农业科学与技术:英文版
農業科學與技術:英文版
농업과학여기술:영문판
Agricultural Science & Technology
2012年
6期
1287-1291
,共5页
陈奕汀%程红光%蒲晓%周坦%李倩%林春野
陳奕汀%程紅光%蒲曉%週坦%李倩%林春野
진혁정%정홍광%포효%주탄%리천%림춘야
冻融作用%铵根离子%强吸附态%旱地土壤%三江平原
凍融作用%銨根離子%彊吸附態%旱地土壤%三江平原
동융작용%안근리자%강흡부태%한지토양%삼강평원
Freeze-thaw action%Ammonium adsorption%Strong adsorption%Dryland soil%Sanjiang plain
[目的]探讨冻融作用对土壤中不同吸附形式铵根离子的影响。[方法]通过室内模拟试验,研究了冻融作用对三江平原旱地土壤吸附铵根离子总量(水浸提)、强吸附态量(0.01mol/LKCl溶液浸提)的影响。[结果]冻融处理和非冻融对照处理下,相比线性方程,旱地土壤吸附的铵根离子总量能更好的由Freundlich方程拟合(R2〉0.99,SE〈1.69)。冻融作用对铵根离子的总吸附量基本没有影响:当土壤中加入的NH4+初始浓度从0mg/L升高到200mg/L时,冻融条件下NH4+总吸附量从-0.52mg/kg升高到39.0mg/kg;非冻融条件下NH4+总吸附量从-0.70mg/kg升高到38.5mg/kg。土壤中强吸附态NH4+的吸附等温线呈线性(R2〉0.99,SE〈0.54),强吸附态NH4+的吸附量经过冻融过程后有明显增加,当土壤中加入的NH4+初始浓度从0mg/L升高到200mg/L时,冻融条件下NH4+强吸附态含量从-2.36mg/kg呈线性升高到28.81mg/kg;非冻融条件下NH4+强吸附态量从-4.25mg/kg呈线性升高到25.12mg/kg。由于冻融作用降低了强吸附态NH4+吸附解吸达到平衡时土壤溶液中NH4+的浓度,因而有利于降低土壤中铵根离子的淋失。冻融作用主要影响的是以离子交换形式吸附于土壤的NH4+。[结论]该研究为控制土壤氮素过量输入水体,防治水体富营养化奠定了理论基础。
[目的]探討凍融作用對土壤中不同吸附形式銨根離子的影響。[方法]通過室內模擬試驗,研究瞭凍融作用對三江平原旱地土壤吸附銨根離子總量(水浸提)、彊吸附態量(0.01mol/LKCl溶液浸提)的影響。[結果]凍融處理和非凍融對照處理下,相比線性方程,旱地土壤吸附的銨根離子總量能更好的由Freundlich方程擬閤(R2〉0.99,SE〈1.69)。凍融作用對銨根離子的總吸附量基本沒有影響:噹土壤中加入的NH4+初始濃度從0mg/L升高到200mg/L時,凍融條件下NH4+總吸附量從-0.52mg/kg升高到39.0mg/kg;非凍融條件下NH4+總吸附量從-0.70mg/kg升高到38.5mg/kg。土壤中彊吸附態NH4+的吸附等溫線呈線性(R2〉0.99,SE〈0.54),彊吸附態NH4+的吸附量經過凍融過程後有明顯增加,噹土壤中加入的NH4+初始濃度從0mg/L升高到200mg/L時,凍融條件下NH4+彊吸附態含量從-2.36mg/kg呈線性升高到28.81mg/kg;非凍融條件下NH4+彊吸附態量從-4.25mg/kg呈線性升高到25.12mg/kg。由于凍融作用降低瞭彊吸附態NH4+吸附解吸達到平衡時土壤溶液中NH4+的濃度,因而有利于降低土壤中銨根離子的淋失。凍融作用主要影響的是以離子交換形式吸附于土壤的NH4+。[結論]該研究為控製土壤氮素過量輸入水體,防治水體富營養化奠定瞭理論基礎。
[목적]탐토동융작용대토양중불동흡부형식안근리자적영향。[방법]통과실내모의시험,연구료동융작용대삼강평원한지토양흡부안근리자총량(수침제)、강흡부태량(0.01mol/LKCl용액침제)적영향。[결과]동융처리화비동융대조처리하,상비선성방정,한지토양흡부적안근리자총량능경호적유Freundlich방정의합(R2〉0.99,SE〈1.69)。동융작용대안근리자적총흡부량기본몰유영향:당토양중가입적NH4+초시농도종0mg/L승고도200mg/L시,동융조건하NH4+총흡부량종-0.52mg/kg승고도39.0mg/kg;비동융조건하NH4+총흡부량종-0.70mg/kg승고도38.5mg/kg。토양중강흡부태NH4+적흡부등온선정선성(R2〉0.99,SE〈0.54),강흡부태NH4+적흡부량경과동융과정후유명현증가,당토양중가입적NH4+초시농도종0mg/L승고도200mg/L시,동융조건하NH4+강흡부태함량종-2.36mg/kg정선성승고도28.81mg/kg;비동융조건하NH4+강흡부태량종-4.25mg/kg정선성승고도25.12mg/kg。유우동융작용강저료강흡부태NH4+흡부해흡체도평형시토양용액중NH4+적농도,인이유리우강저토양중안근리자적림실。동융작용주요영향적시이리자교환형식흡부우토양적NH4+。[결론]해연구위공제토양담소과량수입수체,방치수체부영양화전정료이론기출。
[Objective] This study aimed to investigate the effect of freezing and thawing on ammonium adsorption in dryland soil. [Method] The lab simulation test was conducted to study the effect of freeze-thaw action on the total adsorbed amount of ammonium (deionized water extract) and strongly-adsorbed amount of ammonium (0.01 mol/L KCl solution extract) in the dryland soil of Sanjiang Plain. [Result] Compared with linear equation, Freundlich equation could better fit the total adsorbed amount of ammonium in dryland soil (R 2 0.99, SE1.69). The freeze-thaw action almost had no influence on the total adsorbed amount of ammonium. When the initial concentration of NH 4 + increased from 0 to 200 mg/L, the total adsorbed NH 4 + amount increased from -0.52 to 39.0 mg/kg under freeze-thaw treatment (FTT), while it increased from -0.70 to 38.5 mg/kg under unfreeze-thaw treatment (UFTT). However, the strongly-adsorbed amount of ammonium presented linear relationship with the concentration of NH 4 + (R 2 0.99, SE0.54), and the strongly-adsorbed amount of ammonium increased significantly by FTT. When the initial concentration of NH 4 + increased from 0 to 200 mg/L, the strongly adsorbed amount increased linearly from 2.36 to 28.81 mg/kg for FTT and from -4.25 to 25.12 mg/kg for UFTT. The freezethaw action decreases the concentration of NH 4 + in soil solution when the net strongly-adsorbed NH 4 + in soil is zero., therefore, FTT helped to reduce the leaching of ammonium ions in soil. Freeze-thaw action mainly influenced the exchangeable adsorbed NH 4 + in soil. [Conclusion] This study provides theoretical basis for preventing excessive soil nitrogen from entering into water body and controlling water entrophication.