浙江林学院学报
浙江林學院學報
절강림학원학보
JOURNAL OF ZHEJIANG FORESTRY COLLEGE
2010年
1期
8-14
,共7页
窦春英%徐温新%叶正钱%张圆圆%姚芳%吕家珑
竇春英%徐溫新%葉正錢%張圓圓%姚芳%呂傢瓏
두춘영%서온신%협정전%장원원%요방%려가롱
土壤学%农田土壤%吸附%解吸%锌
土壤學%農田土壤%吸附%解吸%鋅
토양학%농전토양%흡부%해흡%자
soil science%cropland soils%adsorption%desorption%zinc
研究了中国6种典型农田土壤对锌的吸附-解吸特性,其中采自西北陕甘地区和东南地区浙江省的农田土壤各3种.结果表明,6种农田土壤对锌的吸附量均随平衡液锌浓度的增加而增大,均可用Langmuir方程、Freundlich方程和Temkin方程来描述,相关系数均达到显著或极显著水平;6种土壤对锌的解吸量随吸附量的增大而增加,它们的相关性也达到了显著或极显著水平.东南地区土壤对锌的最大吸附量明显高于西北地区,其中青紫泥的吸附量最大,达到3 333 mg·kg~(-1),黄绵土的最小(909mg·kg~(-1));而西北地区土壤对锌的缓冲能力、吸附固定能力和固定量方面强于东南地区的红壤和青紫泥,利用Langmuir方程得出6种土壤(黄绵土、石灰性褐土、塿土、红色石灰土、红壤和青紫泥)对锌的最大缓冲容量依次为213,164,263,294,16和25 mg·kg~(-1);根据土壤锌吸附.解吸的线性回归曲线,计算出当土壤锌解吸量为0时,这6种土壤锌的固定量分别为56,97,126,135,55和98 mg·kg~(-1).浙江红色石灰土由于其pH值与西北地区土壤相似,而有机质质量分数和阳离子交换量又比较高,故对锌的缓冲能力、吸附固定量高于西北地区土壤.
研究瞭中國6種典型農田土壤對鋅的吸附-解吸特性,其中採自西北陝甘地區和東南地區浙江省的農田土壤各3種.結果錶明,6種農田土壤對鋅的吸附量均隨平衡液鋅濃度的增加而增大,均可用Langmuir方程、Freundlich方程和Temkin方程來描述,相關繫數均達到顯著或極顯著水平;6種土壤對鋅的解吸量隨吸附量的增大而增加,它們的相關性也達到瞭顯著或極顯著水平.東南地區土壤對鋅的最大吸附量明顯高于西北地區,其中青紫泥的吸附量最大,達到3 333 mg·kg~(-1),黃綿土的最小(909mg·kg~(-1));而西北地區土壤對鋅的緩遲能力、吸附固定能力和固定量方麵彊于東南地區的紅壤和青紫泥,利用Langmuir方程得齣6種土壤(黃綿土、石灰性褐土、塿土、紅色石灰土、紅壤和青紫泥)對鋅的最大緩遲容量依次為213,164,263,294,16和25 mg·kg~(-1);根據土壤鋅吸附.解吸的線性迴歸麯線,計算齣噹土壤鋅解吸量為0時,這6種土壤鋅的固定量分彆為56,97,126,135,55和98 mg·kg~(-1).浙江紅色石灰土由于其pH值與西北地區土壤相似,而有機質質量分數和暘離子交換量又比較高,故對鋅的緩遲能力、吸附固定量高于西北地區土壤.
연구료중국6충전형농전토양대자적흡부-해흡특성,기중채자서북협감지구화동남지구절강성적농전토양각3충.결과표명,6충농전토양대자적흡부량균수평형액자농도적증가이증대,균가용Langmuir방정、Freundlich방정화Temkin방정래묘술,상관계수균체도현저혹겁현저수평;6충토양대자적해흡량수흡부량적증대이증가,타문적상관성야체도료현저혹겁현저수평.동남지구토양대자적최대흡부량명현고우서북지구,기중청자니적흡부량최대,체도3 333 mg·kg~(-1),황면토적최소(909mg·kg~(-1));이서북지구토양대자적완충능력、흡부고정능력화고정량방면강우동남지구적홍양화청자니,이용Langmuir방정득출6충토양(황면토、석회성갈토、루토、홍색석회토、홍양화청자니)대자적최대완충용량의차위213,164,263,294,16화25 mg·kg~(-1);근거토양자흡부.해흡적선성회귀곡선,계산출당토양자해흡량위0시,저6충토양자적고정량분별위56,97,126,135,55화98 mg·kg~(-1).절강홍색석회토유우기pH치여서북지구토양상사,이유궤질질량분수화양리자교환량우비교고,고대자적완충능력、흡부고정량고우서북지구토양.
Soil zinc (Zn) availability varies very greatly among different soils. Adsorption-desorption charac teristics of six typical cropland soils from northwest(Loess soil, calcareous cinnamon soil, and Lou soil) and southeast(red calcareous soil, red soil, and blue-purple soil) China were studied. Results showed that Zn adsorbed by soils increased with initial concentrations of Zinc added(from 0-149 mg·L~(-1) solutions) and that the soil Zn desorption rate increased with the soil adsorbed Zn. Isothermal curves of Zn adsorption from these six soils fit well to Langmuir, Freundlich, and Temkin equations with all the coefficients, except the blue-purple paddy soil, being>0.9. Soil organic matter content contributed the most to soil Zn adsorption, so regardless soil pH, maximum Zn adsorbed by soils from southeast China was greater than from the northwest. Blue-purple paddy soil had the greatest maximum Zn adsorbed (3 333 mg·L~(-1)) and Loess soil the least(909 mg·L~(-1)). Regardless of soil site locations, for all the calcareous soils, the maximum soil buffering capacity, the intensity of soil Zn adsorption, and the amount of soil fixed Zn were greater than for acid soils. Due to its high organic content and CEC, red calcareous soil showed greater maximum buffering lected from northwest China.