In this section the experimental analysis of the setup has been performed for different soils. The data is presented in the tabular and graphical format. The data was taken during the month of November 2021. Field was irrigated at 2 p.m. and data was recorded each hour. Fig 2 represents the flowchart for different types of actions or steps in the process.
Algorithm
Input
Real time agricultural data (temperature, soil moisture, pH).
Output
1. As per the sensor data from the agricultural farm the required libraries are imported.
2. Coding the microcontroller to read the moisture, temperature and pH data.
3. Setting the code to constantly monitor the changes is field environment at constant interval.
4. Collection of real-time data from the agricultural farm.
5. Load the array of dataset of different crops for various soil conditions.
6. Predict the crop for real-time data by choosing appropriate crops from the given dataset.
7. Send the data accumulated over internet for remote monitoring.
Table 3, 4, 5 illustrates the data obtained by the sensors for different soils. The data is taken over the course of 24 hours before and after irrigation to get the idea of water holding capacity of the soil. The moisture content, temperature, pH of the soil is collected for different time before and after irrigation. Plants display symptoms of extreme water deficiency when the required levels of moisture are unavailable in their habitat soil
(Chadha et al., 2019). while excess water may produce plant stress, water logging, runoff and leaching of fertilizers. Heavy rain or over irrigation can cause soil to be saturated.
Table 4 presents the data obtained from the black soil. The study illustrates that even after 24 hours the moisture content in the soil is around 32.11%. This is due to the presence of Clayey nature of the soil proving its high-water retention capability. While Table 5, presents the water holding capacity of red soil which is lesser than black soil, similar results were reported by (
Malavath and Rajeshwar 2015). Hence the water retention capacity of different soils under study were black soil > alluvial soil > Red soil.
Fig 3 (a), (b), (c) shows the trend of moisture, temperature and pH of all 3 soils. The negative slope of Moisture indicates the decrease in volumetric content of water over the period of time. Slope is steeper just after the irrigation as most of the water moves in the large pores of the soil and drains quickly. The slope at night is gradual incline indicating the lower loss of moisture during night.
Soil temperature is the essential aspect that drives the germination of the crops. Most soil organism work best at optimum soil temperature. The temperature range for maximum growth of most agricultural plants is between 15! and 40
oC. The solubility of various substances in plants depends on temperature.
Soil pH play an important role in availability of nutrients essential for plant growth. The solubility of nutrients as well as chemicals in water are affected by its pH value. Some minerals are readily available under acidic conditions, but some exist under alkaline conditions. Optimum pH is between 6.0 to 7.0. Low pH (<5.5) indicate acidic soils and higher pH (>8) indicate alkaline soils.
From the Tables 3, 4, 5 above it may be concluded that red soil is slight acidic in nature, while alluvial soil and black soil may be considered as neutral and slightly alkaline. (
Dora Neina 2019) refers that acidic soils may lead to aluminum toxicity, manganese toxicity, magnesium deficiency and calcium-deficiency in soil. Alkaline soils can cause a deficiency in zinc, copper
etc. Fertilizers such as ground sulfur and ammonium-based nitrogen fertilizers are used to lower the pH and naturally acidify the soil. Lime or dolomite may be used to increase the pH rate of the soil.
The experiment performed with this device on various soils measured all three parameters and display on the devices as shown in Fig 4 (a), (b). Based on these parameters the system recommends appropriate crop from the array of dataset passed initially. Table 6 lists down the suitable crop for different soil recommended by the system.
Based on the pH of soil the basic and acidic condition of soil is identified. The system also recommeds the type of fertilizers that may be used and also the bacterial condition of the soil as given in Fig 4(a). The user may take the decisions based on the condition of the farm and crops.