新疆农业大学学报
新疆農業大學學報
신강농업대학학보
JOURNAL OF XINJIANG AGRICULTURAL UNIVERSITY
2014年
3期
240-245
,共6页
杨金钰%刘骅%王西和%贾宏涛
楊金鈺%劉驊%王西和%賈宏濤
양금옥%류화%왕서화%가굉도
长期施肥%灰漠土%易氧化有机碳%有机碳
長期施肥%灰漠土%易氧化有機碳%有機碳
장기시비%회막토%역양화유궤탄%유궤탄
longGterm fertilization%greyGdesert soil%readily oxidation carbon%organic carbon
以长期定位施肥下灰漠土易氧化有机碳变化特征为研究对象,于2013年采集不同施肥处理的对照(CK)、单施氮肥(N)、化肥平衡配施(NPK)、化肥配施有机肥(NPKM)、化肥配施秸秆(NPKS)、撂荒(CK0)的土样,分析测定土壤易氧化有机碳及总有机碳含量.结果表明,24 a 后,化肥配施有机肥(NPKM)处理土壤有机碳含量达到17.42 g/kg,比1990年的基础值增加了80%;对照(CK)处理土壤有机碳含量最低,仅为6.46 g/kg 左右,比1990年下降了48%;单施氮肥(N)、化肥平衡配施(NPK)的土壤有机碳下降了30%;化肥配秸秆(NPKS)的土壤有机碳下降了10%;撂荒(CK0)处理的土壤有机碳增加了11%.配施有机肥(NPKM)处理土壤易氧化有机碳含量显著增加了188%;除化肥平衡配施(NPK)处理以外,CK、N、NPKM、NPKS、CK0处理的易氧化有机碳含量均有所增加,但与基础值差异不显著(P >0.05),NPK处理比基础值下降了28%.各处理的活度、碳库管理指数和活度指数都较基础土壤值高(除 NPK处理),NPKM处理明显提高了土壤碳库管理指数.易氧化有机碳与土壤有机碳的相关性达极显著水平(P <0.01),与作物产量的相关性达显著水平(P <0.05).长期化肥配施有机肥有利于土壤有机碳的积累.土壤易氧化有机碳是反映土壤碳素动态变化灵敏而有效的指标,该指标为培肥地力、增加土壤活性有机质含量提供了量化依据.
以長期定位施肥下灰漠土易氧化有機碳變化特徵為研究對象,于2013年採集不同施肥處理的對照(CK)、單施氮肥(N)、化肥平衡配施(NPK)、化肥配施有機肥(NPKM)、化肥配施秸稈(NPKS)、撂荒(CK0)的土樣,分析測定土壤易氧化有機碳及總有機碳含量.結果錶明,24 a 後,化肥配施有機肥(NPKM)處理土壤有機碳含量達到17.42 g/kg,比1990年的基礎值增加瞭80%;對照(CK)處理土壤有機碳含量最低,僅為6.46 g/kg 左右,比1990年下降瞭48%;單施氮肥(N)、化肥平衡配施(NPK)的土壤有機碳下降瞭30%;化肥配秸稈(NPKS)的土壤有機碳下降瞭10%;撂荒(CK0)處理的土壤有機碳增加瞭11%.配施有機肥(NPKM)處理土壤易氧化有機碳含量顯著增加瞭188%;除化肥平衡配施(NPK)處理以外,CK、N、NPKM、NPKS、CK0處理的易氧化有機碳含量均有所增加,但與基礎值差異不顯著(P >0.05),NPK處理比基礎值下降瞭28%.各處理的活度、碳庫管理指數和活度指數都較基礎土壤值高(除 NPK處理),NPKM處理明顯提高瞭土壤碳庫管理指數.易氧化有機碳與土壤有機碳的相關性達極顯著水平(P <0.01),與作物產量的相關性達顯著水平(P <0.05).長期化肥配施有機肥有利于土壤有機碳的積纍.土壤易氧化有機碳是反映土壤碳素動態變化靈敏而有效的指標,該指標為培肥地力、增加土壤活性有機質含量提供瞭量化依據.
이장기정위시비하회막토역양화유궤탄변화특정위연구대상,우2013년채집불동시비처리적대조(CK)、단시담비(N)、화비평형배시(NPK)、화비배시유궤비(NPKM)、화비배시갈간(NPKS)、략황(CK0)적토양,분석측정토양역양화유궤탄급총유궤탄함량.결과표명,24 a 후,화비배시유궤비(NPKM)처리토양유궤탄함량체도17.42 g/kg,비1990년적기출치증가료80%;대조(CK)처리토양유궤탄함량최저,부위6.46 g/kg 좌우,비1990년하강료48%;단시담비(N)、화비평형배시(NPK)적토양유궤탄하강료30%;화비배갈간(NPKS)적토양유궤탄하강료10%;략황(CK0)처리적토양유궤탄증가료11%.배시유궤비(NPKM)처리토양역양화유궤탄함량현저증가료188%;제화비평형배시(NPK)처리이외,CK、N、NPKM、NPKS、CK0처리적역양화유궤탄함량균유소증가,단여기출치차이불현저(P >0.05),NPK처리비기출치하강료28%.각처리적활도、탄고관리지수화활도지수도교기출토양치고(제 NPK처리),NPKM처리명현제고료토양탄고관리지수.역양화유궤탄여토양유궤탄적상관성체겁현저수평(P <0.01),여작물산량적상관성체현저수평(P <0.05).장기화비배시유궤비유리우토양유궤탄적적루.토양역양화유궤탄시반영토양탄소동태변화령민이유효적지표,해지표위배비지력、증가토양활성유궤질함량제공료양화의거.
Compared with the samples as CK,N,NPK,NPKM,NPKS and CK0 in 2013,readily oxidation carbon and total organic carbon content were analyzed.The results showed that soil organic carbon content treated with NPKM reached 17.42 g/kg,which increased by 80%,compared with that in 1990;The soil orG ganic content treated with CK were about 6.46 g/kg,which reduced by 48%,compared with that in 1990;The soil organic carbon of N,NPK reduced by 30%;The soil organic carbon of NPKS reduced by 10%;The soil organic carbon treated with CK0 increased by 1 1%.The combined application of fertilizer treated with soil readily oxidation carbon content significantly increased by 188%;Except for treatment of equilibrium combined application of chemical fertilizer (NPK),the organic carbon content of other treatments CK,N, NPKM,MPKS and CK0 were increased.But there were no significant differences,compared with basic valG ue.NPK treatment reduced by 28%,compared with basic value.The activities,carbon administration indeG xes of carbon sink and activities indexes of different treatments all were higher than those of basic soil valG ue (Except for NPK treatment),thus it can be seen that the soil carbon sink administration indexes were significantly increased by NPKM treatment.The relativity of readily oxidation carbon and soil organic carG bon and crop yield had significant level (P < 0.01).The chemical fertilizer applied with organic fertilizer were advantageous to accumulation of soil organic carbon.The soil readily oxidation carbon reflected sensiG tive change and effective indexes of soil carbon dynamic state,whose indexes provided an important basis for culturing soil fertility,organic content of increasing soil activities.