پايش رطوبت خاك در مراحل رشد گندم ديم به كمك نمايه‌هاي هواشناسي و سنجش از دور

در ايران به دليل كمبود داده ­هاي رطوبت اعماق خاك با توزيع مكاني مناسب، تحقيقات مرتبط با خشكسالي كشاورزي و پايش رطوبت خاك نسبت به خشكسالي از نوع هواشناسي و آب­شناسي كمتر انجام شده است. هدف اصلي از تحقيق حاضر پايش رطوبت خاك در اعماق 10 ، 20، 30، 40، 50 و 70 سانتي­متري به كمك داده ­هاي زميني و سنجش از دور در مراحل رشد گندم ديم (جوانه ­زني تا 4 برگي، ساقه­ دهي و شكم پر تا رسيدگي كامل) در شهرستان نيشابور بوده است. اثر نوسانات رطوبت خاك روي عملكرد گندم ديم در مراحل رشد نيز مورد بررسي قرار گرفته است. به همين منظور تاريخ ­هاي ديدباني شده مراحل رشد گندم ديم در ايستگاه تحقيقات هواشناسي كشاورزي نيشابور طي سال­هاي زراعي 1390-1389 تا 1393-1392 و متغيرهاي هواشناسي به همراه نمايه ­­هاي SPI، SPEI، NDVI، VCI و TCI مورد استفاده قرار گرفتند. نتايج نشان دادند كه تنها رطوبت عمق 10 سانتي­متري خاك با نمايه­هاي NDVImax (r=0.595) و SPEI (r=0.780) ارتباط معني­دار داشته است. براساس نتايج به دست آمده، 35 و 61 درصد تغييرات رطوبت عمق 10 سانتي­متري خاك به ترتيب به كمك NDVImax و SPEI قابل توجيه بوده است. در خصوص تغييرات عملكرد گندم ديم با رطوبت اعماق خاك هر چند روابط معني­ داري حاصل نشد، اما نتايج بيانگر اهميت بارش­هاي فروردين ماه در نوسانات رطوبت خاك و متعاقب آن عملكرد گندم ديم در نيشابور مي­باشد. در پايان مي­توان نمايه­ هايNDVImax و SPEI را به دليل ماهيت ذاتي مؤلفه ­هاي دخيل در محاسبه آن­ها، به عنوان سنجه­ هاي پايش رطوبت خاك معرفي نمود.

Introduction Drought has a huge impact on crop production. Therefore, a better understanding of drought and other atmospheric phenomena is important in order to reduce the damage caused by them. In Iran, most of the studies related to agricultural drought is carried out using remote sensing data due to the lack of in-situ soil moisture data. In fact, because of shortage of soil moisture data alongside a reasonable spatial distribution across the country, the researches pertaining to agricultural drought have been conducted less comparing to meteorological and hydrological drought. However, a few attempts were made to monitor agricultural drought by some researchers in Iran. This study aimed to monitor soil moisture at different depths using in-situ together with remotely-sensed data in Neyshabur City. In addition, the impact of soil moisture on rain-fed wheat yield in different crop growth stages was investigated. Materials and Methods Neyshabur city with an area of 869843.23 ha is extended from center to northwest of Khorasan Razavi province. It is in the neighborhood of Torbat Heydariyeh and Kashmar counties from the south, Sabzevar from the west, Faroj and Quchan from the north and Mashhad and Chenaran from the east. Its’ geographical location ranges from 35° 30 ʹ to 36° 59ʹ N latitudes and 57° 40ʹ to 59° 30 ʹ E longitudes. Farmers cultivate rain-fed wheat in early November and harvest it in late June. The observed data of rain-fed wheat growth stages from Neyishabur agrometeorological research station of 2010-2011 to 2014-2014 were used. The start and end dates of wheat growth stages of Sardari cultivar, together with measured biometric variables were used for further statistical analysis. In addition, measured soil moisture was used at different depths of 10, 20, 30, 40, 50 and 70 cm, in a weekly base during 2010-2011 to 2013-2014. To investigate the impact of meteorological variables on wheat yield, the drought indices, including Standardized Precipitation Index (SPI) and Standardized Precipitation Evapotranspiration Index (SPEI) were calculated. Moreover, remotely-sensed based indices, including Normalized Difference Vegetation Index (NDVI), Vegetation Condition Index (VCI) and Temperature Condition Index (TCI) were derived from different bandwidths of TM, ETM+ and OLI sensors of Landsat satellite. Statistical analysis was performed using Pearson correlation coefficient to find out the correlation among variables. Besides, the simple regression analysis was carried out to calculate the relationship between soil moisture at different depths and meteorological and remote sensing indices. The impact of soil moisture on rain-fed wheat yield was investigated using statistical regression analysis. The statistical analysis was carried out for three wheat growth stages including primary stage (from germination to four leaf), intermediate stage (from tillering to stem elongation) and final growth stage (from booting to physiological maturity). Results and Discussion The results revealed that the maximum and minimum NDVI values during December (germination and four leaf growth stages) were 0.769 and -0.355 in 2011-12 and 2010-11, respectively. It is interesting that wheat yield was 1645 and 3845 kg/ha in 2010-11 and 2011-12, respectively, which correspond to mentioned NDVI values. In addition, the maximum and minimum range of NDVI variations for whole growing season were for 2013-14 and 2011-12 with maximum and minimum wheat yield, respectively (3845 and 1645 kg/ha). Therefore, it could be partly due to appropriate temporal distribution of precipitation and partly because of adequate soil moisture at crop root zone at germination and four leaf growth stages. The statistical regression analysis showed that soil moisture in 10 cm depth had a significant positive correlation with NDVImax and SPEI, with correlation coefficients of 0.595 and 0.780, respectively. In other words, 35 and 61 percent of variations of 10 cm soil moisture depth were accounted for NDVImax and SPEI, respectively. The results showed that, the relationship between rain-fed wheat yield and soil moisture depths was non-significant at different crop growth stages. Although, it should be noted that the April precipitation was important for soil moisture variations and consequently for rain-fed wheat yield. It coincided with start of booting stage of crop. Conclusions The results of this study revealed that NDVImax and SPEI had the most significant correlations with soil moisture at 10 cm depth. However, no significant relationships were found among soil moisture at 20, 30, 40, 50, and 70 cm depths with meteorological and remote sensing indices.