土壤
土壤
토양
SOILS
2010年
2期
190-199
,共10页
王书伟%颜晓元%林静慧%夏永秋%孙磊%胡玉婷%廖千家骅
王書偉%顏曉元%林靜慧%夏永鞦%孫磊%鬍玉婷%廖韆傢驊
왕서위%안효원%림정혜%하영추%손뢰%호옥정%료천가화
三江平原%碳氮%分布规律
三江平原%碳氮%分佈規律
삼강평원%탄담%분포규률
Sanjiang Plain%Soil organic carbon and total nitrogen%Distribution rule
利用在全国采集的1400个典型农田剖面数据(其中在此研究区域有53个剖面),系统分析了不同土地利用方式下三江平原东北部土壤有机C和全N的分布规律.三江平原东北部典型农田0~20 cm土壤有机C和全N的平均含量是22.7g/kg和1.84 g/kg,20~100cm平均含量为13.0 g/kg和1.08 g/kg,不同土壤类型和种植作物下土壤有机C和全N分布没有显著性差异(p>0.05).与第二次土壤普查时三江平原东北部典型剖面土壤有机C和全N数据进行比较发现,O~20 cm有机C和全N含量呈现下降趋势,而20-100cm呈现增加趋势.
利用在全國採集的1400箇典型農田剖麵數據(其中在此研究區域有53箇剖麵),繫統分析瞭不同土地利用方式下三江平原東北部土壤有機C和全N的分佈規律.三江平原東北部典型農田0~20 cm土壤有機C和全N的平均含量是22.7g/kg和1.84 g/kg,20~100cm平均含量為13.0 g/kg和1.08 g/kg,不同土壤類型和種植作物下土壤有機C和全N分佈沒有顯著性差異(p>0.05).與第二次土壤普查時三江平原東北部典型剖麵土壤有機C和全N數據進行比較髮現,O~20 cm有機C和全N含量呈現下降趨勢,而20-100cm呈現增加趨勢.
이용재전국채집적1400개전형농전부면수거(기중재차연구구역유53개부면),계통분석료불동토지이용방식하삼강평원동북부토양유궤C화전N적분포규률.삼강평원동북부전형농전0~20 cm토양유궤C화전N적평균함량시22.7g/kg화1.84 g/kg,20~100cm평균함량위13.0 g/kg화1.08 g/kg,불동토양류형화충식작물하토양유궤C화전N분포몰유현저성차이(p>0.05).여제이차토양보사시삼강평원동북부전형부면토양유궤C화전N수거진행비교발현,O~20 cm유궤C화전N함량정현하강추세,이20-100cm정현증가추세.
Sanjiang Plain is the biggest wetland in China, however through about 50-year development, the wetland area reduced to 959 000hm2 while the cultivated area increased to 5 569 000 hm2 in 2005, which caused obvious influences on the distributious of soil organic carbon and total nitrogen. So using the data of 1 400 typical profiles (53 representative profiles in Sanjiang Plain), we analyze the distributions of soil organic carbon and total nitrogen under different land uses in the northeast of Sanjiang Plain. The mean contents of soil organic carbon and total nitrogen at 0-20cm and 20-100cm soil depths of typical cropland are 22.7g/kg, 1.84g/kg and 13.0g/kg, 1.08g/kg respectively, however, the distributions of soil organic carbon and total nitrogon at 0-20cm and 20-100cm soil depths under different soil types and crops do not show significant differences (p>0.05). Compared with the corresponding data collected in the 2nd soil survey in 1980s, both soil organic carbon and total nitrogen show the declining tendency at 0-20cm soil depths and the increasing tendency at 20-100cm soil depth.