白浆土NH_4~+吸附特征的影响因素

为探究白浆土对氮素的吸附规律及其影响因素,有效指导白浆土氮肥的科学施用,本研究采用平衡吸附法,研究了温度、有机质含量、振荡时间和离子强度等因素对白浆土吸附NH4+的影响,结果表明:(1)随初始NH+4浓度(0~1 000 mg/L)的增加,白浆土对其吸附量也增加,当NH+4浓度≥600 mg/L时,吸附渐趋饱和,温度升高(293~313 K)有利于该吸附反应的进行,表观热力学参数(ΔG0、ΔH0、ΔS0)的变化表明,NH+4在白浆土表面的吸附是自发、吸热且混乱度增加的过程。(2)剖面层次所引起的有机质含量递减亦会对白浆土吸附NH+4的数量有所抑制。(3)振荡时间影响白浆土吸附NH+4的动力学过程,该过程可分为起始的快速反应阶段及经过360 min后的慢速反应阶段,所选用的4个动力学方程均能较好拟合这一动态过程。应用过渡态理论所计算的活化热力学参数(ΔG≠0,ΔH≠0,ΔS≠0)表明,NH+4在白浆土上的动力学吸附过程是耗能且体系有序度增高的过程。(4)共存Na+在其不同浓度范围内对白浆土吸附NH+4的影响机制各有不同,当Na+≥0.4 mol/L时,提升其浓度有利于NH+4在白浆土上的吸附。综上所述,在较高土壤养分含量条件下,后移施用氮肥则更有利于其利用率的提升。     

羟基磷灰石对铅锌矿区土壤吸附Zn2+、Cd2+的影响

为探究羟基磷灰石(HAP)对矿区土壤重金属的固化效果,采用吸附试验,研究施加HAP的铅锌矿区土壤对Cd~(2+)、Zn~(2+)的动力学吸附和等温吸附效果。结果表明:土壤对Cd~(2+)、Zn~(2+)的吸附量随Cd~(2+)、Zn~(2+)初始浓度的增加而增加;在酸性条件下,其吸附量随pH上升而上升;准二级动力学方程能很好地描述两者的吸附过程,土壤吸附能力随HAP的添加量增大而增强;在Zn—Cd共存体系中,当初始浓度为20mg/L时,土壤对Zn~(2+)、Cd~(2+)的吸附无明显差异,2种金属离子竞争力度小,随着初始浓度上升,竞争明显,对Zn~(2+)的最大吸附量能达到单一体系中的79%～87%,而Cd~(2+)的最大吸附量只有单一体系中的57%～72%,Zn~(2+)的竞争力优于Cd~(2+),Zn~(2+)对Cd~(2+)吸附产生严重的抑制。综上可知,HAP能提高矿区土壤的吸附性能,在Zn、Cd污染土壤中,更能提升土壤对Zn~(2+)的吸附固持能力。     

Na~+、Ca~(2+)及Na~+-Ca~(2+)混合离子对胡敏酸胶体稳定性的影响

以胡敏酸为研究对象,通过光散射技术比较土壤中常见盐基离子(Na~+、Ca~(2+)和Na~+-Ca~(2+)混合三种电解质)不同浓度条件下胡敏酸胶体凝聚动力学过程,明确不同价态离子界面行为和陪补离子效应对胡敏酸分散稳定性和凝聚体结构的影响。结果发现,Na~+和Ca~(2+)对胡敏酸胶体聚沉能力的差异远远大于舒尔策-哈迪(Schulze-Hardy)规则中因其化合价不同所引起的差异;Na~+-Ca~(2+)混合体系中Ca~(2+)主导凝聚过程,且Na~+-Ca~(2+)混合与Ca~(2+)两种离子体系中凝聚现象的差异随离子浓度的降低而增大;混合离子体系中Na~+作为陪补离子,其陪补离子效应对临界聚沉浓度、颗粒间活化能和胡敏酸凝聚体结构均有一定影响,尤以对凝聚体的结构特征影响显著;Na~+-Ca~(2+)混合体系中胡敏酸凝聚体的结构紧实程度介于单纯离子体系之间,因此可通过调节溶液中的离子组成实现对凝聚体结构紧实程度的调控。上述结果表明,Ca~(2+)对胡敏酸的聚沉不仅依赖于静电作用,还有Ca~(2+)在强电场中的极化诱导其与胡敏酸表面含氧官能团之间发生的共价键和桥键的贡献;此外,陪补离子Na~+与Ca~(2+)在胡敏酸胶体表面的竞争吸附抑制了Ca~(2+)对胡敏酸的聚沉作用,从而形成紧实程度适中的结构体。研究结果为探究胶体界面反应及土壤胶体凝聚机制提供新的思路和理论。     

诺氟沙星在胡敏酸上的吸附热力学与动力学特征研究

根据OECD Guideline106批平衡实验,研究了诺氟沙星在胡敏酸上的吸附热力学和动力学,并探讨了其可能吸附机理。结果表明,诺氟沙星在经过约12h的快速吸附阶段后,进入缓慢吸附阶段,其吸附平衡时间为48h。伪二级动力学方程能够较好地描述不同pH条件下诺氟沙星在胡敏酸上的吸附动力学特性。诺氟沙星在胡敏酸上的吸附等温线符合Freundlich方程,该方程的拟合系数1/n〈0.5,表明诺氟沙星在胡敏酸上为非线性吸附。ΔH0=-48.85kJ·mol-1和ΔG0〈0,表明诺氟沙星在胡敏酸上的吸附是自发进行的放热过程,且离子交换是其主要吸附机理,同时也可能存在着偶极间作用力、氢键力和电荷转移等吸附机理;ΔS0〈0表明吸附过程中熵在减小。吸附位点的能量随着吸附量的增大而降低,也表明胡敏酸的异质性和吸附的非线性。     

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。     

红壤对铝锰离子的吸附特征 Ⅳ.铝锰交换钙钾离子的化学现象

铝、锰离子与钙或钾质固相之间的交换吸附也出现非等当量交换和非电性吸附,而钙、钾离子对交换反应则为电性吸附;非电性吸附量决定于固相表面的场强,也与离子的水解性质和价数有关,其中以铝离子在砖红壤、红壤中的非电性吸附最为强烈;从能量角度综合说明了k、K、1/ n 与ΔF的联系,铝离子的交换吸附具有最大的k、K和最小的1/ n,ΔF为负值;从热力学进一步证论了红壤铝质化的机理,在自然条件下红壤酸化应是一个连续的自发和不可逆过程。     

新型碱性肥料治酸改土降镉的效果和机理

通过大田试验和模拟实验,研究碱性肥料治酸改土的效果、土壤pH对Cd吸附解吸热力学性能的影响,为碱性肥料治理土壤酸化和降低土壤Cd污染提供理论依据。结果表明:碱性肥料能明显提高大田土壤pH、显著降低土壤有效镉含量,明显遏制土壤酸化和土壤镉污染。施用碱性肥料是提高土壤pH和降低土壤有效镉含量的有效措施。当土壤Cd含量小于等于60mg·L^-1时,pH从5增加到9时几乎不影响Cd的吸附强度(在15.77 mg·kg^-1/(mg·L^-1)～16.67 mg·kg^-1/(mg·L^-1)之间);而当Cd含量大于60 mg·L^-1,Cd的吸附强度随pH的升高而明显增大,但吸附率随浓度的增大而减少。土壤Cd含量相等时,pH越高土壤Cd的吸附量及吸附率越大。土壤Cd的等温吸附曲线适于用Freundlich方程拟合和定量描述。土壤吸附Cd是自发反应过程,表现为Cd的吸附自由能(ΔG°)为负。同一pH下,ΔG°随着土壤Cd含量的增大而增大;ΔG°随着土壤溶液pH的升高而减小。碱性...     

不同土地利用方式对黑土胶散复合体的影响及与酸度的关系

以吉林省黑土玉米带区域内10对长期定位采样点的2种土地利用方式土壤(耕作黑土和防护林带黑土)为研究对象,采用胶散分组法提取土壤胶散复合体,探究长期不同利用方式对黑土胶散复合体和酸度的影响。结果表明:耕作黑土与防护林带黑土均表现为G_0与G_2组的绝对含量增加,G_1组的绝对含量下降,复合体总量分别下降了3.88%和0.28%。耕作黑土和防护林带黑土pH分别平均下降12.12%和3.77%,有机碳含量在耕作黑土和防护林带黑土中分别平均下降23.17%和9.00%,2种利用方式土壤的胡敏酸、富里酸、交换性钙离子和碳酸钙均出现下降;耕作黑土分别平均下降12.18%,3.53%,16.29%,31.53%;防护林带黑土分别平均下降20.07%,13.14%,2.81%,7.81%。G_1组与pH、HA、Ca~(2+)和CaCO_3呈极显著正相关,与FA呈显著负相关;G_2组与pH、HA、Ca~(2+)和CaCO_3呈极显著负相关。pH与HA、Ca~(2+)和CaCO_3呈极显著正相关,与FA呈显著负相关。经过11年的变化,黑土胶散复合体稳定性下降,相比非耕作状态下黑土,耕作模式下的黑土胶散复合体稳定性下降更为严重,胶散复合体总量下降的更多,酸度下降更为明显。Ca~(2+)和HA的变化是影响黑土土壤酸化和土壤团聚体稳定性的主要驱动因素。土壤酸化的结果使土壤胶散复合体数量减少,稳定性变差。     

长江三角洲地区典型土壤对镉的吸附及其与有机质、pH和温度的关系

土壤重金属吸附-解吸反应影响重金属的迁移性、生物有效性和潜在毒性,研究土壤重金属的吸附-解吸过程及其机制对土壤污染评价、修复及环境容量预测至关重要。本文研究了长江三角洲地区四种典型土壤对Cd的吸附行为及有机质、pH和温度对土壤Cd吸附的影响,并运用热力学参数K°、ΔG°、ΔH°和ΔS°解释了土壤镉的吸附机制。研究结果表明,在本实验条件下,四种典型土壤镉吸附反应均很好地符合Fre-undlich模型。土壤镉吸附Kf值大小为:滩潮土(石质淡色潮湿雏形土)(238.8dm3kg-1)>乌黄土(底潜铁聚水耕人为土)(115.4dm3kg-1)>青紫泥(普通潜育水耕人为土)(54.40dm3kg-1)>黄泥砂土(铁聚潜育水耕人为土)(10.74dm3kg-1),滩潮土镉吸附Kf是黄泥砂土的24倍。土壤镉吸附量随溶液初始pH和土壤pH升高而增大;去除有机质后的土壤对镉的吸附量降低。吸附反应热力学表明,K°和ΔS°随温度升高而增大,ΔG°随温度升高而降低。ΔG°为负值表明镉吸附反应为自发反应,ΔH°为正值表明土壤镉吸附为吸热反应。     

磁性壳聚糖微球吸附苹果汁有机酸的动力学及热力学特性

为充分利用中国丰富的苹果资源,开发多品类的苹果深加工产品,以磁性壳聚糖微球为吸附剂,通过磁分离技术,吸附获得苹果汁中的天然有机酸,并对其吸附过程进行研究。利用Lagergren准一级动力学方程、准二级动力学方程、Elovich方程及内扩散方程对吸附反应动力学过程进行拟合;利用Langmuir等温吸附模型、Freundlich等温吸附模型及Temkin等温吸附模型对吸附等温数据进行拟合,并对其吸附反应热力学特性进行分析。通过比较线性拟合方程的决定系数,发现磁性壳聚糖微球吸附苹果汁中有机酸的动力学过程更加符合Lagergren准二级动力学模型,吸附温度越高,吸附速率常数和初始吸附速率越大,但平衡吸附量越低。等温吸附过程更加符合Langmuir等温吸附模型,表明该吸附过程更趋向于单分子层的化学吸附。298 K时,有机酸的饱和吸附量可达到188.679 2 mg/g,表明磁性壳聚糖微球是苹果汁中有机酸的1种高效吸附剂。热力学参数ΔG°0,ΔH°0,ΔS°0,表明磁性壳聚糖微球对苹果汁有机酸的吸附过程为熵增加的可自发进行的放热过程。动力学及热力学结果为磁性壳聚糖微球吸附苹果汁有机酸的研究提供了理论基础与技术支持。     

Response of plant yield and leaf pigments to saline conditions: Effectiveness of different rootstocks in melon plants (Cucumis melo L.)

Two varieties of Cucumis melo (Resisto and Arava) were grafted onto three hybrids of Cucurbita maxima and Cucurbita moschata cultivars (Shintoza, RS-841 and Kamel). Ungrafted Cucumis melo var. Resisto and var. Arava plants were used as controls. Plants were grown under controlled greenhouse conditions and were constantly fertilized with macro- and micronutrients, supplied with irrigation water rich in Na⁺ and Cl^- Contents of chlorophylls a and b, carotene pigments, Cl^- and total and soluble Na⁺ and K⁺ ions were measured in all the scion parts of the plants. The results showed that grafted plants exhibited differences in the leaf content of Na+ and especially Cl^- in comparison with ungrafted plants. In addition, yield as well as leaf pigments appeared to be good indicators of Cl^- levels in scion parts. It is assumed that grafted plants developed various mechanisms to avoid physiological damage caused by the excessive accumulation of these ions in leaf, including the exclusion of Cl^- ion and/or decrease in Cl^- absorption by the roots and the replacement or substitution of total K⁺ by total Na⁺ in the foliar parts.     

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.     

Interactive Effect of Soil Salinity and Water Stress on Growth and Chemical Compositions of Pistachio Nut Tree

ABSTRACT

The effects of three sodium chloride (NaCl) levels (0, 1200, and 2400 mg kg^{? 1} soil) and three irrigation intervals (3, 7, and 14 d) on the growth and chemical composition of two Pistacia vera rootstocks (‘Sarakhs’ and ‘Qazvini’) were investigated under greenhouse conditions. Eight-week-old pistachio seedlings were gradually exposed to salt stress which afterward, water stress was initiated. At any irrigation interval, plant height and shoot and root dry weights of both rootstocks were reduced with increasing salinity. However, increasing irrigation intervals alleviated the adverse effects of soil salinity. A negative relationship observed between relative shoot growth and electrical conductivity of soil saturation extract (EC_e) confirmed the above findings. Under 3-d irrigation interval, the EC_e required to cause a 50% growth reduction was lower than those under 7- and/or 14-d irrigation intervals. Shoot and root chemical analyses indicated that the salinity as well as irrigation regime affected the concentration and distribution of sodium (Na⁺), potassium (K⁺), and chloride (Cl^?) in pistachio. The concentration of Na⁺, K⁺ and C1^? ions increased with a rise in NaCl level, and was generally declined with increasing irrigation interval. Based on plant height, shoot and root dry weights and the concentrations of Na⁺, K⁺, and C1^? in the plant tissues, at lowest irrigation intervals ‘Sarakhs’ shows a higher sensitivity to soil salinity than ‘Qazvini’, but with increasing irrigation interval, ‘Sarakhs’ and ‘Qazvini’ can be classified as resistant and sensitive to salinity, respectively.     

Effects of Cd on the fluxes of K+ and H+ in excised roots

As a result of Cd treatment, K concentrations decreased in Cd sensItive maize and kidney bean calli (Obata et al. 1994) and in intact roots of kidney bean plants (Obata et al. unpublished). Potassium may be extruded from the roots or the absorption of K may be depressed by the Cd treatment in these Cd sensitive plants. Obata et al. (1996) observed that Cd inhibited both the efflux of H⁺ and influx of K⁺ following K⁺ addition in intact roots of bean. Thus Cd may affect the activity of proteins essential to ion movement., i.e. ioncarriers, channels and ATPase embedded in the membranes and/or may affect the permeability of the lipids of the membrane.     

Effect of Soil Fertilizer,Foliar Fertilizer,and Growth Regulator Application on Milk Thistle Development,Seed Yield,and Silymarin Content

Abstract

An important consideration for milk thistle (Silybum marianum L.) cultivation is regulating development to lengthen the reproductive stage and increase seed yield with high silymarin content. The treatment of milk thistle with foliar fertilizers and growth regulators—thidiazuron (Dropp^®), 2,3,5‐triiodobenzoic acid (Tiba^®), mepiquat chloride (Pix^®), and prohexadione‐Ca (Regalis^®)—resulted in an increase in the proportion of mature flower heads. Highest seed yield was observed in plants treated with Pix^® and mineral soil fertilization, whereas in plants treated with foliar fertilizers, highest yields were observed with Pix^® and Regalis^®. The highest content of silymarin was found in plants treated with Dropp^® and foliar fertilizer. Generally, treatment of milk thistle with plant‐growth regulators in combination with soil or foliar mineral fertilizers increased the total amount of silymarin by increasing seed yield per hectare.     

A study of soil and fertilizer phosphorus intake by Barley plants,using Radioactive tracer technique

Introduction

Phosphorus applied on a phosphate deficient soil, by increasing the root development of the plant, or by stimulating the soil microflora especially in the rhizosphere, may increase the amount of phosphorus which the plant takes up from the soil. This present paper is a report on a pot culture investigation of such an effect of added phosphorus.     

Influence of extreme K:Na ratios and high substrate salinity on plant metabolism of crops differing in salt tolerance

Mineral regulation of two soybean varieties Jackson and Lee was investigated in long term water culture experiments using saline solutions. The effects of extreme K:Na ratios using chloride and sulfate as counterions were studied in the early stages of salinity.

The growth rates of both varieties were not affected by salinization. A K⁺ stimulated, intensive acropetal Cl^‐ translocation was observed in the salt sensitive variety Jackson. The varieties did not differ in Na⁺ translocation and in the suppression of Ca²⁺ and Mg²⁺ in the leaves. But the effect of the nature of salinization indicates already differences in Na uptake and translocation of the cultivars.

The avoidance of Cl^‐, but also of Ha⁺, in connection with influences of the resulting ionic imbalance on metabolic pathways are probably the most causative factors for the different tolerance to salinity of the two soybean varieties.     

Atmospheric nitrate deposition and the microbial degradation of cellobiose and vanillin in a northern hardwood forest

Human activity has increased the amount of N entering terrestrial ecosystems from atmospheric NO₃⁻ deposition. High levels of inorganic N are known to suppress the expression of phenol oxidase, an important lignin-degrading enzyme produced by white-rot fungi. We hypothesized that chronic NO₃⁻ additions would decrease the flow of C through the heterotrophic soil food web by inhibiting phenol oxidase and the depolymerization of lignocellulose. This would likely reduce the availability of C from lignocellulose for metabolism by the microbial community. We tested this hypothesis in a mature northern hardwood forest in northern Michigan, which has received experimental atmospheric N deposition (30 kg NO₃⁻-N ha⁻¹ y⁻¹) for nine years. In a laboratory study, we amended soils with ¹³C-labeled vanillin, a monophenolic product of lignin depolymerization, and ¹³C-labeled cellobiose, a disaccharide product of cellulose degradation. We then traced the flow of ¹³C through the microbial community and into soil organic carbon (SOC), dissolved organic carbon (DOC), and microbial respiration. We simultaneously measured the activity of enzymes responsible for lignin (phenol oxidase and peroxidase) and cellobiose (β-glucosidase) degradation. Nitrogen deposition reduced phenol oxidase activity by 83% and peroxidase activity by 74% when compared to control soils. In addition, soil C increased by 76%, whereas microbial biomass decreased by 68% in NO₃⁻ amended soils. ¹³C cellobiose in bacterial or fungal PLFAs was unaffected by NO₃⁻ deposition; however, the incorporation of ¹³C vanillin in fungal PLFAs extracted from NO₃⁻ amended soil was 82% higher than in the control treatment. The recovery of ¹³C vanillin and ¹³C cellobiose in SOC, DOC, microbial biomass, and respiration was not different between control and NO₃⁻ amended treatments. Chronic NO₃⁻ deposition has stemmed the flow of C through the heterotrophic soil food web by inhibiting the activity of ligninolytic enzymes, but it increased the assimilation of vanillin into fungal PLFAs.     

红壤交换性钙、镁和钾的分布及施肥对其影响

A leaching experiment was Carried out with repacked soil columns in laboratory to study the leaching process of a red soil derived from sandstone as affected by various fertilization practices.The treatments were CK(as a control),CaCO3,CaSO4,MgCO3,Ca(H2PO4)2,Urea,KCl,Multiple(a mixture of the above mentioned fertilizers) and KNO3,The fertilizers were added to the bare surface of the soil columns,and then the columns were leached with 120 mL deionized water daily through perstaltic pumps over a period of 92 days,At the end of leaching process,soils were sampled from different depths of the soil profiles ,i.o.,of 92 days,At the end of leaching process,soils were sampled from different depths of the soil profiles,I.e.0-5cm,5-10cm,10-20cm,20-40cm,and 40-60cm,The results showed when applying Ca,Mg,and K to the bare surface of the soil columns,exchangeable Ca^2 ,Mg^2 ,and K^ in the upper layer of the soil profile increased correspondingly,with an extent depending mainly on the application rates of Ca,Mg,and K and showing a downward trend,CaCO3,CaSO4,MgCO3,and Ca(H2PO4)2 treatments had scarcely and effect on movement of exchangeable K^ ,while CaCO3,and CaSO4 treatments singnificantly promoted the downward movement of exchangealble Mg^2 although these two treatments had no obvious effect on leaching losses of Mg,The fact that under Urea treatment,exchangeable Ca^2 and Mg^2 ,were higher as compared to CK treatment showed urea could prevent leaching of exchangeable Ca^2 and Mg^2 ,the obvious downward movement of exchangeable Ca^2 and Mg^2 was noticed in KCl treatment ,In Multiple treatment,the downward movement of exchangeable Ca^2 and Mg^2 was evident,while that of K^ was less evident,Application of KNO3 strongly promoted the downward movement of exchangeable Ca^2 and Mg^2 in the soil profile.