植物营养与肥料学报
植物營養與肥料學報
식물영양여비료학보
PLANT NUTRITION AND FERTILIZER SCIENCE
2013年
6期
1403-1410
,共8页
灌溉方式%微生物量碳%氮%土壤酶活性%硝化细菌%水稻土
灌溉方式%微生物量碳%氮%土壤酶活性%硝化細菌%水稻土
관개방식%미생물량탄%담%토양매활성%초화세균%수도토
Irrigation method%microbial biomass carbon and nitrogen%soil enzyme activity%nitrification bacteria%paddy soil
通过盆栽试验,研究了不同氮肥水平下“薄、浅、湿、晒”灌溉对水稻拔节期、孕穗期和乳熟期土壤微生物量碳( MBC)、微生物量氮( MBN)、硝化细菌和反硝化细菌数量和酶活性的影响,以探讨该灌溉方式下土壤微生物活性变化规律。试验设2种灌水方式,即常规灌溉(CIR)和“薄、浅、湿、晒”灌溉(TIR);3种氮肥水平,即低氮(N 0.10 g/kg)、中氮( N 0.15 g/kg)和高氮( N 0.2 g/kg)。结果表明,与CIR处理相比,TIR处理土壤MBC增加13%240%,而土壤MBN减少6.5%47.3%;高氮水平时3个时期TIR处理土壤硝化细菌有所增加,反硝化细菌拔节期和孕穗期降低12.1%61.2%,而乳熟期增加0.73.0倍;中、低氮水平时孕穗期TIR处理土壤硝酸还原酶活性分别降低63.8%和43.3%。与低氮水平相比,中氮水平可以增加土壤MBC、MBN、硝化细菌和反硝化细菌数量以及过氧化氢酶、脲酶和转化酶活性,而高氮水平则降低土壤MBN,以及过氧化氢酶、脲酶和硝酸还原酶活性。可见,中等氮肥水平下“薄、浅、湿、晒”灌溉方式能有效提高稻田土壤微生物量碳和过氧化氢酶、脲酶、转化酶活性。
通過盆栽試驗,研究瞭不同氮肥水平下“薄、淺、濕、曬”灌溉對水稻拔節期、孕穗期和乳熟期土壤微生物量碳( MBC)、微生物量氮( MBN)、硝化細菌和反硝化細菌數量和酶活性的影響,以探討該灌溉方式下土壤微生物活性變化規律。試驗設2種灌水方式,即常規灌溉(CIR)和“薄、淺、濕、曬”灌溉(TIR);3種氮肥水平,即低氮(N 0.10 g/kg)、中氮( N 0.15 g/kg)和高氮( N 0.2 g/kg)。結果錶明,與CIR處理相比,TIR處理土壤MBC增加13%240%,而土壤MBN減少6.5%47.3%;高氮水平時3箇時期TIR處理土壤硝化細菌有所增加,反硝化細菌拔節期和孕穗期降低12.1%61.2%,而乳熟期增加0.73.0倍;中、低氮水平時孕穗期TIR處理土壤硝痠還原酶活性分彆降低63.8%和43.3%。與低氮水平相比,中氮水平可以增加土壤MBC、MBN、硝化細菌和反硝化細菌數量以及過氧化氫酶、脲酶和轉化酶活性,而高氮水平則降低土壤MBN,以及過氧化氫酶、脲酶和硝痠還原酶活性。可見,中等氮肥水平下“薄、淺、濕、曬”灌溉方式能有效提高稻田土壤微生物量碳和過氧化氫酶、脲酶、轉化酶活性。
통과분재시험,연구료불동담비수평하“박、천、습、쇄”관개대수도발절기、잉수기화유숙기토양미생물량탄( MBC)、미생물량담( MBN)、초화세균화반초화세균수량화매활성적영향,이탐토해관개방식하토양미생물활성변화규률。시험설2충관수방식,즉상규관개(CIR)화“박、천、습、쇄”관개(TIR);3충담비수평,즉저담(N 0.10 g/kg)、중담( N 0.15 g/kg)화고담( N 0.2 g/kg)。결과표명,여CIR처리상비,TIR처리토양MBC증가13%240%,이토양MBN감소6.5%47.3%;고담수평시3개시기TIR처리토양초화세균유소증가,반초화세균발절기화잉수기강저12.1%61.2%,이유숙기증가0.73.0배;중、저담수평시잉수기TIR처리토양초산환원매활성분별강저63.8%화43.3%。여저담수평상비,중담수평가이증가토양MBC、MBN、초화세균화반초화세균수량이급과양화경매、뇨매화전화매활성,이고담수평칙강저토양MBN,이급과양화경매、뇨매화초산환원매활성。가견,중등담비수평하“박、천、습、쇄”관개방식능유효제고도전토양미생물량탄화과양화경매、뇨매、전화매활성。
A pot experiment was carried out to study effects of the “thin-shallow-wet-dry” irrigation method on microbial biomass carbon ( MBC ) , microbial biomass nitrogen ( MBN ) , the numbers of nitrification bacteria and denitrification bacteria and enzyme activities in soils at the jointing , booting and milky stages of rice under different nitrogen( N) levels, and to explore variation of soil microbe activities under the irrigation method .There were two irrigation methods , conventional irrigation ( CIR) and “thin-shallow-wet-dry” irrigation( TIR) , and three N levels , low N(0.10 g/kg soil), middle N(0.15 g/kg soil) and high N(0.2 g/kg soil).Compared to the CIR treatments, the TIR treatments increase soil MBC by 13%-240%, and decrease soil MBN by 6.5%-47.3%.At the high N level, the TIR treatment increases the number of soil nitrification bacteria at three growth stages slightly , and increases the number of soil denitrification bacteria by 0.7 to 3 times at the milky stage and decreases the number of soil denitrification bacteria by 12.1%to 61.2%at the jointing and booting stages .At the low and middle N levels , the TIR treatments reduce the activity of soil nitrate reductase by 63.8%and 43.3% at the booting stage .Under the same irrigation method , compared to the low N level , the middle N level increases soil MBC and MBN , the numbers of nitrification bacteria and denitrification bacteria , and the activities of catalase , urease and invertase , while the high N level reduces soil MBN and the activities of catalase , urease and nitrate reductase .Thus TIR can effectively improve microbial biomass carbon and the activities of catalase , urease and invertase under the middle N level.