中国生态农业学报
中國生態農業學報
중국생태농업학보
CHINESE JOURNAL OF ECO-AGRICULTURE
2010年
2期
352-355
,共4页
杨治平%张强%王永亮%张建杰%冀瑞瑞
楊治平%張彊%王永亮%張建傑%冀瑞瑞
양치평%장강%왕영량%장건걸%기서서
小叶锦鸡儿%土壤水分%黄土丘陵区%土壤水分循环%植被恢复
小葉錦鷄兒%土壤水分%黃土丘陵區%土壤水分循環%植被恢複
소협금계인%토양수분%황토구릉구%토양수분순배%식피회복
Caragana microphylla%Soil moisture%Loess hilly region%Soil moisture circulation%Vegetation restoration
土壤水分是黄土丘陵区植被成活与正常生长的关键因素.对黄土丘陵区不同生长年限小叶锦鸡儿灌丛及其撂荒地土壤水分的动态监测表明, 随种植年限延长, 小叶锦鸡儿灌丛下土壤水分含量呈持续下降趋势, 40年灌丛下土壤含水量明显低于20年和10年的小叶锦鸡儿灌丛, 且所有种植年限的灌丛土壤含水量均低于撂荒地.从周年内土壤水分季节变化看, 整体呈下降趋势, 4~6月不断降低, 6~7月达到最低值, 8~10月逐渐回升.对0~200 cm土体剖面土壤水分分布研究表明, 随种植年限增加, 小叶锦鸡儿灌丛各深度土层土壤含水量呈递减趋势, 在40~80 cm土层随种植年限增加土壤含水量减少幅度明显.整个生长季各年限灌丛的土壤水分循环水平不高, 40年灌丛只有4.63%, 与撂荒地比较相差2.92%, 而各年限灌丛土壤水分表观平衡均表现为亏缺状态.表明目前黄土丘陵区人工种植的小叶锦鸡儿灌丛土壤水分环境不容乐观, 长期处于水分胁迫状态, 不利于其生存生长, 存在灌丛衰退甚至死亡的风险.
土壤水分是黃土丘陵區植被成活與正常生長的關鍵因素.對黃土丘陵區不同生長年限小葉錦鷄兒灌叢及其撂荒地土壤水分的動態鑑測錶明, 隨種植年限延長, 小葉錦鷄兒灌叢下土壤水分含量呈持續下降趨勢, 40年灌叢下土壤含水量明顯低于20年和10年的小葉錦鷄兒灌叢, 且所有種植年限的灌叢土壤含水量均低于撂荒地.從週年內土壤水分季節變化看, 整體呈下降趨勢, 4~6月不斷降低, 6~7月達到最低值, 8~10月逐漸迴升.對0~200 cm土體剖麵土壤水分分佈研究錶明, 隨種植年限增加, 小葉錦鷄兒灌叢各深度土層土壤含水量呈遞減趨勢, 在40~80 cm土層隨種植年限增加土壤含水量減少幅度明顯.整箇生長季各年限灌叢的土壤水分循環水平不高, 40年灌叢隻有4.63%, 與撂荒地比較相差2.92%, 而各年限灌叢土壤水分錶觀平衡均錶現為虧缺狀態.錶明目前黃土丘陵區人工種植的小葉錦鷄兒灌叢土壤水分環境不容樂觀, 長期處于水分脅迫狀態, 不利于其生存生長, 存在灌叢衰退甚至死亡的風險.
토양수분시황토구릉구식피성활여정상생장적관건인소.대황토구릉구불동생장년한소협금계인관총급기략황지토양수분적동태감측표명, 수충식년한연장, 소협금계인관총하토양수분함량정지속하강추세, 40년관총하토양함수량명현저우20년화10년적소협금계인관총, 차소유충식년한적관총토양함수량균저우략황지.종주년내토양수분계절변화간, 정체정하강추세, 4~6월불단강저, 6~7월체도최저치, 8~10월축점회승.대0~200 cm토체부면토양수분분포연구표명, 수충식년한증가, 소협금계인관총각심도토층토양함수량정체감추세, 재40~80 cm토층수충식년한증가토양함수량감소폭도명현.정개생장계각년한관총적토양수분순배수평불고, 40년관총지유4.63%, 여략황지비교상차2.92%, 이각년한관총토양수분표관평형균표현위우결상태.표명목전황토구릉구인공충식적소협금계인관총토양수분배경불용악관, 장기처우수분협박상태, 불리우기생존생장, 존재관총쇠퇴심지사망적풍험.
Soil moisture is a key factor for the growth and survival of vegetation in the loess hilly region. Soil moisture dynamics was monitored under artificial Caragana microphylla shrub at 5 ages (5, 10, 20, 30 and 40 years after germination) in the loess hilly region of Northwest Shanxi Province in 2006. The results show decreasing soil moisture content (SMC) under artificial C. microphylla shrub with increasing age. SMC is lowest under the 40-year shrub. SMC under the shrubs is generally lower than under nearby wastelands. Based on monthly trend, SMC gradually decreases from April to June (hitting the lowest point in June), and then gradually increases from August to October. Vertically, SMC in the 0~200 cm soil layer gradually decreases with soil depth, especially in the 40~80 cm soil layer. During shrub growth period, soil moisture circulation is low. It is only 4.63% under the 40-year shrub, which is 2.92% less than that under nearby wastelands. Furthermore, the overall soil moisture balance is negative. It then implies that the artificial C. microphylla shrub is under moisture stress in the loess hilly region. In the long-term, moisture stress could threaten the growth and survival of artificial C. microphylla shrubs in this region.