农业工程学报
農業工程學報
농업공정학보
2009年
11期
49-54
,共6页
唐晓红%魏朝富%吕家恪%罗友进%谢德体%潘根兴%曾希柏
唐曉紅%魏朝富%呂傢恪%囉友進%謝德體%潘根興%曾希柏
당효홍%위조부%려가각%라우진%사덕체%반근흥%증희백
团聚体%稳定性%有机碳%保护性耕作%水稻土
糰聚體%穩定性%有機碳%保護性耕作%水稻土
단취체%은정성%유궤탄%보호성경작%수도토
aggregates%stability%organic carbon%conservation tillage%paddy soil
长期保护性耕作通过增加土壤有机碳而成为稻田土壤结构改良的一项有效措施,而保护性耕作对土壤团聚体稳定机制的影响尚未完全清楚.本文供试土样采自耕作制定位试验水旱轮作、冬水免耕、垄作免耕和厢作免耕耕层(0~ 20 cm)土壤,土样经过糊化作用、湿润作用和再次糊化作用等预处理,用以阐明稻田土壤团聚体的破碎机制.研究结果表明:糊化作用和湿润作用后紫色水稻土团聚体稳定性差异不明显,而保护性耕作显著影响团聚体的稳定性.糊化作用后团聚体水稳性强弱顺序为:垄作免耕>厢作免耕>冬水免耕>水旱轮作,湿润作用后团聚体水稳性强弱顺序为:厢作免耕>垄作免耕>冬水免耕>水旱轮作.糊化作用下团聚体稳定性与有机碳浓度相关性不显著(r=0.432,p>0.05),湿润作用下团聚体稳定性与有机碳浓度呈极显著正相关(r=0.626,p<0.01).因此,研究结果说明保护性耕作有利于紫色水稻土大团聚体有机碳含量提高,进而增强团聚体的水稳性.
長期保護性耕作通過增加土壤有機碳而成為稻田土壤結構改良的一項有效措施,而保護性耕作對土壤糰聚體穩定機製的影響尚未完全清楚.本文供試土樣採自耕作製定位試驗水旱輪作、鼕水免耕、壟作免耕和廂作免耕耕層(0~ 20 cm)土壤,土樣經過糊化作用、濕潤作用和再次糊化作用等預處理,用以闡明稻田土壤糰聚體的破碎機製.研究結果錶明:糊化作用和濕潤作用後紫色水稻土糰聚體穩定性差異不明顯,而保護性耕作顯著影響糰聚體的穩定性.糊化作用後糰聚體水穩性彊弱順序為:壟作免耕>廂作免耕>鼕水免耕>水旱輪作,濕潤作用後糰聚體水穩性彊弱順序為:廂作免耕>壟作免耕>鼕水免耕>水旱輪作.糊化作用下糰聚體穩定性與有機碳濃度相關性不顯著(r=0.432,p>0.05),濕潤作用下糰聚體穩定性與有機碳濃度呈極顯著正相關(r=0.626,p<0.01).因此,研究結果說明保護性耕作有利于紫色水稻土大糰聚體有機碳含量提高,進而增彊糰聚體的水穩性.
장기보호성경작통과증가토양유궤탄이성위도전토양결구개량적일항유효조시,이보호성경작대토양단취체은정궤제적영향상미완전청초.본문공시토양채자경작제정위시험수한륜작、동수면경、롱작면경화상작면경경층(0~ 20 cm)토양,토양경과호화작용、습윤작용화재차호화작용등예처리,용이천명도전토양단취체적파쇄궤제.연구결과표명:호화작용화습윤작용후자색수도토단취체은정성차이불명현,이보호성경작현저영향단취체적은정성.호화작용후단취체수은성강약순서위:롱작면경>상작면경>동수면경>수한륜작,습윤작용후단취체수은성강약순서위:상작면경>롱작면경>동수면경>수한륜작.호화작용하단취체은정성여유궤탄농도상관성불현저(r=0.432,p>0.05),습윤작용하단취체은정성여유궤탄농도정겁현저정상관(r=0.626,p<0.01).인차,연구결과설명보호성경작유리우자색수도토대단취체유궤탄함량제고,진이증강단취체적수은성.
Long-term conservation tillage is an effective agricultural management to improve soil structure in severely destroyed paddy soil by increase of soil organic carbon (SOC). More work is still needed to understand the impacts of conservation tillage on the mechanisms of aggregates stability. Soil samples in 0-20 cm layer were adopted from the long-term tillage experiment: (1) paddy-upland rotation and plain culture (rice- rape) (PU-R-RR), (2)no-tillage and ridge culture (rice-fallow) (NT-R-RF), (3) no-tillage and ridge culture (rice-rape) (NT-R-RR) and (4) no-tillage and plain culture (rice- rape) (NT-P-RR). Different pretreatments, such as slaking in fast wetting, wetting and subsequent slaking, were applied to simulate the breakdown mechanisms of aggregates in paddy soil. The results showed that no significant difference of aggregate stability between slaking and wetting pretreatments was observed, while tillage patterns affected greatly aggregate stability. The aggregate stability under slaking and wetting pretreatment ranked in the order of NT-R-RR > NT-P-RR > NT-R-RF > PU-R-RR and NT-P-RR > NT-R-RR > NT-R-RF > PU-R-RR, respectively. The organic carbon concentrations in aggregates were significantly positive related to the aggregates stability under wetting(r=0.626, p<0.01), while low correlation linear relationships were observed under slaking treatment (r=0.432, p>0.05). The results suggest that long-term conservation tillage favorably led to the increase of SOC concentrations in aggregates and the enhancement of aggregates water stabilization.