Sorption of pyrene on two paddy soils and their particle-size fractions

In the present study, the sorption of pyrene on two kinds of bulk paddy soils, Gleyic Stagnic Anthrosols, and Ferric accumulic Stagnic Anthrosols as well as their particle-size fractions was investigated. The sorption isotherms fitted well with Freundlich equation. For both soils, the clay fraction（ 〈 2μm） and coarse sand fraction（2000-250μm） had higher sorption capacity than fine sand fraction（250-20 μm） and silt fraction（20-2 μm）. The IogKoc values obtained of each soil and its particle-size fractions were similar, proving that SOM content was a key factor affecting pyrene sorption. The Kd values showed a significant correlation with contents of dithionite-extractable Fe in both paddy soils and a good relationship with CEC in Gleyic Stagnic Anthrosols, indicating possible effects of surface properties of particle-size fractions on the sorption of pyrene.     

黄泥土不同粒径微团聚体对Cd2+的吸附与解吸研究

对采自太湖地区黄泥土进行了低能量超声波分离,采用平衡吸附法研究了不同粒径微团聚体颗粒对重金属Cd²⁺的吸附和解吸特点.结果表明,不同粒径微团聚体对Cd²⁺的吸附特性均符合Freundlich方程,模拟方程得到的K值介于152～503之间,以粘粒级和粗砂级为最大.微团聚体对Cd²⁺的吸附容量与其中游离氧化铁含量、CEC呈显著正相关.不同微团聚体Cd的解吸特点不同,粘粒级的解吸率仅为8.4%,远远低于其它粒径的微团聚体,这些结果有助于了解田间条件下土壤重金属化学行为和微观尺度的化学过程.     

紫色水稻土颗粒有机质对重金属的富集特征

在重庆合川区和铜梁区随机采集了20个紫色水稻土,将其分成颗粒有机质(0.053~2 mm,POM)、砂粒(0.053~2mm)和细土(0.053 mm)这3个组分,通过比较不同组分的有机碳及重金属(Cu、Zn、Pb、Cd)含量和分布状况,研究了紫色水稻土中POM对重金属的富集特征及其与土壤理化性质如pH、CEC、黏粒和土壤有机碳(SOC)等的关系.结果表明,采样区紫色水稻土的POM含量范围为7.31~44.76 g·kg~(-1),平均值为19.20 g·kg~(-1),有机碳含量为96.61~263.17 g·kg~(-1),平均值为151.34 g·kg~(-1),显著高于原土及其他组分,对土壤有机碳的贡献率为8.63%~48.62%,代表了一大部分土壤有机碳库.POM中的Cu、Zn、Pb和Cd平均富集系数分别为3.35、1.14、2.88和2.14,显著高于其他组分,表现出一定的富集作用,对上述重金属的贡献率分别为6.02%、2.22%、5.24%和3.21%,POM对Cu、Pb的富集能力和贡献率均显著大于Zn和Cd.相关分析结果表明,POM含量与SOC、pH、CEC、黏粒(0.002 mm)呈显著或极显著正相关,SOC是主要因素.POM-C含量与总量分别与黏粒含量、SOC呈显著相关.POM中重金属总量与SOC、pH、POM-C总量呈显著或极显著正相关,SOC是最关键因子;与其他重金属相比,Zn在POM中的总量与土壤性质的回归系数最高,关系最为密切.     

Effects of free iron oxyhydrates and soil organic matter on copper sorption-desorption behavior by size fractions of aggregates from two paddy soils

Effects of free iron oxyhydrates (Fed) and soil organic matter (SOM) on copper (Cu2+) sorption-desorption behavior by size fractions of aggregates from two typical paddy soils (Ferric-Accumulic Stagnic Anthrosol (Soil H) and Gleyic Stagnic Anthrosol (Soil W)) were investigated with and without treatment of dithionite-citrate-bicarbonate and of H2O2. The size fractions of aggregates were obtained from the undisturbed bulk topsoil using a low energy ultrasonic dispersion procedure. Experiments of equilibrium sorption and subsequent desorption were conducted at soil water ratio of 1:20, 25℃. For Soil H, Cu2+ sorption capacity of the DCB-treated size fractions was decreased by 5.9% for fine sand fraction, by 40.4% for coarse sand fraction, in comparison to 2.9% for the bulk sample. However, Cu2+ sorption capacities of the H2O2-treated fractions were decreased by over 80% for the coarse sand fraction and by 15% for the clay-sized fraction in comparison to 88% for bulk soil. For Soil W, Cu2+ sorption capacity of the DCB-treated size fraction was decreased by 30% for the coarse sand fraction and by over 75% for silt sand fraction in comparison to 44.5% for the bulk sample. Cu2+ sorption capacities of the H2O2-treated fractions were decreased by only 2.0% for the coarse sand fraction and by 15% for the fine sand fraction in comparison to by 3.4% for bulk soil. However, Cu2+ desorption rates were increased much in H2O2-treated samples by over 80% except the clay-sized fraction (only 9.5%) for Soil H. While removal of SOM with H2O2 tendend to increase desorption rate, DCB- and H2O2-treatments caused decrease in Cu2+ retention capacity of size fractions. Particularly, there hardly remained Cu2+ retention capacity by size fractions from Soil H after H2O2 treatment except for clay-sized fraction. These findings supported again the dominance of the coarse sand fraction in sorption of metals and the preference of absorbed metals bound to SOM in differently stabilized status among the size fractions. Thus, enrichment and turnover of SOM in paddy soils may have great effects on metal retention and chemical mobility in paddy soils.     

稻田土壤性质与稻米镉含量的定量关系

水稻是高累积镉（Cd）的农作物,其吸收累积Cd的量受多种因素影响.为明确田间条件下,土壤中Cd含量和土壤性质与稻米Cd含量的定量关系,在水稻收获时通过对60个不同田块的土壤和稻谷进行点对点采样,分析土壤Cd含量、土壤pH值、土壤有机质（SOM）、土壤阳离子交换量（CEC）和稻米中Cd含量,并通过线性相关与多元回归分析,研究Cd污染稻田土壤性质与稻米Cd含量的定量关系.结果表明：所采稻田土壤Cd含量范围为0.15~2.54 mg·kg^-1,其对应的稻米Cd含量范围为0.02~2.00 mg·kg^-1;简单线性相关分析表明,土壤全Cd含量与水稻籽粒Cd含量达到了极显著相关水平（P<0.01）,相关性系数r=0.392（n=60）;土壤pH、有机质（SOM）和阳离子交换量（CEC）对稻米Cd含量也有一定的影响,但未达到显著水平;土壤pH与稻米Cd含量的关系呈现为：当pH小于6.5时,稻米Cd含量随着pH的升高而增加,当pH大于6.5时,稻米Cd含量随着pH的升高而降低.将土壤全Cd含量、土壤pH、有机质（SOM）、阳离子交换量（CEC）与稻米中Cd含量进行多元回归分析,得到5个稻米中Cd含量预测方程,其相关系数r均达到极显著水平（P<0.01）,其中包括全部变量在内的预测方程的相关性系数最高,可以较好地预测此地水稻籽粒中Cd含量.     

Pb和Cd赋存形态与土壤理化性质相关性研究

选择我国14种具有代表性的重金属污染土壤,测定其主要理化性质（pH、阳离子交换量、有机质、粉粒和黏粒）,采用改进的BCR顺序提取法对其中的Pb和Cd进行形态分析,运用SPSS 20.0软件进行Pearson相关性分析,建立逐步回归模型,研究重金属赋存形态与理化性质的相关性。结果表明,Pb和Cd的酸可溶态与pH值呈极显著负相关,相关性系数r分别为-0.80和-0.78,与阳离子交换量呈显著正相关,r分别为0.54和0.61,与有机质、粉粒和黏粒无相关性;Cd的可还原态与有机质呈显著正相关,r=0.56,与其它理化性质无相关性;可氧化态与有机质和黏粒呈显著正相关,与其它理化性质无相关性;残渣态与主要理化性质均无显著相关性。由逐步回归模型发现,酸可溶态、可还原态、可氧化态与理化性质回归效果均较好。     

芘在土壤不同粒径组分中的形态分布

以芘为PAHs代表物,采用土壤粒径分级和PAHs连续提取方法,研究了老化4周污染黄棕壤中芘在不同粒径组分中的形态分布.结果表明,供试土壤中芘主要以有机溶剂提取态和可脱附态存在,结合态残留量所占比例甚小;细砂粒、粉粒、粗黏粒和细黏粒中芘残留占原土总残留的比例分别为6.00%、4.66%、34.68%和40.88%.各粒径组分中各形态芘含量大小顺序为有机溶剂提取态>可脱附态>结合态,有机溶剂提取态和可脱附态是各粒径组分中芘残留的主要存在形态(占比98.82%以上),芘结合态残留量占比<1.18%.土壤中黏粒(包括细黏粒和粗黏粒)是芘可脱附态、有机溶剂提取态、结合态和可提取态残留储存的主要粒径组分.     

水稻土团聚体Cu2+吸附过程中铝的溶出及土壤溶液pH变化

采用低能量超声波分散和冷冻机干燥法提取太湖地区水稻土(黄泥土)不同粒径团聚体颗粒,用平衡吸附法研究团聚体对重金属Cu2+吸附过程中铝的溶出及土壤溶液pH变化,以及不同pH的Cu2+溶液中铝的溶出量的变化.结果表明,团聚体对Cu2+的吸附过程,发生铝的溶出和土壤溶液pH下降,溶出量和pH下降幅度随Cu2+吸附量增加而增加,相同条件下铝溶出量和pH下降幅度大小顺序为:粗粉砂级>粉砂级>砂粒级>黏粒级,与氧化铁和有机质含量大小顺序相反.Cu2+溶液pH下降,铝的溶出量增加显著.氧化铁和有机质对Cu2+吸附过程铝的溶出和土壤溶液pH下降具有一定的抑制和缓冲作用.     

黑土不同粒径有机-矿质复合体对镉的吸附特性

采用振荡平衡法研究了黑土不同粒级有机-矿质复合体对Cd2+的吸附等温过程和吸附动力学过程,并采用常见数值模型进行了拟合. 结果表明,原土及各粒级复合体对Cd2+的吸附量随平衡液中ρ(Cd2+)的增加而增加. 各粒级组分对Cd2+的吸附量表现为黏粒＞粉粒＞原土＞粗砂＞细砂. Langmuir和Freundlich方程对Cd2+的等温吸附过程均有较好的拟合效果,线性方程拟合效果较差. 最大吸附量与吸附作用强度均呈随粒径增大而减小的趋势. 对影响最大吸附量和吸附作用强度的因子进行回归分析表明,w(有机质)、CEC(阳离子交换量)和比表面积的影响较大,其中w(有机质)是最主要因素,CEC和比表面积的影响次之. 各粒级复合体对土壤吸附Cd2+的贡献率为粉粒＞细砂＞黏粒＞粗砂,99%的Cd2+吸附在＜200 μm的组分上. 不同粒级组分对Cd2+的吸附动力学过程可分为0~20 min的快速反应阶段（吸附量均达到饱和吸附量的90%以上）和慢速反应阶段. 各组分对Cd2+的吸附符合二级动力学过程,表明吸附过程以化学吸附为主,并且吸附速率随颗粒粒径的增大而减小.      

Mechanism and kinetics of aluminum dissolution during copper sorption by acidity paddy soil in South China

Soil aggregates were prepared from a bulk soil collected from paddy soil in the Taihu Lake region and aluminum (Al) dissolution, solution pH changes during copper (Cu^2 +) sorption were investigated with static sorption and magnetic stirring. Kinetics of Cu^2 + sorption and Al dissolution were also studied by magnetic stirring method. No Al dissolution was observed until Cu^2 + sorption was greater than a certain value, which was 632, 450, 601 and 674 mg/kg for sand, clay, silt, and coarse silt fractions, respectively. Aluminum dissolution increased with increasing Cu^2 + sorption and decreasing solution pH. An amount of dissolved Al showed a significant positive correlation with non-specific sorption of Cu^2 + (R² > 0.97), and it was still good under different pH values (R² > 0.95). Copper sorption significantly decreased solution pH. The magnitude of solution pH decline increased as Cu^2 + sorption and Al dissolution increased. The sand and clay fraction had a less Al dissolution and pH drop due to the higher ferric oxide, Al oxide and organic matter contents. After sorption reaction for half an hour, the Cu^2 + sorption progress reached more than 90% while the Al dissolution progress was only 40%, and lagged behind the Cu^2 + sorption. It indicated that aluminum dissolution is associated with non-specific sorption.     

植被恢复对旱区表土颗粒中有机碳和氮分布的影响

采用物理分离的方法,获得植被恢复过程中不同土壤粒径的组分,并进行了各组分中有机碳和全氮含量的测定.结果表明,黏粉粒(<0.05mm)含量的增加和沙粒(0.25～0.1mm)含量的减少,共同导致表层土壤质地细粒化.土壤质地的细粒化伴随着有机碳和氮的固存效应,该效应在固沙20年以后效果显著(P<0.05).沙粒(>0.1mm)含量与有机碳和氮含量呈显著负相关(P<0.001),而极细沙(0.1～0.05mm)和黏粉粒(<0.05mm)含量与有机碳和氮含量均呈显著正相关(P<0.001).产生上述结果的原因是,表层土壤颗粒组成中各粒径结合的有机碳和氮含量均增加相关,其贡献程度为黏粉粒>极细沙>沙粒.植被恢复过程中,表层土壤中黏粉粒含量的增加对维持有机碳和氮固存起着主要的作用,土壤的物理稳定也因为土壤中有机质和黏粉粒含量的增加而增大.     

地层介质对垃圾渗滤液的pH缓冲性能研究

通过一维土柱穿透实验和静态实验,分别从空间和时间2方面研究了不同天然地层介质对垃圾渗滤液的PH缓冲性能.结果表明,细砂、粉砂和粘土的本底pH缓冲容量分别为79.9·pH-1 mmol/kg、207.5·pH-1 mmol/kg、456.4·PH-1 mmol/kg.受垃圾渗滤液污染后,除细砂外,随着时间的延长、离污染源距离的减小,每种介质总的pH缓冲容量都逐渐减小;其中碳酸钙缓冲体系的缓冲容量均逐渐增大;硅酸盐、阳离子交换缓冲体系的缓冲容量无明显变化;铝、氧化铁缓冲体系的缓冲容量逐渐减少,但土壤铝缓冲体系的缓冲容量则呈现出先增大后减少的趋势.细砂各个缓冲体系的缓冲容量随时、空变化均呈现出略微增大的趋势.4种介质对渗滤液的pH缓冲能力的顺序是:细砂<粉砂<粘土<土壤.土壤、粘土对垃圾渗滤液有较好的pH缓冲性能,同时对渗滤液中各种污染物的迁移,扩散也有较好的控制作用.     

不同镉浓度及pH条件下纳米沸石对土壤镉形态及大白菜镉吸收的影响

采用室内培养试验研究了不同镉浓度(1、5、10和15 mg·kg-1)及pH条件下(4、5、6、7和8)纳米沸石和普通沸石施用量(0、5、10和20 g·kg-1)对土壤镉形态分布和CEC的影响,并通过盆栽试验研究了纳米沸石和普通沸石施用量对大白菜生长、镉含量及积累量的影响.结果表明,施用纳米沸石和普通沸石均显著降低了土壤可交换态镉(EX-F)含量和FDC(即土壤中镉的某种形态占总镉的质量分数),增加了碳酸盐结合态(CAB-F)、铁锰氧化态(FMO-F)、有机态(OM-F)和残渣态(RES-F)镉含量和FDC.培养结束时,沸石处理使可交换态镉FDC从0 d时的72.0%~88.0%降至2.4%~10.7%,各处理土壤镉主要以可交换态存在.土壤pH与土壤EX-F镉含量存在极显著的负相关关系(P0.01),与FMO-F和OM-F镉含量存在极显著的正相关(P0.01).土壤CEC与土壤EX-F镉含量均存在极显著负相关关系(P0.01).施用沸石使大白菜植株各部位干重较对照增加了14.3%~131.4%,地上部和根镉含量分别降低了1.0%~75.0%和3.8%~53.2%.新晋菜三号各部位镉含量和镉积累量明显高于山东四号品种.与普通沸石相比,纳米沸石显著提高大白菜生物量的同时,也显著降低了大白菜镉含量及镉积累量.     

长期施肥下浙江稻田不同颗粒组分有机碳的稳定特征

依托浙江水网地区稻田长期定位施肥试验(1996~2013年),利用固态13C核磁共振波谱技术,研究长期不同施肥措施下土壤各颗粒组分有机碳含量及其化学结构特征.结果表明,与不施肥对照(CK)相比,秸秆与化肥配施(NPKRS)、栏肥与化肥配施(NPKOM)、单施化肥(NPK)和单施栏肥(OM)处理均显著(P0.05)增加了砂粒(2~0.02 mm)、粉粒(0.02~0.002mm)和黏粒(0.002 mm)组分中有机碳含量;而单施秸秆(RS)处理仅显著增加砂粒组分有机碳含量.此外,与单施化肥处理相比,有机肥和化肥配施促进了新增有机碳在粉粒和黏粒组分的分配,更有利于新增有机碳的稳定.应用13C-NMR波谱技术进行结构表征,结果表明粉粒和黏粒组分有机碳的化学结构存在明显差异,粉粒组分烷氧碳、芳香碳的相对含量高于黏粒,而烷基碳、羰基碳的相对含量低于黏粒.长期有机肥与化肥配施下粉粒和黏粒烷基碳相对含量较单施有机肥处理分别降低9.1%~11.9%和13.7%~19.9%,烷氧碳的相对含量则分别增加2.9%~6.3%和13.4%~22.1%,表明有机肥与化肥配施处理降低了粉粒和黏粒组分有机碳的分解程度.长期单施化肥处理下粉粒和黏粒组分有机质的芳化度和疏水性低于单施有机肥处理和不施肥处理,有机质的矿化稳定性较低.长期有机肥与化肥配施,尤其是NPKOM处理,通过增加化学抗性化合物和碳水化合物的积累,并且减缓活性组分的分解提高粉粒和黏粒组分有机碳含量,是促进稻田土壤有机碳可持续积累的有效措施.     

Atmospheric lead pollution in fine particulate matter in Shanghai, China

The Pb-monitoring program was extended for 6 years from 2002 to 2007 at 17 representative urban sites (6 traffic, 5 industrial, and 6 residential sites), and 3 suburban sites to assess the lead pollution in fine particulate matter (PM2.5) after phasing out leaded gasoline in Shanghai. Compared with Pb levels reported in other places, the Pb pollution in Shanghai is still serious after phasing out leaded gasoline, which remains at high concentration range (213–176 ng/m3) in PM2.5 in winter. Significant spati...     

菲在大庆黑钙土有机-矿质复合体上的吸附与解吸

利用超声分散法提取了黑龙江大庆黑钙土中不同粒级有机-矿质复合体,并测定了其基本理化性质.其中粘粒复合体的有机质含量最高,比表面积以及阳离子交换容量最大.研究了多环芳烃菲在不同粒级有机-矿质复合体上的吸附和解吸行为.结果表明,菲在各粒级有机-矿质复合体上的吸附和解吸等温线均符合Freundlich方程,随粒径减小,有机-矿质复合体对菲的吸附容量以及吸附的非线性程度都增加.菲在有机-矿质复合体上的解吸表现出明显的滞后现象.高有机质含量的粘粒有机-矿质复合体对菲的吸附和持留能力均较强.      

土壤有机质和镉对金霉素吸附-解吸的影响

金霉素已经广泛应用于兽药生产和疾病治疗.由于动物废弃物的土地应用和其它输入来源,重金属与四环素类抗生素往往共存于土壤环境中.基于OECD 106号指导准则,采用批量平衡实验方法,研究了金霉素及其与镉复合后在褐土及去有机质褐土中的吸附和解吸行为.结果表明,在单一和复合污染条件下,金霉素在褐土和去有机质褐土中的吸附和解吸等温线都可以用Freundlich模型进行良好地拟合.在金霉素单一污染和金霉素-镉复合污染条件下,去除有机质能够增加金霉素在褐土中的吸附容量(Kf)和吸附强度(1/n).金霉素在土壤上的解吸过程存在明显的滞后现象,在单一污染物情况下,金霉素在去有机质褐土的解吸滞后现象增强,其HI从0.81增加到1.06;而加镉后这种现象反而有所减弱,其HI从1.11减低到0.84.本研究为建立更加完善的模型以预测金霉素环境浓度或评价其环境风险,提供了可利用的数据和参数.     

Aqueous and organic extracts of Trigonella foenum-graecum L. inhibit the mycelia growth of fungi

Aqueous extracts from various plant parts of fenugreek (3%) (aerial parts: leaves and stems (LS), roots (R), ground seeds (GS) and not ground seeds (NGS)) and petroleum ether, ethyl acetate and methanolic fractions of the aerial parts were assayed to determine their antifungal potential against Botrytis cinerea, Fusarium graminearum, Alternaria sp., Pythium aphanidermatum, and Rhizoctinia solani. All fenugreek plant parts showed antifungal potential and the magnitude of their inhibitory e ects was species and plant parts dependent. R extract was shown less toxic (30.38%), whereas NGS extract expressed the strongest inhibition, with an average of 71.44%, followed by GS (58.56%) and LS (57.1%). Screening indicated that P. aphanidermatum was the most resistant species, with an average inhibition of 34.5%. F. graminearum, Alternaria sp. and R. solani were the most sensitive species, and were similarly inhibited (63.5%). The stability test indicated that the aqueous extracts of all plant parts lost approximately 50% of their relative activity after one month of storage at 4°C, whilst they lost 60%–90% of their activity when stored at ambient temperature for one month. The antifungal activity resided mainly in the methanol fraction and the minimum inhibitory concentration (MIC) of methanol fraction witch caused total inhibition of R. solani and Alternaria sp. was 60 g/ml. Results of current study suggested that the constituents of Trigonella foenum-graecum have potential against harmful pathogenic fungi. Therefore, fenugreek could be an important source of biologically active compounds useful for developing better new antifungal drugs.     

Crop residue removal and fertilizer N: Effects on soil organic carbon in a long-term crop rotation experiment on a Udic Boroll

Biofuels can be produced by converting cellulose in crop residues to ethanol. This has recently been viewed as a potential supplement to non-renewable energy sources, especially in the Americas. A 50-yr field experiment was analyzed to determine the influence of (i) removing approximately 22% of the above-ground wheat (Triticum aestivum L.) residue each crop year, and (ii) N and P fertilization on soil carbon (C) in the top 15 cm depth of a fallow–wheat–wheat (F–W–W) rotation. The study was conducted from 1958 to 2007 on a clay soil, at Indian Head in sub-humid southeast Saskatchewan, Canada. Soil C concentrations and bulk densities were measured in the 0–7.5 and 7.5–15 cm depths in 1987, 1996 and 2007 and soil C changes were related to C inputs estimated from straw and root yields calculated from regressions relating these to grain yields. Two soil organic matter models [the Campbell model and the Introductory Carbon Balance Model (ICBM)] were also used to simulate and predict the effects of the treatments on soil C change over time, and to estimate likely soil C change if 50% or 95% of above-ground residues were harvested each crop year. Crop residue removal reduced cumulative C inputs from straw and roots over the 50-yr experiment by only 13%, and this did not significantly (P > 0.05) reduce soil C throughout the experiment duration. However, after 50 yr of applying N fertilizer at recommended rates, soil C increased significantly by about 3 Mg ha⁻¹ compared to the non-fertilized treatment. The simulated effect of removing 50% and 95% of the above-ground residues suggested that removing 50% of the straw would likely have a detectable effect on the soil C, while removing 95% of the straw certainly would. Measurements and model simulations suggest that adoption of no-tillage without proper fertilization will not increase soil C. Although it appears that a modest amount of residue may be safely removed from these Udic Borolls (Black Chernozems) without a measurable effect on soil C, this would only be feasible if accompanied by appropriate fertility management.     

影响不同农作物镉富集系数的土壤因素

农作物的Cd富集系数（BCF）受多种因素影响.为明确田间条件下不同农作物的Cd富集系数特征差异及土壤性质对其影响,分别在我国水稻、小麦和玉米主产区不同污染程度的地块上作物收获期采集土壤和作物籽粒点对点样品,研究水稻、小麦、夏玉米和春玉米的Cd富集系数特征及土壤性质对不同农作物的Cd富集系数的影响,并通过多元回归方程建立以上农作物Cd富集系数与土壤性质的定量关系.结果表明,在田间土壤中Cd含量范围为0.15~2.66 mg·kg^-1条件下,水稻、小麦、夏玉米和春玉米Cd富集系数的均值分别为0.915、0.155、0.113和0.102,水稻明显高于小麦和玉米,春玉米的Cd富集系数最低.土壤中的Cd含量与小麦、夏玉米和春玉米的BCF呈极显著负相关;土壤有机质（SOM）与小麦、夏玉米BCF之间的关系呈极显著负相关;土壤pH和阳离子交换量（CEC）对作物BCF也有影响.引入土壤Cd含量、pH、SOM、CEC等因素,建立水稻、小麦、夏玉米和春玉米的Cd富集系数预测方程.水稻、小麦、夏玉米和春玉米的BCF预测方程相关系数分别为0.423^*、0.796^**、0.826^**和0.551^**,均达到显著或极显著水平,可以较好地预测不同土壤条件下不同农作物的BCF值.