资本禀赋、技术认知与农户耕地低碳利用意愿

耕地低碳利用对于减少农业温室气体排放,促进农业持续健康发展具有积极意义。建立资本禀赋、技术认知的理论分析模型和研究假说,利用湖北省347户农户的调研数据,在测度农户资本禀赋、耕地低碳利用技术认知的基础上,采用Logit模型、中介效应模型、调节效应检验方法,就资本禀赋、技术认知与农户耕地低碳利用意愿的关系进行实证研究。结果发现,资本禀赋不仅对农户耕地低碳利用意愿在1%水平上有显著的直接正向影响,还会通过技术认知这一中介变量在1%水平上产生显著的间接正向影响,环境素养在农户自我效能认知和耕地低碳利用意愿间发挥正向调节作用。据此,建议从经济资本、社会资本、文化资本3个角度提升农户的资本禀赋,通过多种渠道提升农户对耕地低碳利用的认知水平,提高农户环境素养。     

巴音温都尔沙漠典型植物群落土壤物理性质研究

巴音温都尔沙漠是我国北方干旱气候带典型的环境敏感区和生态脆弱区,生态建设和植被恢复对巴音温都尔沙漠生态系统服务功能极为重要。本研究以巴音温都尔沙漠梭梭、唐古特白刺、球果白刺、盐爪爪、膜果麻黄群落土壤为试验对象,对不同植物群落类型土壤物理性状和持水能力进行了研究。结果表明:5种群落中土壤孔隙度、土壤毛管孔隙度与土壤非毛管孔隙度最大值均出现在盐爪爪群落,其土壤通透性最好,具备良好的通气透水能力;膜果麻黄群落土壤最为紧实,通气透水能力最差。5种群落中,盐爪爪群落土壤自然含水率最高,膜果麻黄群落最低。盐爪爪群落土壤持水量最高,麻黄群落土壤持水量最低。盐爪爪群落土壤具有良好的保水能力,膜果麻黄群落土壤保水能力处于偏低水平。     

Poorly crystalline iron and aluminium oxides contribute to the carbon saturation and sorption of dissolved organic carbon in the soil

Soil carbon (C) saturation implies an upper limit to a soil's capacity to store C depending on the contents of silt + clay and poorly crystalline Fe and Al oxides. We hypothesized that the poorly crystalline Fe and Al oxides in silt + clay fraction increased the C saturation and thus reduced the capacity of the soil to sorb additional C input. To test the hypothesis, we studied the sorption of dissolved organic carbon (DOC) on silt + clay fractions (<53 µm) of highly weathered oxic soils, collected from three different land uses (i.e., improved pasture, cropping and forest). Soils with high carbon saturation desorbed 38% more C than soils with low C saturation upon addition of DOC, whereas adsorption of DOC was only observed at higher concentration (>15 g kg^?1). While high Al oxide concentration significantly increased both the saturation and desorption of DOC, the high Fe oxide concentration significantly increased the desorption of DOC, supporting the proposition that both oxides have influence on the DOC sorption in soil. Our findings provide a new insight into the chemical control of stabilization and destabilization of DOC in soil.     

2000—2015年西南区县域土地利用变化特征及驱动力分析——以重庆市奉节县为例

综合分析重庆市奉节县土地利用格局时空演变及其驱动力,为优化西南区县域尺度的土地利用规划、生态大保护和区域可持续发展提供理论参考和数据支持。基于RS和GIS技术,利用四期（2000、2005、2010和2015年）土地利用基础数据,从土地利用动态模型和地学信息图谱等方面出发,揭示区域2000—2015年的土地利用动态变化特征及时空演变规律。依据主成分分析模型和线性回归分析模型,并基于奉节县社会经济统计数据,探究研究区土地利用驱动机制。研究期内,研究区土地空间格局呈现以林地和耕地为主体,同时交错分布其它土地类型的特点。耕地、草地和未利用地土地面积分别减少 78.84 km²、3.73 km²、2.54 km²,而林地、水域和居民工矿用地面积分别增加23.36 km²、46.67 km²、9.03 km²。受三峡移民影响,区域土地利用分布格局由整体无序向局部有序的方向发展。研究期的前10年间,土地利用类型转移主要发生在林地、草地和耕地之间,林地→耕地和草地的面积总和分别为849.38 km²和425.17 km²;2010—2015年间林地和居民工矿用地新增面积分别为9.93 km²和7.09 km²。从产业结构调整、政策影响和社会发展等方面探究区域城镇化的驱动机制,城镇化因素、政策因素、经济因素、社会发展因素和农业因素是影响奉节县土地利用类型变化的主要驱动力。     

硫化细菌的分离及对碱土pH的影响

通过对样品的富集，利用选择培养进行化能自养硫化细菌的分离；以大庆本地碱土作为实验材料，通过硫化细菌及辅料的添加，利用pH计测定碱土pH值变化。分离获得了硫化细菌lh-1，利用该菌株改良碱土以添加0.27% 硫粉混合硫化细菌效果最为明显，经过两个半月的改良，pH可从10.53降到8.23。     

Straw mulching with fertilizer nitrogen: An approach for improving crop yield,soil nutrients and enzyme activities

Field experiments were conducted to study soil properties, soil enzymes activities, water use efficiency (WUE) and crop productivity after six years of soya bean straw mulching in the semi‐arid conditions of China. The experiment included four treatments: CK (Control), N (240 kg N ha^‐1), H (soya bean straw mulching at half rate 700 kg ha^‐1 with 240 kg N ha^‐1) and F (soya bean straw mulching at full rate 1,400 kg ha^‐1 with 240 kg N ha^‐1). Soil organic carbon (SOC), soil labile organic carbon (LOC), soil available N (AN), available P (AP) and enzyme activities were analysed after wheat harvesting in 2016 and 2017. Results show that straw amounts had positive effects on the soil fertility indices being higher for treatment F. The SOC, LOC, AN, AP and enzyme activities (i.e. saccharase, urease and alkaline phosphatase) were in the order of F > H > N > CK. High wheat grain yield and WUE were observed for F treatment. A total of six years mulching along with 240 kg ha^‐1 nitrogen fertilizer application is sufficient for wheat yield stability and improving soil properties except urease activities in the semi‐arid condition of China. However, the straw mulching amount should be further studied with minimum nitrogen fertilizer for an environment‐friendly and effective approach for improving the soil biological properties with adequate crop production on a sustainable basis in the semi‐arid region of China.     

Changes in soil and water quality at sediment–water interface of Penaeus vannamei culture pond at varying salinities

The health of the pond environment in shrimp farming is important for sustainable and profitable aquaculture, in which sediment–water interface is the most important influencing area. With this objective, the key parameters of water and sediment at the interface was studied in shrimp ponds with varying salinities and compared with the surface water and soil to understand the variations and the underlying causes. Total ammonia nitrogen and total alkalinity were higher in water at the interface as compared to surface water, whereas pH, nitrite, oxide forms of nitrogen (NO₃), phosphorus (PO₄) and oxidizing bacteria were observed to be lower. There was no significant difference with respect to macrominerals such as sodium, potassium, calcium and magnesium between water at the interface and surface. These changes are profoundly influenced by the uppermost 1.0‐cm thick sediment layer, where the maximum transition of nutrients takes place with the water column. The outcome of the study highlights the effectiveness of water sampling for metabolites at the interface, which reflects at an early stage any potential deterioration of pond environment, which will help the farmer to initiate timely mitigation measures.     

Substitution of chemical fertilizer by Chinese milk vetch improves the sustainability of yield and accumulation of soil organic carbon in a double-rice cropping system

The double-rice cropping system is a very important intensive cropping system for food security in China. There have been few studies of the sustainability of yield and accumulation of soil organic carbon(SOC) in the double-rice cropping system following a partial substitution of chemical fertilizer by Chinese milk vetch(Mv). We conducted a 10-year(2008–2017) field experiment in Nan County, South-Central China, to examine the double-rice productivity and SOC accumulation in a paddy soil in response to different fertilization levels and Mv application(22.5 Mg ha~(–1)). Fertilizer and Mv were applied both individually and in combination(sole chemical fertilizers, Mv plus 100, 80, 60, 40, and 0% of the recommended dose of chemical fertilizers, labeled as F100, MF100, MF80, MF60, MF40, and MF0, respectively). It was found that the grain yields of double-rice crop in treatments receiving Mv were reduced when the dose of chemical fertilizer was reduced, while the change in SOC stock displayed a double peak curve. The MF100 produced the highest double-rice yield and SOC stock, with the value higher by 13.5 and 26.8% than that in the F100. However, the grain yields increased in the MF80(by 8.4% compared to the F100), while the SOC stock only increased by 8.4%. Analogous to the change of grain yield, the sustainable yield index(SYI) of double rice were improved significantly in the MF100 and MF80 compared to the F100, while there was a slight increase in the MF60 and MF40. After a certain amount of Mv input(22.5 Mg ha~(–1)), the carbon sequestration rate was affected by the nutrient input due to the stimulation of microbial biomass. Compared with the MF0, the MF100 and MF40 resulted in a dramatically higher carbon sequestration rate(with the value higher by 71.6 and 70.1%),whereas the MF80 induced a lower carbon sequestration rate with the value lower by 70.1% compared to the MF0. Based on the above results we suggested that Mv could partially replace chemical fertilizers(e.g., 40–60%) to improve or maintain the productivity and sustainability of the double-rice cropping system in South-Central China.     

科尔沁草甸湿地土壤碳氮剖面分布及生长季动态特征

采用定位观测的试验方法,于2016年5-10月及2017年8月对科尔沁草甸湿地0~100 cm土层土壤有机碳、全氮剖面分布及生长季动态特征进行了实验分析,旨在为科尔沁草甸湿地保护提供科学指导并为干旱半干旱地区湿地土壤碳氮储量估算提供借鉴。结果表明:1)科尔沁草甸湿地土壤有机碳、全氮含量整体随土层深度下降,0~20 cm土层间下降显著,20 cm以下趋于相对稳定,范围分别为11.9~23.5 g·kg^-1和0.66~1.50 g·kg^-1。2)各土层土壤碳氮含量月间差异显著(全氮40~60 cm土层除外),变化幅度随土层深度先减小后增大;土壤碳氮密度(100 cm)生长季变化大于年际变化,有机碳密度全生长季呈上升趋势,范围为15.44~20.82 kg·m^-2,全氮密度生长初期明显下降,之后趋于相对稳定,范围为1.01~1.16 kg·m^-2。3)土壤有机碳含量与全氮含量呈极显著正相关;植被和水文是影响其分布、变化的关键因子。科尔沁草甸湿地生长季土壤有机碳、全氮密度变化较大,且表现为潜在的碳汇和氮源,但年际间碳汇潜力未充分发挥,本研究建议禁牧力度应加大并增加氮肥投入以提高科尔沁草甸湿地生态系统功能。     

蚯蚓养殖对幼龄胶园土壤养分及橡胶树根系生长的影响

本研究旨在探讨林下蚯蚓养殖对幼龄胶园土壤养分及橡胶树根系生长的影响。以牛粪作为原料，于 2017年4—11 月在 4 年生幼龄胶园铺设粪垄养殖蚯蚓，并测定土壤养分和根系生长情况。结果表明，与对照（CK）相比，铺设粪垄无蚯蚓养殖（WQ）和铺设粪垄蚯蚓养殖（Q）处理总体上可显著提高土壤硝态氮、速效磷、速效钾和土壤水分含量以及土壤 pH，而对土壤铵态氮、有机质、微生物活性及微生物群系数量无显著影响（p<0.05）；和 CK 相比，WQ和 Q 处理显著促进根的生长，并提高吸收根的比例（p<0.05）。综上所述，在幼龄胶园养殖蚯蚓短期内（半年）可提高土壤速效养分含量，促进根系生长。