湘南第四纪红壤吸附SO^2—4的机理研究

本文研究了湘南第四纪红粘土及其发育地旱地和水田表层土壤对ＳＯ＾２－４的吸附，结果表明这三种土壤吸附ＳＯ＾２－４的顺序为：红粘土＞旱地红壤＞红壤性水稻土，而且随介质ＰＨ的升高，ＳＯ＾２－４吸附量减少，吸附机理也发生改变，当介质ＰＨ＜ＺＰＣ时，以置换水合基（－ＯＨ２）的方式进行，ＰＨ在３．５－６．５之间时，以置换羟基（－ＯＨ）的方式为主，ＰＨ＞６．５以后，解吸占优势。     

福建赤红壤旱地与红壤旱地水分特性的比较

释放80%的有效水时赤红壤旱地的t值（当释放的土壤有效水占有效水库容的比率为80%时的土壤水吸力值）较小，表明赤红壤旱地持水性较红壤旱地更差，植物更容易受到干旱的协迫。赤红壤旱地贮水库容比红壤旱地小，赤红壤旱地的比水容量达到10-2数量级（难效水）在-10kPa~-30kPa就开始出现，而红壤旱地出现在-30kPa以下，表明赤红壤旱地的失水速度快，保水供水性能弱于红壤旱地。最后，讨论了影响旱地土壤水分性质的因素。     

温州红壤的酸沉降临界负荷研究

本文简要介绍了以碱总量守恒为基础建立的兼能描述钙质与非钙质土壤长期酸化过程的动态模型（ＬＴＳＡＭ），并利用该模型讨论了温州红壤的酸沉降临界负荷。结果表明，以硫沉降即酸沉降的硫沉降非酸沉降两观点分别来确定红壤的临界负荷，其值依次为３．９１与１．８４ｇ·ｍ＾－２·ａ＾－１，后者仅是前者的４７％，差异显著应加以区别。     

改性土壤对模拟含硝基苯废水的吸附

研究了季铵盐阳离子表面活性剂四甲基铵离子（TMA）和十六烷基三甲基铵离子（HDTMA）改性的土壤（黑土、黄棕壤、红壤）对水中硝基苯的吸附作用。结果表明：改性土壤和改性土壤均能吸附水中的硝基苯。但改性土壤对水中硝基苯的吸附能力明显高于未改性土壤。改必土壤吸附硝基苯能力的顺序为1CEC－HDTMA黑土＞1CEC－HDTMA黄棕壤＞0．7 CEC－HDTMA黄棕壤＞1 CEC－HDTMA红壤＞0．7 CEC－HDTMA红壤＞1 CEC－TMA黄棕壤＞1 CEC－TMA红壤。未改性土壤和HDTMA改性土壤对硝基苯的吸附通过分配来进行，吸附等温线可用Henry方程表示，其lgKSOM为2．27，lgKHDTMA为2．87。     

红壤对SO_4~（2－）和H_2PO_4~－的吸附与竞争吸附研究

研究红壤对ＳＯ４（２－）和Ｈ_２ＰＯ(４－)的吸附与竞争吸附机理．实验结果表明，红壤吸附Ｈ２ＰＯ４－的量远远大于ＳＯ４（２－），前者几乎是后者的２倍．在两种阴离子共存体系中，Ｈ２ＰＯ４－使ＳＯ４（２－）吸附量明显减少，在浓度低时甚至出现负吸附；ＳＯ４（２－）对Ｈ２ＰＯ４－吸附量的影响很小．说明土壤对Ｈ２ＰＯ４－的吸持力较强，为高强度专性吸附，不易于被其它阴离子解吸；土壤对ＳＯ４（２－）的吸持力则较弱，为低强度专性吸附或非专性物理吸附，能够被吸持力更强的阴离子完全解吸．     

中南地区几种地带性土壤中的氧化铁类型与钼吸附特性

应用X射线衍射和化学分析等手段研究了中南地区几种地带性土壤中的氧化铁类型与钼吸附的关系，结果表明：供试土壤粘粒的氧化铁以晶质氧化铁为主，非晶质氧化铁含量低；砖红壤和赤红壤中的晶质氧化铁以赤铁矿为主．其次为针铁矿；红壤、棕红壤中针铁矿含量比赤铁矿含量稍高，黄棕壤中的晶质氧化铁全为针铁矿；针铁矿的平均晶粒大小（MCD）一般比赤铁矿的小，而比表面积却比赤铁矿的大；针铁矿型氧化铁的钼吸附量比针－赤混合型氧化铁的高，从砖红壤到黄棕壤．单位重量的晶质氧化铁的钼吸附量随G／（G＋H）比值的升高而增大．     

丘陵红壤开发的水土资源保护及农业产业化经营模式

以湖南省桃源县为例,针对目前丘陵红壤开发存在的主要问题,在探明季节性干旱成因和发生规律、水资源合理调蓄利用依据的基础上,提出了红壤丘陵区抗御季节性干旱的水分管理对策和主要措施;通过不同经营模式的水土资源动态观测、分析,提出了红壤丘陵区土壤允许流失值应≤200 t·km-2·a-1、相应的降水径流系数<0.25 等水土资源协调发展的关键技术指标,并在丘陵红壤坡地上建立了土壤侵蚀模数<100 t·km-2·a-1 的“土壤-水分-生物”资源互利型的高效利用模式。同时,以市场为导向,优化产业结构为中心,应用上述研究成果,建立了茶叶、苎麻、果业、庭园高效生态农业等四大科技先导型的产业化规模经营体系,为我国红壤丘陵区的农业产业化开发提供实用模式与示范样板。     

生物炭-锰氧化物复合材料对红壤吸附铜特性的影响

锰氧化物作为改性材料应用于制造复合材料一直是环境领域的研究热点,锰氧化物改性的复合材料在水处理、空气清新剂等领域应用广泛。但目前,将生物炭-锰氧化物复合材料作为吸附材料改变土壤对铜吸持能力的研究还不多见。采用等温平衡吸附法,测定生物炭-锰氧化物复合材料对红壤吸附铜的能力影响,并应用Freundlich方程Cs=KfCen分析红壤对铜的吸附特征。结果表明：不同用量的生物炭-锰氧化物复合材料加入后,均会明显提高红壤对铜的吸附量。添加0.5%、1.0%、2.0%和4.0%生物炭-锰氧化物复合材料的红壤处理,其铜的吸附量较未添加处理分别增加了63.1%、130%,310%和509%。Freundlich吸附方程能较好的描述不同用量生物炭-锰氧化物复合材料影响红壤对铜的吸附特征。添加0.5%、1.0%、2.0%和4.0%炭-锰材料处理的分配系数（Kf值）分别为0.176、0.286、0.653和0.800。生物炭-锰氧化物复合材料用量为4.0%时,分配系数（Kf值）较对照红壤提高了5倍,生物炭-锰氧化物复合材料加入红壤后对红壤pH值影响不大,对CEC（阳离子交换量）有较大的影响;生物炭-锰氧化物复合材料用量为4.0%时,CEC为5.59 cmol·kg-1,较对照增加了14.1%,温度升高,有利于提高红壤对铜的吸附能力。生物炭-锰氧化物复合材料加入红壤后,红壤在1034.63、537.22、471.45 cm-1处有吸收峰出现,红壤表面-OH、Mg-O、Si-O等活性官能团数量明显增加。生物炭-锰氧化物复合材料增加红壤对铜的吸附机制可能是红壤表面Mg-O、Si-O等官能团与铜形成了Mg-O-Cu-、Si-O-Cu-络合物,提高了红壤对铜的吸持能力。从土壤化学与土壤修复的角度出发,生物炭-锰氧化物复合材料可用于铜污染红壤修复。     

阴离子态养分从第四纪红壤中的淋失特征

在实验室条件下，将第四纪红壤进行淋洗试验，旨在研究第四纪红壤中阴离子态养分的含量及其淋失特征。结果表明，第四纪红壤中各种可溶发生 阴离子态养分含量除ＮＯ＾－３和Ｃｌ＾－外，其它都是很低的，６种阴离子在第四纪红壤中的淋失强弱顺序是：Ｃｌ＾－〉ＮＯ＾－３〉Ｈ２ＢＯ＾－３〉ＳＯ＾２－４〉ｍＯｏ＾２－４？〉ｈ２ｐｏ＾－４，而土壤对它们的固定或吸附能力则相反。     

水稻新材料耐淹涝能力的比较研究

以“禾稗”ＤＮＡ导入后代及受体、供体为试验材料，应用地上部干重和根系干重的相对受害率（ＲＤ／％），叶片的电导率（ｋ）和膜脂过氧化物的产物丙二醛（ＭＤＡ）的增加量几个生长、生理指标，在苗期模拟没顶淹水处理２、４、６ｄ，比较研究了“禾稗”ＤＮＡ导入后代与供体、受体耐淹涝能力。结果显示：在淹涝胁迫下，“９４Ｄ－０５”、“９４Ｄ－３４”的干重ＲＤ／％分别小于它们的受 “科长早３号”和“圭６３０”，达到或接     

Phytoremediation of bauxite-derived red mud by giant reed

In 2010 the pond dam of an aluminium manufacturing plant in Hungary broke and flooded many towns with toxic red mud. At least 10 people were dead and over 150 hospitalized. Bauxite residue is often referred as red mud due to the colour of the bauxite ore and iron oxides. Red mud is separated during the refining process. The production of 1 t of alumina generally results in the creation of 1–1.5 t of red mud. Red mud is toxic for the environment due to high alkalinity, salinity and trace metals. Here, we used the plant Arundo donax L. (giant reed) to uptake trace metals and decrease salinity and pH of red mud. We measured plant toxicity, trace metal availability and biomass production. Results show a 25 % decrease in electrical conductivity of red mud and a 6 % decrease in electrical conductivity of mud-polluted soil. Giant reed cultivation decreases available Cd, Pb, Co, Ni and Fe. Biomass of giant reed seedlings in red mud and mud/control soil mixture was increased by 40.4 and 47.2 %, respectively, comparing with control soil. Our findings show that giant reed is promising to decontaminate soils contaminated by red mud.     

Distribution of a Community of Mammals in Relation to Roads and Other Human Disturbances in Gabon,Central Africa

We present the first community‐level study of the associations of both roads and other human disturbances with the distribution of mammals in Gabon (central Africa). Our study site was in an oil concession within a littoral mosaic landscape. We conducted surveys along 199 line transects and installed camera traps on 99 of these transects to document mammal presence and abundance. We used generalized linear mixed‐effect models to document associations between variables related to the ecosystem (land cover, topography, and hydrology), roads (coating, width of rights of way, condition, type of vehicle used on the road, traffic level, affiliation of users, and general type of road), and other human disturbances (urbanization, agriculture, hunting, logging, gathering, and industrial activities) and the abundance or presence of 17 species or groups of mammals including elephant (Loxodonta cyclotis), buffalo (Syncerus caffer), sitatunga (Tragelaphus spekei), red river hog (Potamochoerus porcus), smaller ungulates, gorilla (Gorilla gorilla), chimpanzee (Pan troglodytes), side‐striped jackal (Canis adustus), carnivores, monkeys, and large rodents. Some types of roads and other human disturbances were negatively associated with the abundance or presence of elephants, buffalos, gorillas, sitatungas, some monkeys, and duikers. The pattern of associations of mammals with roads and other human disturbances was diverse and included positive associations with road presence (red river hog, some monkeys, and duikers), agriculture (sitatunga, small carnivores, and large rodents) and industrial activities (sitatunga, red river hog, red duikers, and side‐striped jackal). Our results suggest that the community of mammals we studied was mostly affected by hunting, agriculture, and urbanization, which are facilitated by road presence. We recommend increased regulation of agriculture, hunting, and road building in the area. Distribución de una Comunidad de Mamíferos en Relación a Carreteras y Otras Perturbaciones Humanas en Gabón, Africa Central     

盐碱地农-渔开发对土壤环境的影响

在东北苏打盐碱地进行了稻-鱼-苇-蒲开发试验,并探讨了该模式对盐碱土壤环境的影响。结果表明,开发后土壤有机质含量增加96.8%(平均值,以下同),盐分含量下降43.6%,全量和速效N、P、K质量分数分别增加142.8%和188.2%;阳离子交换量、盐基总量分别增加8.21%及27.71%;土壤腐殖质以富里酸为主,w(HA)/w(FA)比值提高36.15%;养鱼稻田的土壤微生物总量明显高于未养鱼田(P<0.01);优势种为放线菌。土壤酶活性进一步加强。系统废水的盐分质量浓度降至1.0 g/L左右,碱浓度低于水源(7.0~10.0 mmol/L)。该模式不会造成土壤次生盐碱化。     

我国典型土壤上重金属污染对番茄根伸长的抑制毒性效应

采用盆栽试验观测了我国3种典型土壤——黄泥土、褐土、红壤上不同重金属(铜、锌、铅)作用下敏感植物番茄的根伸长,其中黄泥土和褐土上重金属添加量范围为Cu(0～2000mg·kg-1)、Zn(0～4000mg·kg-1)和Pb(0～5000mg·kg-1),红壤上为Cu(0～400mg·kg-1)、Zn(0～750mg·kg-1)和Pb(0～2000mg·kg-1).对不同土壤上Cu、Zn、Pb对番茄的根伸长抑制率进行了比较,以阐明不同土壤上重金属种类及用量对蔬菜根生长的抑制及毒性效应.结果表明,相同Cu、Zn、Pb污染水平(添加量)下,土壤中重金属对番茄的根伸长抑制率大小顺序基本表现为:红壤>黄泥土>褐土.番茄对红壤中的重金属最敏感,其次是黄泥土,再次是褐土.番茄对不同重金属的毒性响应不同,对Cu最敏感,Zn和Pb次之.土壤中有效态重金属含量与番茄根伸长呈显著(p<0.05)或极显著(p<0.01)负相关,表明有效态重金属含量是影响蔬菜根伸长的重要因素.     

Effects of Pond Draining on Biodiversity and Water Quality of Farm Ponds

Farm ponds have high conservation value because they contribute significantly to regional biodiversity and ecosystem services. In Japan pond draining is a traditional management method that is widely believed to improve water quality and eradicate invasive fish. In addition, fishing by means of pond draining has significant cultural value for local people, serving as a social event. However, there is a widespread belief that pond draining reduces freshwater biodiversity through the extirpation of aquatic animals, but scientific evaluation of the effectiveness of pond draining is lacking. We conducted a large‐scale field study to evaluate the effects of pond draining on invasive animal control, water quality, and aquatic biodiversity relative to different pond‐management practices, pond physicochemistry, and surrounding land use. The results of boosted regression‐tree models and analyses of similarity showed that pond draining had little effect on invasive fish control, water quality, or aquatic biodiversity. Draining even facilitated the colonization of farm ponds by invasive red swamp crayfish (Procambarus clarkii), which in turn may have detrimental effects on the biodiversity and water quality of farm ponds. Our results highlight the need for reconsidering current pond management and developing management plans with respect to multifunctionality of such ponds. Efectos del Drenado de Estanques sobre la Biodiversidad y la Calidad del Agua en Estanques de Cultivo     

不同类型土壤镉含量对香芋镉吸收的影响

为探明香芋(Colocasia esculenta)镉(Cd)超标的关键原因,在湖南临武香芋主产区分别选择紫色页岩和第四纪红壤发育的Cd污染水稻土,研究土壤Cd含量、Cd活性及土壤基本理化性质对香芋Cd吸收的影响,以期为香芋的安全种植提供技术支撑。结果表明,两个试验点所有香芋Cd质量分数皆超过食品安全国家标准(0.1 mg·kg^-1),且各试验点内田块间土壤Cd含量、pH差异显著,而土壤有机质和阳离子交换量变异较小;紫色页岩发育的中碱性水稻土壤Cd活性、Cd在土壤-香芋系统中的转移系数(TFstem/taro、TFtaro/soil)皆低于第四纪红壤发育的酸性水稻土;紫色页岩发育的中碱性水稻土中,香芋Cd含量主要受土壤全Cd、TFtaro/soil的正调控;而第四纪红壤发育的酸性水稻土壤中,香芋Cd含量既受土壤全Cd、DTPA-Cd、TFtaro/soil的正调控,还受土壤pH的负调控。为实现香芋的安全生产,紫色页岩发育的中碱性水稻土中,应优先选择Cd吸收能力较低的香芋品种,或选择土壤全Cd低于0.65 mg·kg^-1的土壤进行种植;而在第四纪红壤发育的酸性水稻土壤中,则可优先选择Cd吸收能力较低的香芋品种,或选择土壤全Cd含量低于0.41 mg·kg^-1的土壤,或调理土壤pH至6.26以上,以及钝化土壤DTPA-Cd至0.19 mg·kg^-1以下的技术措施,抑制土壤Cd向香芋的迁移转运。     

施用尿素和硫酸铵对红壤硝化和酸化作用的影响

通过室内恒温培养试验,研究施用CO(NH2)2和(NH4)2SO4对初始pH值分别为5.14、4.77和4.34的红壤酸化速率和硝化速率的影响。结果表明,施用CO(NH2)2显著增加了3种红壤的硝化速率,从而显著加速土壤酸化。培养结束时,3种红壤pH值较培养过程中最高值分别下降2.14、1.23和0.56。施用(NH4)2SO4抑制了初始pH<5.0的2种红壤的硝化作用,从而显著降低这2种红壤的硝化速率和酸化速率,但显著增加了初始pH>5.0红壤的硝化速率,对其酸化速率则未见显著影响。3种红壤的酸化速率与硝化速率间存在显著线性相关关系。硝化作用是导致农田红壤pH值下降的主要原因之一,但不同氮肥对红壤硝化速率和酸化速率的影响不同。     

Gypsum addition to soils contaminated by red mud: implications for aluminium, arsenic, molybdenum and vanadium solubility

Red mud is highly alkaline (pH 13), saline and can contain elevated concentrations of several potentially toxic elements (e.g. Al, As, Mo and V). Release of up to 1 million m³ of bauxite residue (red mud) suspension from the Ajka repository, western Hungary, caused large-scale contamination of downstream rivers and floodplains. There is now concern about the potential leaching of toxic metal(loid)s from the red mud as some have enhanced solubility at high pH. This study investigated the impact of red mud addition to three different Hungarian soils with respect to trace element solubility and soil geochemistry. The effectiveness of gypsum amendment for the rehabilitation of red mud-contaminated soils was also examined. Red mud addition to soils caused a pH increase, proportional to red mud addition, of up to 4 pH units (e.g. pH 7 → 11). Increasing red mud addition also led to significant increases in salinity, dissolved organic carbon and aqueous trace element concentrations. However, the response was highly soil specific and one of the soils tested buffered pH to around pH 8.5 even with the highest red mud loading tested (33 % w/w); experiments using this soil also had much lower aqueous Al, As and V concentrations. Gypsum addition to soil/red mud mixtures, even at relatively low concentrations (1 % w/w), was sufficient to buffer experimental pH to 7.5–8.5. This effect was attributed to the reaction of Ca²⁺ supplied by the gypsum with OH^? and carbonate from the red mud to precipitate calcite. The lowered pH enhanced trace element sorption and largely inhibited the release of Al, As and V. Mo concentrations, however, were largely unaffected by gypsum induced pH buffering due to the greater solubility of Mo (as molybdate) at circumneutral pH. Gypsum addition also leads to significantly higher porewater salinities, and column experiments demonstrated that this increase in total dissolved solids persisted even after 25 pore volume replacements. Gypsum addition could therefore provide a cheaper alternative to recovery (dig and dump) for the treatment of red mud-affected soils. The observed inhibition of trace metal release within red mud-affected soils was relatively insensitive to either the percentage of red mud or gypsum present, making the treatment easy to apply. However, there is risk that over-application of gypsum could lead to detrimental long-term increases in soil salinity.     

Effect of red mud addition on the fractionation and bio-accessibility of Pb,Zn and As in combined contaminated soil

Using soil incubation experiments, the effect of red mud addition on the fractionation and bioaccessibility of Pb, Zn and As in combined contaminated soil was studied. The results showed that red mud addition could significantly decrease the concentration of HOAc-extractable Pb and Zn in soil. Compared with the control, 5% red mud addition could significantly reduce the concentrations of HOAc-extractable Pb and Zn in soil after 1, 2 and 3 months of incubation [62.5, 65.3 and 73.5% decrease (Pb), 56.7, 65.8 and 67.4% decrease (Zn)]. Whereas adding red mud could remarkably increase the concentrations of specific absorbed As and residual As in soil. The result of a simple bioavailability extraction test (SBET) indicated that all treatments with red mud addition markedly reduced the concentration of bioaccessible Zn but increased the concentration of bioaccessible As in soil, while having little effect on the concentration of bioaccessible Pb in soil. After 3 months incubation, all treatments including 1, 2 and 5% red mud addition reduced the concentration of bioaccessible Zn by 53.1–56.7% compared with the control, but increased the concentration of bioaccessible As by 1.81–6.25 times. The results suggested that red mud is an additive with potential for the remediation soil contaminated soil by combinations of heavy metals, although it should be added based on the different heavy metals in the soil. Combined use of red mud and hyperaccumulators to remediate heavy metal contaminated soil needs further study.