湖南主要农田土壤中氮的形态

本试验采集了湖南省八种主要母质发育的２３个农田土壤耕层样本，其中水田土壤１６个，旱地土壤７个．将土壤氮分为七级．即交换性ＮＨ４＋十ＮＯ３－，水解性ＮＨ４＋，氨基糖氮，可溶性碱稳定态氮，酸溶性腐殖质态氮，固定态ＮＨ４＋，难溶性腐殖质态氮。分析结果表明，土壤中交换性ＮＨ４＋十ＮＯ３－的含量为２２．０土９．０ｍｇ／ｋｇ，占全氮的１．７土０．７％；水解性ＮＨ４＋为３２４．４土１０９．５ｍｇ／ｋｇ，占全氮的２３．９±５．６％；氨基糖氮为１１８．９土４３．０ｍｇ／ｋｇ，占全氮的９．１土３．２％；可溶性碱稳定态氮为４９７．１土２０５．８ｍｇ／ｋｇ，占全氮的３６．２土８．３％；酸溶性腐殖质态氮为２９．２土１０．２ｍｇ／ｋｇ，占全氮的１３土０．８％；固定态ＮＨ４＋为４７．２土２４．３ｍｇ／ｋｇ，占全氮的３．６±１．７％；难溶性腐殖质态氮为３４１．３土２７０．８ｍｇ／ｋｇ，占全氮的２２．２土１１．６％。     

PCDDs在氯仿溶液中的紫外光解

使用ＮＤＣ－３型化学反应仪、３００Ｗ汞灯和１５ｍｌ反应管，于４３℃进行了２，３，７，８－ＴＣＤＤ，１，２，３，７，８－Ｐ５ＣＤＤ，１，２，３，４，７，８－ＨｘＣＤＤ，１，２，３，４，６，７，８－ＨｐＣＤＤ和ＯＣＤＤ在氯仿溶中的紫外光解，其一级反应速率常数测得值依次为０．５４，０．２９，０．１５，０．１５和０．１９ｍｉｎ＾－１，反应半衰期ｔ１／２均在５ｍｉｎ以内，还原脱氯是主要的光解途径，并有大量低     

桂东南地区马尾松工程幼林郁闭过程的生态环境变化特征

１９９１ ～１９９６ 年,对桂东南马尾松工程幼林郁闭过程的生态环境变化进行定位观测研究．结果表明：①１ ～３ ａ 林地与灌草坡的主要气象要素无多大差别,４ ａ 后,林地逐渐显示增湿降温等良好的小气候环境,至ａ６ 基本恢复到成熟林的水平．②１～６ ａ 林地的水土流失量为３３８．５９～２１３６．９２ｔｈｍ －２ａ－１ ,径流系数２ ．１４％ ～２１．５０％ ,比灌草坡减少１２．５ ％ ～２９．４％ ,其中１ ～３ ａ 林的泥沙流失量比灌草坡增大１１２．９％ ～２１４．５ ％ ,４ ａ 后,林地泥沙流失量逐渐减少,至６ ａ 林时比灌草坡减少１８．２％ ．③６ ａ 林时的土壤物理性质比造林前有所改善,但土壤的主要养分（ 有机质、Ｎ、Ｐ、Ｋ）含量则比造林前降低４．３％ ～７．０％ ．④６ ａ 林的林木蓄积量为３６．１６ ｍ３／ｈｍ２ ,产出与投入的比值为２ ．９９ ,经济效益极为显著．     

不同菌源的微生物对邻苯二甲酸二甲酯生物降解性的比较

从处理石化厂废水的活性污泥中分离出１ 株邻苯二甲酸酯降解菌 Ｆ Ｓ１（ 荧光假单胞菌 Ｐｓｅｕｄｏｍｏｎａｓｆｌｕｏｒｅｓｃｅｎｓ Ｆ Ｓ１） ,从处理焦化厂废水的活性污泥中分离出２ 株邻苯二甲酸酯降解菌 Ｆ Ｓ２（ 铜绿假单胞菌 Ｐｓｅｕｄｏｍｏｎａｓａｅｒｕｇｉｎａｓａ Ｆ Ｓ２） 和 Ｆ Ｓ３（ 短杆菌 Ｂｒｅｖｉｂａｃｔｅｒｉｕｍ ｓｐ ． Ｆ Ｓ３） ． 研究了邻苯二甲酸酯降解菌 Ｆ Ｓ１ , Ｆ Ｓ２ 和 Ｆ Ｓ３ 对邻苯二甲酸二甲酯（ Ｄ Ｍ Ｐ） 的最适降解条件,比较了其降解特性． Ｆ Ｓ１ 、 Ｆ Ｓ２ 和 Ｆ Ｓ３ 最适酸度分别为ｐ Ｈ６ ．５ ～８ ．０ 、ｐ Ｈ７ ．０ ～８ ．０ 和ｐ Ｈ７ ．０ ～８ ．０ ,温度为２０ ～３５ ℃、１５ ～３５ ℃和１５ ～３５ ℃．邻苯二甲酸酯降解菌 Ｆ Ｓ１ 、 Ｆ Ｓ２ 和 Ｆ Ｓ３ 对邻苯二甲酸二甲酯的降解的半寿期： Ｆ Ｓ１ ＜ Ｆ Ｓ２ ＜ Ｆ Ｓ３ ,邻苯二甲酸酯降解菌 Ｆ Ｓ１ 是一株高效的邻苯二甲酸二甲酯降解菌     

流动注射荧光分析法用于土壤及水系沉积物中铈（Ⅲ）含量的测定

研究表明Ｃｅ＾３＋在ｐＨ〈６．２ＫＣｌ介质中以２５４．０ｎｍ紫外光激发时，在３５２．０ｎｍ处发出具有恒定强度的荧光。因而可选择ｐＨ５－６作为测定酸度条件，利用Ａｌ２（ＳＯ４）３消除Ｆｅ＾３＋等离子的干扰，建立起Ｃｅ＾３＋的流动注射荧光分析法。方法的线性范围是２．０×１０＾－７—２．０×１０＾－６ｍｏｌ／ｌ，一元回归方程△Ｆ＝６６３６００Ｃ－０．０４１（ｎ＝１０，ｒ＝０．９９９７），检测限６．０×１     

四川不同海拔豆地生态及大豆生长发育变化研究

对φ（Ｎ）３２°１４′～３２°５６′,λ（Ｅ）１０４°３６′～１０４°５１′范围内海拔（ｈａｌｔ）４００ ～１ ４００ ｍ 豆地小气候观测结果表明：ｈａｌｔ每升高１００ ｍ ,平均气温递减０．７２ ℃;年降雨量递增６３．０ ｍｍ（４００～６００ ｍ） ～１０６．８ ｍｍ（８００ ～１ ４００ ｍ）;相对湿度递增１％ ;日照时数呈抛物线上升变化． ｈａｌｔ４００ ｍ 日均温稳定通过１２．０ ℃的初期为３ 月中旬,ｈａｌｔ每升高１００ ｍ ,该时间延迟５～７ ｄ． 不同ｈａｌｔ＞１２℃的有效积温分别为３６２１．２ ℃（４００ ｍ）;３ ２４５ ．０ ℃（６００ ｍ）;３ １４９．９ ℃（８００ ｍ） ;２ ８０４ ．８ ℃（１ ０００ ｍ） ;２０８２．１ ℃（１２００ ｍ）;１ ９５０．１ ℃（１ ４００ ｍ） ． 在相对较高的海拔,存在明显的逆温和南北坡效应,相应存在大豆局部高产区． 不同海拔豆地生态及大豆生长发育变化研究结果可为四川不同海拔区大豆品种合理布局和应用高产优质栽培技术提供了理论依据．     

链霉菌碱性脂肪酶的研究

从杭州土壤中获得的一支链霉菌,通过ＵＶ、ＤＥＳ和Ｃｏ６０ － γ射线的５ 代诱变,选育成功了高产的Ｚ９４－ ２ 菌株,经过对Ｚ９４ －２ 的发酵研究,产碱性脂肪酶活力达５９６ ｕｍＬ,其最适培养基（λｕ Ｌ－１） 为：糊精１０、黄豆饼粉３０、尿素１０ 、Ｋ２ＨＰＯ４０ ．５、ＭｇＳＯ４·７Ｈ２Ｏ０ ．５、ＮａＣｌ１ 和ＡＥＯ９ ０．５ ,产酶的最适条件为：初始ｐＨ９．０～１０．０ ,２６℃培养４８ ｈ．对Ｚ９４－ ２ 与其他菌株的碱性脂肪酶的特性作了比较     

具脂肪酶和酯酶活性酵母菌的选育和酶学性质初步研究

从济南市区得到的含油土壤中筛选得到一株酵母Ｓ９ 菌株,它可以同时产生较高酶活的脂肪酶和酯酶．对影响Ｓ９ 产脂肪酶和酯酶的各种因素进行了研究,确定２ ％ 的黄豆粉为最佳氮源,１ ％ 的可溶性淀粉为最佳碳源,最适的初始培养ｐＨ和温度分别为ｐＨ６ ．５ 和２８℃,另外不同的表面活性剂对产酶也有不同的影响．对Ｓ９脂肪酶和酯酶的各种酶学性质进行的研究表明,脂肪酶和酯酶的最适作用温度都为３０℃,最适作用ｐＨ 分别为７ ．０ 和８．０,两者都属于常温酶,在３０℃～４０ ℃范围内比较稳定,前者在中性偏碱的ｐＨ 环境中比较稳定,后者属于碱性酶,在ｐＨ７ ．５～１０ ．５ 范围内相当稳定．     

玉米地氮肥释放N_2O的研究

测定了３种施氮肥处理的玉米地Ｎ＿２Ｏ的排放通量，计算了氮肥以Ｎ＿２Ｏ形式排放成的氮损失率。在玉米生长期内，对照田、施化肥田和施混合肥田排放Ｎ＿２Ｏ通量分别是８．５±２．２、１８．９±１１．７和１５．４±５．９μｇＮ／ｍ￣２·ｈ，尿素和有机肥释放出的Ｎ＿２Ｏ占其相应施肥量的０．１９％和０．１２％。     

土壤中结合态苯氧羧酸类除草剂的测定

利用超临界ＣＯ２流体萃取的方法提取２甲４氯(ＭＣＰＡ),２,４－Ｄ和除草醚在三种土壤中的结合残留．结果表明,在培养２００ｄ的时间内,ＭＣＰＡ的结合残留量为１．０ｌ－５．１２ｍｇ·ｋｇ－１,占添加总量的２．０－１０．１%;２,４－Ｄ的结合残留量为０．２４－２．６５ｍｇ·ｋｇ－１,占添加总量的０．５－５．３%;除草醚的结合残留量为６．５３－１９．３０ｍｇ·ｋｇ－１,占添加总邑的１２．９—３８．２%．农药结合态与游离态含量的比值随时间的延长而增加．     

Nitrogen availability in relation to vegetation changes resulting from grass encroachment in Dutch dry dunes

The encroachment of some tall grass species in open dune vegetation, as observed in a Dutch dry dune area, is considered unfavourable from a conservation viewpoint. This paper investigates differences in vegetation and soil properties between grass-dominated and still existing open dune grassland plots at four locations along the coast. Soil properties studied include nitrogen and phosphorus pools and nitrogen availability by mineralization. Vegetation properties included are above and below-ground biomass and nitrogen and phosphorus concentrations in above-ground biomass. Systematic differences in N-pools between grass-dominated and open dune grassland plots were not observed. However, N-availability by mineralization and its turnover rates are higher in grass-dominated plots than in open dune grassland plots, as well as above and below-ground biomass. In open dune grassland plots, atmospheric N-input is an important source of N, whereas in grass-dominated plots mineralization largely exceeds atmospheric N-input. However, these observations do not explain the mosaic-like vegetation pattern. Grazing intensity is most likely the determinant factor in the dry dune system. It is concluded, that grass encroachment is probably triggered by atmospheric deposition and is enhanced by positive feedbacks in the N-cycle. The relevance of these results for restoration management is briefly discussed.     

不同载畜率对短花针茅荒漠草原土壤呼吸的影响

草地是我国最大的陆地生态系统,土壤呼吸是草地碳循环研究的重要内容,是土壤碳库输出的主要方式,影响大气中CO2浓度变化。放牧是草地主要利用方式之一,通过动物采食和践踏,改变植被冠层结构,对土壤理化性质、土壤有机质和土壤微生物产生影响,进而改变土壤呼吸速率。为探究不同载畜率对短花针茅（Stipa breviflora）荒漠草原土壤呼吸速率的影响,2011—2012年用Li-8100开路式碳通量测定系统,对生长季内（6—10月）4个不同载畜率处理下的土壤呼吸进行测定,测定周期为2周1次。辅助测定地下10 cm的土壤温度及土壤湿度,并分析土壤呼吸与土壤温、湿度的关系。结果表明：1）2011年不同载畜率对土壤呼吸速率无显著影响,表现为对照〉中度放牧〉轻度放牧〉重度放牧的变化趋势。2012年与对照（1.6μmol·m-2·s-1）相比,重度放牧（1.07μmol·m-2·s-1）显著降低土壤呼吸速率。总体而言,2011年土壤呼吸速率低于2012年,但差异不显著。2011年土壤温度（20.73℃）显著高于2012年（14.38℃）,不同处理间无显著差异,重度放牧区偏高。2012年土壤湿度（7.24%）显著高于2011年（4.11%）,对2年数据整体分析发现,轻度放牧区土壤湿度显著低于对照和中度放牧。2011年土壤湿度变化趋势为中度放牧〉对照〉重度放牧〉轻度放牧。2012年,轻度放牧土壤湿度最小,各处理间差异不显著。2）2011年,土壤呼吸与土壤温度月动态无明显规律,与土壤湿度呈现相反的变化趋势。2012年土壤呼吸的月动态与土壤温、湿度变化趋势相似。3）2011年,土壤呼吸速率随温度升高出现波动,与土壤湿度呈负相关。2012年,土壤呼吸速率随土壤温、湿度升高而增大。在干旱年份,降水减少会掩盖放牧对土壤呼吸的影响;在降雨较多的年份,重度放牧显著降低土壤呼吸速率。     

天然草地利用方式改变对土壤排放CO2 和吸收CH4的影响

1997年～ 1998年在内蒙古达拉特旗中国农业科学院草原研究所草原生态试验站对天然草地、天然草地转变为人工草地、玉米和土豆地后 ,土壤 CO2 排放和 CH4 吸收通量进行了测定。天然草地、人工草地和旱地农田均为大气中甲烷的吸收汇 ,天然草地转变为农田后 ,增强了土壤的 CO2 排放量 ,减少了土壤对大气中甲烷的吸收。天然草地和玉米地的 CO2 排放通量与 5cm处土壤温度呈线性相关 ,土壤对甲烷的吸收率与土壤含水量呈线性负相关 ,与土壤温度没有相关关系     

Field measurements of soil CO2 efflux in Heteropogon contortus dominated grassland of semi-arid eco-system

Seasonal changes in soil respiration (SR), soil temperature (ST) and soil moisture (SM) were compared between a barren land with no vegetation (control) and grassland dominated by Heteropogon contortus (L.) of a semi-arid eco-system during 2005-2006. A statistically significant (p<0.001) seasonal change in SR was observed between the two sites. The variation characteristics of soil CO2 effiux rates were observed during wet periods along precipitation gradients and it was consistently higher in grasslands than in control.A maximum soil CO2 efflux of 13.35 +/- 0.33 micromol m2 s-1 in grassland and 7.33 +/- 0.8 micromol m2 s- in control was observed during rainy season-ll, i.e., from October to December, a minimum of 1.27 +/- 0.2 micromol m-2 s-1 in grassland and 0.67 +/- 0.5 micromol m-2 s-1 in control during summer season, i.e., from March to June. A positive significant relation observed between soil respiration and soil moisture (r2above 0.8) and no significant relation was observed between soil CO2 efflux and soil temperature (r2 below 0.3). In water-limited semi-arid ecosystem, rewetting of the soil due to precipitation events triggered the increased pulses of soil respiration especially in grassland when compared to the barren land. The observed soil respiration rates during summer and after the subsequent precipitation events strongly indicated that the soil water-deficit conditions reduce the efflux both in barren land (control) and in grassland of semi-arid eco-system.     

高寒草甸不同植被类型土壤全氮含量变化动态分析

采用凯氏定氮法对高寒草甸不同植被类型土壤全氮进行季节动态测定分析,结果表明:在整个生长季中0～20 cm层土壤全氮质量分数的顺序为:藏嵩草沼泽化草甸(Kobresia-swamp meadow)>露梅灌丛草甸(Dasiphoru fruticosa shrubs)>人工燕麦草地(Avena sativa artficial grassland)>矮嵩草草甸(Kobresia humilis meadow)>矮嵩草退化草地(Kobresia humilis-degraded grassland).原生植被草甸类型下单位面积土壤全氮含量远高于退化草地.藏嵩草沼泽化草甸土壤每平方米的全氮含量最高,达到0.712 kg,金露梅草甸次之,两者之间差异性不显著(p>0.05);其他三种草地类型单位面积土壤全氮含量差异性显著(p<0.05);原生草甸矮嵩草草甸每平方米全氮平均含量为0.406 kg,而退化的矮嵩草草地每平方米全氮平均含量为0.301 kg,可以推算,土地退化导致土壤全氮流失的量为0.105kg,即高寒草地退化导致25.86%氮流失.随着季节的变化,土壤全氮质量分数随生长季均有所增加,最高值都出现在8月份,但各月份之间土壤全氮质量分数变化差异性不显著(p>0.05).原生植被0～10 cm层土壤全氮含量高于10～2O cm层,人工草地与退化草地差异性不显著.     

重庆金佛山岩溶区不同植被条件下土壤-植被系统CO2浓度日变化

对重庆金佛山典型岩溶区林地、裸地表层岩溶生态系统CO2浓度进行短时间尺度变化的野外观测结果表明,林地与裸地不同深处土温变化幅度由地表向土壤深部逐步降低,裸地地表温度和不同深度土温波动幅度均较林地大.林地与裸地各层次土壤CO2浓度变化与土温呈较好的相关关系.林地各层土壤CO2浓度波动微弱,变幅小于裸地.林地与裸地土层中CO2浓度随土层深度增加而增高.植被各层的温度和温度变化幅度从大到小依次为林层、灌层和草层.林层温度最大值滞后于气温约3 h.     

Simulation of soil carbon changes due to land use change in urban areas in China

Land use change can have a strong impact on soil carbon dynamics and carbon stocks in urban areas. Due to rapid urbanization, large areas of land have been paved, and other areas have undergone rapid land use change. Evaluation of the impact of urbanization on carbon dynamics and carbon stock (30 cm) has become an issue of urgent concern. The soil carbon dynamics, due to rapid land use change in Tianjin Binhai New Area of China, have been simulated in this paper using the RothC model. Because this area is saline, a modified version of RothC that includes a salt rate modifier provided more accurate simulations than the original model. The conversion to urban green land was not accurately simulated by either of the models because of the undefined changes in soil and plant conditions. According to the model, changes of arable to grassland resulted in a decline in soil carbon stocks, and changes of grassland to forest and grassland to arable resulted in increased soil carbon stocks in this area. Across the whole area simulated, the total carbon stocks in 2010 had decreased due to land use change by 6.5% from the 1979 value. By 2050, a further decrease of 21.9% is expected according to the 2050 plan for land use and the continuing losses from the soils due to previous land use changes.     

A model of rainfall redistribution in terraced sandy grassland landscapes

A simple model of rainfall redistribution within a terraced sandy grassland landscape has been developed. The model assumes that rainfall redistribution is driven by rainfall impulses and is controlled by characteristic field capacity of soils. When the rainfall intensity is large enough to render soil water content greater than its characteristic field capacity, the excessive soil water can drain very quickly by means of large amounts of non-capillary pores of sandy soils or by means of surface runoff. Exponential distribution of rainfall impulses was assumed and tested with measured daily rainfall at two meteorological stations in the sandy grassland area of north China. The model was solved to give the equivalent rainfall at each terrace in the landscape.     

Effects of Habitat Area on the Distribution of Grassland Birds in Maine

We used multiple and logistic regression analysis to study the breeding-area requirements of 10 species of grassland and early-successional birds at 90 grassland-barren sites in Maine. The incidence of six of the species was clearly sensitive to the area of grassland. Upland Sandpipers, the species with the largest area requirements, were infrequent at sites of less than 50 ha and reached 50% incidence at those of about 200 ha. Grasshopper Sparrows reached 50% incidence at about 100 ha, Vesper Sparrows at about 20 ha, and Savannah Sparrows at about 10 ha. Incidence for three edge species, Brown Thrasher, Common Yellowthroat, and Song Sparrow, was negatively correlated with open area, and incidence for Field Sparrows was not strongly influenced by grassland size. These results indicate that grasslands need to be approximately 200 ha in area if they are to be likely to support a diverse grass land bird fauna. However, large grasslands or grassland-barrens are rare; random samples indicated that in Maine only 1% of hayfields and only 8% of grassland-barrens were more than 64 ha in area. Conservation efforts seeking to protect habitat for rare grassland birds need to consider sites of at least 100 ha—and preferably 200 ha—in size, and these are notably rare in Maine and probably throughout New England and eastern North America. Airports provide some of the last extensive patches of grassland habitat in the northeast. To maintain viable populations of area-sensitive grassland birds, management of these sites for nesting birds will become increasingly important.     

贵州喀斯特地区不同土地利用方式土壤CO_2体积分数变化及影响因素

为了解不同土地利用方式对土壤剖面CO2体积分数的影响,采用气相色谱法对贵州喀斯特地区土壤不同深度空气CO2体积分数进行观测。结果表明：不同土地利用对土壤平均CO2体积分数影响较大,其次序为：次生林（0.35%±0.06%）〉草地（0.34%±0.05%）〉人工林（0.27%±0.03%）〉农田（0.16%±0.03%）。次生林、草地与农田之间土壤CO2体积分数差异性显著,而人工林与农田之间无显著性差异。不同土地利用方式土壤剖面CO2体积分数的时空变化特征比较一致：从春季到夏季逐渐增加而从秋季到冬季又逐渐降低,与该区域的温度和降雨量变化趋势一致。同时随着土壤剖面深度增加CO2体积分数逐渐增大,但在土层12 cm处有突然降低现象（农田除外）。不同土地利用方式土壤空气CO2体积分数变化与大气、土壤温度密切相关（r=0.602~0.886,P〈0.05）,土壤温度升高会导致土壤CO2体积分数上升。土壤湿度虽然也在一定程度上影响了剖面CO2体积分数,但相关性分析表明二者之间并不显著（r=0.105~0.393,P〉0.05）,说明在贵州喀斯特地区,土壤温度对土壤空气CO2体积分数的影响大于土壤湿度。