采煤沉陷区人工林地土壤肥力质量的空间特征

以焦作市韩王矿沉陷区林地土壤为研究对象，测定不同沉陷部位和不同深度土壤中8项肥力指标，基于隶属度函数和灰色关联度分析法，对沉陷区土壤肥力质量进行评价。结果表明：沉陷区林地土壤硝氮、全氮、速效钾、全钾和有机质含量在不同层位之间存在显著性差异（P＜0.05），上层（0 cm～20 cm）硝氮、速效钾和有机质含量显著高于下层（20 cm～40 cm）；土壤肥力质量在空间上呈现出明显的变化特征，坡中处最高，坡底处最低；速效磷是影响沉陷区土壤肥力质量提升的限制性因子。     

生物炭基缓释肥的制备及其对土壤理化性质的影响

通过淋溶试验分析生物炭热解温度、生物炭与尿素比例、粘结剂含量对生物炭基缓释肥缓释性能的影响，采用土壤培育试验研究生物炭基缓释肥对土壤理化性质的影响。结果表明，600 ℃下热解而成的生物炭缓释性能优于300 ℃下热解形成的生物炭；生物炭添加比例和粘结剂含量的增加能提升生物炭基缓释肥的缓释性能；生物炭基缓释肥的加入可降低培育土壤的容重，增大土壤的饱和导水率，提高土壤pH值和土壤有机质含量。     

不同材料复合添加对土壤铬形态的影响

以铬污染黄壤为研究对象,选择有机材料（泥炭）、pH值调节剂（沸石）、生物炭（鸡粪）3种不同种类的土壤重金属污染改良剂,采用正交试验L9（34）设计和室内盆栽试验,考察不同复合材料组对土壤中重金属铬形态、pH值、有机质含量的影响。结果表明：沸石的添加提高了土壤pH值、有机质含量,增加了土壤可还原态、可氧化态铬含量;鸡粪的添加通过提高土壤pH值从而增加土壤可还原态铬的含量;泥炭的添加提高了土壤有机质含量、土壤可氧化态铬含量,降低了土壤可交换态铬含量。     

水环境背景元素的时间差异变化规律

研究化学元素在枯、丰、平三个水季悬浮态、可溶态、沉积态的含量变化。以黄梨树水文站作为动态观测点，三年观测得出水化学要素、重金属元素及稀有、稀土元素变化最大的是丰水季；悬浮体相当于枯水季的２５０倍；悬浮态和可溶态元素含量（原水）同样形成丰水季＞平水季＞枯水季的趋势；而可溶态元素含量（过滤水）各个水期无大的变化差异。沉积物在三个水季中元素含量变化差异也较小，但有机质相反，含量出现枯水季＞平水季＞丰水季这样的规律。     

BDE-47在土壤矿物质与有机质上的吸附解吸特征

以多溴联苯醚典型单体2，2′，4，4′?四溴联苯醚（BDE?47）为研究对象，阐明了其在土壤矿物质与有机质上的吸附解吸行为及特征。结果表明：土壤中无机矿物质对BDE?47的吸附贡献不大，而有机质是调控BDE?47在土壤中吸附行为的关键组分；有机质对BDE?47的吸附能力与其有机碳含量和物理化学特性相关；BDE?47在腐殖酸上的解吸存在显著的滞后现象。     

铅锌矿区土壤微生物区系及酶活性调查

通过对四川省汉源县富泉乡万顺铅锌矿区土壤微生物区系及微生物活性的调查，结果表明，铅锌矿区土壤几种重金属含量明显高于临近非矿区土壤。该矿区土壤微生物区系组成和微生物活性显著不同于临近非矿区土壤，随着重金属含量的增加，土壤微生物数量、微生物多样性指数、微生物生物量碳以及纤维素分解强度均显著降低，但土壤基础呼吸却明显升高；土壤脲酶、碱性磷酸酶、多酚氧化酶对铅锌矿较为敏感，而蔗糖酶和过氧化氢酶受到的抑制作用不明显。     

富蕴县耕地土壤环境质量现状

通过在富蕴县建立测土配方施肥示范点，开展了耕地土壤环境质量的调查，结果表明：在富蕴县不同地貌部位0 cm~20 cm耕层土壤中，土壤常量元素的分布与微量元素相比差异较大；在山区土壤中，常量元素与微量元素的含量较高，而在戈壁沙漠地带，土壤中常、微量元素的含量均表现为最低水平；土壤pH值为7.5~8.5，适合作物生长；土壤耕层盐分含量相对较低，仅表现为轻盐化土壤类型，占总耕地面积的12.52%。     

磨盘山水库溶解性有机质光谱特性及来源分析

结合紫外可见吸收光谱与三维荧光光谱法，利用平行因子分析方法研究哈尔滨市磨盘山水库水体中的溶解性有机质（DOM）。结果表明，水体DOM吸收系数α355平均值为（4.71±0.66）m-1，表明水库中有色溶解性有机质（CDOM）较高；水库水体DOM存在3个荧光组分，分别为类腐殖质C1（345 nm、440 nm）、类腐殖质C2（285 nm、405 nm）和类富里酸组分C3（275 nm、475 nm）；C1、C3呈现显著的正相关性，自生源指数与C1呈显著的负相关性；类腐殖质的荧光强度在深层水体中逐渐增加，且深层水体的腐殖化程度较高，较为稳定；水库中心水体中DOM的自生源特征较其他区域明显，浮游植物和细菌的有机体降解产物增加。     

污水处理厂微生物生态分布初

通过对望塘污水处理厂的细格栅、厌氧池、曝气池、二沉池周边土壤及空气微生物测定，分析微生物分布状况，得知污水处理厂不同功能区域土壤和空气微生物含量随污水处理工艺的进行呈降低趋势。土壤和微生物鉴定结果表明，厂区土壤中微生物与普通土壤无明显差异，而空气微生物中含多种致病菌，形成的微生物气溶胶威胁人类健康。     

贵州东部某燃煤电厂汞排放对周边环境空气及土壤的影响

结合当地气象条件,测定贵州省东部某燃煤电厂下风向环境空气汞浓度分布情况,同时测定该燃煤电厂周边表层土壤中汞含量,并对其污染程度进行评价,探讨了土壤汞与理化性质间的相关性。结果表明,该燃煤电厂下风向环境空气汞浓度远高于北半球大气气态总汞背景值,空气汞浓度在2.7 km范围内随距离的增大而增大,在2.7~5.0 km范围内汞浓度随距离的增大而减小。电厂周边表层土壤汞含量是贵州省A层土壤Hg背景值的8.5倍,存在中度到重度程度的污染,土壤Hg与土壤pH呈正相关性,但与土壤有机质未表现出相关性。     

Saturated hydraulic conductivity of soils in the Horqin Sand Land of Inner Mongolia, northern China

Water is a limiting factor to plant growth in Horqin Sand Land of China. Knowledge of soil saturated hydraulic conductivity (K _sat) is of importance because K _sat influences soil evaporation and water cycling at various scales. In order to analyze the variation of K _sat along with sand types and soil depths, and its relationship with soil physiochemical properties, six typical lands were chosen, including mobile dune, fixed dune, pine woodland, poplar woodland, grassland, and cropland, and K _sat was measured in situ by Guelph Permeameter at each type of land. Soil bulk density, organic matter content, and soil particle size distribution were determined in parallel with K _sat measurement. The results showed that (1) The averaged K _sat was decreased in the order: mobile dune > fixed dune > pine woodland > poplar woodland > grassland > cropland; changes in K _sat varied considerably as soil depth increased, e.g., the changes of K _sat along with soil depth in fixed dune was fitted by exponential model, but it was fitted by parabola model in the pine woodland and grassland. (2) The K _sat values of fixed dune and mobile dune were varied considerably among three slope positions (dune top, windward slope, and leeward slope). (3) The relationships of K _sat and soil physiochemical property revealed that soil bulk density, organic matter content, and coarse sand fraction (2～0.1 mm) were the key factors affecting K _sat in Horqin Sand Land. Compared with clay and silt content proportion, sand fraction in this region showed a more significant positive correlation with K _sat.     

The effects of land use changes on some soil properties in İndağı Mountain Pass – Çankırı, Turkey

Understanding spatial variability of dynamic soil attributes provides information for suitably using land and avoiding environmental degradation. In this paper, we examined five neighboring land use types in Indagi Mountain Pass - Cankiri, Turkey to spatially predict variability of the soil organic carbon (SOC), bulk density (BD), textural composition, and soil reaction (pH) as affected by land use changes. Plantation, recreational land, and cropland were the lands converted from the woodland and grassland which were original lands in the study area. Total of 578 disturbed and undisturbed soil samples were taken with irregular intervals from five sites and represented the depths of 0-10 and 10-20 cm. Soil pH and BD had the lower coefficient of variations (CV) while SOC had the highest value for topsoil. Clay content showed greater CV than silt and sand contents. The geostatistics indicated that the soil properties examined were spatially dependent to the different degrees and interpolations using kriging showed the dynamic relationships between soil properties and land use types. The topsoil spatial distribution of SOC highly reflected the changes in the land use types, and kriging anticipated significant decreases of SOC in the recreational land and cropland. Accordingly, BD varied depending on the land use types, and also, the topsoil spatial distribution of BD differed significantly from that of the subsoil. Generally, BD greatly decreased in places where the SOC was relatively higher except in the grassland where overgrazing was the more important factor than SOC to determine BD. The topsoil spatial distributions of clay, silt, and sand contents were rather similar to those of the subsoil. The cropland and grassland were located on the very fine textured soils whereas the woodland and plantation were on the coarse textured soils. Although it was observed a clear pattern for the spatial distributions of the clay and sand changing with land uses, this was not the case for the silt content, which was attributed to the differences of dynamic erosional processes in the area. The spatial distribution of the soil pH agreed with that of the clay content. Soils of the cropland and grassland with higher amounts of clay characteristically binding more cations and having higher buffering capacities had the greater pH values when compared to the soils of other land uses with higher amounts of sand naturally inclined to be washed from the base cations by the rainwater.     

基于遥感和GIS的四川省草地动态变化分析

利用地理信息系统技术,在空间数据库平台的支持下,对四川省20世纪90年代中期到2000年间的草地动态变化特征、草地动态变化的背景特征及其空间分布特征进行了分析。研究表明,净增草地部分主要来源于耕地,净减草地部分的主要去向是林地。总体上,净增草地面积3812公顷,净增草地部分主要是在轻度土壤侵蚀区、中度土壤侵蚀区、剧烈土壤侵蚀区和强度土壤侵蚀区,坡度等级5、6和1的区域,环境等级5、6、4和1的区域;净减草地部分主要是在微度土壤侵蚀区和极强土壤侵蚀区,坡度等级3、2和4的区域,环境质量等级7和8的区域。净增草地的区域为川西北高原、丘陵和川西南山区,净增草地面积的前四个地州市是遂宁市、泸州市、巴中地区和广安市,净减少草地的区域为盆周山地和平原,净减少草地面积的前四个地州市是广元市、绵阳市、达川市和宜宾市。     

呼伦贝尔地区草原表层土壤中总有机碳与有机质初探

通过非分散红外线吸收法测定呼伦贝尔地区具有代表性的16个草原表层土壤(0~20 cm)中总有机碳、溶解性有机碳,使用重铬酸钾容量法测定有机质,并对其总有机碳与有机质水平及两者相关性进行了分析。初步分析了造成各样品之间总有机碳水平差异的原因。结果表明,只以打草场作为利用方式的土壤总有机碳含量较常年放牧场的总有机碳含量高。从草原类型和土壤类型上看,草甸草原总有机碳含量明显高于典型草原,黑钙土总有机碳含量明显高于栗钙土。综上,过度放牧会使草原土壤总有机碳大量释放。总有机碳含量与有机质含量有显著正相关性,相关系数达到0.902。     

Effect of the behavior and availability of heavy metals on the characteristics of the coastal soils developed from alluvial deposits

An investigation of the behavior and availability of heavy metals (HMs), i.e., Cu, Zn, Ni, Pb, Cr, and Cd, based on the analysis of correlation between HMs and physical and chemical properties of coastal soils developed from alluvial deposits in Shanghai, China, has been conducted, in order to reveal the effect of the soil formation and development and the unsuited human activities on the activities and mobility of HMs in agricultural soils. The results showed that (1) the soils still meet the needs of plant growth due to the moderate fertility with a soil texture of silty loam although the content of organic matters is lower, (2) total heavy metal content had a increase trend from the inland area to the coastal area, indicating the impact of alluvial deposits related to the soil formation on the distribution of HMs; (3) a significant positive correlation was found between HMs and some soil properties (i.e., clay content, cation exchange capacity, organic matters, total Phosphorous content, etc.), indicating that the regulation of these properties could give some great effect on the behavior and availability of HMs; (4) the positive correlation among Cu, Zn, Ni, and Cd, and between Pb and Cr is very significant, suggesting the most similar, if not the same, origins of HMs; These findings are helpful to the soil remediation, fertility adjustment, and plant cultivation.     

The effect of visitors’ pressure on the spatial variability of sandy soil in an urban parks in Tel Aviv

The effect of visitors' pressure on the spatial variability of soil properties was investigated in three open green areas in Tel Aviv. Six types of micro-environments were chosen: under oak and pine tree canopy with low (OL and PL) and high (OH and PH) visitors' pressure; herbaceous area without visitors' pressure (HE); and resting area under high visitors' pressure (RA). For each micro-environment soil samples were collected from the upper 0-5 cm depth for organic matter content and moisture determination. Before sampling, soil surface compaction and litter biomass were measured. Soil properties were affected by visitors' pressure and by the type of micro-environment. Soil organic matter content and soil moisture proved significantly higher under oak trees at low visitors' pressure. Average litter biomass significantly decreased with increasing visitors' pressure in the tree micro-environments. Average penetration depth decreased significantly with increased visitors' pressure in all micro-environments. In all the cases where averages significantly decreased, variance significantly decreased too, but the coefficient of variations increased. This means that variances changed slower than averages. Changes in averages were accompanied by a change of data population structure, which indicated more soil spatial homogeneity under high visitors' pressure. The data from different intervals of data population of soil properties demonstrated the different sensitivity to visitors' pressure.     

上海地区土壤碳汇功能评估

利用上海市第二次土壤普查资料，2004年-2005年上海耕地地力调查资料，以及2009年实地调查采样、实验分析获得的数据，研究了3个时期上海土壤有机碳的变化特征。结果表明，20多年：来上海土壤有机碳平均含量没有明显变化，土壤有机碳库逐渐减小，从而使得上海城市化过程中土壤成为一种碳源，而不是碳汇。城市郊区以扩大蔬菜、果树、苗木种植为特征的旱地作物种植方式代替水稻田，是城市化影响土地利用类型变化的明显特征，而水稻田土壤有机碳含量高于林地、菜地。种植结构的变化对土壤有机碳含量有重要影响，同时，耕作制度、耕作方式、施肥等农业管理方式也有一定影响。虽然园林绿地得到快速发展，但没有弥补城市化过程导致农田面积减少带来的有机碳损失。     

黑臭河道底泥特征分析及处理工艺筛选

以深圳市前海片区代表性河道黑臭底泥为研究对象,对其p H值、含水率、有机质、氮磷含量、重金属含量及粒径进行分析。结果表明,黑臭底泥主要为呈碱性的无机砂质成分,有机质含量低,重金属含量虽高但分布稳定。根据其特性,最终确定其主要处置方式为疏浚后机械脱水。     

Effects of treated sewage sludge levels on temporal variations of some soil properties of a Typic Xerofluvent soil in Menemen Plain, Western Anatolia, Turkey

The aim of this study is to determine effects of treated sewage sludge (TSS) levels as an organic matter (OM) resource on temporal variations of some soil properties of a Typic Xerofluvent soil. The experiment was conducted in Menemen Plain, in the Western Anatolia Region of Turkey (latitudes 38 degrees 34'48.22'-38 degrees 34'49.24' N; longitudes 27 degrees 1'23.05-27 degrees 1'24.14' E) in the years of 2003 and 2004. Moist TSS was added to the soil at the rates of 0, 30, 60 and 90 t ha(-1) on May 1, 2003. Peanut (Arachis hypogaea) was planted as first crop. On the other hand, mixture of green barley (Hordeum vulgare) and common vetch (Vicia sativa L.) was planted as second crop. During the experiment, soil samples were taken in five different periods (1st, June 18, 2003; 2nd, November 13, 2003; 3rd, April 30, 2004; 4th, October 10, 2004 and 5th, May 12, 2004). The results showed that increasing TSS application to Typic Xerofluvent soil was significantly increased total salt, OM, total porosity, micro porosity, macro porosity, field capacity, wilting point, available water content, structure stability index and aggregation percentage values of soil when compared with control. Meanwhile, particle density, dry bulk density and nonaggregated silt + clay values of soil decreased. On the other hand, soil reaction (pH), lime content and total silt + clay values of soil did not significantly change. In the course of time, depending on decomposing of TSS organic materials in soil, effect of TSS levels on soil properties decreased particularly in the last periods. For this reason, it can be recommended that 90 t ha(-1) moist TSS can be added once in 2 years for improving soil properties of Typic Xerofluvent soil, which are characterized by low OM content.     

Visualising the equilibrium distribution and mobility of organic contaminants in soil using the chemical partitioning space

Assessing the behaviour of organic chemicals in soil is a complex task as it is governed by the physical chemical properties of the chemicals, the characteristics of the soil as well as the ambient conditions of the environment. The chemical partitioning space, defined by the air-water partition coefficient (K(AW)) and the soil organic carbon-water partition coefficient (K(OC)), was employed to visualize the equilibrium distribution of organic contaminants between the air-filled pores, the pore water and the solid phases of the bulk soil and the relative importance of the three transport processes removing contaminants from soil (evaporation, leaching and particle erosion). The partitioning properties of twenty neutral organic chemicals (i.e. herbicides, pharmaceuticals, polychlorinated biphenyls and volatile chemicals) were estimated using poly-parameter linear free energy relationships and superimposed onto these maps. This allows instantaneous estimation of the equilibrium phase distribution and mobility of neutral organic chemicals in soil. Although there is a link between the major phase and the dominant transport process, such that chemicals found in air-filled pore space are subject to evaporation, those in water-filled pore space undergo leaching and those in the sorbed phase are associated with particle erosion, the partitioning coefficient thresholds for distribution and mobility can often deviate by many orders of magnitude. In particular, even a small fraction of chemical in pore water or pore air allows for evaporation and leaching to dominate over solid phase transport. Multiple maps that represent soils that differ in the amount and type of soil organic matter, water saturation, temperature, depth of surface soil horizon, and mineral matters were evaluated.