云南省城市生活垃圾处理温室气体排放特征

根据《IPCC国家温室气体清单指南》和《省级温室气体清单编制指南》方法,建立2018年云南省16个州(市)城市生活垃圾处理温室气体排放清单,包括生活垃圾填埋和焚烧处理过程,并分析了温室气体排放的时间分布、空间分布和影响因素等。结果表明;(1)2018年云南省生活垃圾处理温室气体总排放量为536万t CO_2当量,各州(市)间排放量差异明显,滇中经济发达地区和滇东北人口密度较高地区排放量明显高于滇西北地区。(2)2005—2018年,云南省生活垃圾处理排放的温室气体量增长了191.3%,温室气体排放组成发生明显变化,CH4比重不断下降,CO_2比重不断增加。(3)城镇人口数量、生活垃圾处理量、经济发展水平与温室气体排放量显著相关,其中人口数量更为明显。     

The potential of current legal structures to support Aboriginal and Torres Strait Islander interests in the Australian bush food industry

There are complex connections between Australia’s native plants and first peoples, the Aboriginal and Torres Strait Islander peoples. The maintenance of these connections is central to Aboriginal and Torres Strait Islander culture and well-being and the tangible realisation of Australian policy commitments. Diverse cultural connections combine with other motivations to underpin an array of Aboriginal and Torres Strait Islander interests in the commercial development of traditional plant foods (‘bush foods’). Despite nation-wide policy support for these interests, there is no national legal framework to support them. This fortifies the popular call for a new (sui generis) law that transforms the interests of Aboriginal and Torres Strait Islander peoples into enforceable legal rights. It is unclear the extent to which a single sui generis law might help Aboriginal and Torres Strait Islander peoples realise their diverse interests in the development of gourmet bush food products and new bush food varieties. It is also unlikely that Australia will implement such a law in the near future. This paper offers a preliminary study of the capacity of current legal structures to support some key Aboriginal and Torres Strait Islander interests that might arise in these two development contexts. The study can inform the future development of practical legal strategies to support the diverse interests of Aboriginal and Torres Strait Islander peoples in the bush food industry.     

长三角农田土壤中滴滴涕的污染特征与生态风险

以长江三角洲地区农田土壤为研究对象,分析了土壤和蔬菜中滴滴涕(DDTs)的残留水平和空间分布特征,评估了DDTs对土壤生态和人体健康的潜在风险。结果显示,长三角地区农田土壤中DDTs含量范围为0.2~3 520 ng·g-1,平均63.8 ng·g-1,主要残留在土壤耕作层(0~30 cm)。土壤中DDTs及其代谢产物残留量较低,98.5%的点位土壤符合《中国土壤环境质量标准》的二级标准。15%的蔬菜样品中检出DDTs,其浓度为相应土壤DDTs浓度的9%~18%,土壤残留的DDTs通过食物链进入人体导致的健康风险很小。低残留DDTs对土壤微生物的群落结构和多样性无显著影响(-0.25R0.25,0.307P0.979)。应用美国环保署(USEPA)方法评估了土壤中DDTs对人体的健康风险,其中致癌风险级别为非常低,对儿童和成人具有非致癌风险的样品比例分别为1.1%和0.7%。因此,长三角地区大多数点位农田土壤DDTs残留量较低,不会对生态环境和人体健康产生危害。     

Environmental deterioration of farmlands caused by the irrational use of agricultural technologies

Without considering the ecosystem-dependence of agricultural production, irrational use of agricultural technologies could bring only short-term economic benefits but leave long-term environmental deterioration. If some agricultural lands have to be abandoned because of these technologies such as chemical films or groundwater depletion, it will aggravate the burden of remaining lands for maintaining or enhancing production. Thus, agricultural production should be a part of public services, requiring the consideration of interests of different stakeholders and sustainability.     

农业活动干扰下地下水无机碳循环过程研究

为准确识别浅层地下水污染来源及污染过程,选择我国北方某集约化蔬菜种植基地浅层地下水作为研究对象,借助水化学组成、氢氧同位素以及溶解性无机碳(DIC)碳同位素组成,探讨浅层地下水来源以及DIC来源和迁移转化特征.结果表明:浅层地下水阳离子以Ca²⁺和Mg²⁺为主,阴离子以HCO₃^-和SO₄^2-为主,沿地下水流向,水化学类型由HCO₃^?-Ca²⁺-Mg²⁺型转变为HCO₃^--SO₄^2--Mg²⁺-Ca²⁺型;浅层地下水δD组成范围为-69.6‰~-52.7‰,均值为-63.5‰,δ¹⁸O组成范围为-9.29‰~-6.80‰,均值为-8.45‰.大气降水是浅层地下水重要补给来源,靠近河水的浅层地下水还接受地表水的补给;浅层地下水δ¹³C_DIC组成范围为-11.76‰~-5.85‰,均值为-10.43‰.浅层地下水DIC来源包括土壤CO₂、碳酸盐矿物以及有机质分解.河水DIC侧渗对局部浅层地下水DIC碳同位素造成影响,化学肥料引起的酸性物质参与碳酸盐矿物风化作用以及浅层地下水CO₂去气作用对地下水δ¹³C_DIC组成产生影响,在利用DIC碳同位素识别地下水污染来源时需要引起重视.     

基于油耗调查的2010年天津市农业机械排放研究

通过问卷调查,采用基于燃油消耗量的方法估算出天津市2010年农业机械氮氧化物(NOx)和颗粒物(PM)的总排放量.2010年天津市农业机械总保有量为57.5万台,其中种植业机械最大约占52.5%;总动力为588万kW,运输机械占比最大为47.3%.估算出2010年天津市农业机械总油耗(主要为柴油)为6.7万t,其中运输机械耗油量为4.5万t.再根据燃油消耗量估算了天津2010年农业机械污染物排放量,NOx和PM年排放量分别为3470t和303t.     

珠江三角洲机动车排放控制措施协同效应分析

预测了2015年珠江三角洲机动车空气污染物和温室气体排放量,设计了6类单一控制、技术控制、结构控制以及综合控制措施的情景,并运用基准线年排放清单编制和协同效应坐标系法分析了污染物与温室气体减排的协同效应.结果表明,按目前机动车保有量增长趋势,2015年污染物和温室气体将以18%~120%的幅度增加;各控制措施下污染物和温室气体排放量均有下降,且均具有正向的协同效应,但减排的贡献差异较大.6类单一控制措施中淘汰黄标车和结构性控制措施分别对各污染物和温室气体的削减效果最明显,减排幅度均在40%以上,且正向协同效应突出,但相比其他措施,结构性控制措施实施难度大.     

崇明东滩芦苇湿地温室气体排放通量及其影响因素

通过静态箱-气相色谱法对崇明东滩芦苇群落在生长周期内的3种温室气体——CH₄、N₂O和CO₂的排放、吸收特征进行研究. 结果表明:芦苇群落湿地CH₄排放通量受温度影响较大,夏季排放通量明显高于其他季节,年均排放通量为74.46μg/(m2·h);N₂O年均排放通量为2.22μg/(m2·h),冬季排放通量最大;CO₂的吸收率季节变化明显,年均排放通量为-101.93mg/(m2·h). 温度、芦苇植株光合作用及呼吸作用是影响CH₄产生和排放的主要因素;而沉积物氮素不足和限制,则是促使芦苇群落表现出对N₂O吸收的原因;芦苇的光合作用及土壤呼吸作用随温度和季节的变化是控制芦苇湿地CO₂的排放和吸收的主要因素. 芦苇植株发达的通气组织是CH₄和N₂O由大气向沉积物扩散的通道,同时分子扩散过程也是沉积物产生的CH₄、N₂O和CO₂扩散到大气中的途径和方式.      

互花米草入侵盐沼湿地CH4和N2O排放日变化特征研究

甲烷（CH4）和氧化亚氮（N2O）是导致全球气候变暖的2种重要温室气体,探索其源汇及地域排放特征一直是全球变化研究领域的核心内容。CH4和N2O通量的日变化研究是正确估算大时间尺度下CH4和N2O排放量的基础。利用静态箱法原位观测了江苏沿海芦苇（Phragmites australis）、盐蒿（Suada salsa）、光滩、水面以及互花米草（Spartina alterniflora）入侵湿地CH4和N2O排放的日变化特征。结果表明,1）互花米草湿地地上部生物量为1.70 kg·m^-2,土壤有机碳质量分数为13.55 g·kg^-1;分别是芦苇和盐蒿湿地的2.50-3.43和2.15-4.15倍。2）互花米草和芦苇湿地土壤10 cm处氧化还原电位（Eh）有明显日变化,最低值出现在3：00,最高值出现在12：00;光滩和盐蒿湿地没有明显的日变化。3）互花米草湿地 CH4日平均排放通量为0.52 mg·m^-2·h^-1,是其他湿地的2.12-6.40倍;N2O日平均通量为-3.24μg·m^-2·h^-1,显著低于盐蒿湿地、光滩和水面（P＜0.05）。互花米草和芦苇湿地CH4排放通量最高值（0.73 mg·m^-2·h^-1和0.30 mg·m^-2·h^-1）出现在15：00,最低值（0.37 mg·m^-2·h^-1和0.17 mg·m^-2·h^-1）出现在3：00,均与土壤孔隙水中CH4浓度呈显著负相关（P＜0.05）。互花米草湿地CH4排放通量与10 cm土温、Eh和生态系统CO2净交换量（NEE）显著正相关（P＜0.05）。互花米草和芦苇湿地N2O通量9：00-18：00为负值,21：00—6：00为正值,均与NEE呈显著负相关（P＜0.05）。盐蒿湿地、光滩和水面CH4和N2O排放通量没有明显日变化特征。互花米草入侵提高了沿海湿地CH4排放,但降低了N2O排放,植物对CH4传输作用以及向根际传输O2和易分解有机物是导致互花米草和芦苇湿地CH4和N2O排放表现出日变化特征的原因。     

N2O emission from a sequencing batch reactor for biological N and P removal from wastewater

Nitrous oxide （N2O） is a greenhouse gas that can be released during biological nitrogen removal from wastewater. N2O emission from a sequencing batch reactor （SBR） for biological nitrogen and phosphorus removal from wastewater was investigated, and the aims were to examine which process, nitrification or denitrification, would contribute more to N2Oemission and to study the effects of heterotrophic activities on N2O emission during nitrification. The results showed that N2O emission was mainly attributed to nitrification rather than to denitrification. N2O emission during denitrification mainly occurred with stored organic carbon as the electron donor. During nitrification, NaO emission was increased with increasing initial ammonium or nitrite concentrations. The ratio of N2O emission to the removed ammonium nitrogen （N2O- N/NH4-N） was 2.5% in the SBR system with high heterotrophic activities, while this ratio was in the range from 0.14% to 1.06% in batch nitrification experiments with limited heterotrophic activities.