非损伤微测Zn2+选择性微电极的研发及应用

非损伤微测技术(Non-invasive Micro-test Technology, NMT)是一种通过微电极实时测定进出活体材料离子和小分子流速的技术,已广泛应用于植物的生长发育和逆境胁迫等研究领域中。目前该技术专用的重金属微电极种类非常少,因此其在重金属胁迫研究中的应用也受到了限制。本文在前期工作的基础上开发了一种基于非损伤微测技术的Zn~(2+)选择性微电极,首次实现了活体条件下植物根际Zn~(2+)离子流的实时、动态检测。研发的微电极在去离子水中对Zn~(2+)的线性响应范围为10–6～10~(–1) mol/L,能斯特斜率为30.2mV/decade(浓度每增加或减少10倍电位值的变化),响应时间t_(95%)≤1s,正常工作pH范围为3.5～7.0;在简易模拟土壤溶液(0.1mmol/L Ca(NO_3)_2、0.1 mmol/L KNO_3、0.1 mmol/L Mg(NO_3)_2和1 mmol/L NaNO_3)中,其线性响应范围变为5×10~(-5)～10~(-1) mol/L,能斯特斜率为28.1mV/decade,对土壤溶液中的共存阳离子具有较好的抗干扰性。利用构建的非损伤微测Zn~(2+)选择性微电极对Zn/Cd超积累植物伴矿景天(Sedum plumbizincicola)根际不同微区的Zn~(2+)离子流进行了实时检测。该技术的成功研发为活体条件下深入认识Zn~(2+)在植物根际的微界面过程与机制提供了一种强有力的研究手段。     

西南地区典型农田土壤中Cd~(2+)、Pb~(2+)的吸附特性研究

为了解西南地区土壤对污染毒性较强的Cd和Pb元素的吸附过程及作用机制,针对性地为预防和治理土壤污染提供理论依据,采用批试验的方法研究了典型黄棕壤和紫色土对Cd~(2+)、Pb~(2+)的吸附动力学、等温吸附过程以及土壤有机质、溶液pH对吸附过程的影响。结果表明:土壤吸附Cd~(2+)、Pb~(2+)均能在12 h内达到平衡,土壤对Pb~(2+)平衡吸附量远大于Cd~(2+),准二级动力学模型最适合表征其动力学过程(R~2≥0.99)。吸附等温线可用Langmuir方程和Freundlich方程拟合,土壤对Pb~(2+)的吸附能力和缓冲能力较Cd~(2+)更大,吸附是自发进行的物理化学作用并存的过程。黄棕壤对Pb~(2+)的吸附为放热反应,紫色土对Pb~(2+)以及两种土壤对Cd~(2+)的吸附为吸热反应。去除有机质的土壤对重金属的吸附量降低,Cd~(2+)在黄棕壤和紫色土中的试验最大吸附量分别减少了37.89%、29.62%;Pb~(2+)则分别减少了12.87%、20.71%。土壤对金属离子的吸附量随溶液初始pH的增加而增加。     

恒电荷土壤及可变电荷土壤与离子间相互作用的研究Ⅲ Cu2+和Zn2+的吸附特征

研究了3种典型可变电荷土壤和4种典型恒电荷土壤在不同pH和不同浓度下单纯及共存体系中Cu2 和Zn2 的吸附及其影响因素。结果表明,两类土壤对Cu2 或Zn2 的吸附量均随平衡浓度增加而增大,符合Langmuir吸附等温式;当Cu2 、Zn2 浓度一定时,pH升高使Cu2 、Zn2 吸附量增大,但当pH >5时,Cu2 、Zn2 吸附量随pH变化甚微,出现一个接近最大吸附量的“平台”。当添加Cu2 、Zn2 浓度相同,但二种离子的总浓度不同时,平衡液的Cu2 /Zn2 浓度比均小于1,说明两类土壤对Cu2 的吸附选择性大于Zn2 ,且这种趋势不因pH和离子浓度而改变。当Cu2 、Zn2 共存时,使可变电荷土壤的Zn2 吸附量减小约70 % ,是恒电荷土壤降低量的约1.5倍;可变电荷土壤吸附一个Cu2 或Zn2 时所释放H 的平均数,明显大于恒电荷土壤者,说明可变电荷土壤对Cu2 及Zn2 的吸附中专性吸附的比例较恒电荷土壤大     

黄土钙质结核对水体重金属离子的吸附性能研究

以黄土钙质结核作为吸附剂,以重金属离子(Cu~(2+),Zn~(2+),Cd~(2+)和Pb~(2+))作为吸附质,通过单一重金属吸附试验,研究不同粒径、吸附时间、pH、吸附剂用量、重金属初始浓度和温度等因素对钙质结核吸附重金属离子的影响,并确定钙质结核吸附重金属离子的最优条件。结果表明:随粒径增大,Cu~(2+),Zn~(2+)和Pb~(2+)的吸附率逐渐下降,但对Cd~(2+)无明显影响;随吸附时间、吸附剂用量和温度的增加,Cu~(2+),Zn~(2+),Cd~(2+)和Pb~(2+)的吸附率逐渐升高;随重金属离子初始浓度的增加,Cu~(2+),Zn~(2+)和Cd~(2+)的吸附率逐渐下降,而Pb~(2+)的吸附率则呈先增加后减少的趋势;随pH增大,Cd~(2+)的吸附率先陡然增加后缓慢增加,而Cu~(2+),Zn~(2+)和Pb~(2+)的吸附率先增加后减少。钙质结核对4种重金属离子的吸附能力呈Pb~(2+)Zn~(2+)Cu~(2+)Cd~(2+)的顺序;在粒径为0.25 mm、吸附时间为120 min、用量为0.6 g时,钙质结核对Pb~(2+),Zn~(2+)、Cu~(2+)和Cd~(2+)能达到较好的吸附,吸附率分别能达到其最大吸附率的83.33%,77.78%,73.81%和81.93%。钙质结核对Pb~(2+),Zn~(2+)、Cu~(2+)和Cd~(2+)的最优吸附pH分别为7,6,5,8,最优温度为50℃。     

含Ni六方水钠锰矿的表征及其对Pb 2+ (Zn2+)环境行为的影响

六方水钠锰矿是土壤中普遍存在、活性最强的氧化锰矿物。它常常富集各种过渡金属如Ni等,对其地球化学行为具有重要影响。在六方水钠锰矿形成过程中加入Ni²⁺,Ni以+2价存在于矿物中。进入水钠锰矿结构中的Ni大部分以[NiO₆ ]八面体形式存在于层内;仅有小部分Ni存在于八面体空位上下方。含Ni水钠锰矿沿c轴方向堆叠锰氧八面体层数逐渐减小,而a-b板面晶体大小没有明显变化,即层片状晶体逐渐变薄,比表面积显著增大。随着Ni含量的增加,水钠锰矿结构中锰氧八面体空位数减少,而层边面吸附位点数基本保持不变,其对重金属离子(Pb²⁺/Zn²⁺)吸附去除能力逐渐降低。本文为明确过渡金属离子(Ni)对土壤中氧化锰矿物的形貌、结构及其性质的影响提供了参考。     

不同pH下有机酸对针铁矿和膨润土吸附Cd2+、Pb2+的影响

用平衡吸附法研究了不同pH下,三种有机酸(乙酸、酒石酸和柠檬酸)对针铁矿和膨润土等温吸附Cd2 、Pb2 的影响。结果表明:在加入的Cd2 、Pb2 浓度分别小于0.2 mmol L-1和4.0 mmol L-1时,针铁矿和膨润土吸附平衡体系的pH随加入重金属浓度的增加而降低,膨润土体系的pH降低更明显。在有机酸作用下,pH对针铁矿和膨润土吸附Cd2 、Pb2 的影响差异显著。3酒石酸>乙酸,其对膨润土吸附的影响差异不明显。     

柠檬酸对茶园紫色土微团聚体竞争吸附Zn、Cd影响

采用批量培养和平衡吸附法,选取原土及微团聚体颗粒组为对象,研究Zn(II)、Cd(II)单一存在、二元竞争及竞争体系中加入柠檬酸(0.1,1,10mmol/L)等3种处理的等温吸附特性及影响。结果表明:(1)以专性吸附方式为主的多层吸附随Zn~(2+)、Cd~(2+)强度增加逐渐饱和,吸附能力以0.002mm最优、0.05~0.002mm和原土次之,0.25~0.05mm和2~0.25mm结合能力稍差,不同条件下Cd较Zn更易积累。吸附过程为自发吸热反应,热力学Freundlich方程(Zn:R2=0.960~0.997;Cd:R2=0.957~0.995)拟合结果优于Langmiur方程(Zn:R2=0.952~0.995;Cd:R2=0.913~0.991)。最大吸附量与有机质含量具有显著相关性。(2)单一处理Zn、Cd的固持效果明显、共存处理时Zn、Cd竞争行为表现为彼此削弱,Zn对Cd的吸附具有更强抑制作用。(3)添加不同浓度柠檬酸后Zn、Cd吸附水平介于单一及共存处理之间呈动态变化(Zn、Cd接近),0.1~1mmol/L利于Zn、Cd固持,增至10mmol/L后加速淋洗,仅0.002mm粒径富集量持续提升。表明柠檬酸作为一种调节剂,能适度保持土壤Zn供给并弱化Cd迁移活性,缓解茶园土壤复合污染。     

SO42-和Cl-对稻田土壤养分及其吸附解吸特性的影响

利用长期定位试验 ,比较了长期施用含SO₄^2-和Cl^- 化肥 22年后稻田土壤的 pH值、养分状况及其吸附解吸特性。结果表明 ,长期施用含SO₄^2-化肥 ,土壤有机质、速效氮和速效钾的含量较高 ,但全量氮磷钾的含量较低 ;长期施用含Cl^- 化肥 ,土壤全量氮磷钾和速效磷的含量较高 ,但pH值相对较低。长期施用含上述二种阴离子的化肥后 ,土壤对H₂PO₄^-的最大吸附量均较大 ,且在Cl^- 处理下土壤对H₂PO₄^-吸附的结合能较大 ,而SO₄^2-处理下土壤在同等吸附量时对H₂PO₄^-的解吸量相应较多。长期施用含SO₄^2-的化肥亦使土壤对钾素的供应强度较大 (ΔK0的绝对值较大 )、缓冲能力增强 (AR0值较高 ) ,而长期施用含Cl^- 的化肥时则与SO₄^2-相反     

不同浓度Hg2+ 、Cr3+ 和Pb2+单一胁迫对绿豆膜脂过氧化物含量及抗氧化酶活性的影响

研究了不同浓度Hg2+、Cr3+ 和Pb2+胁迫条件下,绿豆花荚期叶片中膜脂过氧化物（MDA）含量及抗氧化酶,包括(超氧化物歧化酶(SOD)、过氧化物酶(POD)和过氧化氢酶(CAT))活性的变化情况。结果表明,Hg2+、Cr3+和Pb2+胁迫后,随着浓度的升高,绿豆叶片中MDA含量也逐渐升高,与对照相比均呈差异显著性;在Cr3+和Pb2+胁迫下,绿豆叶片中SOD酶活性随着浓度的升高呈现升高的趋势;在低、中浓度Hg2+胁迫下,SOD酶活性低于对照,但高浓度下,SOD酶活性高于对照;Hg2+处理后,POD随着浓度的增加,表现出先升高后降低又升高的趋势;低、中浓度Cr 3+处理使绿豆叶片内POD活性降低,但在高浓度时表现出POD活性增强;随着Pb2+处理浓度的增加,POD活性逐渐降低;Hg2+ 和Cr3+处理使CAT活性升高,但Pb2+处理后,CAT活性随浓度的升高先下降,再升高,然后又下降。研究表明Pb2+对绿豆的生态毒性较大。     

不同土地利用方式土壤对铜、镉离子的吸附解吸特征

采用一次平衡法对Cu²⁺、Cd²⁺在城市及城郊农田、林地、草地3种土地利用方式土壤中的吸附解吸过程进行比较研究, 结果表明: Cu²⁺、Cd²⁺在3种土地利用方式土壤中的吸附量均随平衡液浓度的增加而增大, Cu²⁺、Cd²⁺在农田土壤上的吸附量均高于林地和草地土壤。分别用Langmuir和Freunlich两种等温吸附方程对吸附过程进行拟合, 3种土壤对Cu²⁺的吸附过程运用Langmuir方程拟合效果好, 而对Cd²⁺的吸附过程运用Freunlich方程拟合效果更好。Cu²⁺在3种土壤的解吸量大小顺序为农田>林地>草地, Cd²⁺在3种土壤的解吸量大小顺序为农田>草地>林地。两种离子在3种土壤中的动态吸附是个快速反应的过程, 随时间延长, 吸附反应趋于平衡。运用双常数函数方程和Elovich方程能较好地拟合重金属在土壤上的吸附动力学过程。Cu²⁺、Cd²⁺的吸附与土壤黏粒含量、有机质含量、CEC和pH均有关。     

阴离子对可变电荷土壤吸附铜离子的影响机理

根据NO-3、Cl-和SO24-对可变电荷土壤和恒电荷土壤吸附Cu2+的影响的比较,探讨了阴离子对可变电荷土壤吸附Cu2+的影响机理。结果表明,当3种阴离子的浓度相同时,在SO24-体系中铁质砖红壤对Cu2+的吸附率较在NO3-和Cl-体系中大得多,而在浓度相同的3种阴离子体系中,黄棕壤对Cu2+的吸附率相差不大。在离子强度相近的NaCl体系中,砖红壤对Cu2+的吸附率相近。在3种阴离子体系中,随着pH升高,砖红壤对Cu2+的吸附率均增大;但在NO-3体系和Cl-体系中Cu2+的吸附率相近;而在SO24-体系中Cu2+的吸附率最大。随着Na2SO4浓度的增大,铁质砖红壤和砖红壤对Cu2+的吸附率减小。但在0.005 mol L-1和0.05 mol L-1Na2SO4体系中,Cu2+的吸附率大于在不含Na2SO4的体系中者。而在0.5 mol L-1Na2SO4体系中,Cu2+吸附率小于在不含Na2SO4体系中者。在3种浓度的Na2SO4体系中,黄棕壤对Cu2+的吸附率均小于在不含Na2SO4体系中者。总之,阴离子可通过离子强度、专性吸附和形成离子对影响土壤对Cu2+的吸附。在可变电荷土壤中,阴离子对Cu2+吸附的影响机理较在恒电荷土壤中复杂得多。     

KINETICS OF ION EXCHANGE IN SOIL ORGANIC MATTER. IV. ADSORPTION AND DESORPTION OF Pb2+, Cu2+, Cd2+, Zn2+ AND Ca2+ BY PEAT

The equilibria as well as the rates of adsorption and desorption of the ions Pb²⁺, Cu²⁺, Cd²⁺, Zn²⁺, and Ca²⁺ by soil organic matter were determined in batch experiments as a function of the amount of metal ions added to an aqueous suspension of HCl-washed peat. Simultaneous determination of the metal ions and hydrogen ions in the solution by atomic absorption spectrophotometry and pH-measurements showed that the adsorption of one divalent metal ion by peat was coupled with the release of two hydrogen ions. Since this equivalent ion-exchange process causes a corresponding increase of the electric conductivity of the solution, the rates of the adsorption and desorption processes were determined by an immersed conductivity electrode. The distribution coefficients show that the selective order for the metal adsorption by peat is Pb²⁺ > Cu²⁺ > Cd²⁺≌ Zn²⁺ > Ca²⁺ in the pH range of 3·5 to 4·5. The slope of -2, as observed in a double logarithmic plot of the distribution coefficients versus the total solution concentration confirms the equivalence of the ion-exchange process of divalent metal ions for monovalent H₃O⁺ -ions in peat. The absolute rates of adsorption, as well as the rates for the fractional attainment of the equilibrium, increase with increasing amounts of metal ions added. This behaviour is also observed for the subsequent desorption of the metal ions by H₃O⁺-ions. At a given amount of metal ions added, the absolute rates of adsorption decrease in the order Pb²⁺ > Cu²⁺ > Cd²⁺ > Zn²⁺ > Ca²⁺, while the rates for the fractional attainment of the equilibrium decrease in the order Ca²⁺ > Zn²⁺≌ Cd²⁺ > Pb²⁺ > Cu²⁺. The half times for adsorption and desorption were in the range of 5 to 15 sec.     

The Adsorption Behavior of Pb<Superscript>2+</Superscript> and Cd<Superscript>2+</Superscript> in the Treated Black Soils with Different Freeze-Thaw Frequencies

Batch experiments were conducted to study the effect of freeze-thaw frequency on the adsorption behavior of Pb²⁺ and Cd²⁺ and its related mechanisms. The results indicated that the adsorption capacities of Pb²⁺ and Cd²⁺ to the freeze-thaw treated soil were lower than those to the unfrozen soil, and with increasing freeze-thaw frequency, the adsorption capacities of them decreased. These were attributed to the fact that freeze-thaw cycles reduced pH value, CEC, organic matter content, and free iron oxide content of soil, and these soil properties presented negative correlations with freeze-thaw frequency. Freeze-thaw cycles reduced specific adsorption capacities of Pb²⁺ and Cd²⁺ and enhanced nonspecific adsorption ratios of Pb²⁺ and Cd²⁺ compared with the unfrozen soil. The higher freeze-thaw frequency, the higher nonspecific adsorption ratio was. However, the relationship between specific adsorption capacities of Pb²⁺ and Cd²⁺ and freeze-thaw frequency was opposite. Furthermore, the adsorption processes to the unfrozen and freeze-thaw treated soils were spontaneous, for Pb²⁺, its adsorption to soil was endothermal process, for Cd²⁺, on the contrary.     

NO-3胁迫下K+、Ca2+对黄瓜幼苗膜质过氧化及活性氧清除酶系统的影响

通过水培试验探讨了NO^-₃胁迫下K⁺、Ca²⁺对黄瓜幼苗膜质过氧化及活性氧清除酶系统的影响。结果表明，在相同NO^-₃浓度胁迫7d后， Ca²⁺浓度越大，膜脂过氧化产物丙二醛(MDA)含量越高，而K⁺浓度越大，电解质相对渗透率越高，由此说明K⁺、Ca²⁺对细胞膜造成伤害的机理不同。黄瓜幼苗活性氧清除酶系统对K⁺、Ca²⁺的响应亦不同，在一定程度上，K⁺和Ca²⁺ 可提高SOD、POD和CAT活性，保护植物免受自由基伤害，继而可增强植物对逆境的适应能力。     

Two-stage Batch Adsorber Design: A Time-Dependent Langmuir Model for Adsorption of Pb2+ and Cd2+ onto Modified Kaolinite Clay

The kinetics of the adsorption of Pb²⁺ and Cd²⁺ by sodium tetraborate (NTB)-modified kaolinite clay adsorbent was studied. A one-stage and two-stage optimization of equilibrium data were carried out using the Langmuir and time-dependent Langmuir models, respectively. Increasing temperature was found to increase the pseudo-second order kinetic rate constant and kinetic data for Pb²⁺ adsorption were found to fit well with the pseudo-second order kinetic model (PSOM) while that for Cd²⁺ were found to show very good fit to the modified pseudo-first order kinetic model (MPFOM). Binary solutions of Pb²⁺ and Cd²⁺ reduced the adsorption capacity of the modified adsorbent for either metal ion with increased initial sorption rate due to competition of metal ions for available adsorption sites. The use of NTB-modified kaolinite clay adsorbent reduces by approximately 72.2% and 96.3% the amount of kaolinite clay needed to adsorb Pb²⁺ and Cd²⁺ from wastewater solutions. From the two-stage batch adsorber design study, the minimum operating time to determine a specified amount of Pb²⁺ and Cd²⁺ removal was developed. The two-stage batch adsorption process predicted less than half the minimum contact time to reach equilibrium in the one-stage process for the adsorption of Pb²⁺ and Cd²⁺ by NTB-modified kaolinite clay adsorbent and requires 0.05 times the mass of the adsorbent for the single-stage batch adsorption at the same operating conditions.     

Effects of Salinity and Water Stress on Echophysiological Parameters and Micronutrients Concentration of Pomegranate (Punica granatum L.)

In order to study the effects of salinity and drought stress on echophysiological parameters and micronutrients concentration of pomegranate leaves, a factorial experiment was conducted based on completely randomized design with 0, 30, and 60 mM of salinity levels of sodium chloride and calcium chloride (1:1) and three irrigation intervals (2, 4, and 6 days) with three replications on ‘Rabab’ and ‘Shishegap’ cultivars of pomegranate. The results analysis of shoot and root indicated that the water salinity and drought affected the concentration of iron (Fe²⁺), zinc (Zn²⁺), copper (Cu²⁺) and manganese (Mn²⁺) in pomegranate leaves and roots. Mineral concentration of zinc (Zn²⁺), copper (Cu²⁺) and manganese (Mn²⁺) in roots and manganese (Mn²⁺) in shoot was increased with increasing salinity. Drought treatments decreased the concentration of Zn²⁺ in the shoot and increased Zn²⁺ in roots. Both cultivars showed significant differences in the Fe²⁺ concentrations of shoot, however the most accumulation of Fe²⁺ was observed in ‘Shishegap’ cultivar.     

几种铵盐对土壤吸附Cd2+和Zn2+的影响

采用平衡吸附法,研究了不同铵盐对潮褐土、红壤吸附Cd2+、Zn2+的影响。结果表明,土壤对Cd2+、Zn2+的吸附量随平衡溶液中Cd2+、Zn2+浓度的增加而增加;潮褐土和红壤对Cd2+、Zn2+的最大吸附量为:Zn2+ Cd2+,且潮褐土红壤;随NH4HCO3浓度的增加,两种土壤对Cd2+、Zn2+的吸附率显著提高,NH4Cl、NH4NO3和(NH4)2SO4抑制红壤对Cd2+、Zn2+的吸附及潮褐土对Cd2+的吸附,对潮褐土Zn2+的吸附率影响不显著;铵盐浓度相同时,红壤对Cd2+吸附率为:NH4HCO3NH4ClNH4NO3≈ (NH4)2SO4,红壤对Zn2+吸附率为:NH4HCO3NH4Cl NH4NO3(NH4)2SO4。     

The in vivo and in vitro effects of Ca2+ and Al3+ upon ATPases from barley roots

Experiments were performed to test the effect of Ca²⁺ and Mg²⁺ upon ATPases (E.C. 3.6.1.3) from barley roots (Hordeum distichon L. cv. MULTUM) that had or had not taken up Al³⁺. Furthermore, the effect of the uptake period was examined. With longer duration of the Al³⁺ uptake, the activity of the ATPases dropped, independently of whether they were activated by Ca²⁺ or by Mg²⁺. Mg²⁺ stimulated the activity of the ATPases if no Al³⁺ had been taken up with lacking Ca²⁺ in the assay. If Al³⁺ had been taken up no additional activation by Mg²⁺ to the Ca²⁺ stimulation could be observed, and in some cases Mg²⁺ decreased the Ca²⁺ stimulation.     

锌离子活度对水稻产量及子粒锌含量的影响及基因型差异

试验采用HEDTA螯合缓冲营养液培养法,选用子粒含锌量有明显差异的两个水稻基因型(碧玉早糯和浙农921),采用4种锌离子活度(pZn2+9.7,10.3,11.0,11.4),研究了锌离子活度对水稻产量和子粒锌积累、分配与子粒品质的影响及基因型差异。结果表明,锌离子活度通过对水稻有效穗数、每穗颖花数、结实率和千粒重的影响而显著影响水稻单株产量,其中影响最大的是单株有效穗数,其次是每穗颖花数,而对结实率的影响相对较小,但均存在明显的基因型差异。锌离子活度显著影响水稻子粒锌含量,随锌离子活度下降,水稻子粒含锌量降低,当锌离子活度低于pZn2+10.3时,两基因型水稻的含锌量均显著降低,但基因型间存在明显差异。不论在何种锌离子活度下,碧玉早糯的子粒含锌量均显著高于浙农921。从子粒锌分配看,颖壳、糙米、精米锌含量均随着锌离子活度提高而提高,当pZn2+从10.3升高到9.7时,碧玉早糯的糙米和精米锌含量开始降低,颖壳锌含量则开始超过糙米的锌含量继续升高;而浙农921糙米和精米锌含量的升高幅度较颖壳锌含量小。不同锌离子活度下,糙米和精米锌含量的比值在0.790~.90之间变化,并以pZn2+为9.7时为最小。因此,通过筛选子粒富锌水稻品种来提高稻米锌含量经济可行;通过增加环境锌离子活度,改善水稻的锌营养能显著提高水稻子粒的锌含量。     

添加生物质炭对红壤性水稻土Cd2+吸附解吸特性的影响

为探讨生物质炭对红壤性水稻土中镉(Cd)元素吸附解吸特性的影响,采用一次平衡法研究添加生物质炭后Cd2+在红壤性水稻土中的吸附动力学、等温吸附和解吸过程。结果表明:施用CK(0t/hm^2)、A10(10t/hm^2)、A20(20t/hm^2)、A30(30t/hm^2)和A40(40t/hm^2)生物质炭后,红壤性水稻土对Cd2+的吸附过程是以化学吸附为主、非均匀的多表面吸附。施用CK(0t/hm^2)、A10(10t/h2)、A20(20t/hm^2)、A30(30t/hm^2)和A40(40t/hm^2)生物质炭处理的最大吸附量和最大解吸量分别为2933~3346mg/kg和171~192mg/kg。添加生物质炭可以提高红壤性水稻土对Cd2+的吸附固持能力,同时增强土壤对外源Cd2+的缓冲能力。生物质炭添加量对红壤性水稻土的吸附解吸能力的改良效果具体表现为:A30>A40>A20>A10。高剂量的生物质炭处理使土壤吸附点位饱和,生物质炭吸附能力相对降低。因此,添加30t/hm^2生物质炭是一种有效预防和治理红壤性水稻土镉污染的措施。