农业环境科学学报
農業環境科學學報
농업배경과학학보
Journal of Agro-Environment Science
2009年
10期
2092-2097
,共6页
丁秋祎%白军红%高海峰%肖蓉%崔保山
丁鞦祎%白軍紅%高海峰%肖蓉%崔保山
정추의%백군홍%고해봉%초용%최보산
植被群落%湿地土壤%养分含量%黄河三角洲
植被群落%濕地土壤%養分含量%黃河三角洲
식피군락%습지토양%양분함량%황하삼각주
plant communities%wetland soil%nutrient contents%Yellow River Delta
以黄河三角洲潮上带湿地为对象,通过采样、分析,研究了4种典型的植被群落下水盐梯度和土壤养分含量的变化特征.结果显示,沿植物群落演替方向,土壤水分含量无显著差异,土壤盐分呈逐渐降低的趋势,在一定程度上反映了植物群落的不同演替阶段.在这种水盐梯度下,植被群落的变化能够影响土壤养分含量,沿着植被演替方向,全碳与有机质含量随着演替方向呈先逐渐降低后增加的趋势,土壤碳氮比((C/N)在植被演替中期相对较高;全氮含量沿着演替方向呈现增加趋势,硝态氮与铵态氮先增加后降低;全磷与有效磷随演替变化系数较小,演替中期各理化性质变异系数相对较大.各群落土壤C/N值均小于25.相关分析表明,全氮、有机质与有效磷两两显著相关(p<0.01),有效磷还与含水率显著相关(p<0.05),硝态氮、钱态氮和全磷未显示出与其他理化性质的相关关系.含水率与pH值显著相关(p<0.05),且二者均与土壤盐分显著负相关(p<0.01).
以黃河三角洲潮上帶濕地為對象,通過採樣、分析,研究瞭4種典型的植被群落下水鹽梯度和土壤養分含量的變化特徵.結果顯示,沿植物群落縯替方嚮,土壤水分含量無顯著差異,土壤鹽分呈逐漸降低的趨勢,在一定程度上反映瞭植物群落的不同縯替階段.在這種水鹽梯度下,植被群落的變化能夠影響土壤養分含量,沿著植被縯替方嚮,全碳與有機質含量隨著縯替方嚮呈先逐漸降低後增加的趨勢,土壤碳氮比((C/N)在植被縯替中期相對較高;全氮含量沿著縯替方嚮呈現增加趨勢,硝態氮與銨態氮先增加後降低;全燐與有效燐隨縯替變化繫數較小,縯替中期各理化性質變異繫數相對較大.各群落土壤C/N值均小于25.相關分析錶明,全氮、有機質與有效燐兩兩顯著相關(p<0.01),有效燐還與含水率顯著相關(p<0.05),硝態氮、錢態氮和全燐未顯示齣與其他理化性質的相關關繫.含水率與pH值顯著相關(p<0.05),且二者均與土壤鹽分顯著負相關(p<0.01).
이황하삼각주조상대습지위대상,통과채양、분석,연구료4충전형적식피군락하수염제도화토양양분함량적변화특정.결과현시,연식물군락연체방향,토양수분함량무현저차이,토양염분정축점강저적추세,재일정정도상반영료식물군락적불동연체계단.재저충수염제도하,식피군락적변화능구영향토양양분함량,연착식피연체방향,전탄여유궤질함량수착연체방향정선축점강저후증가적추세,토양탄담비((C/N)재식피연체중기상대교고;전담함량연착연체방향정현증가추세,초태담여안태담선증가후강저;전린여유효린수연체변화계수교소,연체중기각이화성질변이계수상대교대.각군락토양C/N치균소우25.상관분석표명,전담、유궤질여유효린량량현저상관(p<0.01),유효린환여함수솔현저상관(p<0.05),초태담、전태담화전린미현시출여기타이화성질적상관관계.함수솔여pH치현저상관(p<0.05),차이자균여토양염분현저부상관(p<0.01).
Soil nutrient contents were measured in 31 study plots of the supratidal zone wetland of Yellow River Delta( YRD) in order to reveal their changes in marsh soils with different plant communities. By the methods of spatial distribution as a substitute for time succession, differ-ent plant communities were chosen to substitute different periods of plant community succession. Results showed that there were obvious rela-tionships among four plant communities and soil salt contents (SC ) but there were no significant differences among water contents ( WC), which also showed different succession periods of plant community to some certain. Along the positive succession direction of pant communi-ty, both the contents of soil organic matter( SOM) and their variation coefficients showed the trend of "decreasing before increasing" along the water-salt gradients. The ratios of C/N were relatively higher in the middle of the successions than at the beginning or later stage. Total nitro-gen(TN) contents showed an increase while NH~+_4-N and NO~-_3-N showed the trends of "decreasing after increasing". Total phosphorus (TP) contents had no significant variations with the succession. No significant differences were observed in total phosphorus(TP ) and available phosphorus(AP) contents of wetland soils under four plant communities. The middle of the succession had the higher variation coefficients. In wetland soils under four plant communities, the ratios of C/N were all lower than 25. Correlation analysis showed that there were significantly positive correlations between TN、SOM and AP(P<0.01). TP was significantly positively correlated with WC(P<0.05). No significant correla-tions were found between NH~+_4-N、NO~-_3-N and TP with other soil properties. WC were significantly positively correlated with pH(P<0.05) and both of them were negatively correlated with SC(P<0.01).