| 黑河中游边缘绿洲农田退耕还草的土壤碳、氮固存效应 |
| 摘要点击 2654 全文点击 1564 投稿时间：2005-08-21 修订日期：2005-10-31 |
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| 中文关键词 农田 苜蓿地 土壤有机碳、氮 颗粒有机碳、氮 碳固存 |
| 英文关键词 cultivated land alfalfa grassland soil organic C and N particulate organic C and N C sequestration |
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| 中文摘要 |
| 研究黑河中游边缘绿洲农田退耕种植苜蓿5a后土壤碳、氮库的变化,通过对2个土类(开垦耕种的风沙土和灰棕漠土)退耕苜蓿地和相邻农田0～5、5～10和10～20cm土层土壤有机碳(SOC)和全氮(TN)、颗粒有机碳和氮(POC、PON)储量的分析表明:开垦耕种的风沙土和灰棕漠土有极低的SOC和TN含量,退耕种植苜蓿后0～20cm SOC储量提高了22.1%～27.8%,SOC的固存率平均为0.47 Mg/(hm2·a),0～5cm表层SOC储量变化最大,提高32%～66%;TN储量0～20cm储量变化不显著,在0～5cm表层TN储量风沙土和灰棕漠土分别提高12.8%和48.1%.退耕后POC和PON较SOC和TN有更显著的变化,其分配比例增加,0～20cm土层POC和PON储量分别提高22.8%～42.7%和18.6%～57.6%,在0～5cm变化最大;在瘠薄耕地转变为多年生苜蓿地后土壤C库的增加主要是由于POC的形成量增加.SOC含量相对更低的灰棕漠土比风沙土退耕后土壤C、N的增加更为明显. |
| 英文摘要 |
| Changes in soil organic carbon(SOC) and total nitrogen(TN) stocks were studied following croplands were converted to forage grasslands(alfalfa) for five years on the marginal land at the edge of oasis in the middle reaches of Heihe river basin.Soil from 12 paired forage land/ adjacent cropland on the two soil types(Typic Torripsamments and Typic Calciorthids) was sampled at the three depths of 0～5,5～10 and 10～20 cm and analyzed for SOC and TN,particulate organic carbon(POC) and nitrogen(PON).The studied soils had very low SOC and N concentrations.SOC stock at the 0～20 cm depth increased by 22.1%～27.8% after conversion of annually crop to perennial alfalfa for four years,and carbon sequestration rate was estimated to be on average 0.47Mg/(hm2·a).The greatest change in SOC stock occurred at the 0～5 cm surface layer with an increase of 32%～66%.No significant TN stock was found at the 0～20 cm depth,however,it increased at the 0～5 cm surface layer by 12.8% and 48.1% for Typic Torripsamments and Typic Calciorthids,respectively.Changes in POC and PON stocks were more significant than those in SOC and total N following conversion of crop to forage,and the percentage of distributions of POC and PON increased.POC and PON stocks at the 0～20 cm depth increased by 22.8%～42.7% and 18.6%～57.6% with the greatest increases at the 0～5 cm layer.The increase in soil C pool was mainly attributed to the increase of POC formation after the marginal lands converted to perennial forage cover.Typic Calciorthids with lower SOC concentration had relatively lower C sequestration rate but more significant effects of C and N sequestration compared with Typic Torripsamments. |
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