四川林业科技
四川林業科技
사천임업과기
JOURNAL OF SICHUAN FORESTRY SCIENCE AND TECHNOLOGY
2012年
2期
46-48,34
,共4页
闵安民%刘敏%王莉%鄢武先%张小平
閔安民%劉敏%王莉%鄢武先%張小平
민안민%류민%왕리%언무선%장소평
若尔盖%湿地%草地%退化%土壤%颗粒组成%水分%养分元素
若爾蓋%濕地%草地%退化%土壤%顆粒組成%水分%養分元素
약이개%습지%초지%퇴화%토양%과립조성%수분%양분원소
Zoigê%Wetland%Grassland%Degradation%Soil%Particle size composition%Moisture%Nutrient element
通过对若尔盖湿地和草地的退化沙化调查及采样分析,结果表明:在若尔盖湿地和草地退化沙化演变过程中,土壤的有机质含量、养分元素N、P的全量和有效性N、P、K含量呈明显的下降趋势;土壤粘粒、粉砂粒含量不断降低,沙粒含量不断升高,退化为沙地时,土壤粘粒、粉砂粒含量合计不足10%,沙粒含量高达90%以上;土壤的持水和保水能力下降,土壤含水量呈降低的趋势,沙化地土壤0 cm~10 cm含水量仅57.88 g.kg-1,不到湿地土壤含水量的1/10,仅为草地土壤含水量的1/7。
通過對若爾蓋濕地和草地的退化沙化調查及採樣分析,結果錶明:在若爾蓋濕地和草地退化沙化縯變過程中,土壤的有機質含量、養分元素N、P的全量和有效性N、P、K含量呈明顯的下降趨勢;土壤粘粒、粉砂粒含量不斷降低,沙粒含量不斷升高,退化為沙地時,土壤粘粒、粉砂粒含量閤計不足10%,沙粒含量高達90%以上;土壤的持水和保水能力下降,土壤含水量呈降低的趨勢,沙化地土壤0 cm~10 cm含水量僅57.88 g.kg-1,不到濕地土壤含水量的1/10,僅為草地土壤含水量的1/7。
통과대약이개습지화초지적퇴화사화조사급채양분석,결과표명:재약이개습지화초지퇴화사화연변과정중,토양적유궤질함량、양분원소N、P적전량화유효성N、P、K함량정명현적하강추세;토양점립、분사립함량불단강저,사립함량불단승고,퇴화위사지시,토양점립、분사립함량합계불족10%,사립함량고체90%이상;토양적지수화보수능력하강,토양함수량정강저적추세,사화지토양0 cm~10 cm함수량부57.88 g.kg-1,불도습지토양함수량적1/10,부위초지토양함수량적1/7。
Investigation and soil sampling analysis were made of degraded wetland and deserted grassland in Zoigê.The results were as follows:the content of organic matter,total N,P and available N,P,K in soil significantly reduced in the process of Zoigê wetland degradation and grassland desertification;and the content of clay and powder sand in soil continuously declined and the sand content increased;the content of clay and powder sand was less than 10% and the sand content reached more than 90% in deserted grassland;and the water retention ability of soil dropped,the soil moisture reduced.The moisture in the soil of 0 cm~10 cm depth was only 57.88 g·kg-1 in deserted grassland,less than 1/10 of soil moisture in the wetland,and only 1/7 of the soil moisture in the grassland,respectively.