北京师范大学学报(自然科学版)
北京師範大學學報(自然科學版)
북경사범대학학보(자연과학판)
JOURNAL OF BEIJING NORMAL UNIVERSITY
2014年
2期
189-194
,共6页
穆晓东%刘慧平%杨晓彤%朱寿东%郭兰萍%黄璐琦
穆曉東%劉慧平%楊曉彤%硃壽東%郭蘭萍%黃璐琦
목효동%류혜평%양효동%주수동%곽란평%황로기
川续断%土壤水分%遥感监测%MODIS%时间序列
川續斷%土壤水分%遙感鑑測%MODIS%時間序列
천속단%토양수분%요감감측%MODIS%시간서렬
Dipsacus asperoides%soil moisture%remote sensing monitoring%MODIS%time series
以栽培川续断为研究对象,选择贵州省黔南州龙里县、贵定县的栽培基地为试验区,利用贵州省2010年全年的 MODIS植被和温度产品,采用Ts-NDVI特征空间模型,先构建温度植被干旱指数(temperature-NDVI dryness index, TVDI),再通过TVDI与土壤水分的经验关系,反演得到试验区的土壤水分分布图。利用时间序列分析,得到了试验区土壤水分的年内变化特征。从总体上看,从春末到秋初,栽培区的土壤水分比较稳定,变化相对其他时段较小。初春时节,土壤含水量最低。进入秋季后,土壤含水量变化剧烈。在冬季,土壤水分则是先上升后下降,且变化幅度最大。此外,将遥感反演结果与同一时段的两次实地测定的土壤水分进行对比验证,发现遥感反演的结果与实测值较接近。研究结果表明利用本文的方法监测中药材栽培区的土壤水分含量切实可行。
以栽培川續斷為研究對象,選擇貴州省黔南州龍裏縣、貴定縣的栽培基地為試驗區,利用貴州省2010年全年的 MODIS植被和溫度產品,採用Ts-NDVI特徵空間模型,先構建溫度植被榦旱指數(temperature-NDVI dryness index, TVDI),再通過TVDI與土壤水分的經驗關繫,反縯得到試驗區的土壤水分分佈圖。利用時間序列分析,得到瞭試驗區土壤水分的年內變化特徵。從總體上看,從春末到鞦初,栽培區的土壤水分比較穩定,變化相對其他時段較小。初春時節,土壤含水量最低。進入鞦季後,土壤含水量變化劇烈。在鼕季,土壤水分則是先上升後下降,且變化幅度最大。此外,將遙感反縯結果與同一時段的兩次實地測定的土壤水分進行對比驗證,髮現遙感反縯的結果與實測值較接近。研究結果錶明利用本文的方法鑑測中藥材栽培區的土壤水分含量切實可行。
이재배천속단위연구대상,선택귀주성검남주룡리현、귀정현적재배기지위시험구,이용귀주성2010년전년적 MODIS식피화온도산품,채용Ts-NDVI특정공간모형,선구건온도식피간한지수(temperature-NDVI dryness index, TVDI),재통과TVDI여토양수분적경험관계,반연득도시험구적토양수분분포도。이용시간서렬분석,득도료시험구토양수분적년내변화특정。종총체상간,종춘말도추초,재배구적토양수분비교은정,변화상대기타시단교소。초춘시절,토양함수량최저。진입추계후,토양함수량변화극렬。재동계,토양수분칙시선상승후하강,차변화폭도최대。차외,장요감반연결과여동일시단적량차실지측정적토양수분진행대비험증,발현요감반연적결과여실측치교접근。연구결과표명이용본문적방법감측중약재재배구적토양수분함량절실가행。
Soil moisture is an important environmental factor affecting the growth of Chinese herbal plants. This paper tries to use remote sensing to monitore soil moisture for cultivated Dipsacus asperoides in two cultivation bases in Longli and Guiding counties in Qiannan city,Guizhou province.MODIS vegetation and temperature data for Guizhou in 2010 were fed into model of Ts-NDVI feature space to construct Temperature-NDVI Dryness Index (TVDI).Soil moisture was retrieved using empirical relationship between TVDI and soil moisture.Time series analysis was used,change pattern in soil moisture was then analyzed.Early spring was found to have the lowest soil moisture.From late spring to early autumn,soil moisture was found to be relatively stable compared with other periods.In late autumn,soil moisture was found to start to change dramatically.When winter starts,soil moisture increases initially then decreases,with the largest fluctuations. After testing and verifying two remote sensing inversions with true soil moisture data of the same time period, ideal results showed that the present approach was practicable in monitoring soil moisture for Chinese herbal medicine.