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3:1.5.1 Nitrogen in Rainfall

Lightning discharge converts atmospheric N2N_2N2​ to nitric acid which can then be transferred to the soil with precipitation. The chemical steps involved are:

step 1: N2+O2β†’arcofelectricity2NON_2+O_2\xrightarrow{arc of electricity}2NON2​+O2​arcofelectricity​2NO (monoxide)

step 2: 2NO+O2β†’NO22NO+O_2\rightarrow NO_22NO+O2​→NO2​ (dioxide)

step 3: 3NO2+H2Oβ†’2HNO2+NO3NO_2+H_2O\rightarrow 2HNO_2+NO3NO2​+H2​Oβ†’2HNO2​+NO (nitric acid and monoxide)

More nitrogen will be added to the soil with rainfall in areas with a high amount of lightning activity than in areas with little lightning.

The amount of nitrate added to the soil in rainfall is calculated:

3:1.5.1

where is nitrate added by rainfall (kg N/ha), is the concentration of nitrate in the rain (mg N/L), and is the amount of precipitation on a given day (mm HO). The nitrogen in rainfall is added to the nitrate pool in the top 10 mm of soil.

The amount of ammonia added to the soil in rainfall is calculated:

3:1.5.2

where is nitrate added by rainfall (kg N/ha), is the concentration of ammonia in the rain (mg N/L), and is the amount of precipitation on a given day (mm HO). The nitrogen in rainfall is added to the ammonia pool in the top 10 mm of soil.

Table 3:1-4: SWAT+ input variables that pertain to nitrogen in rainfall.

Definition
Source Name
Input Name
Input File

.atm

NO3rain=0.01βˆ—RNO3βˆ—RdayNO_{3rain}=0.01*R_{NO3}*R_{day}NO3rain​=0.01βˆ—RNO3β€‹βˆ—Rday​
NO3rainNO_{3rain}NO3rain​
RNO3R_{NO3}RNO3​
RdayR_{day}Rday​
2_22​
NH4rain=0.01βˆ—RNH4βˆ—RdayNH_{4rain}=0.01*R_{NH4}*R_{day}NH4rain​=0.01βˆ—RNH4β€‹βˆ—Rday​
NH4rainNH_{4rain}NH4rain​
RNH4R_{NH4}RNH4​
RdayR_{day}Rday​
2_22​

RNO3R_{NO3}RNO3​: Concentration of nitrogen in the rain (mg/L)

RCN

.bsn

Atmospheric deposition of ammonium (mg/L) values for entire watershed

rammo_sub

.atm

Atmospheric deposition of nitrate (mg/L) for entire watershed

Rcn_sub