垃圾渗滤液在土壤中的生物降解动态

通过室内好氧、厌氧2种培养,研究了3种不同填埋年限垃圾渗滤液在红壤和潮土中的生物降解动态.鲜样、天井洼样、水阁样垃圾渗滤液分别为填埋0年、4～5年和12年的垃圾渗滤液.结果表明,垃圾渗滤液在前7 d降解相对较快.在好氧培养条件下,红壤鲜样、天井洼样、水阁样渗滤液在前7 d的表观降解率为88.9%、60.5%、25.0%;潮土中的表观降解率更大,分别为96.6%、80.4%和65.0%;7 d后下降趋势均趋于平缓.在相同土壤中,填埋龄越短的垃圾渗滤液的表观降解率越大,在厌氧培养条件下的情况与此类似,但降解率不如好氧条件下高.在没有土壤介质参与的条件下(如低洼处积存的渗滤液),3种垃圾渗滤液自身降解速率均符合一级动力学方程.鲜样垃圾渗滤液降解的半衰期为12～16 d,其余垃圾渗滤液降解的半衰期为20～30 d.垃圾渗滤液一旦进入土壤环境,降解速率会大大加快.土壤处理垃圾渗滤液有一定的功效.     

施污土壤重金属有效态分布及生物有效性

以城市污泥为研究对象,将城市污泥与土壤按照一定的质量比配成污泥混合土壤.采用6种不同性质提取剂(0.05mol/L EDTA、0.1 mol/L CH3 COOH、0.01 mol/L CaC12、1 mol/L CH3COONH4,0.05 mol/L NaHCO3和0.05 mol/L Tris-HCl)分别对污泥混合土壤中重金属(Cd、Pb、Cu和Zn)的螯合态、酸溶态、中性交换态、中性结合态、碱性交换态和蛋白质结合态进行提取,考察污泥的添加对土壤中不同形态重金属的消长规律.通过黑麦草盆栽试验,探究污泥混合土壤中不同形态重金属的植物可利用性.结果表明:污泥混合土壤中重金属螯合态比例较大,占总量的20.3％-40.0％;其次为酸溶态和中性结合态,而中性交换态、碱性交换态和蛋白质结合态的含量较低.污泥的添加促进了黑麦草对Cd、Cu和Zn的吸收,在污泥添加率为44.4％时根部对其吸收量达最大,分别较CK处理增加了0.3、2.3和6.5倍.抑制了对Pb的吸收,在污泥添加率为37.5％时,根部对Pb的吸收较CK处理下降0.4倍.Pearson相关系数分析结果表明:污泥混合土壤中以螯合态、酸溶态和中性结合态存在重金属可被黑麦草吸收利用.     

施用污泥对土壤重金属形态分布和生物有效性的影响

采用盆栽技术和BCR连续浸提法研究了污泥的添加对土壤Cd、Pb、Cu和Zn形态分布的影响及重金属在黑麦草-施污泥土壤中迁移转化规律.结果表明:污泥的添加使土壤中生物有效态的Cd和Zn含量显著增加,生物有效态Pb含量显著降低,残渣态Pb的比例较CK增加了33.3％～74.5％,而可交换态和可还原态Cu含量在污泥与土壤添加比为1∶1时,仅占总量的0.7％和0.2％.污泥的添加能促进黑麦草对Cd、Cu和Zn的吸收,抑制对Pb的吸收.多元线性回归分析结果表明,黑麦草体内Cd、Zn和Cu含量分别与土壤中可还原态Cd、Zn和可氧化态Cu含量存在正相关,草体中Pb的含量则受土壤中可交换态和可氧化态Pb含量共同影响.种植黑麦草后根际土中可氧化态Cd和Cu分别向可交换态Cd和残渣态Cu转化,可交换态和可还原态Zn向可氧化态Zn转化,Pb的生物有效性基本未受影响.     

强还原过程对设施菜地土壤重金属形态转化的影响

设施菜地由于污水灌溉、粪肥施用等导致重金属污染.本文通过土柱淹水同时添加玉米秸秆培养和后期通水淋洗,研究强还原法对设施土壤重金属(Cd、Cu、Pb和Zn)形态转化的影响.结果表明: 强还原处理使土壤pH显著降低,玉米秸秆处理变化更显著;土壤氧化还原电位(Eh)迅速下降至-280 mV左右.玉米秸秆处理可以促进土壤中Cd、Cu、Pb和Zn活化,第9天土壤中有机物及硫化物结合态和残渣态Cd、Cu、Pb和Zn含量比重下降;至15 d培养结束,土壤中4种重金属含量较对照分别减少18.1%、19.0%、16.1%和15.7%.玉米秸秆处理可以增加土壤中Cd和Zn的溶出量,但是Cu的溶出量减少;胶体结合态Cd和Pb含量较对照增加、Cu较对照显著减少、Zn没有显著变化.强还原可以引起设施土壤重金属活化,提高蔬菜积累重金属的风险,而且其随土壤水分的运移可能导致水体的污染.     

芜湖钢铁厂周边土壤及油菜籽中镉、铜、锌、铅含量和形态分布研究

研究了污染土壤、油菜籽中Cd、Cu、Zn、Pb含量、形态分布特征和重金属富集状况及可能存在的生物毒性.结果表明,土壤中Cd、Zn、Pb以铁锰氧化物结合态、Cu以残留态占5种形态最高比例,分别为31.1%、39.3%、53.79%、46.24%;Cd、Pb交换态比例较高,为23.47%、16.32%,Cu、Zn的交换态比例较小,为3.14%、0.54%;土壤中不同重金属与各重金属形态相关关系有差别,5种重金属形态转化为有效态重金属难易程度不同;油菜籽和油菜籽壳中不同重金属累积趋势有差异,Cu易在油菜籽壳中累积,Cd、Zn、Pb易在油菜籽中累积;油菜籽中不同重金属累积率不同,Cd累积率最高,为0.56.油菜籽中重金属累积率与土壤中重金属总量呈显著负相关关系(P＜0.05),土壤中重金属的形态、转化差异是此种负相关关系的主要原因;油菜籽中Cd、Cu、Pb以氯化钠态为主,分别为32.50%、22.94%、34.69%,Zn以EDTA态为主,为45.97%.油菜籽中重金属形态可能影响其毒性,但其毒性的人类膳食风险还需进一步研究证实.油菜籽中重金属形态与油菜中重金属总量相关性不好.     

利用乙二胺四乙酸淋洗修复重金属污染的土壤及其动力学

通过室内模拟试验,采用振荡淋洗的方法研究了乙二胺四乙酸(EDTA)浓度、pH、淋洗时间对重金属去除效果的影响.利用一级反应动力学模型对试验数据进行拟合,并测定了EDTA处理前后土壤中重金属形态的变化.结果表明,EDTA溶液在浓度为0.1 mol·L^-1、pH 7、淋洗时间1 d的条件下能达到对污染土壤重金属的最大去除率,去除率分别为Cd 89.14%、Pb 34.78%、Cu 14.96%、Zn 45.14%.模型拟合结果表明,Cd的质量转移系数最大,其次是Zn、Pb和Cu.说明在土壤淋洗过程中,Cd和Zn最先达到质量转移的平衡状态,然后是Pb和Cu.形态分级结果表明,EDTA能有效地去除交换态、碳酸盐结合态和氧化物结合态重金属,而对有机态和残余态部分重金属作用效果不明显.     

绿洲土Cd、Pb、Zn、Ni复合污染下重金属的形态特征和生物有效性

通过模拟基于干旱区绿洲土壤Cd-Pb-Zn-Ni复合污染下的油菜盆栽试验,采用Tessier五步连续浸提法探究了重金属复合污染对油菜生长的影响及其各形态的转化归趋和生物有效性.结果显示,随着Cd-Pb-Zn-Ni复合胁迫水平的升高,油菜的干重先增加后减小,根系的生长由促进作用转变为抑制作用;对照土壤中4种重金属元素均以残渣态为主要赋存形态,可交换态的含量均很小;随着外源重金属的添加,油菜种植土壤中4种重金属元素的各形态含量随之增加,Cd、Pb、Zn的可交换态和Ni的碳酸盐结合态对外界胁迫响应强度最大,Cd、Pb、Zn、Ni的活性增加,且Cd、Pb的主要赋存形态迅速转变为碳酸盐结合态和铁锰氧化态,Zn的主要赋存形态由残渣态和碳酸盐结合态过渡到碳酸盐结合态和铁锰氧化态,Ni的主要赋存形态为碳酸盐结合态;Cd、Zn在茎叶中的含量大于根系,Pb、Ni反之,油菜能将Cd、Zn更多的运输至茎叶,Pb、Ni则主要积累在根系;油菜茎叶吸收Cd和油菜各部位吸收Zn的主要贡献形态为可交换态,根吸收Cd的主要贡献形态由可交换态转变为有机结合态,根吸收Pb和油菜各部位吸收Ni的主要贡献形态为碳酸盐结合态.     

碳酸钙对水稻吸收重金属(Pb、Cd、Zn)和As的影响

选用重金属(Pb、Cd、Zn)和As复合污染土壤进行水稻盆栽试验,结果表明,碳酸钙的添加显著提高了土壤pH值,显著降低了土壤中交换态Pb、Cd、Zn和As的含量,与对照相比,交换态Pb、Cd、Zn和As含量分别最多降低了98.35%,93.72%,98.52%和69.48%。碳酸钙对水稻根、稻谷干重和总生物量没有显著影响,添加量过高时显著降低了水稻分蘖数和茎叶干重,说明过量施用碳酸钙对水稻生长会产生负面作用。因为碳酸钙的添加,水稻植株各部位重金属Zn含量显著降低,糙米中Zn含量最多减少了34.95%;根、谷壳中Pb、Cd含量显著降低,但糙米中含量却未显著降低;水稻各部位As含量均没有显著降低。参照《食品中污染物限量》(GB2762—2012),试验糙米中Pb、Cd、无机As含量均未达到限量标准。显然,碳酸钙的添加降低了Pb、Cd、Zn的生物有效性(水稻根系对Pb、Cd、Zn的吸收累积减少),但并未有效地抑制Pb、Cd向糙米转运;碳酸钙显著降低了土壤的交换态As含量,但并未使土壤中As的生物有效性明显降低(水稻植株各部位的As含量并未显著减少)。     

稻麦轮作下水稻土重金属形态特征及其生物有效性

在成都平原稻麦轮作下86个土样中重金属全量和各形态含量分析的基础上,采集分析相应点位上种植的主要粮食作物小麦和水稻籽粒的重金属含量,通过描述性统计分析、相关性分析及线性回归方程的模拟,研究了土壤中重金属的形态分布特征及其生物有效性。统计分析结果表明：土壤中Cr、Cu、Pb、Zn各形态含量的分配顺序为：残渣态〉有机物结合态〉铁锰氧化物结合态〉碳酸盐结合态〉可交换态,而Cd各形态含量的分配顺序为：铁锰氧化物结合态〉残渣态〉碳酸盐结合态〉有机物结合态〉可交换态。若以活性态（非残渣态含量）而论,Cd的活性最高,Cr的活性最低。除Cr外,各元素全量与各活性形态之间的关系较为密切。土壤中全Cd含量与4种活性形态Cd含量间的相关性均达极显著水平;Cu、Zn全量分别与其铁锰氧化物和有机物结合态含量,Pb全量分别与其可交换态和铁锰氧化物含量间的相关系数达显著或极显著水平。用卫生部颁布的食品中重金属限量卫生标准评价稻麦籽粒重金属累积情况,其结果表明,小麦籽粒（旱作）中的Cd、Cr、Cu、Pb分别超标14.71%、8.70%、6.50%和17.40%,而水稻籽粒（水作）仅有Pb和Cd含量超标10.90%和8.70%。不同形态重金属对水稻和小麦籽粒中重金属累积的影响效应不同，从多元线性回归方程的回归系数来看：稻一麦籽粒中Cd含量受到土壤中各活性形态Cd含量的影响。除铁锰氧化态Cd和有机物结合态Cd含量分别对小麦和水稻籽粒中Cd的累积表现出负效应外，其余均为正效应。可交换态Cu含量对稻-麦籽粒Cu累积的效应最大，其次受碳酸盐结合态Cu含量的影响。稻一麦籽粒Pb含量的累积受土壤各活性态Pb含量影响效应的差异不甚明显。稻-麦籽粒Zn含量与土壤各活性态Zn含量间无显著线性关系。     

淹水条件下控释氮肥对污染红壤中重金属有效性的影响

采用淹水培养方法研究了不同氮水平(100、200和400 mg/kg,分别记为1、2、3)下普通尿素(PU)、硫包膜尿素(SCU)、树脂包膜尿素(PCU)和硫加树脂双层包膜尿素(SPCU)对污染红壤中Cd、Pb、Cu、Zn有效性的影响.结果表明,不同包膜尿素对土壤pH值和水溶性SO42-含量有较大影响.各施氮处理红壤pH值随着施氮量的增加(除5d时PU和60 d时SCU)而增加,不同包膜尿素对土壤中水溶性SO42-含量有较大影响,在同一施氮水平下不同包膜尿素处理间土壤pH值和土壤中水溶性SO42-含量差异较大.60 d培养期间PU、SCU、PCU和SPCU处理pH值比对照分别升高0.17-0.38、0.08-0.27、0.07-0.36和0.10-0.21;水溶性SO42-含量PU、SCU和PCU处理比对照分别升高39.5％-157.3％、40.9％-94.5％和7.55％-55.8％,而SPCU处理降低5.67％-90.7％.不同尿素类型和氮肥的施用量对红壤Cd、Pb、Cu和Zn有效性的影响均存在显著差异.60 d培养期间红壤有效态Cd含量以树脂包膜尿素100 mg N/kg下最低,其有效态Cd含量比对照显著降低20.7％-69.8％;有效态Pb、Cu和Zn含量以普通尿素400 mg N/kg下最低,其有效态Pb、Cu和Zn含量比对照分别显著降低17.0％-54.2％、18.5％-34.6％和15.6％-59.5％.随施氮量提高,PU处理有效态Cd含量先升高后降低,有效态Pb、Cu和Zn含量逐渐降低;SCU处理有效态Pb含量逐渐降低,有效态Cd、Cu和Zn含量变化规律不一致;PCU处理有效态Cd含量逐渐升高,有效态Pb、Cu和Zn含量变化规律不一致;SPCU处理有效态Cd、Pb、Cu和Zn含量逐渐降低.有效态Pb和Zn含量与pH值和水溶性SO42-含量呈显著负相关,有效态Cd与水溶性SO42-含量呈显著正相关.在多重金属污染红壤中,可考虑不同控释氮肥的配合使用,降低土壤中重金属的有效性.     

Effects of microplastics and biochar on soil cadmium availability and wheat plant performance

Biochar is a promising amendment to promote cadmium (Cd) sorption and fixation in agricultural soil, where microplastics are emerging contaminants in soil. Herein, a greenhouse pot experiment was conducted to elucidate the effects on Cd availability in a soil–plant system by biochar and fresh/aged microplastics application. The fresh microplastics led to an obvious increase in soil Cd availability and Cd uptake by wheat plant, while the aged microplastics increased the available Cd in soil but had no effect on Cd uptake by wheat plant, which was likely attributed to the blocking effect of the aged microplastics on Cd transportation from the soil to the wheat plant. Unexpectedly, biochar had increased Cd availability and Cd uptake. The increased soil soluble Cd was because of both decreased soil pH and elevated dissolved organic matter (DOM) content resulted by biochar addition. Also, the unchanged Cd adsorption of the soil was likely responsible for the increased tested soil Cd availability. In addition, the combined effects of a greater decrease in soil pH, an increase in soil DOM content, and a reduction in Cd adsorption after the addition of microplastics to biochar-amended soil resulted in a significant increase (ranging from 2.63% to 47.73%) in Cd availability compared to soil treated with biochar alone. Moreover, fresh microplastics inhibited wheat growth, and greater inhibition effect was observed for their aged ones. The biochar elevated the wheat biomass; however, the coexistence of microplastics and biochar decreased the wheat plant biomass compared with biochar alone, due to the negative influence of microplastics in plant growth.     

垃圾填埋场渗滤液灌溉对土壤理化特征和草本花卉生长的影响

以草本花卉植物一串红和石竹为材料,通过盆栽试验研究了不同浓度垃圾渗滤液灌溉对土壤理化性质及生物学性质、植物生长、氮磷和重金属吸收的影响。渗滤液灌溉提高了土壤有机质、氮含量和电导率,其中,黄壤盐分积累速度大于紫色土,而对土壤磷和重金属含量的影响不明显,土壤脲酶活性随渗滤液浓度的提高呈先升高后降低趋势,紫色土和黄壤在渗滤液灌溉浓度分别为60%和40%时脲酶活性最强;随渗滤液浓度提高紫色土过氧化氢酶活性略为上升,黄壤过氧化氢酶活性降低。渗滤液灌溉使两种花卉根系生长受到抑制,但对植物地上部的生长发育存在低浓度促进高浓度抑制的双重作用。渗滤液灌溉可提高两种植物地上部的氮含量,对一串红磷含量影响不明显,使石竹磷含量降低,对Cu、Zn含量的影响因土壤和植物的不同而异,但高浓度渗滤液灌溉使两种植物Pb、Cr和Cd含量均提高。结果表明,适当浓度渗滤液灌溉具有改善土壤肥力,促进植物地上部生长发育的作用,渗滤液灌溉不会引起土壤和植物体内重金属过量积累,土壤氮过量积累导致的氮磷营养失调和盐分过度积累是高浓度渗滤液抑制植物生长的重要原因。从土壤性质变化和植物生长反应看,渗滤液灌溉浓度以20%—40%为佳。     

Pollution characteristics and risk assessment of heavy metals in the soil of a construction waste landfill site

Heavy metals found in construction waste can enter soil and water bodies through surface runoff and leachate, where they represent an environmental hazard. In this study, we investigate the pollution characteristics and ecological risks of eight heavy metals (Cd, Cr, Cu, Mn, Ni, Pb, Zn, and As) in the soils of an unofficial construction waste landfill site in Beijing, China. The results indicate that long-term disposal of construction waste in the dry riverbed can reduce the pH value of the soil, increase the soil organic carbon content, and affect the total amount and distribution of heavy metals. Moreover, the landfill site pollutes the external soil environment, with Cd, Zn, Pb, and Cu as the characteristic pollutants. According to the Nemerow comprehensive pollution index and potential ecological risk assessment, heavy metal pollution decreases in the following order: internal soil > bottom soil > boundary soil. Cd, Zn, Pb, and Cu pollution is higher in the internal region, with single heavy-metal pollution indexes (Pi) of 1.41, 1.65, 1.26, and 1.28, respectively. Conversely, the Pi for Cr is higher in boundary and bottom soils (1.91 and 1.94, respectively). Risk assessment codes indicate that Cd and Mn pose the greatest environmental risk (31.9% and 17.8%, respectively) as they have the highest effective content, bioavailability, and mobility. Thus, environmental monitoring is a necessity for these metals.     

Soil seed bank of the waste landfills in South Korea

The restoration of urban landfill is a topic of growing interest in reclamation ecology as the acreage of abandoned sites near cities increases. The goals of this study were to assess the ecological status of waste landfills and to elucidate the role of seed banks in the establishment of vegetation at these sites. The study sites were located at five landfills around Seoul and Kyongki Province. On average, soils were sampled on 20 plots per landfill in 2001 to record species composition and to estimate the number of seeds in the soil. Soil seed bank vegetation and the individual number of seedlings that germinated were recorded using the seedling emergence method. Relative density per species was calculated from the number of individual seedlings. We conducted canonical correspondence analysis (CCA) using the program CANOCO to survey the relationships between 23 environmental variables and plant importance values. Environmental variables included categorical and numerical variables (landfill age, landfill size, distance from landfill edge, human disturbance level, slope, periodic management level) and soil physico-chemical variables (bulk density, soil moisture content, organic matter content, total N, available P, K, Na, Ca, Mg, Cd, Cr, Cu, Fe, Mn, Ni, Pb, and Zn). The mean seedling density per m ² differed significantly among sites (P < 0.05). As landfill age increased, the mean seedling density per m ² decreased. The mean seedling density of the Sangpaedong landfill, which was less than 1 year old, was higher than that found in 6- and 7-year-old landfills. The Sangpaedong landfill mainly contained seeds of Chenopodium albumL. and Digitaria ciliaris(L.) SCOP. With regard to early vegetative colonization in landfills, our results highlighted the importance of seed banks occurring in cover soils. Cover soils, derived from various sources, will determine landfill landscapes because of different seed banks present in them. The first axis of the CCA was correlated with landfill age, Na, and human disturbance level, while the second axis was correlated with landfill size, slope, periodic management level, Zn, total N, and organic matter content. Understanding seed banks in landfill cover soils is important, therefore, for proper landfill management and restoration.     

Characterisation and reactivity continuum of dissolved organic matter in forested headwater catchments of Andean Patagonia

相似文献   

Composition,Dynamics, and Fate of Leached Dissolved Organic Matter in Terrestrial Ecosystems: Results from a Decomposition Experiment

Fluxes of dissolved organic matter (DOM) are an important vector for the movement of carbon (C) and nutrients both within and between ecosystems. However, although DOM fluxes from throughfall and through litterfall can be large, little is known about the fate of DOM leached from plant canopies, or from the litter layer into the soil horizon. In this study, our objectives were to determine the importance of plant-litter leachate as a vehicle for DOM movement, and to track DOM decomposition [including dissolve organic carbon (DOC) and dissolved organic nitrogen (DON) fractions], as well as DOM chemical and isotopic dynamics, during a long-term laboratory incubation experiment using fresh leaves and litter from several ecosystem types. The water-extractable fraction of organic C was high for all five plant species, as was the biodegradable fraction; in most cases, more than 70% of the initial DOM was decomposed in the first 10 days of the experiment. The chemical composition of the DOM changed as decomposition proceeded, with humic (hydrophobic) fractions becoming relatively more abundant than nonhumic (hydrophilic) fractions over time. However, in spite of proportional changes in humic and nonhumic fractions over time, our data suggest that both fractions are readily decomposed in the absence of physicochemical reactions with soil surfaces. Our data also showed no changes in the ¹³C signature of DOM during decomposition, suggesting that isotopic fractionation during DOM uptake is not a significant process. These results suggest that soil microorganisms preferentially decompose more labile organic molecules in the DOM pool, which also tend to be isotopically heavier than more recalcitrant DOM fractions. We believe that the interaction between DOM decomposition dynamics and soil sorption processes contribute to the ¹³C enrichment of soil organic matter commonly observed with depth in soil profiles. published online 2004     

Dissolved organic matter (DOM) concentration and quality in a forested mid-Atlantic watershed, USA

Understanding the quantity and quality of dissolved organic matter (DOM) in potential watershed sources is critical for explaining and quantifying the exports of DOM in stream runoff. Here, we examined the concentration and quality of DOM for ten watershed sources in a 12?ha forested catchment over a two-year period. DOM composition was evaluated for: throughfall, litter leachate, soil water (zero and tension), shallow and deep groundwater, stream water, hyporheic zone, and groundwater seeps. DOM quality was measured using a suite of optical indices including UV–visible absorbance and PARAFAC modeling of fluorescence excitation-emission matrices (EEMs). DOM concentrations and quality displayed a pronounced trend across watershed sources. Surficial watershed sources had higher DOM concentrations and more humic-like DOM with higher molecular weight whereas deeper groundwater sources were rich in % protein-like fluorescence. The greater % contribution of protein-like fluorescence in groundwater suggested that a larger fraction of groundwater DOM may be bioavailable. DOM for wetland groundwater was more aromatic and humic-like than that at the well-drained riparian location. Principal component analyses (PCA) revealed that the differences in surficial watershed compartments were dictated by humic-like components while groundwater sources separated out by % protein-like fluorescence. Observations from optical indices did not provide any conclusive evidence for preferential association of dissolved organic carbon (DOC) or dissolved organic nitrogen (DON) with any particular DOM quality pools.     

超积累植物东南景天根际可溶性有机质对土壤锌吸附解吸的影响

采用盆栽和模拟试验研究了锌超积累植物东南景天根际土壤可溶性有机质(DOM)对土壤锌吸附解吸的影响.结果表明: 采用矿山土壤种植锌超积累植物东南景天后,根际土壤水溶性锌和乙酸铵提取态锌含量显著降低,而非根际土壤有效锌无明显变化.与不种植东南景天的对照土壤相比,根际土壤pH值降低了0.3个单位,有机质和DOM含量分别提高13.6%和20.9%.东南景天根际DOM对土壤锌吸附解吸的影响方式和程度与土壤类型有关.与对照DOM相比,在矿山土、黄筋泥和黄松土中,添加根际DOM使锌的最大吸附量(X_m)分别降低了17.8%、21.9%和27.7%,而非根际DOM对锌的最大吸附量没有影响.在3种供试土壤中添加根际DOM促进了锌的解吸,其中以黄松土最明显.东南景天根际DOM能降低土壤锌吸附容量,减少土壤对锌的吸附,促进吸附态锌的解吸,从而提高了根际锌的生物有效性.     

隔离降雨对亚热带米槠天然林土壤可溶性有机质数量及光谱学特征的影响

全球气候变化背景下区域降雨格局变化可能深刻影响土壤可溶性有机质(DOM)的数量和质量.为了解亚热带森林土壤DOM对降雨减少的响应,通过6年不同强度(对照、-30%、-60%)的隔离降雨模拟试验,采用光谱技术,研究了降雨减少对亚热带米槠天然林不同深度土壤DOM数量和结构的影响.结果表明: 与对照相比,隔离降雨使0～10 cm土层中可溶性有机碳(DOC)和可溶性有机氮(DON)含量显著降低,其中-30%处理DOC下降幅度小于DON, 而-60%处理DOC下降幅度大于DON,0～10 cm土层中DOC和DON含量都显著高于10～20 cm土层.-30%处理土壤DOM中源于微生物代谢的芳香类腐殖质和烷烃比例上升;-60%处理土壤DOM中微生物代谢产物的相对贡献率减少.除了隔离降雨后水分变化等直接影响外,微生物活性也是本试验区影响DOM数量和结构的重要因素.