生育率及人口年龄结构影响展开分析,对2016—2050年的出生率、人口总数及人口结构作出预测,最终发现"全面放开二孩"政策会促进人口结构相对优化,但不能从根本上扭转劳动力供求关系失衡和老龄化加剧的趋势。为防止落入人口超低生育率陷阱,适度抑制老龄化快速增长趋势,实现人口与社会经济全面协调发展,必须对现行的生育政策进行完善,短期内,应积极出台配套措施,全面贯彻"全面放开二孩"政策,积极应对老龄化趋势;长期内,应逐步过渡到自主生育政策,形成人口自然生长的均衡发展长效机制。     

负载TiO2浮石对污水处理厂二沉池出水的矿化与灭菌研究

城市污水处理厂第二沉淀池出水的污染物浓度较低,经过矿化及灭菌等深度处理后可以回用,从而减轻对淡水资源的需求。本实验采用溶胶-凝胶法制备了负载TiO2的浮石光催化剂,对城市污水处理厂第二沉淀池出水进行了矿化及灭菌处理研究。采用低压汞灯对处理水样照射2h,有机物降解率可以达到50％,灭菌效率达到100％。处理后的水可以作为农作物灌溉、城市绿化和娱乐用水。负载在浮石表面的TiO2薄膜经过10次的光催化循环实验后,没有明显破损,可以再次循环使用。TiO2浮石具有质轻、机械性能好和价格低等优点,该方法处理废水的适用浓度低,可以广泛应用于微污染水和城市污水处理厂出水的深度处理。     

DOC removal paradigms in highly humic aquatic ecosystems

Background, aim, and scope  Dissolved humic substances (HS) usually comprise 50–80% of the dissolved organic carbon (DOC) in aquatic ecosystems. From a trophic and biogeochemical perspective, HS has been considered to be highly refractory and is supposed to accumulate in the water. The upsurge of the microbial loop paradigm and the studies on HS photo-degradation into labile DOC gave rise to the belief that microbial processing of DOC should sustain aquatic food webs in humic waters. However, this has not been extensively supported by the literature, since most HS and their photo-products are often oxidized by microbes through respiration in most nutrient-poor humic waters. Here, we review basic concepts, classical studies, and recent data on bacterial and photo-degradation of DOC, comparing the rates of these processes in highly humic ecosystems and other aquatic ecosystems. Materials and methods  We based our review on classical and recent findings from the fields of biogeochemistry and microbial ecology, highlighting some odd results from highly humic Brazilian tropical lagoons, which can reach up to 160 mg C L⁻¹. Results and discussion  Highly humic tropical lagoons showed proportionally lower bacterial production rates and higher bacterial respiration rates (i.e., lower bacterial growth efficiency) than other lakes. Zooplankton showed similar δ¹³C to microalgae but not to humic DOC in these highly humic lagoons. Thus, the data reviewed here do not support the microbial loop as an efficient matter transfer pathway in highly humic ecosystems, where it is supposed to play its major role. In addition, we found that some tropical humic ecosystems presented the highest potential DOC photo-chemical mineralization (PM) rates reported in the literature, exceeding up to threefold the rates reported for temperate humic ecosystems. We propose that these atypically high PM rates are the result of a joint effect of the seasonal dynamics of allochthonous humic DOC input to these ecosystems and the high sunlight incidence throughout the year. The sunlight action on DOC is positive to microbial consumption in these highly humic lagoons, but little support is given to the enhancement of bacterial growth efficiency, since the labile photo-chemical products are mostly respired by microbes in the nutrient-poor humic waters. Conclusions  HS may be an important source of energy for aquatic bacteria in humic waters, but it is probably not as important as a substrate to bacterial growth and to aquatic food webs, since HS consumption is mostly channeled through microbial respiration. This especially seems to be the case of humic-rich, nutrient-poor ecosystems, where the microbial loop was supposed to play its major role. Highly humic ecosystems also present the highest PM rates reported in the literature. Finally, light and bacteria can cooperate in order to enhance total carbon degradation in highly humic aquatic ecosystems but with limited effects on aquatic food webs. Recommendations and perspectives  More detailed studies using C- and N-stable isotope techniques and modeling approaches are needed to better understand the actual importance of HS to carbon cycling in highly humic waters.